Marian Wagner: My Final Words and Hurricane Irene’s in Charge, August 23, 2011

NOAA Teacher at Sea
Marian Wagner
Aboard R/V Savannah
August 16 — 26, 2011

Mission: Reef Fish Survey
Geographical Area: Atlantic Ocean (Off the Georgia and Florida Coasts)
Date: Tuesday, August 23, 2011

A Fine Bunch to Live with at Sea: Front: Katie Rowe (Scientist), Sarah Goldman (Scientist Watch Chief, Night), Stephen Long (Scientist), Warren Mitchell (Lead Scientist). Middle: Marian Wagner (Teacher-at-Sea), Shelly Falk (Scientist), Christina Schobernd (Scientist, Video). Back: John Bichy (Marine Technician), Richard Huguley (Engineer), Harry Carter (2nd Mate), Raymond Sweatte (Captain), Michael Richter (1st Mate), David Berrane (Scientist Watch Chief, Day), Mike Burton (Scientist). Missing: Joel Formby (Master of the Galley)

Weather Data from the Bridge (the wheelhouse, where the controls of the ship are)

E-NE Wind at 10 knots  (This means wind is travelling 10 nautical miles per hour,
1.15 statute miles = 1 nautical mile)

Sea depth where we traveled today ranged from 33 meters to 74 meters

Seas 2-4 feet (measure of the height of the back of the waves, lower the number = calmer seas and steadier boat)

Science and Technology Log

IRENE: On Tuesday evening, we discussed the impact of Hurricane Irene on our cruise plans, and scientists and crew needed to make a decision about when we should return to dock. Originally, the plan was to return in the morning on Friday, August 26, but due to projections of Irene, they predicted that the seas would be too rough for us to lay traps beyond Wednesday (8/24).  When the seas are too rough, the traps bounce around and cameras do not pick up a steady, reliable picture.  When seas get to be 6-7 feet+ on a boat the size of the R/V Savannah (92 feet long), it also makes our work (and life) on the boat very difficult. Additionally, with Irene’s landfall projected in North Carolina, where half of the scientists live, they would need to get home in time to secure their homes and potentially evacuate.  Not in the case of Irene, but if a hurricane was expected to hit Savannah/Skidaway, where the boat moors, the ship’s crew would need to prepare for a hurricane-mooring.  To do this, they would run the ship up the Savannah River and put on a navy anchor that weighs 3,000 pounds.  Even with the use of the electric crane, it’s not an easy task to pull a 3,000 pound anchor onboard.  This would not be done unless a direct hit to the area was expected.  It has been done once before to the Savannah in the 10 years of her existence.  The forecast did not project Savannah to be affected by Irene, so we did not need to prepare for a hurricane mooring.

After difficult deliberation on Tuesday night about hurricane Irene’s potential Category (see how hurricanes are ranked here), and considering the success of the research accomplished on the trip already, scientists decided the most practical and reasonable decision was to dock Tuesday night, unpack Wednesday morning, and allow North Carolina scientists to return to their homes by Wednesday night.  (From reports I received post-Irene, there was landfall of the hurricane eye over their houses, but the storm weakened between Wednesday night and Saturday and was Category 1 when it came ashore.  None of them sustained significant loss.  Many downed trees and three days without power, but no floods or structure damage. Phew!)

NOAA’s National Weather Service is the sole official voice of the U.S. government for issuing warnings during life-threatening weather situations.  Follow Seattle’s “Weather Story” at NOAA’s National Weather Service.

OUR RESEARCH PROCESS…A STORY CONCLUDED

Here on my final blog entry, I want to finish the story of our research process.  Here’s the story I’ve told so far, in outline form:

  1. research begins with baiting fish traps and attaching cameras, and we stand-by on deck
  2. when we arrive at a research location with reef fish habitat (as observed via depth sounder and GPS), we drop the trap to the bottom and it sits for 90 minutes; buoys float above each trap so we can find and retrieve them near where traps were deployed, we run the Conductivity, Temperature, and Depth Profiler (CTD) to get information about abiotic conditions at each sampling site. The CTD takes vertical water column profiles, measuring: Pressure, Temperature, Conductivity/Salinity, Chlorophyll fluorometer, Color dissolved organic matter fluorometer (CDOM), Photosynthetic Active Radiation (PAR), Backscatter, Dissolved oxygen, and Transmissometer -10 and 25 cm path lengths
  3. after 90 minutes have passed, we return to the traps and pick them up, and secure the fish caught
  4. we identify each fish, measure length, weight, and frequency (how many fish were      caught), and then keep the fish that our research is targeting
  5. in the wet lab, we dissect target fish, removing parts of fish that are sent back to the lab for further research

AT THIS POINT, WE ARE DONE with our research with the bodies of the fish, but we have 99% OF THE FISH’S BODY LEFT! What should we do?

I was very impressed with the compassionate and humane action the scientists do with the fish after research.  Scientific research guidelines don’t dictate what a research study should do with edible fish flesh. We could have just discarded fish back into the ocean. However, scientists see an opportunity to provide food to people in need of  nutritional support in our communities, and they coordinated with a regional food bank in Savannah to do just that. Despite the work and time it takes to process the fish for donation, it did not seem to be considered a burden at all by any of the scientists.

I am perfecting my fillet!

Fresh fish fillets ready for food bank distribution

To process the fish for donation, we cut fish into fillets, wrap the fillets in butcher paper, and freeze them onboard the ship.

When we reached land, Warren
contacted the regional food bank, who came out to the dock with a refrigerated truck to pick up fish.  Within a few days the fish was distributed through charitable organizations in the region to people who were most in need.

These scientists are not just natural scientists but social scientists too! (just as I fancy myself!)

Personal Log

Captain Raymond Sweatte and First Mate Michael Richter

Interview with Raymond Sweatte, captain of R/V Savannah

Marian: What  makes a good crew?

Raymond: A crew that sees things that need to be done and does them because they know it all goes smoother when they do.

 

M: Have you ever run into or had a close call running into another ship?

Raymond: No, but the closest I came was when I was passing under the bridge at the Skidaway when a barge was coming through at the same time. Because it was easier for me to maneuver, I pulled over to side to let the barge use the majority of the channel. But the barge stayed on my side of the channel and was coming right at me. My boat was leaning upon the bank so there was no where for me to go.  I got him on the horn and asked, “What’s going on?”  He pulled over right away. He was new and very apologetic. 

