Johanna Mendillo: Hello pollock…. can you hear me now? August 7, 2012

NOAA Teacher at Sea
Johanna Mendillo
Aboard NOAA ship Oscar Dyson
 July 23 – August 10

Mission: Pollock research cruise
Geographical area of the cruise: Bering Sea
Date: Tuesday, August 7, 2012

Location Data from the Bridge:
Latitude: 59 52 ’ N
Longitude: 177 17’ W
Ship speed:   8.0 knots ( 9.2 mph)

Weather Data from the Bridge:
Air temperature: 7.3C (45.1ºF)
Surface water temperature: 8.4C (47.1ºF)
Wind speed:  4 knots ( 4.6 mph)
Wind direction: 75T
Barometric pressure:  1018 millibar (1 atm)

Science and Technology Log:

We are wrapping up our final few sampling transects.  Now that you are practically fisheries biologists yourselves from reading this blog, students, we must return to the fundamental question— how do we FIND the pollock out here in the vast Bering Sea?  The answer, in one word, is through ACOUSTICS!

Look at all of these birds off the stern!  Why do you think they are following us?  Are we about to haul up a catch, perhaps?

Look at all of these birds off the stern! Why do you think they are following us? Are we about to haul up a catch, perhaps?

Hydroacoustics is the study of and application of sound in water.  Scientists on the Oscar Dyson use hydroacoustics to detect, assess, and monitor pollock populations in the Bering Sea.

Now, you may have heard of SONAR before and wonder how it connects to the field of hydroacoustics.  Well, SONAR (SOund Navigation and Ranging) is an acoustic technique in which scientists send out sound waves and measure the “echo characteristics” of targets in the water when the sound waves bounce back— in this case, the targets are, of course, the pollock!  It was originally developed in WWI to help locate enemy submarines!  It has been used for scientific research for over 60 years.

(PLEASE NOTE: The words sonar, fishfinders, and echosounders can all be used interchangeably.)

The transducer sends out a signal and waits for the return echo...

The transducer sends out a signal and waits for the return echo once it bounces off the fish’s swim bladder… (Source: http://www.dosits.org)

On the Dyson, there is, not one, but a collection of five transducers on our echosounder, and they are set at five different frequencies.  It is lowered beneath the ship’s hull on a retractable centerboard.  The transducers are the actual part of the echosounder that act like antennae, both transmitting and receiving return signals.

The transducers transmit (send out) a “pulse” down through the water, at five different speeds ranging from 18-200kHz, which equals 18,000-200,000 sound waves a second!

When the pulse strikes the swim bladders inside the pollock, it gets reflected (bounced back) to the transducer and translated into an image.

First of all, what is a swim bladder?  It is simply an organ in fish that helps them stay buoyant, and, in some cases, is important for their hearing.

Swim Bladder (Source: www.education.com)

Swim Bladder (Source: http://www.education.com)

Now, why do the pulses bounce off the swim bladders, you ask?  Well, they are filled mostly with air and thus act as a great medium for the sound waves to register and bounce back.

Think of it this way: water and air are two very different types of materials, and they have very different densities.  The speed of sound always depends on the material through which the sound waves are traveling through.  Because water and air have very different densities, there is a significant difference in the speed of sound through each material, and that difference in speed is what is easy for the sonar to pick up as a signal!

It is the same idea when sound waves are used to hit the bottom of the ocean to measure its depth- it is easy to read that signal because the change in material, from water to solid ground, produces a large change in the speed of the sound waves!

Here is a sonar system measuring the depth of the ocean...

Here is a sonar system measuring the depth of the ocean… (Source: http://www.dosits.org)

Interestingly, different types of fish have different shaped and sized swim bladders, and scientists have learned that they give off different return echos from sonar signals!  These show up as slightly different shapes on the computer screen, and are called a fish’s “echo signature”.  We know, however, that we will not encounter many fish other than pollock in this area of the Bering Sea, so we do not spend significant time studying the echo signatures on this cruise.

So, what happens when these signals return to the Dyson?  They are then processed and transmitted onto the computer screens in the hydroacoutsics lab on board.  This place is affectionately known as “the cave” because it has no windows, and it is, in fact, the place where I spend the majority of my time when I am not processing fish!  Here it is:

Here is Anatoli observing potential fish for us to go catch!

Here is Anatoli observing potential fish for us to go catch!

We spend a lot of time monitoring those computer screens, and when we see lots of “specks” on the screen, we know we have encountered large numbers of pollock!

Here we are approaching a LARGE group of pollock!

Here we are approaching a LARGE group of pollock!

When the scientists have discussed and confirmed the presence of pollock, they then call up to the Bridge and announce we are “ready to go fishing” at a certain location and a certain depth range!  Then, the scientists will head upstairs to the Bridge to work with the officers and deck crew to supervise the release, trawling, and retrieval of the net.

Now, in addition to the SONAR under the ship, there are sensors attached to the top of the net itself, transmitting back data.  All of the return echos get transmitted to different screens on the bridge, so not only can you watch the fish in the water before they are caught, you can also “see” them on a different screen when they are in the net!  As I told you in the last post, we will trawl for anywhere from 5-60 minutes, depending on how many fish are in the area!

Left: Echosounder at work/  Right: The "return signature" is visible on the computer!

Left: Echosounder at work/ Right: The “return signature” is visible on the computer!  (Source: http://www.dosits.org)

A full catch- success!  Without acoustics, it would be much harder for NOAA to monitor and study fish populations.

A full catch- success! Without acoustics, it would be much harder for NOAA to monitor and study fish populations.

Personal Log:

In these last few days, we have crossed back and forth from the Russian Exclusive Economic Zone (EEZ) and the U.S. several times.  There were some nice views of Eastern Russia before the clouds and fog rolled in!

I can see Russia from my ship!

I can see Russia from my ship! (Photo Credit: Allan Phipps)

In addition, we crossed over the International Date Line!  It turns out that everyone on board gets a special certificate called the “Domain of the Golden Dragon” to mark this event.  This is just one of a set of unofficial certificates that began with the U.S. Navy!  If you spend enough time at sea, you can amass quite a collection- there are also certificates for crossing the Equator, Antarctic Circle, Arctic Circle, transiting the Panama Canal, going around the world, and more…

I will award a prize to the first person who writes back to tell me what does it mean when one goes from a “pollywog” to a “shellback”, in Navy-speak!

Here is a picture of me with the largest pollock I have seen so far- 70cm!

If I am 5' 4", how many 70cm pollock would it take to equal my height?

If I am 5′ 4″, how many 70cm pollock would it take to equal my height?

Lastly, on to some, perhaps, cuter and more cuddly creatures than pollock- pets!  Here in the hydroacoustics lab, there is a wall dedicated to pictures of pets owned by the officers, crew, and scientists:

Those are some pretty cute pets left ashore...

Those are some pretty cute pets left ashore…

Clearly, this is a dog crowd!   I did learn, however, that our Chief Scientist, Taina, has her cat (Luna) up there!  Students, do you remember the name of my cat and, what do you think, should I leave a picture of her up here at sea?

Marsha Skoczek: Plotting Our Course, July 15, 2012

NOAA Teacher at Sea
Marsha Skoczek
Aboard NOAA Ship Pisces
July 6-19, 2012

Mission: Marine Protected Areas Survey
Geographic area of cruise:  Subtropical North Atlantic, off the east coast of Georgia.
Date:  July 15, 2012

Location:
Latitude:  32.47618N
Longitude: 78.19054 W

Weather Data from the Bridge
Air Temperature:  27.6C (81.7 F)
Wind Speed:  6 knots (6.9 mph)
Wind Direction:  From the SE
Relative Humidity: 75 %
Barometric Pressure:  1018.3
Surface Water Temperature:  28.4C (83.12 F)

Science and Technology Log

In order for the scientists to find the fish they are studying on this cruise, they need to know where the areas of favorable habitat are located.  Old nautical charts are not one hundred percent accurate–sometimes they can be hundreds of kilometers off. Early ocean floor mapping used long lines with a lead weight which was hung off the side of the ship.  As the ship moved forward through the water, the long lines would get behind the ship making it very difficult to get an exact reading.  It wasn’t until sonar came into general use during World War II, that it was discovered to be useful for bathymetric mapping.

Sonar works by sending a single sound wave to the ocean floor.  As it reflects back toward the ship, a hydrophone listens for the return sound.  The length of time it takes for that sound wave to return to the ship can be used to calculate the depth of the ocean in that location. The speed of sound in water travels at approximately 1,500 meters per sec (m/s) which is about five times faster than sound travels in air.  The problem with single beam sonar is that the data only plots the one single line beneath the ship.  It does not give the complete picture and gaps in data were often filled in using the readings taken around the area as an estimate.

Planned acoustic survey lines

So how is multibeam sonar different from single beam sonar?  With multibeam sonar, it is just as the name implies–multiple sound beams are sent toward the ocean bottom.  For the depths we are working on, the multibeam sonar on the Pisces sends out 70 beams of sound every .67 seconds.  Within a fraction of a second, these “pings” are reflected off of the ocean bottom and back to the transducer.  The time it takes for all 70 of those pings to return to the transducer determines the depth at each point.  The echogram screen illustrates the bottom features in real time and will even pick up large schools of fish in the water column.  As the ship continues to move up and down the survey lines, the raw data is collected.  The distance between the survey lines is determined by the depth of the area to be mapped.  To set the survey lines, we are using 1.5 times depth so, if the water depth averages 100 meters at the mapping location, the survey lines are set at 150 meters, (.08 nautical miles) apart.  Tonight, the ocean depth at our mapping location is about 60 m so the survey lines are set at 90 meters (.05 nm) apart.  The goal when laying out the survey lines is to overlap the previous lines by about 25%.  This will insure a more complete picture.

Echogram of ridge

It is not simple enough to just take the raw data from the return pings.  The temperature, salinity and depth of the ocean in the mapping area can create slight variations in the return speed.   Temperature, salinity and depth can influence the speed of the return signal, so we use the CTD to gather readings each morning as they are wrapping up the mapping for the night.  This information along with the information on the ship’s roll, pitch, and yawl from the Position and Orientation System for Marine Vessels (POSMV)  are plugged into software that helps process and clean up the data.  From there, the data is converted into a “geo tif” file where it can be  plugged into GIS mapping . The final product is a full color 3-dimensional image of the mapping area.

Completed multibeam image

Ideally the scientists would have multibeam information for each of the sites they want to study that day.  To make this happen, the night before the ROV dive the ship will make its way to the next day’s study area so the geographers can map all night.  The survey lines are selected using bathymetry maps as well as looking at the existing multibeam maps of the area to see if there are any gaps that need to be filled in.  The idea is to give the scientists as much information as possible so they can make informed decisions about where to study.  Time on the ship is extremely expensive and they want to make sure they take full advantage of that time by finding the best habitats to study.  Without the multibeam images, the scientists have to make a best guess as to where to map using old and possibly out of date information.

Personal Log

This is the engine monitoring station.

Today I took a tour of the  Pisces’ engine roomEngineer Steven Clement was nice enough to show me around and explain everything for me.  It is amazing to me how this ship is like its own little city.  The ship creates its own electricity using diesel-powered generators.  It takes four generators to power the ship at full speed which is about 15 knots.  The engines are so loud that I had on double ear protection and it was still extremely loud to walk past them. Using all four engines all day would burn up 3,000 gallons of diesel fuel.  The Pisces is capable of holding 100,000 gallons of fuel which should last the ship several months at sea.  The electricity that is left over from powering the engines is used as the power supply for all of the electronics on board.

Other ways that the Pisces reminds me of a small city is the water.  The ship creates its own drinking water with a reverse osmosis system complete with UV filter and is capable of producing 2.8 gallons per minute.  It also has two hot water heaters attached to a compressor to keep the hot water pumped up into the pipes of the ship.  I do have to say that the hot water on this ship is extremely hot!!  There is no need to wait for hot water, it comes out instantly when I turn on the faucet.  When I shower, I have the cold on full blast and just a smidge of hot water to get a normal temperature shower.  Even our waste water is cleaned up in the Pisces’ own waste water treatment facility which uses microbes to break down the waste products before it is released back out to sea.

Other than pulling into port occasionally for fuel and supplies, the Pisces is really a self-contained vessel capable of cruising at sea for long periods of time.

Ocean Careers Interview

In this section, I will be interviewing scientists and crew members to give my students ideas for careers they may find interesting and might want to pursue someday.  Today I interviewed Dr. Laura Kracker.

Dr. Laura Kracker

What is your job title?  I am a Geographer with NOAA National Ocean Service in Charleston, South Carolina.

What type of responsibilities do you have with this job? Usually I work on projects using acoustics to map fish in the water column.  Using fisheries acoustics, we can map the distribution of fish in an area and detect large schools as well. On this mission, I am using multibeam to map seafloor habitats.

What type of education did you need to get this job?  I earned my Associate’s Degree in agriculture from Alfred College in New York.  When my children were little, I stayed home with them.  While I was home with them I earned my Bachelors in Painting.  Then I went to work in a fisheries office for a couple of years before deciding to go back to college to get my Master’s Degree in Interdisciplinary Science from the University of Buffalo.  I then continued on to my PhD in Geography and GIS, also from the University of Buffalo.  My dissertation was on Using GIS to Apply Landscape Ecology to Fish Habitats.  So I have combined all of my experiences to get me to where I am today.

What are some of your best experiences have you had with this job?  I love being on a ship.  I spend as many as 55 days a year on ships, often at the request of other scientists that need help with multibeam sonar.  I love geography, it gives us  a framework to put everything together, you can layer more and more information onto a map to find a complete picture.

What advice do you have for students wanting a career in marine biology?  Get a broad foundation before you specialize.  You don’t have to take a direct route to where you want to go.  

Amanda Peretich: Awesome Acoustics, July 13, 2012

NOAA Teacher at Sea
Amanda Peretich
Aboard Oscar Dyson
June 30, 2012 – July 18 2012

Mission: Pollock Survey
Geographical area of cruise:
Bering Sea
Date:
July 13, 2012

Location Data
Latitude: 59ºN
Longitude: 174ºW
Ship speed: 11.7 knots (13.5 mph)

Weather Data from the Bridge
Air temperature: 7.3ºC (45.1ºF)
Surface water temperature: 7.6ºC (45.7ºF)
Wind speed: 4.3 knots (4.9 mph)
Wind direction: 12ºT
Barometric pressure: 1010 millibar (1.0 atm, 757.5 mmHg)

Science and Technology Log

How sonar works: energy (sound) waves are pulsed through the water. When it strikes an object, it bounces back to the receiver. (from http://www.dosits.org/)

How sonar works: energy (sound) waves are pulsed through the water. When it strikes an object, it bounces back to the receiver. (from http://www.dosits.org/)

Before stepping onto the Oscar Dyson, I wasn’t quite sure about much of the science going on. Did they just put the nets in the water every so often and hope to catch some fish? Carefully lean over the side of the ship saying “here fishy fishy” with the hope that the pollock would find their way into the net? Neither of these scenarios is correct (good thing I’m not actually a fisherman!). So today’s lesson is going to be all about what the chief scientist actually uses to find fish: hydroacoustics (hydro meaning water and acoustics meaning sound). This also involves SONAR, which is short for SOund Navigation And Ranging.