M: Have you ever been in a terrible storm before?

Raymond: A few times we’ve had 15-16 foot seas coming back from the Gulf. When you have a north wind at 35 knots [strong wind coming from the North] and north-going current opposing the wind, the seas get very rough. Waves were coming up over the ship. [picture Marian’s eyes VERY wide at this point in the conversation] When seas are really rough, you get lifted up out of bed and down again. I remember trying to sleep one night in rough seas when my head kept hitting against the wall, so I turned around so my feet were up hitting against the wall.

M: What were things like before radar, satellite, and so many electronic navigation tools
you use today?

Raymond: Things were not as accurate. Communication was on a single sideband, navigation was with Loran-C, though VHF radio was somewhat the same as now.  To follow ships and determine their speed we had radar on dash but we had to use an eye cup we looked into to correlate with the radar, and then go over to the chart to plot them.  Then, we did it again six minutes later and multiplied by 10 to find their speed.  Now we have an automatic identification system [we can click on a ship on the radar] that tells us where they are, who they are, where they came from, where they are going, and what they are doing.  

M: What are the right-of-ways when vessels are crossing paths; who moves when two vessels are in course to collide?

Raymond: [On ships, aircraft and piloted spacecraft] a red light is on the left or port side of the craft and a green is on the right or starboard side. When two vessels have crossing paths, each will see a red or green light. If you’re looking at another vessel’s port side you see red, and it’s his right-of-way. If you are on their starboard side, you see the green light, and the right is yours.

Also, right-of-way rules give priority to vessels with the most difficulty maneuvering. The ranks in right-of-way, starting with the highest are:

1)Not under command

2)Restricted in ability to maneuver

3)Constrained by draft (stay away from shallower water to avoid running aground)

4)Fishing

5)Sail

6)Power

7)Sea Plane

Remember this mnemonic: New Reels Catch Fish So Purchase Some.

M: Who’s easier to talk to, a Navy Sub Captain or a Coast Guard Helicopter Pilot?

Raymond: I don’t have a problem talking with any of them. Coast Guard generally would call you first. Navy sub pilots I’ve found to be very cordial. They have changed their course when we had traps out.

M: What message would you say to students interested in being a captain?

Raymond: All kids have to follow their own heart. If they like water and this environment, they should follow their heart and become a captain.

Thank you Captain Raymond! It was a genuine pleasure to talk to you and experience life at sea under your command and with such a stellar crew. It is no wonder you are revered by everyone you work with.  Read more about Captain Raymond Sweatte in the Savannah Morning News!

The powerful significance of this trip for me was that I did not just study a science lesson from a book or lab, but I was essentially given a chance to live a different life, that of a fisheries field biologist.  I did not dabble in the work; it was a full explosion into the curiosities, reasonings, and daily routines of working with live fish and fish guts while sharing friendship, humor and stories with scientists and crew aboard a boat that was a small bounded island of rich human culture within a vast ocean of life and scientific questions waiting to be answered.  I loved it.  If only I didn’t love teaching more…I could definitely live that life.  Thanks NOAA, thanks NC SEFIS folks, thanks SC DNR folks, and thanks Skidaway Institute of Oceanography folks.  You are all in my heart and in my classroom!

FASCINATING EXTRAS!

Flying fish!

At night especially, when looking out at the seascape, I noticed flying, bug-looking specimens scurrying out of and into the ocean’s surface.  WHAT WERE THEY?! I wondered. So I asked and learned they were FLYING FISH! A few of them flew right up on the vessel’s work deck.  Their wings are modifications of the pectoral fins.  They are so fascinating and their coloring was greenish/blue iridescence, a stunningly beautiful color!

RED SNAPPER: PROTECTED STATUS

“The Gulf and South Atlantic red snapper populations are currently at very low levels (overfished), and both red snapper populations are being harvested at too high a rate (overfishing).” See more where this quote came from at Fish Watch: US Seafood Facts.

It was clear to me how significant the concern for the red snapper population was when I learned that funding for this fisheries survey was drastically increased following the recent determination that red snapper were overfished and overfishing was occurring.  Fisheries managers, field biologists and members of the general public all want to see the red snapper population improve.  This cruise provided scientific data that will be useful when the status of the U.S. South Atlantic red snapper population is assessed again.

The lionfish's spines are so poisonous the only way to hold them is placing fingers in their mouths.

History of measuring speed in NAUTICAL MILES:

Wonder how a vessel’s speed was measured hundreds of years ago? Log Lines, knotted ropes with a log tied to one end and knots every nautical mile and one-tenth of a nautical mile, were tossed off the end of the ship while the knotted rope unraveled behind it. When the sand on a minute sand glass ran out, the rope was reeled back in and the knots counted to determine ship’s speed in knots-per-minute.

 LIONFISH: INVASIVE SPECIES

In its native waters of the Indian and Pacific Oceans, the lionfish population is not a problem. There it has natural predators and natural parasites to keep it from overpopulating, yet it can survive well enough to maintain a healthy sustainable population. However, in the Caribbean waters and along the Eastern Coast of the United States, the lionfish has recently been introduced, and the effects are alarming. “Lionfish have the potential to become the most disastrous marine invasion in history by drastically reducing the abundance of coral reef fishes and leaving behind a devastated ecosystem.”  See more where this quote came from at NOAA’s research on invasive lionfish here. In the U.S. south Atlantic, they consume large quantities of reef fish and have no natural predators or parasites. Their population is thriving in large numbers, and it is devastating other fish species.  Mark Hixon, Oregon State University zoology professor, co-authored a study in 2008 with Mark Albins that showed “a lionfish can kill three-quarters of a reef’s fish population in just five weeks.” Read NPR story here. This is a cool way to view an environmental problem: see this animated map of the lionfish invasion! Red Snapper

Kaci Heins: Shoreline Verification and Auroras, September 27-29, 2011

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

Heading Back to the Rainier After Shoreline Verification

Mission: Hydrographic Survey
Geographical Area: Alaskan Coastline, the Inside Passage
Date: Thursday, September 29, 2011


Weather Data from the Bridge

Clouds: Overcast/Drizzle/Rain
Visibility: 2 Nautical Miles
Wind: 15 knots
Temperature
Dry Bulb: 8.2 degrees Celsius
Barometer: 1001.1 millibars
Latitude: 55.42 degrees North
Longitude: -133.45 degrees West

Science and Technology

Waterfall on Shore

When we are out on a launch acquiring data there are so many beautiful shorelines to see.  From far away they look inviting, but in reality there are usually numerous boat hazards lurking below or on the shoreline.  I have written a lot about the hydrographic survey aspect of this mission and how it is important to ships so that they can navigate safely.

However, when we are out on a survey launch the first priority is safety of the crew, the boat, and the technology.  This means that we normally do not go anywhere that is shallower than about eight meters.   Consequently, this leaves areas near the shore that is not surveyed and leaves holes in the chart data.  This is where shoreline verification comes in using single beam sonar.  However, since the launch with the single beam is not operational at this time we have been using the multibeam instead.  The Marine Chart Division (MCD) gives the Rainier specific items that need to be identified because they are considered Dangers to Navigation,  or they need to be noted that they do not exist.  The MCD compiles a priority list of features that come from numerous sources such as cruise ships, aircraft pilots, and other boats that have noted that there may be a danger to navigation in a certain area.  Many of these charts have not been updated since they were created in the early 1900′s or never charted at all!

Before we leave the Sheet Manager and the Field Operations Officer (FOO) come up with a plan for what shoreline they want to verify for the day.  A plan must be made because there is a small window to acquire the information needed to satisfy the requests of the Marine Chart Division.  The shoreline verifications must be done at Mean Low or Low Water.  This means that it has to be done when the average low tide of each day comes around, which has been in the early morning and afternoon for us.

Shoreline 4 Meter Curve

Using the launches we head up to what is called the four meter curve.  This curve is the limit to where we can go during meal low or low water.  If we get any shallower or move closer to the shore then we will put everyone and everything in danger on the boat.  We bring with us  a camera to document the features, a clinometer, which allows us to document headings and angles, a laser range finder, charts that they can draw and note features on, and their computer software.   Once we get underway and arrive to our first rock that we have to document, the officers make sure they maintain good communication with the coxswain, or boat driver.  We make sure we circle everything in a counterclockwise motion so that he can see everything off to his starboard, or right side as we move.  We can see the rock become exposed as the waves move over it, but the tricky part is getting as close to it as possible without hitting it.  This is so we can get a precise location as possible for the chart.  Our coxswain was very experienced so we were able to get right next to it for photos, the heading, and to drop a target, or the location, in the software.

Notes Documenting Various Features

The rest of our shoreline verification was a lot less intense as we confirmed that there was a lot of kelp around the rocks, the shoreline, and specific rocks were in the correct place.  LT Gonsalves, the Hydrographer-in-Charge (HIC),  showed me how he draws some of the features on his chart and makes notes about whether the features are there or not.  I took photos and noted the photo numbers for the chart, as well as the range and height of various features.  Shoreline verification is very important for nautical charts so that ships and their passengers know exactly where dangers to navigation lie.  It takes 120 days from the final sounding for all the data to get submitted to the Hydrographic Survey Division.  From there the information gets looked over by numerous agencies until about 2 years later the updated chart is available.  This is quite a long time to wait for changes in dangers to navigation.  To be safe, the chart stays the same even if there is not a dangerous rock lurking around at mean low or low water.  It is best to just avoid the area and err on the side of caution.  There is still a lot of work to be done in Alaska that will take many, many years to complete.  However, it is thanks to hydrographic ships like the Rainier and its crew that get the job done.

Personal Log

NASA SOHO Image of Solar Wind and the Magnetic Field

Tonight was very special because we could actually see an aurora, or the northern lights,  in the night sky.  An aurora is a natural light display in the arctic and antarctic, which is caused by the collision of charged particles in the upper atmosphere.  Auroras start way back about 93 million miles (or 1 astronomical unit- AU) at the sun.  When the sun is active, usually due to coronal mass ejections, it releases energetic  particles into space with the very hot solar wind.  These particles travel very quickly over those 93 million miles until they reach the Earth’s magnetic field.   Most of these energetic particles are deflected around the Earth, but some get trapped in the magnetic field and are moved along towards the polar regions until they strike the atmosphere.  We knew there were possibilities to see an aurora while we were anchored, but usually it has been cloudy at night so we couldn’t see the stars.  However, on the 27th Officer Manda came through saying he had seen the lights.  Low and behold there was a green glow in the sky behind some clouds and a couple of times some of the energized particles made bands across the sky.  If there hadn’t been so many clouds I think it would have been even more spectacular, but I was so glad I did get to see them.  Very quickly, more clouds moved in and it was just a green glow on the horizon.  I also was able to see the milky way in all its glory and the brightest shooting star I have ever seen.  These amazing photos of the aurora were taken by Ensign Manda and I am very grateful he was willing to share.

Aurora and Shooting Star Courtesy of Ensign Manda

Aurora in Alaska Courtesy of Ensign Manda

Click HERE for a link to a neat animation of how an aurora is formed.

Student Questions Answered

Animals Spotted!

Seal On a Rock We Were Documenting

Seals – species unknown

 

 

 

 

 

 

 

 

Question of the Day

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

Kaci Heins: September 21-23, 2011

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

NOAA Ship Rainier

Mission: Hydrographic Survey
Geographical Area: Alaskan Coastline, the Inside Passage
Date: Friday, September 23, 2011


Weather Data from the Bridge

Clouds: Overcast
Visibility: 10 Nautical Miles
Wind: 25 kts
Waves: 1- 2 feet
Temperature
Dry Bulb: 10.3 degrees Celsius
Barometer: 1002.6 millibars
Latitude: 55 degrees North
Longitude: 133 degrees West

Science and Technology

Rainier Skiff Boat

Now that there is a small window of clear weather I am able to go out on one of the small boats called a skiff.  This boat holds about 8 people max and is mainly being used to move people and equipment around to the different stations.  The night before I was scheduled to leave I learned that my task on this outing was going to be reading the tide staff every six minutes for 3 hours.  I know the initial reaction might be, “Why would you want to do that?”  Well, it is actually really important for the data that we are collecting.  When the equipment (primary benchmark, tide gauge, tide staff, orifice, etc.) was placed on Block Island this allowed the scientists to be able to know what the actual water levels would be for the launches when they head out. This in turn, is important because the height of the water levels will affect the data that is being collected on the launches (survey boats).  The first few hours started giving us pretty good data, but then we stopped getting anything at all.  We had been hit by a storm so numerous scenarios were being brainstormed so we could be prepared for anything that we might find when we got there to fix the problem.