Fishfinding Basics

Fishfinding basics.

If you’ve ever been on a smaller boat, yacht, fishing vessel, or the like, you may have seen something called a fishfinder. The basic concepts are the same as what is happening on the Oscar Dyson. An echosounder sends a pulse of energy waves (sound) through the water. When the pulse strikes an object (such as the swim bladder in fish), it is reflected (bounced) back to the transducer. This signal is then processed and sent to some sort of visual display.

Swim Bladder

Swim bladder in a fish.
(from https://www.meted.ucar.edu/)

The Oscar Dyson uses acoustic quieting technology where the scientists can monitor fish populations without altering their behavior. The Scientific Sonar System and various oceanographic hydrophones (underwater microphones) are raised and lowered through the water column beneath the ship on a retractable centerboard. This is important so that the transducers can be lowered away from the flow noise generated by the hull, which in turn will improve the quality of data collected. In addition, there is a multibeam sonar system located on the forward hull. Ultimately the hydroacoustic data is all used as one piece to the puzzle of measuring the biomass of fish in the survey area.

OD acoustics

The different sonar signal transmitter/receivers (transducers) used on this leg of the pollock survey and their location on the ship.

Neal at work

Chief scientist Neal working away in the Acoustics lab. The second screen from the left on the upper row is showing the information from the ME70 multibeam.

So how does this all work when we are looking for fish? The chief scientist (Neal on the 0400-1600 watch) or another scientist (Denise on the 1600-0400 watch) will spend a lot of time analyzing the various computer screens in the acoustics lab, which has been affectionately termed the “cave” (no windows). They are looking at the information being relayed from both the multibeam and the EK60.

What is a multibeam? The Oscar Dyson has the Simrad ME70 scientific multibeam echosounder. It is located on the hull (underside) of the ship on the front half and sends 31 sonar beams per second down to the bottom of the sea floor.

Multibeam

Multibeam echosounder.
(from http://www.simrad.com/)

Aft of the multibeam (on the centerboard) are the five Simrad transducers. It may seem confusing, but hopefully I can walk you through a teensy little bit of how it works when we are looking to trawl for fish.

EK60 Transducer

Information from the EK60 transducer at 18kHz (top) and 38kHz (bottom).

Information from the EK60 echosounder is displayed on the far left screen in the acoustics lab while information for the ME70 multibeam is displayed on the next screen. The darker patches are showing that there are fish in that area. When the scientist first starts to see a good amount of fish, they will “mark” it and keep watching. If the screen fills up with fish (as in the EK60 image), the scientist will call upstairs to the bridge and tell them where to head back to on the transect line to start trawling. Depending on the location of the fish in the water column, it may be a bottom trawl (83-112 net), a midwater trawl (AWT net), or a methot trawl. Side note: the 83-112 midwater comparison trawl that I’ve mentioned before is done almost immediately after an AWT midwater trawl to compare the fish caught in a common area.

ME70 Multibeam

Information from the ME70 multibeam. You can determine the sea floor depth and there are five narrow beam slices from the mid-section of the multibeam (of the 31 different beams that span 120 degrees) displayed on screen.

Neal on bridge

Chief scientist Neal up on the bridge.

Then the scientist will head upstairs as the deck crew is preparing the net. One of the many sensors attached to the net is called the FS70 fishsounder or “the turtle”, and it is only used during trawls (because it is attached to the headrope). The scientist can “watch” the fish swimming under the ship using the EK60 information combined with the information from the fishsounder. The yellow “turtle” on the right in the image shows how the FS70 is flying in the water. You want minimal pitch and roll and for the front of it to be facing the back of the ship. This way, we can “see” the fish as they are going through the net. The officer of the deck and lead fisherman or head boatswain can adjust various things to keep the turtle in the right orientation. The middle image below is constantly changing on the screen in the bridge as the sonar is sweeping back and forth, so you can almost watch the individual fish enter the net. It was interesting to watch the delay between when you would see the fish from the EK60 (on the left) and when you saw them with the FS70 (middle).

Trawl Fishsounder

Display screens on the bridge used during a trawl.

Once the scientist is satisfied that enough fish have been caught for a sufficient sample size, the net will be hauled back and the acoustics work is done for just a little bit (giving Neal some time to grab some well-deserved coffee and the rest of us time to get our rain gear on to process the fish).

So some of the questions I had asked (that don’t really fit nicely in the information above):

Why do we use different frequencies in the acoustic studies?

Frequency Wavelength

Relationship between frequency and wavelength. (from http://emap-int.com)

This ties right back in to chemistry (and other sciences) with an equation and the relationship between frequency and wavelength (yay!). Basically there is an inverse relationship which means that at a high frequency there is a smaller or shorter wavelength (wavelength is the distance for peak to peak of a wave). At a low frequency, there is a higher or longer wavelength.

At a low frequency, you will see only see things that are larger, like pollock, whereas you will see very small things like krill and zooplankton at higher frequencies. Having information from both types of frequencies is necessary to complete the scientific research on the Oscar Dyson.

Single Fish

Traveling at 1 knot, showing single fish from EK60 sonar.

Is it possible to see a single fish?
Yes! From sunset to sunrise, the Oscar Dyson doesn’t actually travel the transect lines. This is because the pollock behave differently during darkness than during the day. So instead of traveling between 11 and 12 knots (which is what happens between trawls), it’s almost like the boat is just sitting around for a couple of hours. But during this time, since the boat isn’t moving along quickly, it’s possibly to see individual fish on the sonar as shown in the image.

Hydroacoustics

Hydroacoustic surveys can involve any number of different types and locations of the transducers. (from http://btechgurus.blogspot.com/2012/06/sonar.html)

Personal Log
Today is Friday the 13th but it was far from unlucky – I finally saw something out in the water other than fog: a boat! Again, all good sightings seem to come from up on the bridge, so I’m thankful for Lieutenant Matt for allowing me to ask a billion questions while I’m up there and teaching me more than I ever thought my brain could hold. He has all of the qualities of a great teacher, which is nice to see.

Ship

The ship we saw up on the bridge this morning from about 5 nautical miles away (left), on the sonar (middle), and through the binoculars (right).

Dancing in the fish lab on the Oscar Dyson

Neal and I dancing while waiting for the fish!

Highlight from the other day? Chief scientist Neal finally dressed out in his Grundens (rain gear) and came to help process a catch in the fish lab! While waiting, he even took a quick second to dance in the doorway (we were “Dougie”-ing) to my music that was playing over the speaker system.

References
NOAA Oscar Dyson flier
NOAA Oscar Dyson Ship Electronics Suite
HTI Sonar
Wikipedia: Sonar
Simrad

Lesley Urasky: Do You See What the Pisces “Hears”?, June 22, 2012

NOAA Teacher at Sea
Lesley Urasky
Aboard the NOAA ship Pisces
June 16 – June 29, 2012

Mission:  SEAMAP Caribbean Reef Fish Survey
Geographical area of cruise: St. Croix, U.S. Virgin Islands
Date: June 22, 2012

Location:
Latitude: 18.5472
Longitude: -65.1325

Weather Data from the Bridge:

Air Temperature: 28.6°C (83.5°F)
Wind Speed:  9 knots (10.5 mph), Beaufort scale: 3
Wind Direction: from SE
Relative Humidity: 77%
Barometric Pressure: 1,014.80  mb
Surface Water Temperature: 28.1°C (82.6°F)

Science and Technology Log

Another aspect (much more technical) of the scientific research conducted on this cruise is the collection of acoustic data.  This field is continually evolving as the detection resolution improves allowing scientists to more precisely identify fish.  This has been used with more success in fisheries farther north because the schools of fish are more likely to be monospecific (a single species).  However, the technique still needs improvement in warmer waters where the fish assemblages tend to be multi-specific (having a much greater variety of fish).

General idea behind an acoustic sounder being used to detect fish. (Source: www.biosonicinc.com)

This field of study is called Hydroacoustics (hydro- means water, and acoustics refers to sound).   It is the science of  how sound moves through water. Leonardo da Vinci noticed how sound travels through water in 1490.  He noticed that, “If you cause your ship to stop and place the head of a long tube in the water and place the outer extremity to your ear, you will hear ships at a great distance from you.” (Urick, Robert J. Principles of Underwater Sound, 3rd Edition. New York. McGraw-Hill, 1983.)  World War I helped promote innovation in the field, especially with the need for anti-submarine detection devices (Wood, A. B., From the Board of Invention and Research to the Royal Naval Scientific Service, Journal of the Royal Naval Scientific Service Vol 20, No 4, pp 1-100 (185-284)).

Hydroacoustic instruments utilize SOund Navigation and Ranging, more commonly referred to as SONAR.  The ship Pisces is equipped with a system located on the center board; this is a flat structure that can be raised/lowered through the water column beneath the center of the ship.

Line drawing of the NOAA ship Pisces showing the location of the center board.

The system used is a sonar beam that is split into quadrants.  This instrument is used to assist in determining fish abundance and distribution.  The premise is relatively simple: an echo sounder transmits a pulse of energy waves (sound), when the pulse strikes an object, it is reflected (bounced) back to the transducer.  The echo sounder is then processed and sent to a video display.  This is the same general process behind the recreationally available fishfinder.

Acoustic beam split into quadrants (Source: http://www.htisonar.com

A short burst of energy is focused into a narrow beam.  When this beam encounters an object such as a fish, a school of fish, plankton, or other object, some of the energy bounces back up through the water to the transducer.   It is the detection of these reflections that allow scientists to determine location, size, and abundance of fish.  These reflections show up on our video monitor.  These measurements are combined with groundtruthed data (for example, fish collected in the field, camera images).

One of the difficulties in data interpretation is that often, the signals that appear on the computer monitor have false readings.  This is a result of the sound wave bouncing multiple times.  It travels to the bottom from the transducer, strikes an object, returns to the ship, bounces off the ship back toward the bottom, strikes another object, and is detected yet again.

Real-time annotated echogram at sampling site.

The Pisces is actually home to one of six multi-beam acoustic instruments in the world.  Of the six in existence, NOAA has five of them.  The benefit of running a multi-beam instrument is that each beam can be set to measure a different frequency (kHz), thus enabling detection of many more features (different species of fish, etc.)

Scientific multibeam echo sounder (Source: www. simrad.com)

Personal Log

Last night the crew of the Pisces carried out a task that they don’t normally perform.  The Pisces was created for fisheries research projects – it focuses on collecting fish samples either by bandit reel, longline, or trawling.  This particular operation was to deploy the anchor for a buoy that will be attached at a later date.  When the buoy is ready to be attached, another vessel will bring it out to the site and divers will go down to the anchor to make the final attachment.

The anchor consists of a huge rebar-reinforced concrete block with a very long chain that has marker floats attached at the end.  Logistically, this took some planning; the A-frame had to be raised and the anchor lifted with the Gilson winch with a 1″ spectra line (has an enormous tensile strength).  The gate to the ship’s ramp was lowered and the A-frame (or as the deck hands call it, the “Tuna Tower”)  repositioned so the anchor was hanging over the water.  The rope holding the anchor, chain, and float was cut through, and the anchor plunged to the ocean bottom.  Again, the crew made the operation go smoothly and demonstrated their ability to complete unexpectedly assigned tasks.

Today was a slow fishing day – no fish at all.  Without any fish to “work up” (collect samples from), the day goes more slowly and we have more down time.  With the extra time, I had a chance to interview Kevin Rademacher, the Chief Scientist on the cruise.

LU: What is your official job title and what are your job duties?

KR: I’m a Research Fisheries Biologist.  I work for the Reef Fish Unit at the NOAA Fisheries Lab in Pascagoula, MS.  I am the Senior Tape Reader/Reviewer, in charge of the readers that analyze  the video data we collect from Reef Fish Surveys.  I also help plan, organize, and run the surveys.  Additionally, I participate in trawl surveys and anything else the lab needs done.

LU: When did you first become interested in the ocean and marine sciences?

KR: I guess that would have been when I was really young.  There is a photo from the Panama City, Florida newspaper, two weeks after I was born with my parents pulling me in a homemade wagon along the beach!  I knew in junior high school that I wanted to be a cross between Jacques Cousteau and Marlin Perkins of Mutual of Omaha’s Wild Kingdom.

LU: It’s such a broad field; how did you narrow your focus down to what you’re currently doing?

KR: I got lucky and kind of fell into reading underwater videos at the initial stages of the project and fell in love with being the proverbial “fly on the wall”! It has allowed me to see the fish in their natural  habitat, different color phases, behavior, etc.

LU: If you were to go into another area of ocean research, what would it be?

KR: Marine Mammal Studies.  After college I trained dolphins and sea lions and put on shows with them for a local Oceanarium on the Mississippi Gulf Coast.

LU: What is the biggest challenge in your job?

KR: Communicating with people and writing papers.

Ariane Frappier and Kevin Rademacher reviewing a dichotomous key in order to determine the species of a fish we caught.

LU: What do you think is the biggest issue of contention in your field?

KR: The impression that commercial fishermen have regarding the work we do to regulate the fisheries they work in.

LU: What are some effects of climate change that you’ve witnessed during your career in fisheries research?

KR: The decline of coral reefs and overfishing of some species.

LU: In what areas of marine science do you foresee a lot of career paths and job opportunities?

KR: Ecosystem management and data modelers.  There has also been a decline in taxonomists over the past few decades.

LU: How would you explain your work to a layperson?

KR: I use underwater cameras to help assess populations of reef fish, especially snappers and groupers.  The data collected is used to manage those fisheries.

LU: If a high school student wanted to go into your field of study/marine science in general, what kinds of courses would you recommend they take?

KR: Math, Biology, Chemistry, and any other science courses available.

LU: Do you recommend students interested in your field pursue original research as high school students or undergraduates?  If so, what kind?

KR: Most definitely! Whatever they are interested in would be beneficial.

Well, only two more days left with the scientists before we pull into San Juan, Puerto Rico.  We have 17 more daytime sites to sample and then this survey will be over.  The scientific crew will be flying home on the 25th, and once home, their work will really begin.  Back in the lab, they will be analyzing the data and reviewing the video.  Some of them will be going back out on other cruises.  Kevin Rademacher will be going out on another reef fish survey in the eastern Gulf of Mexico.  It is currently delayed because of the potential formation of tropical storm Debby.  Joey Salisbury has a couple more; he will be going on a longline cruise and then another reef fish survey, both of which will be in the Gulf of Mexico.  Arian Frappier will be heading off to begin a masters program in marine systems and coastal studies at Texas A&M Corpus Christi.

After a day’s shore leave in San Juan, I’ll continue on to Mayport on the Pisces.  During this time, I’ll focus on the crew members and their jobs.  The cruise will definitely take on a different feel at this point, but it will give me an opportunity to explore other ocean related careers.