Garmin Route to Block Island Courtesy of Todd Walsh

We traveled from the Rainier to Block Island, which was about 19 miles away.  When we got there the tide staff was in good shape and even the antennas and GPS looked good.  However, upon further inspection they found that there were glitches in the software files that had made it stop collecting data.  Once they got it going again, my partner Starla, and I went straight to work collecting the high and low wave of the tide.  We then used this data to calculate the mean (average) of the two.  We had to collect this data every six minutes for three hours because that is the same data that the tide gauge is collecting.

Tide staff at Block Island

We had to use GPS time–which was the same as the tide gauge–and not our own watches. This is because we needed the same time stamp for the data, which allows the scientists to see that the data was collected at exactly the same time.  Scientists can then look to see if the data we collected and the data the tide gauge collected are the same or if there are errors.  Then, they can see if it was human error or if something is still wrong with the tide gauge.  These first three hours were very important for the data collection, but the scientists will continue to monitor the station every three to four days for one hour throughout the month to make sure it is collecting data properly.

Mrs. Heins Taking Tide Staff Measurements

As we collected the data, one of us would watch the clock while the other would very intently watch the tide staff.  Once it would come to the time we would have to collect the data she would say “Mark!” and that would be my cue to note the high and low of the wave against the tide staff.  I would tell her my observations up to four digits, such as 1.967 meters.  However, because we would use quick observations to collect our data, our precision would probably be only to three significant figures. Significant figures are digits of a number that carry meaning and factor  into its precision. Starla would record the data and then we would wait six minutes until the next time to make our observations. When we were done, we downloaded the data from the tide gauge, packed up the skiff, and head back to the Rainier. Overall, it was a really great day being able to collect this important data and contribute to the mission of the ship.

Heading Back to the Rainier

Personal Log

Calculating Radar Ranges on a Nautical Chart

Math, math everywhere!!  Since the first day I have been on the Rainier I have seen math being used all day, every day.  Even though I don’t specifically teach math I do integrate it within science and social studies.  However, I have heard from students, “Why do I have to learn this?” in regards to their math homework.  There isn’t always enough time in the day to give a thorough explanation of how different math skills are used in the real world.  However, from my past NASA experiences and now with NOAA on the Rainier, I am here to tell you that once you enter the real world, especially if you enter a science, math or engineering field, then you will be immersed in math.  It will become a part of your daily routine without you really realizing it.  One place where math is used constantly, and is also one of my favorite places on the ship, is the bridge.

Math is used in navigation, such as setting a course, calculating distances, speeds, and times.  I also got some practice with calculating radar ranges, which can give the officers their location based off of 3-4 points of land nearby.  GPS is being used all day, every day and there are multiple GPS systems in case one fails.  Again, the officers use this information in their calculations throughout the day while we are at sea.  When I have been collecting weather data on the bridge math is being used to calculate the wind speed and direction.

Finding an Azimuth

Then there are conversions being calculated because some of the charts are in meters, some are in feet, and some are in fathoms.  A fathom is used more for deeper water because 1 fathom equals 6 feet.  Because these are dealing with depths it is very important to make sure the conversions are correct so that the ship stays safe.  Then of course there is math used in other ways on the ship.  For example, the Executive Officer (XO) has to work with the ship’s budget, the cooks work with measurements in the galley, and the scientists work with math formulas as they process the data in their projects.

Overall, I highly encourage my students and any other young minds that are reading this to do your best in math and ask for help if you need it.  It can be an intimidating subject area at times, but if you want to work for NOAA, be a scientist, or engineer then it will be an important part of your job.  Once you have an idea of what kind of job you want to have when you get older, try to find out what kind of skills you need to have and start early.  See how the math is used in the real world, the job you are interested in, and learn how to have fun with it!

Student Questions Answered!

Animals Seen

Sea Lion

Whales (not sure of the species)

California Sea Lion

Moon Jellyfish

Question of the Day

Jennifer Goldner In the News

NOAA Teacher at Sea Jennifer Goldner is interviewed by NewsOn6.

NOAA Teacher at Sea Jennifer Goldner was interviewed by NewsOn6.com about her cruise.

Read this article and this article and this article about Jennifer’s cruise in the Grand Lake News.

Read this article and this article about Jennifer as well as this interview with Jennifer on grandlakenewsonline.com

Lindsay Knippenberg: Women are taking over the Dyson! September 15, 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 15, 2011

Weather Data from the Bridge

Latitude: 55.41 N
Longitude: -167.98
Wind Speed: 25.86 kts
Wave Height: 10 – 13ft with some larger wind-blown waves
Surface Water Temperature: 8.7 C
Air Temperature: 8.7 C

Science and Technology Log

Real women aren't afraid of piles of jellyfish.

Real women aren't afraid of piles of jellyfish.

I will admit that before I met the scientists and crew onboard the Dyson I had imagined that the majority of the people on the boat would be men. I had wrongly gone along with the stereotypical view that scientists, engineers, fishermen, and the crew onboard ships were mostly men. Therefore when I finally met the people who I would be sailing with for the next two weeks, I was surprised and very happy to see that women had taken over the Dyson. For example, of the 12 scientists onboard the Dyson for this cruise, 9 are women including the Chief Scientist who is in charge of us all.

The seabird observers looking for birds.

The seabird observers looking for birds.

On the ship there are also NOAA Corps officers. The NOAA Commissioned Officer Corps is one of the seven uniformed services of the United States. Officers can be found operating one of NOAA’s 18 ships or 12 aircraft to provide support to meet NOAA’s missions. Their duties and areas of operations can range from launching a weather balloon at the South Pole, conducting fishery surveys in Alaska, maintaining buoys in the tropical Pacific, to flying P-3 Hurricane Hunter airplanes into hurricanes. I have met several NOAA Corps officers while I have been at NOAA and they have mostly been men. I was excited to see that of the six officers onboard the Dyson three are women.

NOAA Corps Officers - Rene, Sarah, and Amber taking a break from their duties to pose for a picture.

NOAA Corps Officers - Rene, Sarah, and Amber taking a break from their duties to pose for a picture.

There are also several other women onboard the Dyson and my mission today was to meet some of these amazing women and interview them to see what they do onboard the Dyson and what motivated them to choose this as their career. Let’s meet them:

Name: Ellen Martinson

Hometown: Juneau, AK

Position: Research Fisheries Biologist and Chief Scientist for Leg 2 of BASIS

Ellen showing off a tiny squid that she was measuring on the scale.

Ellen showing off a tiny squid that she was measuring on the scale.

Ellen has always loved solving puzzles and has had a curiosity for nature and how it works. That love of nature and problem solving led her to become a fisheries biologist. She has worked at NOAA since 1995 and she does research to support the management of federally-controlled commercial fisheries. She is currently a Ph.D. candidate and is doing her research and dissertation on developing indexes of ecosystem health in the Bering Sea that includes climate and fish growth factors. Pollock is her species of choice and she is looking at the success rate of Age 0 (zero) pollock surviving their first year to become Age 1 pollock as a prediction of the future health of the commercial pollock fishery.

What does she like the best about her job? She gets to work with a variety of people ranging from scientists and fisheries managers to fishermen and even teachers like me. She listens to their problems and ideas and then looks for the important questions to address all of those viewpoints. She also gets to travel to a lot of cool places, learn new things from a variety of topics, and her job is often an adventure. How did she get such a cool job? Going to college is the first step. Ellen has a bachelor’s degree in Marine Biology and a master’s degree in Fisheries Resources. She is currently finishing up her Ph.D. at the University of Alaska Fairbanks and then she will be Dr. Martinson.

Name: Kerri Curtin

Hometown: Chicago, IL

Position: Able-Bodied Seawoman

Kerri tying up the trawl net after pulling in a big haul of salmon.

Kerri tying up the trawl net after pulling in a big haul of salmon.

Kerri is one tough cookie. All week I have been amazed by her as she shuffled around the back deck pulling in fishing nets, lifting heavy science equipment, and tying all different types of knots. She is the only able-bodied seawoman onboard and her responsibilities include various deck maintenance jobs, setting up the nets for fishing and bringing in the catch, tying and untying the boat when we are at port, serving time on the bridge as an observer, and helping to launch the small boats. Her favorite part about her job is that she gets to go to work at sea and be outside in the fresh air. She also gets to travel to unique places and see the world. So far her favorite place that she has been to are the Greek Isles. How do you get a job like this? Kerri went to school in Maryland at Seafarers International and did an apprenticeship program. Through that program she gained the basic training necessary to get an entry-level position on a boat. Since then, she has continued her training and has taken several other Coast Guard certification tests. All her time at sea and trainings have paid off because she just received her 3rd Mates license.

Name: Amber Payne

Hometown: Fenton, MI

Position: Navigation Officer

Amber is in control of the Oscar Dyson as the trawl net is being brought in.

Amber is in control of the Oscar Dyson as the trawl net is being brought in.

Amber is a NOAA Corps officer onboard the Dyson. Her job as the Navigation Officer is to plot all the routes that the ship takes on paper and electronically. She also updates all the charting publications and she gets to stand watch on the bridge every day for eight hours. When she is on watch she is responsible for driving the ship and is in charge of all the operations. Amber has been onboard the Dyson for a year and a half and has several favorite things about her job. She likes that being on a ship in the Bering Sea is an adventure that many people may not get experience. She also likes the authority and trust that she is given to correctly navigate and drive the ship when she is all alone on the bridge. How did Amber get from Michigan to navigating a ship through the Bering Sea? Amber went to a four-year college in St. Petersburg, FL and studied Marine Biology. While in college she joined the search and rescue team and learned a lot about driving small boats. She knew that she wanted to go into a career that included both boats and science and her college advisor told her about the NOAA Corps. She applied to the NOAA Corps after graduation, was accepted, spent 4 months in basic trainings with the NOAA Corps, and then was placed on a ship. She loves that she gets to be a part of scientific research going on in the Bering Sea and she gets to drive boats all as a part of her job.

Name: Wendy Fellows

Hometown: Liberty Lake, WA

Position: Junior Engineer

Wendy has a lot of screens and buttons to monitor when she is on watch.

Wendy has a lot of screens and buttons to monitor when she is on watch.

When I first met Wendy she was sitting in the galley with the other engineers wearing her cover-ups from working in the engine room and I thought to myself, this girl is pretty cool. There aren’t too many female marine engineers and Wendy has a great story. When she graduated from high school she didn’t know what to do. She wanted to see the world so she took a job working in the kitchen of an oil tanker. She traveled all over the world and learned a lot about the different jobs on the ship throughout her journey. Her dad had been a marine engineer and she liked the work that the engineers did, so she went to school at the Seattle Maritime Academy to learn the trade. As a part of a year-long program she became a qualified member of the engineering department and did an internship onboard the Oscar Dyson. She liked it so much that she decided to stay on the Dyson as a Junior Engineer. Her job on board the Dyson is to basically make sure the ship is working properly. She tests emergency batteries, monitors the generators and pumps, services the small boats, fuels the ship when it is in port, fixes random things that break around the ship, and tests the drinking water. Her favorite part about her job is when she gets to use the welding skills she learned onboard the Dyson to fabricate things for the ship or scientists.

Name: Kathy Hough

Hometown: Kodiak, AK

Position: Senior Survey Technician

Kathy is busy on the hero deck connecting plankton nets to be lowered over the side.

Kathy is busy on the hero deck connecting plankton nets to be lowered over the side.

As the senior survey technician onboard the Dyson, Kathy has the responsibility of working with the scientists to insure that the collection of their data goes smoothly. She helps the scientists to collect their data by lowering and monitoring the CTD, helping with the various nets, and making sure that all of the equipment in the labs are functioning properly. She also collects data of her own. As the Dyson cruises around the Bering Sea, Kathy is in charge of collecting the weather and oceanographic data that is sent to scientists and posted on the NOAA Ship Tracker website. What does she like best about her job? Kathy likes the diversity of operations that she gets to be a part of. The science teams that are doing research onboard the Dyson only stay for 2 – 4 weeks and then another team gets on and might be doing a completely different project. As the science teams constantly rotate, Kathy stays on and helps with a variety of projects and different types of scientists. Does this job sound cool to you? To get an entry-level position as a survey technician you need a bachelor’s degree in science or mathematics. Kathy’s background is in ecology/biology, but a background in engineering, mathematics, or chemistry can be helpful too. If you want to move up to be a senior survey technician like Kathy, you need time and experience working on boats and with the instruments the scientists use for their research.