Maria Madrigal: Understanding the Sampling Methods: April 4, 2012

NOAA Teacher at Sea

Maria Madrigal

NOAA Ship Oscar Elton Sette

April 2-18, 2012

Mission: Comparison of Fishery Independent Sampling Methods

Geographical area of cruise: Tutuila, American Samoa

Science & Technology Log: April 4, 2012

The goal of the study is to get a better picture of the coral reef fish assemblage using three different sampling methods. Two NOAA research vessels based in Honolulu, Hawaii (Oscar Elton Sette and Hi’ialakai) are working concurrently to assess coral reef fish assemblages around the island of Tutuila in American Samoa.

Three observational methods will be used to assess these reef fish assemblages; stationary point count divers (SPC), baited remote underwater video stations (BRUVS) and an autonomous underwater vehicle (AUV).

In the shallower areas being sampled (0 – 30 meters), all three survey methods will be used. In the areas ranging from 30-100 meters, only the BRUVS and AUV systems will be used as the divers can not reach these depths. This study will allow for a comparison among all three methods in the shallow-water depth range. The use of the BRUVS and AUV in the 30-100 m depths will also allow comparisons to be made between the shallow and deeper portions of the reef ecosystem to see if the patterns apparent in the shallow areas are similar to or different than those found in deeper waters.

SE12-02 Tutuila Comparison of Fishery Independent Sampling Methods for Coral Reef Fish

SE12-02 Tutuila Comparison of Fishery Independent Sampling Methods for Coral Reef Fish

The Hi’ialakai will be the base for the SPC (Stationary Point Count) divers.  Teams of two divers will work side-by-side sampling across a 30-meter transect. One diver is centered at the 7.5 meter mark and the other diver is centered at the 22.5 meter mark. Each diver samples a cylinder with a radius of 7.5 meters. Each diver spends the first five minutes noting the fish species present within their cylinder. After noting what fish species are present, the diver keeps a tally of how many representatives of each species are within their cylinder. Divers must work systematically to record additional data including total fish length and habitat type.  For a more detailed description of the SPC method, you may read the procedure as provided by PIFSC.

The Oscar Elton Sette will be the base for the BRUVS (Baited Remote Underwater Video Stations) and the AUV(Autonomous Underwater Vehicle) operations.

BRUVS are deployed from small boats at predetermined locations previously sampled by the SPC divers. They are placed on the seafloor and are equipped with two cameras that allow for accurate measurement of the fish that come into view. The BRUVS are deployed at each site for 20-minutes without bait and again for 60-minutes either with or without bait. The video can be instantly reviewed to ensure successful recording at each site. Captured video is reviewed and analyzed at a later date. Final video processing and data analysis will take place once the scientists return to the lab.

The AUV, named Lucille, is designed to hover 2-4 meters above the seafloor. It is programmed to navigate a predetermined survey track before it is deployed. It is equipped with a pair of forward-looking stereo-video cameras, two still-image cameras, a CTD (Conductivity-Temperature-Depth) sensor and a SONAR (Sound Navigation and Ranging) unit. It can dive down to 1,500 meters and can go on missions that last up to eight hours. It is programmed to come back to the ocean’s surface at the end of its mission.  The video and still photographs are later reviewed and analyzed. All the data collected by the AUV allows scientists to get a better picture of the ocean floor, what lives there and how many organisms are living within that community.

Comparison of Survey Methods

Comparison of Survey Methods

Kaci Heins: September 24-26, 2011

NOAA Teacher at Sea
Kaci Heins
Aboard NOAA Ship Rainier
September 17 — October 7, 2011

Mrs. Heins Acquiring Data For The Hydrographic Survey

Mission: Hydrographic Survey
Geographical Area: Alaskan Coastline, the Inside Passage
Date: Tuesday, September 27, 2011


Weather Data from the Bridge

Clouds: Overcast
Visibility: 10 Nautical Miles
Wind: 10.40 knots
Temperature
Dry Bulb: 11.3 degrees Celsius
Barometer: 1000.1 millibars
Latitude: 55.28 degrees North
Longitude: -133.68 degrees West

Science and Technology

I have received many questions from students asking “What is hydrography?”.  According to the International Hydrographic Organization,  hydrography is “the branch of applied science which deals with the measurement and description of the physical features of the navigable portion of the earth’s surface [seas] and adjoining coastal areas, with special reference to their use for the purpose of navigation.” Lets break that word down to find the meanings of the prefixes and suffixes using dictionary.com.

hydro – means water,

graph – means to write or chart

graphy – means the science or process of recording

Another question I have received is what is a hydrographic survey?  Most of the surveys that you may have heard of are used on land.  For example, construction workers may survey a site before they start construction, or you may take a survey at school about what types of food you would like in the cafeteria.  Any kind of survey is the acquiring of information that is used for various purposes.  In the case of a hydrographic survey, the technicians acquire and chart information about the sea floor.  I was fortunate enough to go out on a survey launch to see that a hydrographic survey is conducted using sonar to look through the water to see what the sea floor actually looks like.

Launch Boat

The boat that NOAA uses to conduct the surveys is called a launch.  This means we use a large motorboat to get to where we need to go.  It costs tens of thousands of dollars a day to operate the Rainier, her launches, and the technology.  It is the technology that allows scientists to be able to “see” through the water to map what the ocean floor actually looks like.  The first, and most important, piece of technology on the launch that enables us to “see” the sea floor is the sonarSonar (SOund NAvigation and Ranging) is the process of using sound waves to bounce off objects we cannot see and then acquiring the return sound to create an image.  However, it does get a little more complicated than that.  There are two different types of sonar that the NOAA National Ocean Service (NOS) goes into detail about.

1) Active Sonar – Transmits a pulse or acoustic sound into the water. If the sound pulse hits an object in its path, such as the sea floor, then the sound bounces off  and returns an “echo” to the sonar receiver.  By determining the round-trip travel time between the emission of the sound pulse and its reception, the transducer can determine the range (how far away) and orientation (location) of the object.  The formula for this is

Distance = (two way travel time x speed of sound through water) / 2

2) Passive Sonar – Is a sonar system that does not emit its own signal, but listens to sound waves coming towards it.

Multibeam Sonar

Both the Rainier and the smaller launches have  both active sonar called multibeam sonar. Multibeam sonar sends out numerous sound waves from directly beneath the ship on the boat’s hull that fans out its coverage over the seafloor.  This coverage is called a “swath”.  Before we leave the ship to head out on the launches we have a briefing to go over the weather, safety, and any other important information for the coxswains, scientists, or crew.  We also get a plan for the day for what polygons, or areas we have to survey.  On our way we turn on some of the expensive (and top secret!) technology called the Position and Attitude System (POS).  This technology collects the vessels motion data (roll, pitch, and yaw), that later will be incorporated into the Caris software that produces the final chart. The multibeam transmits around 512

Polygon Coverage Area for the Day

beams each second.  The frequency of the sound waves depends on the depths that we are working in.  We worked in waters that were around 50 meters deep so we used the 400 kilohertz frequency.  However, if we would have been working in deeper water we would have gone to 200 kilohertz.  By lengthening the wavelength the beams can travel into deeper water with less error or scattering.

Before we start acquiring data we make sure to have good communication with the coxswain, or driver, of the boat.  It is extremely important that there is good communication and that the coxswain can maintain their heading and speed throughout the polygon so that the data can be collected without too many errors.

Conductivity, Temperature, and Depth Cast

We want to make sure we only go about 6-8 knots so that the sonar echo has time to make it back up to the receiver and we can collect good data.  The scientists also conduct a CTD cast before we start and every four hours while they collect data.  CTD stands for Conductivity (or salinity), Temperature, and Depth (pressure).  The data from the CTD can be used to calculate the speed of sound through water.  All of these factors can cause errors in the survey data so scientists need to collect this information so that the finished product has fewer errors and depths can be corrected from the sonar.  Other features that can cause errors in the data are bubbles, vegetation such as kelp, schools of fish, and the type of material that is on the sea floor.  For example, if the sea floor consists of a softer material it won’t reflect the sonar beams back as well.

To collect the survey data we basically drive the launch back and forth over our assigned polygons with the multibeam sonar.  This is sometimes called “mowing the lawn” or “painting the bottom”.  When we get to one edge of the polygon we stop logging data, turn around, and make a new swath as close as we can to the previous one and continue collecting data.  We cover around 50 nautical miles each day collecting data with the overall goal to collect the best data quality that we can during our acquisition.

As we head back to the Rainier all the computer data is downloaded from the day and is later transferred to the plot room.  This is where survey technicians add all the other information and make corrections to the data such as tides, vessel motion (POS), GPS, sound velocity from the CTD, and other programs so that the data is as accurate as possible.  Technicians still must go through and clean out “noise” which is scattering of some of the data.  The finished survey chart is sent to the Pacific Hydrographic Branch for post processing and quality assurance.

What We Surveyed Today!

Personal Log

In my last blog I wrote about how math skills are very important not only as a strong skill needed on a NOAA ship, but also as a life-long skill.  As I continue learning more about hydrography I have also found that computer skills are extremely valuable in this work environment.  Most people have basic computer skills to check email and run office programs, but out here it takes a little more.  There is quite a bit of training that the survey technicians and the NOAA Corps officers must go through to learn about all the different software that collects data and then using more software to combine them to make the finished hydro chart.  Numerous hours of collecting data, combining data, cleaning data and finishing projects all have a significant amount of work done by or at a computer.  Everyone from the captain to the junior officers must know how to use it and how to troubleshoot when things don’t work right.  It is not as easy as picking up the phone and calling customer service.  Minds among the ship must come together to solve problems when they arise.

Using the Computer to Collect Survey Data

While underway whether it is on the ship or on one of the launches the high seas are always around.  At first they made me nervous because I was afraid I would get sick.  However, it has turned out to be quite the opposite!  Whenever the seas get rough I actually start to get sleepy as we sway back and forth!  Usually, we are so busy that there isn’t time to take a nap so I’m learning to work through it.  Going along those lines of being busy, there are usually no breaks during the weekends.  In most people’s lives the weekend is time to take a break, hang out with family and friends, and sometimes do absolutely nothing at all.  Out here on a working ship this is not the case.  The NOAA ships have to meet certain deadlines and with some of their past major repairs, time has been ticking away with not much work being done.  This means when Saturdays and Sundays roll around at the end of the week we keep on working like a regular day.  I have the utmost respect for all of the crew, scientists, and officers that spend their time out here working for weeks straight.  It is not an easy lifestyle, but they are committed to it and I admire them and their strength.

Student Questions Answered

Wildlife Spotted!

Sea Otters

Humpback Whale

Sea Otter

Sea stars

Sea Urchins

Question of the day

Lindsay Knippenberg: Acoustics Day! September 13, 2011

NOAA Teacher at Sea
Lindsay Knippenberg
Aboard NOAA Ship Oscar Dyson
September 4 – 16, 2011

Mission: Bering-Aleutian Salmon International Survey (BASIS)
Geographical Area: Bering Sea
Date: September 13, 2011

Weather Data from the Bridge
Latitude: 56.91 N
Longitude: -169.08 W
Wind Speed: 10.07 kts
Wave Height: 4 – 6 ft
Surface Water Temperature: 6.5 C
Air Temperature: 7.5 C

Science and Technology Log

The Oscar Dyson uses several different types of sonar to get the best image of what is beneath the ship.

The Oscar Dyson uses several different types of sonar to get the best image of what is beneath the ship.

Today I learned about acoustics with Paul. The Oscar Dyson is one of NOAA’s newer ships and has a hull-mounted sonar system which uses sound waves to “see” what is underneath the ship. The Oscar Dyson was also built to have a low acoustic signature and be “quiet” in the water. This is helpful to the scientists using acoustics to study fish onboard the Dyson because the fish don’t hear the ship and swim away. On our cruise the acoustics data is used to get a picture of where there is life in the entire water column. For the most part we have just been trawling on the surface, but the ocean is much deeper and there could be a lot more life underneath our nets that we will never catch. If we get very few fish in our nets, it could mean that the fish are just at a deeper depth and not that there are not any fish in that area. Since the scientists are getting a better picture of what is really going in that ecosystem, they can make more accurate stock assessments. All throughout the cruise I have been curious about the images displayed on the screens in the acoustics room and on the bridge. Today I would finally learn what they were all about.

Since the sonar is attached to the bottom of the boat, the top 14 meters aren't seen in the images. To solve that problem, a sonar transducer is lowered over the side to get the top 14 meters when we at station.

Since the sonar is attached to the bottom of the boat, the top 14 meters aren't seen in the images. To solve that problem, a sonar transducer is lowered over the side to get the top 14 meters when we at station.

Basically how acoustics work is that a sound or ping is sent from the ship and it travels through the water. When it hits something in the water column or the bottom of the ocean it bounces back and the ship’s echosounder records the length of time that it took for the sound wave to travel there and back. Depending on the temperature and depth of the water, the pings are sent at different time intervals and pulses. The pings can also be sent at different frequencies to “see” different types of organisms. For instance zooplankton can be viewed best at one frequency and jellyfish can be viewed best at another frequency. As the sound waves are returning to the vessel, the computer translates the returning sound waves into images for the scientists to analyze.

A sonar image at dawn. The dark red line at the bottom of the screen is the ocean floor. Notice all the greens and blues at the top of the water column. Those are pollock.

A sonar image at dawn. The dark red line at the bottom of the screen is the ocean floor. Notice all the greens and blues at the top of the water column. Those are pollock.

On our cruise Paul is comparing the sonar signatures produced by the different organisms under the boat to what we are actually catching in the nets. The use of acoustics technologies for stock assessments is fairly new and individual species can’t be recognized by the sonar images, but Paul can use the images to detect if an area will have a greater density of organisms. We are also selecting several locations between stations to do mid-water trawls. Paul selects areas that have a high density of organisms underneath the depth that our surface trawl nets reach and we do a mid-water trawl. He then compares what we find in the trawl to the sonar signatures that he saw in the images to see if he can find any patterns between specific species and sonar signatures. It will be amazing if some day fisheries biologists will be able to assess the stock of fisheries by using sonar instead of net trawls which are a lot more work and often result in the death of the fish.

Personal Log

Today's weather after the two low pressure systems had entered the area. The weather was pretty crappy the last two days, but today it is beautiful.

Today's weather after the two low pressure systems had entered the area. The weather was pretty crappy the last two days, but today it is beautiful.

We have had several lo- pressure systems blow through during our cruise and so far we have had two gale warnings. The first one occurred when we had only been out to sea for a day so it was easy to head back in to Dutch Harbor. The last one occurred a couple of days ago and we were too far out into the Bering Sea to turn back. We had no choice but to ride it out. Two low-pressure systems were colliding and the Bering Sea turned into a washing machine. There were consistent 10 – 13 ft waves coming from one direction, large 20ft swells coming from another direction, and the occasional 8 – 10 ft wave coming from a different direction. The ship just kind of bobbed from side to side and up and down and we were all along for the ride. Thank goodness I didn’t get sick, but I definitely didn’t sleep well.

Face to face with some angry seas.

Face to face with some angry seas.