Name: Rachelle Sloss

Hometown: Juneau, AK

Position: Lab/Research Technician

Rachelle with a huge king salmon from one of our hauls.

Rachelle and I have gotten to know each other pretty well these last couple of weeks as we sorted through piles of fish and did a lot of counting to fifty. Rachelle just graduated from college in May and for the past two summers she has worked in the NOAA labs in Juneau as a lab/research technician. She works in a lab that is studying bioenergetics. While onboard the Dyson, she has been collecting and sorting zooplankton and looking for specific species of krill that will be used for bioenergetic experiments back in Juneau. She has also been collecting juvenile fish species like pollock and herring for similar experiments. While at the lab back in Juneau, Rachelle does lipid class analyses of fish to look at the energy content of their lipids by season. Does this sound like a cool summer job? Rachelle thinks that it is because she gets to work with some really cool people, she is gaining great experience for the future, and she got to spend two weeks on the Bering Sea seeing tons of species of fish. What lies ahead for Rachelle? She got a degree in Biochemistry, Biophysics, and Molecular Biology from Whitman College and is thinking about becoming a high school science teacher. For now she is headed to a much warmer South America and will be traveling around for the next couple of months on her next adventure.

Personal Log

We finally made it back to land and now we are all heading off in opposite directions towards home.

We finally made it back to land and now we are all heading off in opposite directions towards home.

By now I am safely back to my warm living room and I owe all of the women above and the men of the Oscar Dyson my deepest gratitude. I had an incredible adventure on the Bering Sea and I learned so much. Even though we had some rough seas, I still loved seeing all the different fish that we caught in our nets and I loved being a part of a research project that has so much importance to our fisheries. The NOAA Corps officers, crew, and scientists were all incredible teachers and had a lot of patience as they took time out of their day to answer all of my questions. I can’t wait to share my experiences with my students and other teachers and I couldn’t be more thankful for the experiences that I gained as a NOAA Teacher at Sea.

Kaci Heins: September 19-21, 2011

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

Mission: Hydrographic Survey
Geographical Area: Alaskan Coastline, the Inside Passage
Date: Wednesday, September 21, 2011

Mrs. Heins at the Helm

Weather Data From The Bridge

Clouds: Overcast
Visibility: 4 miles
Wind: 20 kts
Waves: 0-1 feet
Temperature
Dry Bulb: 11.7 degrees Celsius
Barometer: 1000.1 millibars
Latitude: 55 degrees North
Longitude: 133 degrees West

Science and Technology Log

Launch Lowered Into The Water

Today was the first day that the survey launches left the Rainier to install and recover benchmarks and a tidal gauge.  The weather was not great and the crew had a lot of work to do so I was not able to go with them this time.  A benchmark is a small brass disk with information inscribed on it that relates to the station it represents. The benchmark holds the height of the datum.  The purpose of setting a tide gauge is to measure the water level. The water level information is used to reduce the bathymetric data acquired to the chart datum (mean lower-low water, MLLW).   Finding benchmarks has become quite popular through the hobby of geocaching.  This is where participants use latitude and longitude within Global Positioning Systems (GPS) as a way to hunt down “treasures” hidden by other participants.  This also includes finding benchmarks.


I’ve been trying to head up to the bridge as much as I can to learn as much as I can during this Teacher at Sea experience.  The first time I went up at night I had no idea about the environment that the officers work in on the bridge.  At night the officers on the bridge actually work in complete darkness.  All of the computer screens have dimmers or red filters so that the least amount of light affects their eyes in the darkness.  The reason it is so dark is because the officers need to be able to see the lighted navigation buoys to stay on course and to spot the lights of other ships that are heading in our direction.  There are also one or two deck personnel that are lookouts either on the flying bridge or bow to keep watch for ships, lights, and other objects that could potentially be a hazard to the Rainier.  A flying bridge is usually an open area above an enclosed bridge where the ship’s officers have a good view of everything around the front and sides of the ship.  We are traveling through the Inside Passage off the Southeastern coast of Alaska, which is extremely narrow in some places along the way.  This means that it is very important that the officers know exactly where they are and what is around them.

Personal Log

Anchor's Away!

I have been able to do some other neat tasks on the ship while the majority of the crew were out on their launches.  We finally were able to find a place to anchor at Ulloa Channel because we had a good “bite” with the anchor–it is protected somewhat from the weather we are dealing with, and it is close to our tide station.  They also let me run out some chain for the anchor and I was able to practice using the crane on the ship.  However, the best part so far has been being at the helm, or the steering gear of the ship.  I will admit I was pretty nervous the first time I grabbed the wheel because it was at night so I couldn’t see hardly anything.  Today, the officer of the deck (OOD) let me at the helm again because we were in open water.  When I am at the helm I have to watch my gyro-heading, which shows me true North, and my magnetic compass, which is more of a back up if the electronic gyro-heading fails.  If I have a heading of 150 then I have to make tiny adjustments or corrections to try and stay on or close to that number as possible.  Even when I make the tiniest adjustment I can see how much the ship moves.  I did start getting the hang of it and one officer even said he had never seen a visitor do so well!

One other item that I will mention in this blog is that the weather in Alaska during this time of year is overcast, rainy, and cold.

Beautiful Scenery Along the Inside Passage

However, going into this I had an idea of what to expect and I enjoy the fact that I get to see the non-glamorous side of this type of work.  It does not matter if it is rainy, cold, what you are wearing, or what you look like because there is a job to do.  It has been overcast every day, but the pine trees are amazing shades of green and the pictures do not do them justice.  We have also had 15 foot waves and 115 knot wind (this is the same as a category 3 hurricane!).  The wind didn’t bother me as much as the waves did.  I thought it was fun for the first 30 minutes, but then I had to lie down for a while because I wasn’t feeling too well.  I never threw up, but it did become uncomfortable.  Now that we are anchored and have stopped moving I feel funny because my body has been used to moving around so much for the past three days.  I sure hope I don’t get land sickness when I am done with this cruise!

Student Questions Answered: Here are student questions answered about feeding so many people on a boat over 3 weeks time.

Animals Seen

Puffins

Questions of the Day

We experienced 115 knot winds Monday night.  What category hurricane would that be the equivalent to?  Use the website if you need help.

http://www.nhc.noaa.gov/sshws.shtml


Kaci Heins: September 16-18, 2011

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

Mission: Hydrographic Survey
Geographical Area: Alaskan Coastline, the Inside Passage
Date: Sunday, September 18, 2011

Me in front of the Rainier.

Weather Data From The Bridge

Clouds: Overcast
Visibility: 9 miles
Wind: North North West 11 knots (One knot = 1.15 miles)
Waves: Wind waves 1-2 feet
Temperature Wet Bulb: 11.9 degrees Celsius
Dry Bulb: 12.1 degrees Celsius
Barometer: 1017.2 millibars
Latitude – 50 degrees North
Longitude – 125 degrees West

Science and Technology Log

We will not be to our hydrographic survey destination until Tuesday so I thought I would write about the science of keeping this large research vessel heading in the right direction.   My second day on the Rainier I was able to head up to the bridge today to see how the ship is run.  The bridge is where NOAA Commissioned Officers command the ship, or make and execute decisions to keep the ship safe and on course.  There is at least one officer of the deck (OOD) and one helmsman on the bridge, but they don’t want too many more than that because it starts to get too crowded.  Since I was one more body in the room I tried to stay towards the back to make observations and ask questions when the officers were not busy.

This was a neat experience for me because I am able to see science, social studies, math, and language arts all being used at the same time.  Many of the officers carry notebooks with them to write down important information almost like science notebooks.

Officer Gonsalves' notebook.

There are also deck logs, which are legal records of everything that happens on the boat from spills to when the CO comes up on the bridge.  Commands between officers are verbally given  and then repeated to ensure that the correct orders were given and that there is confirmation that they were received.  There is also a lot of math being used on the bridge as distances are calculated, calibrations are made, and speed is documented.  For social studies and science, sunrise and sunset data is collected for the logs based on latitude and longitude for our position.  This can be important for when they need a lookout, for the deck log, and to overall know what to expect so that they can have the resources they need.  For science, we had to collect data each hour about the current weather.  The weather data above is what I collected with one of the officers this morning on the bridge.  The barometer is an instrument that measures

Nautical Chart of the Inside Passage

the atmospheric pressure.  This means if the barometric pressure drops then there is probably a storm coming.  This information is really important for the officers to know so that they can make decisions in regards to how to keep the ship and its occupants safe.

There is also a lot of technology in the bridge.  First, there is the radar which is a backup in case the GPS (Global Positioning System) happens to fail.  GPS and the radar are two separate pieces of technology, but are both helpful with navigation.  There are two radars that the ship uses.  They are X and S band radar.  Both of the radar help produce a picture of the surrounding area, which is helpful for imaging traffic and hazards.  However, radar does not give the ship’s position. The S band radar has a wavelength of 10cm, which allows it to penetrate rain better, but does not have great resolution.  X band radar has a 3 cm wavelength which has great resolution, but it cannot travel as far.  GPS is used for the positioning of the boat as we travel to do our work.

Personal Log

My travel day from Flagstaff to Seattle went really well yesterday as we headed up for our first stop at Ulloa Channel. No flights were delayed and no lost luggage. When I first saw the Rainier I was so excited! It is a fairly large. Rainier is a ship with five 30-foot survey launches and two small boats.  I had a thorough tour of the boat where I got to see everything from the bridge to the engine room. All of the crew have been very welcoming and helpful as well. My room is nice and so is my roommate Andrea.

My State Room

I actually expected to have less room and storage than we actually have. It reminds me a lot of a college dorm including the fact I have the top bunk! The scenery here is so beautiful with all the green pine trees next to the ocean. However, it is pretty cold! I’m so glad I brought my hat, gloves, and winter coat!

Immersion Suit Training!

Safety is very important on all the NOAA ships so I have been getting all of my trainings and briefings today before we left Seattle. I have to wear closed-toe shoes all the time on the ship unless I am in my stateroom. I have to be careful going up and down the stairs, (they are really steep), making sure to pick my feet up higher when I go through doorways, and overall being mindful that I don’t put myself or others in a dangerous situation. I then had to make sure my hard hat fit well and I had to put on my Immersion Suit. An Immersion Suit is also known as a survival suit in case we happen to go overboard.  These suits are made of  neoprene, which is a waterproof material, and can significantly improve your chances of survival in the event that we end up in the ocean.  My suit has a flashlight, it is BRIGHT orange, and it has a whistle so that I could be easily spotted in an emergency.  Today during our abandon ship drill we had to meet at our location, check to make sure everyone was there, and then put on our survival suits.  Even though we may look silly when we are wearing these, it is so important that we know exactly what we need to do in this particular emergency.  The last thing they want on the boat is for people to panic.  Finding our drill locations through practice and wearing the suits prepares us for what to expect so that we can calmly react in these situations.  I am very glad that I had the trainings and the drills so that I know exactly how to respond if it were are in a real-life situation.

Animals Seen Today

Orca off the port side of the Rainier.

Blue Heron

Canadian Geese

Sea Otter

Orcas

Question of the Day

Staci DeSchryver: A Front Row Seat to the Bottom of the Ocean, August 12, 2011

NOAA Teacher at Sea
Staci DeSchryver

Onboard NOAA Ship Oscar Dyson
July 26 – August 12, 2011 

Mission: Pollock Survey
Geographical Area:  Gulf of Alaska

Location:  Kodiak, AK
Heading: back to the docks
Date: August 12, 2011

Weather Data From the Bridge: N/A

Science and Technology Log

My last night on the Oscar Dyson was a busy one!  Because our trip was cut so short, we had to “break protocol” so to speak.  Typically, nighttime operations consist of seafloor mapping (which I will get to in a minute), and do not consist of trawling for Pollock.  For science students, you probably have a good idea why – running operations only in the daytime means that the experiment is controlled.  Since Pollock behave differently in the night-time, it is important to only run operations when their behavior is consistent.  However, because we were so short on time, we had to make a “run” for the shelf break that got us to the area well after dark.  So we got to do one more trawl!  This one was the best kind, in my humble opinion.  We completed a bottom trawl, which means that the net went almost down to the bottom of the ocean – within a couple of meters.  The reason why bottom trawls are so neat is because there are plenty of ocean critters down there that the average Joe doesn’t get to see on a daily basis.  Of course, the scientists do their absolute best to catch only Pollock to minimize bycatch, but one or two fish of different species are difficult to avoid.  On this trawl, we had a few jellies, two Pacific Ocean Perch, and a Herring.  We finished late – right around one in the morning.  At that time, we began our night-time operations.