I was also amused by how life went on for everyone onboard the ship. Dinner was hilarious as everyone held onto their dishes and your chair moved from side to side with the waves. Walking around was pretty funny too. There was no way that you could walk in a straight line. I would choose something to grab onto, walk another couple of steps, and then grab onto something else. As I tried to sleep at night I could hear the things that we had thought we had secured roll around the room. Who knew that a roll of paper towels could make so much noise? The curtain on my bed was making me crack up because it would roll open with one wave and close shut with another. It just kept opening and closing all night and there was nothing that I could do about it but laugh. Thankfully by today the seas had calmed down significantly and the sun is actually out.

Francesco was a lost shorebird who found his way to our ship in the middle of the Bering Sea.

Francesco was a lost shorebird who found his way to our ship in the middle of the Bering Sea.

There was one casualty though, and that was Francesco. Francesco was a shorebird, an American Pipit, that was blown way off course during the storm. He ended up cold and hungry on our back deck last night. We were able to catch him and we put him in a warm box with some dead flies, water, and crackers. He managed to eat and drink, but he was a juvenile and had very little body fat. He was pretty much skin and bones. He lasted until this afternoon and when we went to check on him, he was dead. We gave him a burial at sea and were reminded that the Bering Sea is a harsh, harsh environment.

Caitlin Thompson: Zooplankton, Ocean Currents, and Wave Gliders, August 7, 2011

NOAA Teacher at Sea
Caitlin Thompson
Aboard NOAA Ship Bell M. Shimada
August 1 — 14, 2011

Mission: Pacific Hake Survey
Geographical Area: Pacific Ocean off the Oregon and Washington Coasts
Date: August 7, 2011

Weather Data from the Bridge
Lat. 47 degrees, 00.8N
Long. 124 degrees, 29.8W
Present weather: Cldy 8/8
Visibility: 10 n.m.
Wind direction: 323
Wind speed: 08 kts
Sea wave height: 1 feet
Swell waves – direction: –
Swell waves – height: –
Sea water temperature: 13.7 degrees C
Sea level pressure: 1018.8 mb
Temperature – dry bulb: 15.8 degrees C
Temperature – wet bulb:  14.7 degrees C

Science and Technology Log

On the fish deck in my work clothes

On the fish deck in my work clothes

The Shimada conducts research around the clock, with crew members working twelve-hour shifts. So far, I have worked with the acoustics team studying hake during the day, when the hake school together and are easy to fish. Last night I branched out, staying up with Steve Pierce, the oceanographer studying ocean currents, Jennifer Fisher, a faculty assistant at Oregon State University (OSU) who is studying zooplankton, and her intern, Angie Johnson, a graduate student at OSU. All the different research on this trip complements each other, and I learned more about the acoustic team’s work from the night people.

Gray's Harbor Transects

Gray's Harbor Transects

The map at right shows the transects we follow and the stations that the night team takes samples, which Steve chooses. Just like the acoustics team, he only chooses sites on the east-west transects. The night team usually works one transect ahead of the day team, and must have the ship back where they started by sun-up. Steve is mapping small currents because, he says, surprisingly little is known about ocean currents, even though they have a tremendous impact on ocean life.

He is especially interested in the polar undercurrent that brings nutrient-rich water from the south up along the west coast. A small current, it is nonetheless important because of the nutrients it carries, which come to the surface through upwelling. He uses an acoustic device, the Acoustic Doppler Current Profile (ADCP), to find the velocity of the water at various depths. The data from the ADCP is skewed by many factors, especially the velocity of the ship. Later, Steve will use trigonometry to calculate the true velocity. He also uses the Conductivity, Temperature, Depth (CTD) meter, lowered into the water at every station during the night. The CTD gives much more information than its name would suggest, including salinity, density, and oxygen. It is deployed with a high-speed camera and holds bottles to capture water samples. I was impressed by the amount of work – and math! – that Steve does in between cruises. When he has down time on this cruise, he told me, he is calculating work from two years ago.

Jennifer divides a sample in the Folsom plankton splitter

Jennifer divides a sample in the Folsom plankton splitter

Jennifer and Angie are studying plankton, the organisms at the very bottom of the food web. Immediately, I recognized euphausiids, or krill, from the contents of hake stomachs. Actually I recognized their small black eyes, which always reminded me of poppy seeds when I saw them in hake stomachs. Jennifer is conducting this work through her group Northwest Fisheries Science Center, which, as she describes it, gives her a wonderful freedom to research different projects related to ocean conditions, especially salmon returns. In this project, they measuring phytoplankton, tiny, photosynthetic organisms, by measuring chlorophyll and nutrients. They are also looking at zooplankton, like euphausiids, salps, and crab larvae, which we examined other the microscope. To help the acoustics team refine their ability to use sonar to identify zooplankton, Jennifer and Angie record certain species. The acoustics team will match up the acoustics data that is continuously generated on this ship with the samples.

Angie

Angie takes water samples from the CTD.

Today, the second catch of the day was aborted because of whales too close to the ship. However, the NOAA’s Pacific Marine Environmental Laboratory (PMEL), had asked the Shimada to investigate its waveglider. A waveglider is type of robot called an autonomous underwater vehicle (AUV). Programmed to travel and record data, it does not need an operator. The PMEL folks were concerned, however, that its AUV might have a problem.The bridge set the course for the AUV, described as a yellow surfboard, and I headed up to the flying deck, the highest deck and an ideal spot for observation, to watch for it. Immediately we saw a humpback whale, just starboard of the ship, spout and roll through the water, its tail raised in the air. Soon the AUV appeared. We saw nothing wrong with it but communicated our observations, photographs, and video tape of it to PMEL. The PMEL’s system of wavegliders monitor carbon dioxide levels and use the kinetic energy of ocean waves to recharge the batteries. The acoustics team hopes to get their own waveglider next year to collect acoustic data in between transects. As I was peering  over the edge of the boat, examining the surfboard-like robot below, I heard a loud splash. A bout ten  Dall’s porpoises were playing around the bow of our boat, rippling in and out of the water. Dall’s porpoises are tremendously playful creatures, and will often play around ships. But our ship was barely moving, and the porpoises soon lost interest and swam away.

Wave Glider

Wave Glider, seen from above

Personal Log

I’m getting a little of everything on this cruise. I would have stayed up two nights ago for the deploymentof the CTD and zooplankton samples, but the propeller developed a loud enough whamming sound to suspend all operations indefinitely. I woke up at 4:00 AM yesterday because the boat was swaying back and forth violently. (Violently by my standards, that is; more experienced mariners insist the swell is nothing.) Since our bunks go port to starboard, I could feel my weight sliding from hip to head to hip to head as I was rocked back and forth in bed. Meanwhile a discarded lightbulb in a metal shelf was rolling back and forth steadily – rattle-rattle-WACK! rattle-rattle-WACK! – until Shelby Herber, a student at Western University and my roommate, got up, found the culprit, and wrapped it in a shirt. When I woke again, it was eleven hours after the discovery of the problem with the prop and well past breakfast, and I started to get up until Shelby told me we were off transect, headed to shore because of the propeller.

Wave Glider

Wave Glider from beneath the water, taken from PMEL's website

So we took our time getting up. But when I finally arrived in the acoustics lab, Rebecca was running up the hall, saying, “Caitlin, I was looking for you! There’s a great big shark outside, and we’re pulling up the ROV!” The ROV is the remotely controlled vehicle, a robot like the AUV, but one that requires an operator to make it move. Unfortunately, out on the fish deck, the ROV was being put away and the shark gone off on his fishy business. To console me, John had the videotaped footage from the ROV and the dorsal fin of the shark, and showed me both. The ROV revealed no damage and I was invited down to the winch room, where the bang-bang-bang coming from the propeller was unnerving.

ROV

Puzzled birds approach the ROV

Everyone was in an uproar trying to decide what to do, an uproar made all the more dramatic by the steady lurching and swaying of the ship, which throughout the day has sent most of the scientists to their room for at least a few hours and most of the deck hands to tell stories of unhappy tourists who couldn’t find their sea legs. Finally, the engine guys decided the warped propeller would not prevent us from getting to Port Angeles, and Rebecca decided it would not interfere with the acoustics, and we got back on transect.

ROV

ROV

I’m getting a little bit of everything on this cruise. I’ve seen sharks and marines mammals, calm seas and rockier seas, an impressively well-functioning ship and a number of technological problems. I’ve interviewed scientists, NOAA Corps officers who command the ship, and crew members who recount endless adventures at sea. I’m even signed up for the cribbage tournament, which I’m not entirely thrilled about since I don’t know how to play bridge. I’ve been impressed by how much time and information everyone seems to have for me. I am constantly thinking how I can bring this experience back to my students. Some ideas are to have a science and math career day, collect weather data like the data the bridge collects, dissect hake, and examine zooplankton under a microscope. Various people on board have volunteered to help with all my ideas.

Steven Wilkie: July 3, 2011

NOAA TEACHER AT SEA
STEVEN WILKIE
ONBOARD NOAA SHIP OREGON II
JUNE 23 — JULY 4, 2011

Mission: Summer Groundfish Survey Geographic Location: Northern Gulf of Mexico Date: July 3, 2011 Ship Data

Latitude 29.27
Longitude -94.39
Speed 9.30 kts
Course 298.00
Wind Speed 6.70 kts
Wind Dir. 281.88 º
Surf. Water Temp. 29.90 ºC
Surf. Water Sal. 24.88 PSU
Air Temperature 29.30 ºC
Relative Humidity 75.00 %
Barometric Pres. 1015.75 mb
Water Depth 15.70 m

Science and Technology Log

One of the first expeditions devoted to the study of the world’s oceans was that of the H.M.S. Challenger.  This voyage covered a distance of more than 68,000 nautical miles.   Although other expeditions prior to the Challenger expedition would periodically collect data about the ocean environment, none were devoted solely to the exploration of the chemical, biological and physical attributes of the oceans.

The Voyage of the HMS Challenger

The HMS Challenger’s voyage spanned 4 years and covered close to 70,000 nautical miles.

A sounding device used by the Challenger expedition. This weighted line would be lowered over the side of the ship and the amount of line let out would indicate depth.

If you have read my previous posts, you know how important monitoring the abiotic factors are.  This was no different aboard the Challenger expedition.

And remember it took 23 years to process and publish all of the data, well with the help of computers and the internet, the Oregon II’s data is available in hours.

Michael Hendon (lead scientist) performs a winkler titration to determine dissolved oxygen content. See wet chemistry skills are still important!

Michael Hendon (lead scientist) performs a winkler titration to determine dissolved oxygen content. See wet chemistry skills are still important!

Although technology plays a pivotal role in collecting and analyzing the data, computers still need to be cross referenced against tried and true scientific processes.  In order to ensure that all of the CTD equipment is accurate, random water samples are pulled using the CTD’s sample bottles.  A chemical titration, known as the Winkler titration is used to determine the amount of dissolved oxygen present in the water samples.

The method for sampling the living organisms along the bottom of the seafloor has not changed much since the Challenger expedition.  Trawl nets are still the name of the game, although the way they are deployed might vary a bit!

Mike and Cliff bring the Oregon II's trawl aboard complete with catch.

Once the catch is on board, the process begins to collect data (remember that is why NOAA is out here) to better understand how populations are changing in order to set catch limits and analyze human impact.  In the day’s of the Challenger expedition, the work of analyzing samples and collecting their would have been done in a lab aboard ship, and we rely on similar if not more automated facilities onboard the Oregon II.  Follow this link to take a virtual tour of the Challenger’s “Wet lab”. The wetlab onboard the Oregon II is where I spend the majority of my 12 hour watch.   It is here that the catch is brought after we bring it on deck, we sort the catch, count and measure a subsample of what is brought on board.  If we had to measure everything that came up with the net we would never get finished.  By taking a subsample we can split the catch into percentages depending on the weight of the entire catch and count a smaller sample of the catch.  This subsample’s diversity can then be used as a basis for the entire catch.  This saves time and effort on our part and still provides an accurate representation of what was in the net.  A few species are selected to be counted in their entirety, that includes all commercially important shrimp (brown shrimp, pink shrimp and white shrimp) and all red snapper.  We will also pull organisms into our subsample that are unique to the catch such as sharks, rays, skates etc.

Now I am not quite sure how the Challenger expedition determined where it would sample and when, perhaps if they saw something interesting they would simply drop their nets in the water, but with the Oregon II, the sampling sites are predetermined and the method to set up those sites is quite sophisticated.  In order to ensure that the cruise covers the majority of the Gulf of Mexico NOAA uses a method known as independent random sampling.  This method uses a computer program to randomly select stations based on depth data, and spatial area.  By choosing random samples independently, the scientists can rest assured that they haven’t purposefully singled out an area with “good fishing” or “bad fishing” and that the data they collect will represent a more accurate count of the actual fish populations in the Gulf of Mexico.

Jason Moeller: June 14-16, 2011

NOAA TEACHER AT SEA
JASON MOELLER
ONBOARD NOAA SHIP OSCAR DYSON
JUNE 11 – JUNE 30, 2011

NOAA Teacher at Sea: Jason Moeller
Ship: Oscar Dyson
Mission: Walleye Pollock Survey
Geographic Location: Gulf of Alaska
Dates: June 14-16, 2011

Personal Log

Welcome back, explorers!

June 14

I think I posted my last log too soon, because as soon as I hit the send button interesting things began to happen. First, I was called up to see some Mountain Goats feeding in the wild! I was able to take a picture of them as well! (Well, kind of…)

goats

The mountain goats were so far away I had to use binoculars just to spot them. If you can spot the two tiny white dots to the right of the snow, that is them! There is also one that is on the left hand side in the middle of the photograph. You will have to take my word for it.

While this was going on, the professional members of the science team were still calibrating the sonar that we are going to use to catch the fish! I have explained the process in the captions of the following photographs.

sonar balls

Calibrating starts with these little balls. The one used to calibrate our sonar was made of Tungsten (like the black ball at the top)

Pole

The ball was suspended underneath the water on three poles, placed in a triangular shape, around the ship. This is a photo of one of the poles.

Screen.

Once the ball was placed underneath the boat, the scientist swept sound waves off of the ball and used the above screen to see where the sound waves were striking the ball and reflecting. This allowed them to adjust the sound waves to hit the ball (or out in the ocean, the fish) exactly where they wanted it. This optimizes the amount of sound coming back to the boat and paints a better picture of what is under the water.

The process took several hours, but once we finished, we headed back out to sea to start the two-day journey towards our first fishing spot!

June 15-16

The most common sight off of the boat for the past two days has been this one.

Water

Water, water, everywhere

We are currently in Unimak Pass, which will lead us to the Bering Sea! Unimak Pass is the fastest sea route from the United States into Asia, and as a result is a common merchant route between Seattle and Japan. It is also the best way to avoid rough seas and bad weather when travelling between the Gulf of Alaska and the Bering Sea, as it receives some cover from the landmass.

The Bering Sea likely needs no introduction, as it is arguably the best crab fishing waters on the planet and is well-known from the television show The Deadliest Catch. Aside from crab, the Bering Sea is teeming with life such as pollock, flounder, salmon, and halibut. As a result of this diverse and tasty biomass, the Bering Sea is an incredibly important area to the world’s fisheries.

Steaming towards our destination has kept us away from any land, but there are still things to do and to see! We did a second dry cast of the net, but this time two different pieces of equipment were tested.

The net

The first piece of equipment was a special net for taking samples. The net has three sections, called codends, which can be opened and closed individually. You can see two of the codends in this photo. On top of the green net, you should see black netting that is lined with white rope. These are the codends.

net 2

This is a better view of the codends. The codends are opened and closed using a series of six bars. When the first bar is dropped, the first codend is able to take in fish. When the second bar is dropped, the codend is unable to take in fish. The bar system has not worked incredibly well, and there is talk of removing one of the codends to make the net easier to use.

camera

The second piece of equipment was this camera, which was attached to the net. It allowed us to see what was coming in the net. Even though this was a dry run and we were not catching anything, I still saw a few Pollock in the camera!

Even though this was a test run and we did not catch any fish, the birds saw the net moving and came to investigate. The remaining photographs for the personal log are of the several species of birds that flew by the boat.

Bird 1

A Northern Fulmar flies alongside the Oscar Dyson

Bird 2

An albatross (by the thin wire just below the spot the water meets the horizon) flies away from the Oscar Dyson

Bird 3

Fulmar's and Gulls wheel about the Oscar Dyson, looking for fish.

Science and Technology Log

This section of the blog will be written after we start fishing for Pollock in the next day or so!

New Species

Mountain Goats

Northern Fulmar

Albatross

Gulls

Reader Question(s) of the Day!

First, I owe a belated shout out to Dr. John, Knoxville Zoo’s IT technician. He lent me the computer that I am currently using to post these logs, and I forgot to mention him in the last post. Thanks Dr. John!

The two questions of the day also come from Kaci, a future Teacher at Sea with NOAA.

1. What is it like sleeping on the boat?

A. Honestly, I am being jostled around quite a bit. Part of this is due to the way the beds are set up. The beds go from port to starboard (or right to left for the landlubbers out there) instead of fore to aft (front to back). This means that when the boat rolls, my feet will often be higher than my head, which causes all of blood to rush to my head. I still haven’t gotten used to the feeling yet.

Part of the jostling, though, is my fault. I had heard that most individuals took the bottom bunks given the option, and since I was one of the first individuals on board, I decided to be polite and give my roommate, who outranked me by some 10-15 years at sea, the bottom bunk. It turns out that the reason people pick the bottom bunk is that the top bunk moves around more since it is higher off the floor. I’ve heard stories about people being thrown from the top bunk in heavy seas as well.

The most comfortable place to sleep has turned out to be the beanbag chair in the common room. It is considered rude to go into your room if your shift ends early, as your roommate may still be sleeping. My shift ended two hours early the other night, so I sat down on the beanbag chair to catch some zs. The ship’s rocking was greatly reduced by the bean bag chair, and I slept very well for the next couple of hours.

2. Is it stressful so far?

A. The only stressful part of the trip so far has been the seasickness, which I have not yet been able to shake. The rest of it has been a lot of fun!

Sue Zupko: 10 Steamin’ an’ a Beamin’

NOAA Teacher at Sea: Sue Zupko
NOAA Ship: Pisces
MissionExtreme Corals 2011; explore the ocean bottom to map and study health of corals and their habitat
Geographical Area of Cruise: SE United States deep water from off Mayport, FL to St. Lucie, FL
Date: June 4, 2011

Weather Data from the Bridge
Position: 29.1° N  80.1°W
Time: 11:00 EDT
Wind Speed: calm
Visibility: 10 n.m.
Surface Water Temperature: 27.6°C
Air Temperature:27.6°C
Relative Humidity: 72%
Barometric Pressure:1018.4 mb
Water Depth: 85.81 m
Salinity: 36.55 PSU

When the strong current from the Gulf Stream stretched the tether of  the ROV  and broke one of the three fiber optic cables inside, it was time to come up with a new plan.  What do you do in the middle of the ocean if the main gear is not functioning?  Plan B.  Well, Plan B was using the spare fiber optic in the tether.  The spare one then broke as a result of being rubbed, most likely, by the sharp end of the original broken fiber during the next dive.  Now we had to go to Plan C .  Fortunately the ROV crew is experienced, and, like Boy Scouts, were prepared.  They brought a spare ROV and tethers from their lab in La Jolla (pronounced La Hoya), CA just in case.    The ship is running the sonar gear back and forth over the area we plan to dive tomorrow, mapping out the bottom, looking for coral mounds.  This process is called “mowing the lawn” since you run the beams back and forth to get complete coverage of the bottom, and it looks like the lines on the lawn left by the mower.  Think of the beam as having the shape of a flashlight’s beam shining on the floor.  Another interesting feature is that the acoustic beam can also read what fish are present.  It needs to have a swim bladder for the signal to bounce back.  When it does, based on the sound, an experienced acoustician can read what fish the signal represents.  Sharks don’t have a swim bladder like most fish do so their signals are a bit more difficult to read.

I was just up on the bridge and it seems we hit “pay dirt” (like gold miners).  The captain had been explaining to me a symbol shown on the Electronic Chart Display System (ECS).   It looks like a graphic math problem showing the intersection of lines, in this case one line running on a 110° angle with three lines parallel to each other intersecting it.  The line in the middle is a bit longer than the other two.  I asked how he knew what that symbol meant.  Apparently, there is a book for everything on the bridge.  He whipped out his handy-dandy book entitled, Chart No. 1.  It is a key to reading nautical charts (maps).  He searched for the correct page with bottom obstructions of all types and showed me that symbol and what it means.  Whenever I have a question, the bridge crew whips out a book of some type to let me see the answer.  It’s really interesting.  The Pisces is a really modern ship with the latest electronic navigation and scientific features.  The other day I asked about navigating without power.  There is a book for that.  Bowditch American Practical Navigator has everything you need to know about crossing the ocean without electronics.  As it says on my classroom door, “Reading makes life a lot easier.”  Turns out that symbol is a shipwreck.

Laura sitting in front of computer screen

Laura Kracker looks at maps

But I digress.  Back to the pay dirt (we struck gold).  Laura Kracker, our geographer started getting excited.  “Look at this!  Look at this!  Write down these coordinates.”

She went running back to the acoustics lab (where they use sound echos to map the ocean floor and the presence of fish) to mark the location along the transect (lines we’re running) because we apparently were over coral mounds.  Using  information gathered by others in years past as a guide, they were mowing the lawn with the sonar to find interesting habitat to study with the ROV.  As the ship went back and forth along the planned transect to develop a much better map than existed, Laura would radio the bridge about any changes to the courseto pinpoint the best areas for us to study over the next couple of days.

ROV crew working on transferring gear from one ROV to the other on deck

ROV crew swtiches gear from one ROV to the other

Everyone was very excited.  So, although the ROV had to be switched out, which took a lot of work, we made good use of the time on the ship.  After a whole day of mapping, it’s now late at night and the map looks gorgeous.  This is important work and many cruises are devoted entirely to mapping.  Andy David, our lead scientist, says this acoustic mapping is useful to many people and will allow more precise coral surveys for years to come.

Margaret Stephens, May 25-27

NOAA Teacher at Sea: Margaret Stephens
NOAA Ship:
Pisces 
Mission: Fisheries, bathymetric data collection for habitat mapping
Geographical Area of Cruise: SE United States continental shelf waters from Cape Hatteras, NC to St. Lucie Inlet, FL
Dates: May 25-27, 2011

Weather Data from the Bridge 

View from the Pisces bridge: calm seas

View from the Pisces bridge: calm seas

As of 11:43 May 27, 2011
Latitude 29.94
Longitude 80.29
Wind Speed 0.60 knots; calm
Wind Direction 167.50 º
Surface Water Temperature 26.60 ºC
Air Temperature 25.70 ºC
Relative Humidity 81.00 %
Barometric Pressure 1013.70 millibars (mb)
Water Depth 54.59 m
Skies: clear to partly cloudy

Science and Technology Log 

I struggle to measure a squirmy black sea bass, Centropristis striata.

I struggle to measure a squirmy black sea bass, Centropristis striata.

Previous logs describe in some detail the three principal components of this research work aboard Pisces: overnight mapping using acoustics (SONAR) technology; daytime fish trapping; and underwater videography. The nighttime mapping is used to identify the hardbottom habitats favored by red snapper and grouper species and helps the science team determine where to set traps the next day. The videography provides additional visual clues to the contours and composition of the sea floor, water clarity, and marine life in the area.

Scientific research at sea is far from neat, clean and predictable. Messy, hot, smelly, sometimes frustratingly unpredictable – and not for the weak-stomached– are better descriptors. The work goes on as long as it takes, well past the scheduled twelve hour shifts. The “wet” lab could just as well be called the “fishy” lab. For good reason, the seasoned researchers wear special waterproof bibs and boots and clothing they don’t mind getting dirty. A distinctly fish-infused aroma fills the air and embeds skin, hair and garb. The best laid plans go awry. Equipment and instruments are checked, double- and triple-checked; nevertheless, they don’t always function properly or yield the expected results. Despite using high-tech SONAR to locate what appear to be promising locations, and baiting traps with the most appetizing bait imaginable (dead menhaden), the fish move around and are not always lured into the traps we set so carefully. While this project has been graced so far with unusually calm seas, the currents, other boat traffic, threatening weather and other factors can cause the ship to deviate from its appointed path.

These scientists seem to thrive as they meet the challenges of the ever-changing seascape, solving problems and continuing the hard work day and night.

Todd Kellison (l) and Warren Mitchell (r) confer at sunrise as their long night’s acoustics lab work continues past dawn. Photo credit: David Berrane

Todd Kellison (l) and Warren Mitchell (r) confer at sunrise as their long night’s acoustics lab work continues past dawn. Photo credit: David Berrane

After spending the first few days south of Cape Canaveral, mapping and trap sampling, calibrating and making adjustments to the instruments and deployment procedures, we headed north, because strong currents and turbid (cloudy) waters were limiting the team’s ability to deploy traps and capture useful underwater video images. When the currents are too strong (>2.5 – 3 knots, or nautical miles per hour), the moving water tends to drag the traps, making it very difficult to position them in the desired locations on the sea floor. In addition, the currents swirl sediments around, reducing visibility and yielding video images that are less than revealing. Since moving north of Cape Canaveral, the currents have been less of a problem, and the water clarity has improved.

The mapping, trapping, and video procedures all went more smoothly after the team made adjustments guided by the first days’ experiences. The acoustics team leaders, Warren Mitchell and Todd Kellison, have worked assiduously throughout the taxing, tiring overnight shifts to produce useful bathymetry maps with the ship’s state-of-the-art ME70 multibeam sonar unit. Investigator Jen Weaver has applied her expertise with GIS and mapping software to help Warren and Todd translate the sonar data into three dimensional maps most useful for Nate Bacheler, the Chief Scientist, to plan the trapping routes.

Sonar image shows ledges and outcrops. Photo credit: Christina Schobernd

Sonar image shows ledges and outcrops. Photo credit: Christina Schobernd

By the second and third nights on the acoustics team, I was getting better at recognizing the features on the sonar screen displays, such as ledges and rocky outcroppings, that are indicative the hardbottom habitats we were seeking. Chief Scientist Nate has perfected the timing and communications with the deck crew so that the traps are released off the stern deck at just the right time, sinking to the bottom in the desired locations. Radio transmitter in hand, Nate studies an array of monitors displaying the sonar images of the sea bottom mapped the night before, the navigation system with the ship’s position and path, and a live video feed showing the crew awaiting instructions on the deck. The helmsman alerts Nate that the ship is approaching the next drop point and slows the ship.

Nate issues a series of commands to the deck crew by radio:

Crew deploys baited trap above guard rail on

Crew deploys baited trap above guard rail on

Ready the cameras. Ready the cameras.” – A few minutes before the ship approaches each trap point, a team member activates the two video cameras attached to the trap.

Crew deploys baited trap above guard rail on

Go on standby; stand by to deploy trap.”- The deck crew positions the trap at the edge of the stern (back) deck and makes sure all the lines are clear.

Deploy trap; deploy trap.” The deck crew pushes the trap over the edge of the stern and lets the line attaching it to the ship run free. Once the line goes slack, indicating the trap has reached the bottom, the crew releases the bright orange buoys to float on the surface, marking the trap locations to warn other ships to steer clear and facilitate retrieval.

The deck crew then positions the next trap, and the helmsman, Nate and crew repeat the choreographed sequence until all six traps in each set are in place. Soon after, the helmsman maneuvers the ship for the deck crew to retrieve the traps and their contents one by one using a pothauler, a special hoist.

Technical/Logistical Challenges 

We ran into some initial difficulties with the video cameras attached to the traps when they turned off and failed to record. As good scientists, the team observed the procedures closely and determined that the force of the cameras hitting the water upon release was probably causing them to shut off. At first, the traps with cameras attached were being pushed off the stern above a fixed guard rail, which sits about 1.5 meters above the deck, with three removable guard wires below the rail. A simple adjustment seems to have fixed that problem – instead of releasing the traps above the guard rail, the crew lowered the traps to the deck floor and pushed them off more gently from there. This modified procedure seems to have done the trick, as the cameras have not shut off since.

Science team adjusts camera-trap arrays on stern deck

Science team adjusts camera-trap arrays on stern deck

We are constantly reminded of the ship’s mantra, “Safety first!”, as anyone working on deck while machinery is in operation is required to wear a hardhat and personal flotation device (PFD). He or she who forgets to do so is quickly alerted by others. Because the change in the trap release procedure necessitated removing the three safety wires below the stationary guard rail, leaving a gap large enough for a person to slip overboard, the crew members tied themselves to tethers attached to the deck. Falling off the stern of the ship is dangerous, not least because the propellers turn rapidly and create a backwash effect that could draw a person underwater, even one wearing a PFD.

After each set of six traps is collected, the crew and wet lab team prepare them for redeployment. They empty any fish caught from the traps into bins, separate them into species, then weigh, measure, and release or preserve them for further study. With the help of the deck crew, two or three members of the science team stay on the side deck, dressed in waterproof bibs, boots, life vests and helmets. They detach and dry the cameras and hand them to the dry lab video coordinator, Christina Schobernd, who immediately removes the memory cards, sets up the video to view, and readies the cameras for the next trapping sequence. Occasionally, a camera tilts out of alignment, possibly in the jolt of travel or by hitting something underwater or on the bottom. Each time that happens, Christina meticulously assesses the situation and adjusts the cameras’ attachments.

Under these conditions, working with expensive equipment, it is crucial to anticipate possible problems and build redundancy into the operations as much as possible. This year, the team added a second, high-definition camera to the video array, and each camera is attached to the trap frames with at least six heavy-duty plastic ties and a tether wire and clip. That tether has been a camera-saver, as in one instance the cameras somehow broke free and would have been lost without it.

Fish measuring “assembly line” in the wet lab

Fish measuring “assembly line” in the wet lab

Thanks to good planning, enhanced by a measure of good luck, so far we have not lost any traps or equipment. It is not unheard of to have a trap break free from impact, from a boat propeller running over and cutting the line, or for some other reason. If a trap breaks loose in a place that’s too deep for human divers to search, or if the ship is not equipped with diving capability or a ROV (remote operating vehicle), the trap must be given up for lost.

Once the traps’ fishy contents are brought in and separated by species, three to four people in the wet lab process the fish in assembly-line fashion, as described in the previous log. With traps containing one hundred fifty (150) fish or more, we have to work fast and furiously to weigh, measure and release them before the next haul is aboard. The fish flop and squirm and squirt, and as I learned the first time I handled them, the black sea bass have some mighty sharp spines that can penetrate even the heavy, protective gloves we wear.

To ready the array for the next trap set, the team then

  •  “freshens” the bait by taking out any fully or partially eaten bait and replacing it with the same number of whole menhaden fish;
  •  reattaches the cameras;
  • lines up the numbered traps on deck, ready to go again.

Sometimes, the interim between trap sets coincides with the ship’s lunch time: 11 a.m. If so, the science team takes a short break to refuel with Steward Jesse Stiggens’ tasty culinary creations. If not, the stewards leave the lunch buffet available for whenever the team can get away for a few minutes. While the traps are “soaking” (sitting on the sea floor for the required ninety minute intervals), the science team keeps busy viewing video from the previous haul, processing fish specimens, tidying the deck and lab area, speculating about what the next trap might yield, and telling fish stories from past field work. As anyone who has spent time around fishers (the gender-neutral form of fishermen) knows, fishing stories always get better with time!

Processing and Collection of Biological Samples 

Otolith showing age rings Photo source: dnr.state.oh.us

Otolith showing age rings Photo source: dnr.state.oh.us

To assess fish stock and population trends, scientists must do more than identify species and catch, weigh and measure fish. They also determine the sex, size and ages of fish and genetic diversity within the populations studied. Connecting size and age can help determine the fishes’ growth rates, where they are in their reproductive cycles, and how likely they are to spawn, or reproduce.

Why is it important to determine the age of fish? By knowing the age of fish, fisheries managers can better understand and monitor how fish populations change over time, and how they are affected by environmental stresses or disturbances, including environmental changes, storms, pollution, commercial and recreational fishing, natural mortality, predation, and changes in the availability of food. The age information helps inform policies promoting fishing practices that protect the fish resources for sustainable, long-term benefit.

David Berrane removes otoliths from red snapper, Lutjanus campechanus Photo credit: Christina Schobernd

David Berrane removes otoliths from red snapper, Lutjanus campechanus Photo credit: Christina Schobernd

To determine fish age most accurately, the scientists remove otoliths, two bones located on either side of fish’s skull that are analogous to the human ear bone. The otoliths show annual growth rings, so the technique used is similar to counting tree rings. You may clickhere to try aging a sample fish.

On board Pisces, the experienced scientists remove the otoliths from dead fish with a sharp knife and scalpel, then place the otoliths in small envelopes, labeled with the date and location caught, ready to be analyzed back in laboratories on land. At the same time, they preserve tissue samples used for DNA/genetic analysis. They may also remove the gonads, or egg sacs, of female fish, if they are needed for further study. They can approximate how close the fish are to spawning based on the condition of the egg sac. The closer they are to spawning, the fuller and larger the sacs become.

Removing egg sacs from female black sea bass, Centropristis striata

Removing egg sacs from female black sea bass, Centropristis striata

Through laboratory analysis using DNA from tissue samples, scientists can evaluate the genetic diversity within each species and other population dynamics. Genetic diversity among fish populations, as in other animal and plant species, is desired because more genetically diverse populations are generally more resilient, more resistant to disease and more able to withstand changes in environmental conditions, availability of food, and other stresses.

Personal Log 

We’ve been fortunate to have had a stretch of unusually fine weather and calm seas. Thank goodness, not a single person has shown a hint of sea sickness. It may be bad luck to say this while we are still out on the water, but I have never been seasick, and I certainly would not want this to be the first time. I’ve seen people who literally turned green and felt absolutely miserable while traveling on rough seas. Some of the crew members who served in the United States Navy or on commercial vessels told me that they had been violently sick every day for weeks when they first went to work at sea. Most eventually get over that. I cannot imagine how debilitating and horrible it must be to feel so wretched. There’s no place to go once you are on a ship — you cannot just jump overboard and swim home through long distances and possibly shark-infested waters, although if you are sick enough, that prospect might seem a welcome relief!

Significant events 

Late one afternoon, I noticed that we had changed direction. We had been heading south, and then turned back north. Since this was not the planned route, I thought perhaps I had missed or misunderstood something, so I went up to the bridge to investigate. Commander Jeremy Adams (the CO = Commanding Officer) informed me that he had turned the ship around in response to a radio call from the Coast Guard, the branch of the armed services of the United States in charge of monitoring the coasts for navigation, safety and law enforcement. The radio call was a Pan-pan alert, one step short of the emergency Mayday call that mandates immediate action. A Pan-pan is urgent but not imminent, and ships in the area are not required to respond. In this case, the Coast Guard announced that they had received a report of a partially submerged small boat with possible man overboard/missing. Since Pisces was the closest vessel to the reported location, CO Adams made the decision to deviate from the planned course and redirect her at nearly full speed, approximately fourteen knots (nautical miles per hour), to search and assist if necessary. As Captain Jerry put it, even though he was not obligated to respond, he would not have been able to rest knowing there was a possibility the ship under his command could have helped. While en route there, another radio relay from the Coast Guard canceled the Pan-pan, because the initial report was apparently a false alarm. The CO informed me that false alarms of this kind occur all too often. Sometimes disgruntled or troublemaking recreational boaters, perhaps annoyed with the Coast Guard’s vigilance or just pulling a prank, call in alarms. These are akin to and at least as dangerous as intentionally false bomb scares or fire alarms on land. Such maliciously false reports take emergency personnel and resources away from true emergencies, cause tremendous waste of public funds, and can put emergency responders and others at risk. At sea, if the perpetrators are caught, they can be fined heavily and held responsible for all the costs incurred.

Devastation in Joplin, Mississippi 

On Sunday, May 22, news of the catastrophic tornado in Joplin, Mississippi reached Pisces. One of the crew members watched the news feed in horror, as the images of an elementary school that had been completed flattened played over and over again on the large screen in the mess. His friend lived just two blocks from that same school and had probably been at home when the powerful twister hit. The crew member tried in vain to call her cell phone or reach anyone who might have heard from her.

In the next hours, we learned that this NOAA ship’s crew is like family. The CO authorized the crew member to take personal leave and arranged for Pisces to meet a Coast Guard vessel the next morning to transport the young man to shore, so he could catch a flight and drive to Mississippi to search for his friend. Since he is also a certified medic, he would be allowed in to the town, despite any official restrictions.

We all felt for him and waited anxiously for word from Joplin. Thankfully, a day later, the ship received a message that his friend was alive and physically intact, although her home and entire neighborhood were destroyed, and so many other residents were critically injured, missing or dead.

It would be terrible to be isolated at sea in such circumstances and feel utterly helpless. I was reminded of the sacrifices so many service members make. As other crew members who had served in the U.S. Navy and other military branches know all too well, home leave, even in emergencies, is not always possible. Many of them had missed key personal events and tragedies while they were away from home on active duty.

Links & Resources

Barbara Koch, October 4, 2010

NOAA Teacher at Sea Barbara Koch
NOAA Ship Henry B. Bigelow
September 20-October 5, 2010

Mission: Autumn Bottom Trawl Survey Leg II
Geographical area of cruise: Southern New England
Date: Tuesday, October 4, 2010

Weather from the Bridge

Latitude 39.94
Longitude -73.47
Speed 1.10 kts
Course 22.00
Wind Speed 34.25 kts
Wind Dir. 69.54 º
Surf. Water Temp. 19.70 ºC
Surf. Water Sal. 31.85 PSU
Air Temperature 15.80 ºC
Relative Humidity 88.00%
Barometric Pres. 1015.72 mb
Water Depth 45.00 m
Cruise Start Date 10/02/2010

Science and Technology Log

The Bridge

The Bridge

I visited the bridge of NOAA Ship Henry B. Bigelow to see how the ship is run. Thebridge sits atop the ship and is the command center for all navigation andcommunications operations during the cruises. Windows surround the entire bridge, giving NOAA Corps officers a 360 degree view of the surrounding ocean. Here, Commanding Officer, Anne Lynch, and Junior Officer, ENS Kyle Sanders stand at the main bridge console of the ship. NOAA Corps officers chart the ship’s course, control the speed, steer the ship, detect other objects in the ocean via sonar, monitor weather conditions, and communicate with others at sea, on the ship, and on shore from this console.

Console for steering the ship

Console for steering the ship

Aft Control Station

Aft Control Station

The Aft Control Station (ACS) is located at the rear of the bridge and overlooks the working deck. The ACS provides control ofthe Auto Trawl System to pull the research net at a constant andstraight trawl. A closed circuit television improves the crew’s visibility while operating the gear from the bridge. Here is a picture of the ACS control panel on the bridge and the research net on the rear deck.

Henry B. Bigelow is also equipped with two scientific SONAR systems used for gathering data on fish and plankton and for collecting oceanographic data, such as water salinity and water temperature. Transducers are mounted at the center of the hull and extend below the ship to take acoustic readings of water depth or the location of schools of fish. One of the SONAR transducers on this ship can work at depths as deep as 5000 meters and can detect objects under water as close as one meter or as far away as 800 meters. It also detects objects on the sea floor, as well as in the water column. This system is controlled from the bridge, as well.

SONAR controls

SONAR controls

A separate control panel is used to monitor and control power and water usage on board the ship. Two generators provide electricity for the ship. There are also tanks in the hull designated for different purposes, such as holding water, fuel, and potable water. This control board monitors all of the tank and power usage levels for the entire ship.

Personal Log

The lounge

The lounge

Today is my birthday! Spending my birthday aboard a NOAA research vessel is a great gift! Today is also the second day spent waiting for the seas to calm down so we can take more samples. Wind speeds are 34.25 kts. and the waves are about 11-16 feet high. The boat is rocking and rolling, and makes it very difficult to move around. The night watch is sleeping, so we cannot go in our staterooms, and we must be quiet everywhere we go. It is too windy to go outside on the deck, as well. The only thing we can do is wait in the lounge. The lounge is equipped with a television, two computers, couches, a conference table, games, movies, and reading material. Since it is my birthday, I have the honor of selecting one of the movies we will watch. That’s a hard thing to do when you are with a group of people with so many different tastes and personalities. . . the “A Team” it is! It’s great that the crew and scientists have a place to go for entertainment, because waiting for so many hours on end can start to get on everyone’s nerves.

Gym

Gym

Luckily, the ship also has a workout room, which I visited briefly. It’s very difficult to lift weights when the ship is rocking, and the elliptical machine seemed to run by itself. The stationary bicycle was a little easier to manage, and it felt good to move my legs after sitting for so long in the lounge.

Galley

Galley

However, I think the biggest morale booster for me, the crew and the scientists is thewonderful food that Dennis and Randy make in the galley. Their menus rival those of some finer restaurants I’ve visited, and we are treated to their artistry every day way out here in the ocean. I’ve truly been spoiled!

Rebecca Kimport, JULY 3, 2010

NOAA Teacher at Sea Rebecca Kimport
NOAA Ship Oscar Dyson
June 30, 2010 – July 19, 2010

Mission: Summer Pollock survey
Geograpical Area:Bering Sea, Alaska
Date: July 3,  2010

Here fishy fishy

In a previous post, I briefly mentioned that acoustics helps Oscar Dyson scientists locate aggregations of pollock. I didn’t know much about acoustics surveying before I arrived on board but think its pretty cool.The Oscar Dyson has 5 transducers on its center board and 1 temporary transducer on the side of the center board that looks horizontally. The transducers allow us to see where the fish are. Because of where the transducers are placed, we can only see the pollock from 16m to the bottom. This means that if there are any fish between the surface and 16m they will not be detected. This is the near surface “dead zone”. At right you will see a picture of the acoustic data picked up by the transducers. Why this happens? The transducers are mounted on the bottom of the centerboard about 9 m below the water line, and near the transducer face (first 7 m), no good data are collected. Why it’s okay? Pollock tend to hang out in mid-water. Although a few baby pollock might be in the near surface “dead zone,” the majority of pollock will be in the area we are watching. There is also a bit of a “dead zone” at the other end near the ocean floor.
Acoustic Data

Acoustic Data

Why acoustics? 
Ideally, the acoustic data collection would allow us to track aggregations of pollock without actually having to fish them out of the water. All parties involved (scientists, fish, bank accounts) would benefit from this change but scientists are still in the process of perfecting this process. The Oscar Dyson is part of a fleet of five boats that was specifically designed for acoustics. Specifically, it is considered a “quiet boat” where the engine noise is decreased to prevent scaring the fish. Other acoustic projects include: Pacific hake off the coast from California to Vancouver Island (run as a joint project with Canada), herring in the northwest Atlantic, and krill in the Antarctic. Acoustics are used throughout the globe and many countries depend on acoustics for their fish surveys.

Sonar

Sonar

Looking in more than one direction
Along with the transducers, there is also a multibeam SONAR that produces the same information as the transducers but with a wider angle range. Scientists use this program to help separate species in the water column. The multibeam ME70 sends its signal out after the transducers information is sent and returned. They alternate about 1.5 seconds apart. Scientists around the world are working to improve this technology and we use information from a group at University of New Hampshire along with a program from Tasmania to analyze these data. Scientists utilize the multibeam ME 70 along with the transducers and fish trawling to ensure they are capturing an accurate picture of the mid-waters.

How the survey data we collect are used.
The data we collect on the Oscar Dyson during the summer pollock surveys are used by scientists and policy makers to determine the fishing quota (the “take”) of pollock for the next season. Quotas are important for maintaining the population of pollock (and other species) for this generation and generations to come. The data we collect on the Oscar Dyson help ensure that maximum stock can be taken without negatively impacting the Eastern Bering Sea pollock population.Thought Question: What could happen if we didn’t regulate the amount of fish that could be caught? Bonus points for anyone who can identify an area where overfishing has impacted the ecosystem.

David Altizio May 24-26 2010

NOAA Teacher at Sea
David Altizio
Onboard NOAA Ship Fairweather
May 17 – May 27, 2010

NOAA ship Fairweather
Mission: Hydrographic survey
Geographical Area of Cruise: SE Alaska,
from Petersburg, AK to Seattle, WA
Dates: Monday, May 24 and Tuesday, May 25,
Wednesday, May 26

Weather Data from the Bridge

Position: Hassler Harbor
Time: 0800 on 5/24
Latitude: 550 13.06’ N
Longitude: 1310 27.15’ W
Clouds: Light drizzle
Visibility: 8 miles
Position: Inside Passage
Winds: Light with variable directions
Time: 0800 on 5/25
Waves: Less than one foot Latitude: 52024.5’N
Dry Bulb Temperature: 11.20C
Longitude: 128030.0’W
Wet Bulb Temperature: 10.00C
Clouds: Mostly Cloudy
Barometric Pressure: 1006.4 mb
Visibility: 10 + miles
Tides (in feet):
Winds: 10 knots from the NE
Low @ 0439 of 0.1
Waves: One to three feet
High @ 1055 of 13.1
Dry Bulb Temperature: 11.00C
Low @ 1637 of 2.2
Wet Bulb Temperature: 10.10C
High @ 2254 of 16.4
Barometric Pressure: 1009.1 mb
Sunrise: 0422
Sunset: 2105

Science and Technology Log

On Monday we were testing one of the multi‐beam sonar transmitters that had not been working properly on the Fairweather, in Hassler Harbor near Ketchikan, AK. In order to verify that the device is working properly the ship went back and forth over an area that has previously been mapped from all different directions. This is called patch testing. Ideally you are looking for no difference in the data from one test to another test.

Me,at the helm,driving the Fairweather.

Me, practicing using the line throwing device.

While on board Monday, we also practiced using a line throwing device. This piece of equipment can be used for ship to ship rescue operations, or to get a line onto a pier if needed, or for other rescue operations. The device is powered by 3000 lbs. of compressed air. Today we only fired a test line, but the real one can travel almost 200 meters. Being prepared and knowing what to do in the case of an emergency is extremely important while out at sea. Not only was I allowed to use the device, but so was anyone else on board who had not learning how to use it properly.

Marine aneroid barometer measures air pressure.

Digital anemometer showing wind speed and wind direction.

I have also been collecting and recording the weather data from the bridge of the ship. These observations are made every hour. There are many different meteorological instruments on the Fairweather. The atmospheric pressure is recorded using an aneroid barometer. The dry and wet bulb temperature readings were taken off of a sling psychrometer, just outside of the bridge. The wind direction and wind speed were taken from a digital anemometer and verified using the vectors of the wind direction and the heading of the ship. The visibility, wave height and the cloud cover are estimated visually by observing them from the bridge of the ship.

One of the ship’s officers, tracking our plot by hand on the chart.

Me taking the temperatures off of a psychrometer outside of the bridge.

I was also given the opportunity to man the helm and drive the Fairweather, for about 10 minutes as we headed south towards British Columbia, Canada. The bridge of the Fairweather has a many different screens, monitors, sensors and gauges. In order to see where we are going there are digital charts, which have our path projected on them. Also, some of the ship’s officers will verify our position along our course by hand. The depth to the bottom is determined by a fathometer, which works by using SONAR, not as complex as the multi‐beam mapping but more similar to a fish finder. In many maritime activities the depth is measured in fathoms. One fathom is approximately 1.8 meters or 6 feet. Knowing where you are and where other vessels are is extremely important.

Some of the Fairweather’s navigation systems.

Digital fathometer, measuring depth to the bottom using SONAR

The Fairweather has enough beds to hold a maximum of 58 crew members. The ships personnel is divided between: NOAA Corps officers, survey, deck, engineers, stewards,  electronics technician and visitors. There are almost 15 NOAA officers on the Fairweather, including the CO (commanding officer), XO (executive officer), FOO (field operations officer), and all the way thru captain lieutenant commander, 3rd mate, lieutenant, and ensigns. The survey group has approximately 10 people including the chief survey technician, senior, regular, and assistants.

More of the Fairweather’s navigation systems.

Digital readout of ship’s GPS (global positioning system) for precise latitude & longitude, speed in knots, and heading in degrees.

The deck group has 12 people and they help to maintain the deck areas, drive the launch boats, and help out in the anchoring and docking processes. There are 10 engineers who  make sure the ship is running properly. There are three stewards (cooks) who are amazing and make sure everyone is fed very well. There are 2 electronics technicians, and anywhere from two to five visitors, such as teachers at sea, technology support, mission/NOAA related personnel.

My stateroom on the Fairweather’s.

Fairweather’s store.

The Fairweather was originally commissioned in October 1968, deactivated in 1989 but a critical backlog of surveys for nautical charts in Alaska was a motivating factor to reactivate it in August 2004. The home port for the Fairweather is Ketchikan, AK and it operates mostly in Alaskan coastal waters. It is designed and outfitted primarily for  conducting hydrographic surveys in support of nautical charting, but is capable of many other missions in support of NOAA programs. The ship is equipped with the latest in hydrographic survey technology – multi‐beam survey systems; high‐speed, high‐resolution side‐scan sonar; position and orientation systems, hydrographic survey launches,  and an on‐board data‐processing server. It is 232 feet long, with a beam of 42 feet. It weighs 1,591 tons and the hull is made of welded steel. The Fairweather has a range of 6,000 autical miles, can stay at sea for 30 days, and has an average cruising speed of 12 knots.

The galley (kitchen) on the Fairweather.

Dish washing station on the Fairweather.

Mess hall (dining area) on the Fairweather.

One of the food storage areas on the Fairweather.

The staterooms on the Fairweather are fine for two people to live in. There is a bunk bed, dresser/desk area, closets, sink, small refrigerator, and a TV. The food on the Fairweather is really good, not just for being at sea, but really good with a lot of different options. There is also a small store where you can buy candy, soda and clothing with logos and images of the ship. There is a small workout room that people do use to keep active. There are three different food storage areas, one for dry goods, a refrigerated area, and a freezer. The Fairweather also has laundry facilities and a sick bay.

Laundry room on the Fairweather.

Fairweather at Customhouse Cove.

Personal Log

It is hard to believe that we are already heading south towards Seattle, WA. I have really enjoyed my time onboard the Fairweather and will never forget these experiences. Being a Teacher at Sea is amazing and I highly recommend it. I have seen so many different and new things that I can now add to my “teacher toolbox”.

On Monday, being able to learn how to use the line throwing device was very cool, but that was not the highlight of my day. I was also given the opportunity to man the helm, and drive the Fairweather for about 10 minutes. It is amazing that a ship this big is so responsive to small changes in the angle of the rudders. It was sort of like driving a really big car, in the sense that when you turn the wheel right the ship goes right and turning left makes the ship go left. There is a lot to do when at the helm. You have to make sure that we are following the correct heading, going the proper speed, not heading towards any other vessels or obstructions such as logs or other debris, and in water that is deep enough for the ship. As much fun as it was it was a little nerve racking, my palms were definitely sweaty.

Along the Inside Passage

I did have the help of four other NOAA officers to assist me and help me know what to do. It is not only up to the person at the helm to make decisions about what to do or which course to follow. The Fairweather is definitely a place where the junior officers are being trained and learning what to do in all types of situations. This aspect of helping and learning was prevalent in many aspects of what I observed while onboard the Fairweather and was great to see.

A while after I manned the helm, the seas got a little rougher as we went through Dixon entrance which marks the boundary between SE Alaska and British Columbia Canada. Here we were exposed to ocean swell from the Pacific Ocean/Gulf of Alaska. I was very glad this did not go on for too long. I made the mistake of trying to write this log while the ship was rocking and rolling a little bit. Not such a good idea. One of the officers told me to put down the computer, go out on the stern (back) of the ship, and look at land along the horizon. Being outside in the fresh air, while looking at land made me feel much better.

The sick bay on the Fairweather.

The rest of the trip towards Seattle has been very nice. The seas have not been too rough, and I am really enjoying the scenery as we go through the inside passage of British Columbia, Canada. Coming home and going back to New Rochelle High School will definitely be a change from the last two weeks. I will never forget the places, people and the science I have been exposed to in my time on the Fairweather in SE Alaska. We are now in the Puget Sound, and Seattle is almost in sight and I am ready to be home, back in New York.
Signing out, David Altizio Teacher at Sea

David Altizio, May 22 – 23, 2010

NOAA Teacher at Sea
David Altizio
Onboard NOAA Ship Fairweather
May 17 – May 27, 2010

NOAA ship Fairweather
Mission: Hydrographic survey
Geographical Area of Cruise: SE Alaska,
from Petersburg, AK to Seattle, WA
Dates: Saturday, May 22 and Sunday, May 23

Me standing on the rocks, making tidal observations.

Weather Data from the Bridge

Position: Customhouse Cove                  Position: Customhouse Cove
Time: 0800 on 5/22                                   Time: 0800 on 5/23
Latitude: 550 56.01’ N                              Latitude: 55006.5’N
Longitude: 1310 13.75’ W                       Longitude: 131013.7’W
Clouds: Mostly Cloudy                               Clouds: Mostly Cloudy
Visibility: 10 miles                                      Visibility: 10 miles
Winds: 6 knots from the NW                     Winds: 6 knots from the SE
Waves: Less than one foot                         Waves: Less than one foot
Dry Bulb Temperature: 12.20C         Dry Bulb Temperature: 11.00C
Wet Bulb Temperature: 10.20C        Wet Bulb Temperature: 9.80C
Barometric Pressure: 1015.0 mb     Barometric Pressure: 1010.0 mb
Tides (in feet):                                             Tides (in feet):
Low @ 0224 of 2.8                                         Low @ 0335 of 1.5
High @ 0828 of 12.2                                      High @ 0943 of 12.4
Low @ 1436 of 1.6                                          Low @ 1537 of 2.0
High @ 2105 of 14.6                                      High @ 2159 of 15.4
Sunrise: 0424                                               Sunrise: 0423
Sunset: 2100                                                 Sunset: 2101

Science and Technology Log

On Saturday morning I went out and made observations at a tide gauge in Customhouse Cove. We took measurements over a three hour period every six minutes for a one minute interval. We used a pair of binoculars to read the tide staff, which was about 20 feet away, to the nearest millimeter. The purpose of taking this reading over a period of one minute is because the water is constantly moving both toward the shoreline and away from it. This interval ensures that you can get the most accurate reading as possible.

Tide staff, used for measuring rising and falling tides

On Sunday, I again went out on a small launch boat. This time we needed to complete a few more holidays using the multi‐beam sonar, then we went to two small islands, Smeaton and South Twin, to recover the GPS (global positioning systems) base stations.

Computer screen,showing live acquisition of multi-beam SONAR data from one of the holidays.

The GPS base station data is recorded daily, while the survey project is underway. The data is then uploaded during the processing phase and used to correct the precise position of the Fairweather and its launches to within a few centimeters of accuracy. This allows the survey technicians to know the exact horizontal position when all of the data was collected by the multi‐bean sonar. Sunday was the last day that data was collected on this project, and that is why we recovered both of the GPS bases stations.

Me,in the process of removing one of the GPS base

When the tide gauge was established for measurements, during April of 2010, a three hour period of observations was made, similar to what I did on Saturday morning. In the time since April, observations are to be made each week for at least 1‐2 hours. Due to the remote nature of some of the tide gauge locations this is not always possible. The purpose of the observations of the rising and falling tide is to establish the vertical location of the tide gauge sensor, which is submerged below the surface, in relation to the tide staff. These observations help in correlating the height observed on the tide staff, with benchmarks that were previously installed by the Fairweather crew along the beach.

Maritime activities throughout the world depend on accurate tidal and current information for safe operation. NOAA’s National Ocean Service collects studies and provides access to thousands of historical and real‐time observations as well as predictions of water levels, coastal currents and other data.
Ocean tides move in response to gravitational forces exerted by the moon and sun. Since the moon is much closer to the Earth it is the dominant force that affects Earth’s tides. Whichever side of the Earth is facing the moon experiences a greater gravitational attraction, and the oceans get pulled towards it causing a bulge.

Me, holding the rod for leveling measurements (with the Fair weather in the background).

When the highest part or crest of the wave reaches a particular location, high
tide occurs; low tide corresponds to the lowest part of the wave, or its trough. The difference in height between the high tide and the low tide is called the tidal range. Here, in SE Alaska there is almost a 15 feet difference between high and low tide.

Me,reading the level off of the leveling rod(again with the Fairweather in the background).

Most coastal areas, experience two high tides and two low tides every lunar day. Almost everyone is familiar with the concept of a 24‐hour solar day. A lunar day is the time it takes for a specific site on the Earth to rotate from an exact point under the moon to the same point under the moon the next day.

One of the benchmarks on the beach.

On Saturday afternoon, we went back to the tide gauge to take elevation levels of five benchmarks on the beach. The purpose of these measurements is to establish a vertical height of the tide gauge with five existing benchmarks. When the gauge was started in April 2010, the same measurements were made. We verified that the opening and closing measurements were within an acceptable range. After taking height measurements, I helped take out one of the prototype tide gauges since the data was not needed anymore. The regular gauge was later removed on Sunday.

Part of the tide gauge instruments, solarpanel, GPS transmitter.

I was able to help out with these height measurements by holding a rod on top of the benchmarks, while another member of the crew looked through a scope and read the levels off of the rod. We also documented the entire site by taking photographs.

A humpback whale tale.

Personal Log

The weather on Saturday was probably the best I have had in SE Alaska so far. It was sunny and in the low 60’s. I learned a few days ago, that when you are out at sea and it is sunny you need sunscreen and a baseball hat in order to not get sunburn. As I told you, on Saturday morning I was dropped off by a small boat to observe the level of the tide. Nothing too exciting, but the weather made it just fine. Since we were very close to the ship, I was able to come back on and have “hot” lunch rather than sandwiches and stuff. In the afternoon, we went back to the same tide gauge and I helped out with elevation studies is the easiest way to say it. This was better than the morning for me.

In the morning one other guy and I were literally dropped off on a barely exposed rock just offshore from the tide gauge. When we started there was water between the two of us, but we knew the tide was dropping so we were fine. However, we were sort of stranded there until the small boat picked us up for lunch. We had to take levels of the water every six minutes. Sounds boring but it went by rather quickly. As the tide dropped small tidal pools were exposed and I was able to explore. There was tons of sea life. It reminded me of Point Loma near San Diego, where I vacationed once. While we were there, of course there were bald eagles and even a few seals.

In the afternoon we actually went onto the beach and I got to explore a little. First time on land since Ketchikan; which we are still very close to. I was in my full on geologist mode, breaking and smacking rocks to see what they looked like on the inside. I saw some cool stuff, possibly some small flakes of gold, garnet crystals, and maybe some silver flakes. The captain (CO) also came along with us, which was pretty cool.

Dinner was good. Baked potato bar, some interesting tofu dish (most people ate prime rib, very rare, uncle Jerry style), salad, and coconut lemon cake for dessert. I am getting spoiled from all this good food. I watched another amazing sunset from Customhouse Cove on Saturday (that makes 3 from the same anchor spot).

Sunset on Saturday 5/22

Sunday, the weather was not as nice as Saturday; at least it did not rain. However I really did enjoy the day. The crew that I was with was great. We all got along very well. I was able to get onto land three times and explore and climb around on the rocks. Also we saw two humpback whales, a bunch of seals, more Dall’s porpoises, and yes more bald eagles.

Being able to go onshore was really special for me. I was not sure this was something I would be able to do. From here we will start making our course to Seattle. We were just told that we WILL be going through the “inside passage” which is supposed to be absolutely spectacular. I can’t wait.

For now the project is almost complete. There is only a small amount of data and bottom samples that need to be collected. I am enjoying my time onboard the Fairweather. Everyone has been very nice. I have developed a routine. I get up at 0640, breakfast begins at 0700, there is a safety meeting on the bow of the ship at 0800, then if you are on a launch you leave and come back in the late afternoon. Dinner is served at 1700, then after dinner we have a debriefing meeting to discuss the day’s work and any problems that may have been encountered.

As I said I have a little routine. Even the breakfast steward (cook) knows me by now. I come into the mess hall (dining area) and ask for my usual. Three scrambled eggs with scallions and cheese. I also have one piece of toast, three strips of bacon, some hash browns and fresh fruit, some coffee and orange juice. Not too bad. If you are doing survey work from the ship there is hot lunch at 1200, otherwise on the launches it is a bag/picnic style lunch. Yes I know I am getting spoiled with all of this good food.

Me enjoying my time on shore.

Sunset on Sunday 5/23

David Altizio, May 19 – 20, 2010

NOAA Teacher at Sea
David Altizio
Onboard NOAA Ship Fairweather
May 17 – May 27, 2010

NOAA Teacher at Sea: David Altizio

NOAA ship Fairweather
Mission: Hydrographic survey
Geographical Area of Cruise: SE Alaska,
from Petersburg, AK to Seattle, WA
Dates: Wednesday, May 19 and Thursday, May 20

Weather Data from the Bridge

Position: Customhouse Cove                       Position: Behm Canal
Time: 0800 on 5/19                                        Time: 0800 on 5/20
Latitude: 550 05.97’ N                                   Latitude: 55017.77’N
Longitude: 1310 13.8’ W                                Longitude: 130058.03’W
Clouds: Overcast                                               Clouds: Mostly Cloudy
Visibility: 10 miles                                           Visibility: 10 miles
Winds: 6 knots from the SE                            Winds: 14 knots from the SW
Waves: Less than one foot                              Waves: Less than one foot
Dry Bulb Temperature: 13.00C                   Dry Bulb Temperature: 12.50C
Wet Bulb Temperature: 12.50C                   Wet Bulb Temperature: 10.50C
Barometric Pressure: 1010.5 mb                Barometric Pressure: 999.9 mb
Tides (in feet):                                                      Tides (in feet):
High @ 0447 of 14.6                                        High @ 0558 of 14.0
Low @ 1128 of ‐0.7                                           Low @ 1233 of 0.2
High @ 1802 of 13.2                                         High @ 1909 of 13.9
Low @ 2349 of 4.0
Sunrise: 0429                                                      Sunrise: 0418
Sunset: 2055                                                        Sunset: 2102

Science and Technology Log

On Wednesday, May 19, I was able to go out on a small boat launch. Four such boats were deployed from the Fairweather that morning. They all use 400 kilohertz multi‐beam sonar to map the bottom of the channels we are currently in, near Ketchikan, AK. This type of SONAR sends out 512 beams/ping of sound, and is most effective in shallow water. The area or swath that can be scanned at anytime is about 5 times the depth of the water. Therefore in shallow water the swath is much narrower and in deeper water the swath is much wider. Most of the work today on all of the launches was filling in small areas in the chart in which data was missing or not dense enough to complete the project. These areas are referred to as “holidays”, because they are areas where previous survey launches have been through the area and the data was not good enough. Some possible reasons for this could be that they are areas where acoustic noise was picked up by the multi‐beam SONAR, or where shadows were cast from the surface bedrock or boulders on the bottom of the channels. The area that we surveyed first is called Cascade Inlet.

Me on a small boat (launch) to survey the bottom of channels around

Me operating the multi‐beam sonar on the small boat launch

Not only did I get to use the computers on board to operate the SONAR and collect data, I was also able to deploy an instrument called a CTD that measures the conductivity, temperature and density of the water. This is very important because the speed of sound in water changes depending on the waters temperature density and conductivity. For example, the top layer of the water is typically a little warmer, less dense and less salty than deeper water due to influences from rain and inputs from rivers. When using SONAR you must know all of these factors in order to understand the speed at which sound waves will travel through the water. The sound waves will travel faster in cold deeper water, and the computer models take this into account before finalizing a chart. Ideally when using the CTD the sample must be taken at a depth that is greater than any spot you have surveyed so as to have a complete profile of these factors.

Me on a small boat (launch) pulling the CTD sampler back onto the boat.

In the afternoon we spent most of our time performing shoreline verification of small features around an area called Hog Rocks that have been previously identified. Here we used GPS (Global Positions Satellites), latitude and longitude, azimuth bearings, elevation and photos. As the name implies we were visiting small features to double check their exact location and exact heights.

On Thursday, May 20 I was scheduled to go out on a launch boat again but things did not go accordingly. There was a problem with the Davit, a mechanical crane that picks the 7 ton, 28 foot survey launch off the decks of the Fairweather and deploys them into the water. Since I was unable to go out and scan shallow water from the launch, I stayed on the Fairweather to scan and plot deeper water (approximately 400 meters) in and around Behm Canal. From the plot room of the ship I helped operate the computer, by starting and stopping the collection of data. In addition to filling in “holidays” we also mapped some cross lines. Cross lines are lines that run perpendicular to the main channel and are a means of verifying previous scans or quality control.

Example of shoreline features near Hog Rocks that we were verifying from the launch boats

Me, in the plot room on the Fairweather, collecting data.

Personal Log

I can’t say that the launch on May 19 was fun, but it was very cool and interesting. One thing no one told me was that after the morning rain was over that the sun would come out and it would reach almost 60 degrees, and that I should have brought sunscreen and a hat: warmer than it was in NY on this day. I now know for future launch days. I am usually going to be scheduled on a different launch team, doing slightly different tasks each day.

For now I just finished dinner, and yes it was very good again. In the meantime I am awaiting a debriefing of the day’s launches, and then hang out until bed. Before going to bed I went up to the highest deck on the Fairweather, called the flying bridge and watched one of the most beautiful sunsets unfold in front of my eyes.

What else, is on my mind…..Well SE Alaska is ridiculously beautiful, this coming from someone who has traveled a lot and used to work in the Grand Canyon. All over the place there is something new to see. I am still waiting for major whale sightings. Tuesday night before bed I caught a glimpse of some tails of a few porpoises (similar to dolphins), and Wednesday morning at the safety meeting on the stern of the boat (back) I sort of saw a whale surface for a moment. On Thursday, again at the safety meeting on the stern, a few of us saw a humpback whale at a distance breach the water a few times.

While at port, a picture showing the Davit, that picks up the launch boats to deploy them

Sun set on the Fairweather on May19

Bald eagle taking off on May19 from a shoreline feature we were verifying

David Altizio, May 17-18, 2010

NOAA Teacher at Sea
David Altizio
Onboard NOAA Ship Fairweather
May 17 – May 27, 2010

NOAA ship Fairweather
Mission: Hydrographic survey

Geographical Area of Cruise: SE Alaska, from Petersburg, AK to Seattle, WA
Dates: Monday, May 17 and Tuesday, May 18

Weather Data from the Bridge

Position: Petersburg to Ketchikan
Time: 0800 on 5/18
Latitude: 550 18.4’ N
Longitude: 1310 29.1’ W
Clouds: Overcast
Visibility: 10 miles
Winds: 10 knots from the NE Waves: Less than one foot
Dry Bulb Temperature: 13.50C
Wet Bulb Temperature: 13.00C
Barometric Pressure: 1004.0 mb
Tides (in feet):
High @ 0358 of 15.8
Low @ 1038 of ‐1.5
High @ 1711 of 13.6
Low @ 2246 of 3.9

View out the window of the plane to Petersburg of a meandering river

View out the window of the plane to Petersburg of a meandering river

View out the window of the plane to Petersburg

View out the window of the plane to Petersburg of a
meandering river

Science and Technology Log

The main purpose of the Fairweather is to conduct hydrographic surveys which measure the depth and bottom configuration along SE Alaska. This work assists in the production of nautical charts and ensures safe navigation in the U.S. The surveys also identify sea‐floor materials, dredging areas, cables, pipelines, wrecks and obstructions. The Fairweather supports a variety of activities such as port and harbor maintenance (dredging), coastal engineering (beach erosion and replenishment studies), coastal zone management, and offshore resource development. Hydrographic surveys are conducted primarily by using side scan and multibeam sonar. SONAR (Sound Navigation and Ranging) uses sound waves to find and identify objects in the water and determine water depth.
Side scan sonar is most useful to locate sea‐floor features and possible obstructions, but does not provide depth information. While multi‐beam sonar systems emit sound waves directly beneath the ship’s hull to produce fan‐shaped coverage of the sea floor. These systems measure and record the time elapsed between the emission of the signal to the sea floor or object and back again. Multi‐beam sonar produces a “swath” of soundings (i.e., depths) to ensure full coverage of an area.
Safety is hugely important while out at sea. Today we performed two safety drills, a fire/emergency situation, and an abandon ship drill. During the first drill I reported to the mess hall (dining area), and a fire was supposedly going in the paint room. When more help was needed I and one of the engineers scurried to the bow (front) of the ship and climbed down a hatch to help determine if the “fire” was spreading. Moments after that we tested two of the ship’s fire hoses, which definitely work. A little while later another alarm sounded signaling an abandon ship drill. For this I needed to go to my room and get my survival suit, and life vest, and then reported to my life raft. Practicing these drills is vital to life at sea. The officers of the Fairweather also become firefighters and we all need to communicate and work together to ensure everyone’s safety.

Here I am operating one of the ship’s fire hoses

Personal Log

Let me start off by saying that I feel like I have won a science teacher lottery. I feel so lucky and privileged to be able to represent New Rochelle High School, and be part of a science research cruise. My first two days in SE Alaska have been absolutely amazing. I flew from New York to Seattle, and then on to Anchorage, AK. I spent one night there and then in the morning flew to Petersburg, with a brief stop at the Juneau airport. Once on the ground in Petersburg I was met and picked up by the Executive Officer (XO) and a Junior Officer (JO). Within two minutes of being on the ground I was asked if I would like to play softball. I told him I could be considered “a ringer”.

Me in my survival (Gumby) suit

The setting was truly surreal. There were snow capped mountains in all directions, and I spotted my first bald eagle of my trip. We played 7 innings on a gravel ballfield; with members of both the Fairweather and its sister ship The Rainier, which is being serviced currently. I smacked the ball around pretty good and almost made a sliding catch in the outfield. Once the game was over (we lost), I went to dinner with some of the ships officers. After a long night in town, I finally made it to the Fairweather. We spent most of Monday at the dock, waiting for the tide to come up. The first stretch of the journey is a place called Wrangell Narrows. As the name implies it is a very narrow stretch of water and it is best for a ship the size of the Fairweather to pass at high tide. The first few hours of the trip were absolutely beautiful. From the time on the ship until now I must have seen over a dozen bald eagles, almost too many to count. From there we entered Sumner Strait, and then went through Snow Pass and into Clarence Strait. Next, after dark (the sun does not set until 9 p.m., and it is not dark until an hour or so after that), we cruised through Nicholls Passage and in the morning through Tongass Narrows and into the port of Ketchikan.

Dinner the first night was delicious; I had roasted eggplant ragout over polenta, with roasted broccoli on the side. Yum. I have heard people onboard say that the Fairweather has the best food in the NOAA fleet and I already agree. After a long nights sleep, our first day of work started. At 0800 there was a safety briefing on the stern (back) of the ship. The two survey teams were launched from the ship. Those who stayed onboard went into Ketchikan to get almost 30,000 gallons of marine diesel fuel. For dinner the second night I had Halibut with a curried corn sauce, mushroom risotto, and snap peas. Again it was great. In my next log I will show you some of the ships facilities.

Here I am hitting a double to right centerfield, in a losing effort

Animals Seen Today

Bald Eagles – so many I lost count, at least a dozen
A few people said that bald eagles in Alaska are as common as pigeons in New York. A few seals while in Petersburg
Many other birds while out at sea

Linda Tatreau, MARCH 9, 2010

NOAA Teacher at Sea: Linda Tatreau
Onboard NOAA Ship Oscar Elton Sette

Mission: Fisheries Surveys
Geographical Area of Cruise: Equatorial Pacific
Date: March 9, 2010

TOAD

Sunset

Sunset

It would be easy to start every post with a beautiful sunrise or sunset photo. In this one, you can see Anatahan Island in the background. Just before the sunset, 3 large wahoo were caught. Poke and fried fish are the favorite items on recent menus (breakfast, lunch and dinner).

Steve, Frances and Mills show off their catch.

This photo/diagram shows how sonar waves ping the seafloor and also shows the bathymetric map that is made from the data.

We used the multibeam sonar to map shallow banks north of Farallon de Mendinilla and east of Anatahan and Sarigan. The multibeam work continued day and night and produced huge amounts of data that needed to be processed. I can only sit at the computer for short periods, but the map team members work 10 hour shifts and most of that time is spent processing the data and making new maps. There are always 2 or 3 people processing the data.

The TOAD seen with cameras facing forward.

Monday night, we put out the TOAD (Towed Optical Assessment Device). This camera is towed behind the ship and sends video directly to the control room. We were able to see some of the seafloor we had been mapping. The first run of the camera went for 2.25 hours, covered a distance of 3 miles and went to a maximum depth of 400 feet. The second run went for 3.5 hours, over 4.5 miles to a maximum depth of 300 feet. Towing the camera sounds easy, but someone must be on the controls to keep the camera from crashing into the bottom. The camera needs to be close to the bottom for the best video, but without someone on the controls, it can crash. Driving requires constant attention. Most of the seafloor had a sand coverage with some algae. Occasionally, there would be oohs and aahs over something other than sand and sea weed: sea stars, large sea cucumbers, sponges, sea urchins or the infrequent fish. I really enjoy watching real time video of previously unseen seafloor, but I found myself falling asleep on my feet. I finally had to give up and head to the bunk.

Steve & Viv prepare the TOAD for launch.

Today, we are near Saipan planning to do BRUV work during the day and the TOAD tonight. A nap might be a good plan so I can watch the TOAD through the night, but I don’t want to miss the BRUV action either.

Linda Tatreau, FEBRUARY 12, 2010

NOAA Teacher at Sea: Linda Tatreau
Onboard NOAA Ship Oscar Elton Sette

Mission: Fisheries Surveys
Geographical Area of Cruise: Equatorial Pacific
Date: February 22, 2010

Sonar and CTD

Jeff & Jonathan prepare the CTD

Retrieving the CTD (check the feet)

All day Friday, all night, and into Saturday has been spent with the multibeam sonar collecting data and mapping the area of study. The “fish people” need an idea of the bottom contours to decide where to put the cameras. Yesterday afternoon, the scientists used a CTD tool to measure conductivity, temperature and density. The results of this test were used by the map makers to most effectively use the sonar data for accurate maps. Currently the camera crew is preparing to launch 5 sets of cameras. The BotCam (bottom camera bait station) has an anchor and floatation that will keep it a few feet above the bottom. The BRUVs (Baited Remote Underwater Video) will sit directly on the bottom. We should have fish data later tonight but, 10 cameras will make a lot of video to watch.