Night time operations are run by Dr. Jodi Pirtle.   Dr. Pirtle is a Post-Doctoral Research Associate at the University of New Hampshire  Center for Coastal and Ocean Mapping.  Her research is a collaborative effort between the UNH CCOM and the NOAA Alaska Fisheries Science Center.   Even though Jodi is traveling all the way from New Hampshire,  she is actually very close to home right now.  She is quite connected to the Alaska fisheries – she grew up in Alaska, and has both family and friends who are involved in the commercial fishing industry.  The fisheries hold a place very close to her heart, and her passion for her current line of work is well evident.

So, why, then, does Dr. Pirtle work in the cover of night?

acoustics lab

Here, the scientists are working in the acoustics lab on daytime operations. As you can see, most of the electronic equipment is used during the day. At night, Dr. Pirtle gets the opportunity to chart her own path and select an area to map without interfering with the ship's primary operations.

At first I suspected it was some sort of secret service operation, but the reality is much more strange and explainable.  Her line of work is a side project on the Oscar Dyson, which means that she can work when the ship is not working for its primary purposes.  Hence, she works from 6pm until 6am.   One focus of her research is to identify whether or not certain areas of the Gulf of Alaska are trawlable or untrawlable by the Alaska Fisheries Science Center bottom-trawl survey for groundfish.   How is an area determined to be untrawlable?  Let’s say, for example, there is a commercial fishing ship somewhere in the Gulf of Alaska.  This ship decides to do a similar trawl as the one that I did earlier this evening, but they use a net that makes contact with the seafloor because they are fishing for groundfish species – say, Rockfish, for example.  But, something happens.  When the net comes up, it is all torn up – as though it got caught on a series of rocks or ledges.  In order to warn other ships of the dangers of losing a very expensive net, the fisherman deems the area “untrawlable.”  It’s kind of like putting caution tape around the area.

Untrawlable areas are problematic for scientists because every area deemed untrawlable is an area where they can’t sample with the bottom-trawl gear.  For example, a large component of the groundfish fishery are several species of rockfish (Sebastes spp.) that associate with a rocky habitat.  Rockfish are delicious with garlic and butter, but they are sneaky little guys because they like hanging out around rocks (who knew?).  Many rockfish could be in areas that are untrawlable, but scientists would never know because it is inadvisable to tow a bottom-trawl net in the area to find out.  In a sense, untrawlable areas are a source of error, or uncertainty in the population estimate for species of groundfish in those areas.  This is where Dr. Pirtle’s research starts.

A few years ago, a group did research in an area called Snakehead Bank – a location previously deemed to be untrawlable.  They wanted to tighten the definition of “untrawlable.”  For example, there is a possibility that an untrawlable area is covered with steep cliffs, many sharp, large rocks, and impossibly tough relief.  However, there is also the possiblity that the area is relatively flat and trawlable, but the fisherman was just unlucky enough to drag his or her net over a rogue boulder that found its way onto the vast, flat, continental shelf.  So, the scientists decided to see what kind of “untrawlable” this particular area was.   The group took the time to make a bathymetric profile of the area and couple that research with camera drops – video cameras that would make the trek to the bottom of the ocean and provide a second set of data for scientists to confirm what the bathymetric profile showed them.  From the camera drops and the bathymetry, the scientists determined that Snakehead bank was not completely untrawlable – in fact, most areas could support trawl nets without the risk of tearing the nets.  Dr. Pirtle is continuing with this important work.

One focus of the research is determining seafloor trawlability in the Gulf of Alaska using the same acoustic transducers that we use to catch fish in our daytime operations.  The fishery that the  survey is concerned about  is groundfish –   a general term that encompasses many species such as flatfish, cod, and rockfish.  These sneaky guys enjoy habitats that are associated with rocky areas, so we are not getting the best estimate of populations in those areas.  Dr. Pirtle is looking in to alternative methods to determine whether an areas of the seafloor is untrawlable or trawlable using the mulibeam sonar.  Not only is she looking for areas that can now be considered trawlable, she’s also using the data she collects to determine certain seafloor characteristics.  Hardness, roughness, and grain size are all data that can be collected using the acoustic transducers.  This information will help her to determine the relative trawlability of an area, as well.  Therefore, the groundfish survey benefits because she is either finding areas to be trawlable (thus, they can now sample there) or somewhat trawlable, which can tell them ahead of time that alternative sampling methods might be needed in a particular area.

Her research is also concerned with developing alternative sampling methods for untrawlable locations.  These methods could involve a combination of acoustic seafloor mapping to characterize seafloor habitats for groundfish, acoustic midwater data (to observe the fish that like to hang out on tall pinnacles and rocky banks) and, the most fun method – dropping a camera to the ground to identify species and biomass assessment (which is a fancy term for seeing how many fish are in a particular area).  Improved understanding of groundfish habitats can lead to better management models, and the work Dr. Pirtle is doing can also contribute to conservation of areas that are sensitive to fishing gear that touches the seafloor.

The area that Dr. Pirtle decided to survey this evening was an area that was deemed to be untrawlable surrounded by many trawlable areas.  These areas are often good candidates for mapping and camera surveys because both untrawlable and trawlable seafloor types are likely to be encountered, so the area can more easily be compared against existing data.  We began our transects – driving transects with the ship over the area while sending sound waves to the bottom of the ocean to figure out differing ocean depths and seafloor type.  Transect lines are close together and driven in a pattern similar to mowing a lawn, which gives Dr. Pirtle 100% coverage of her targeted area.  Dr. Pirtle selects a location to drop a CTD – Conductivity, Temperature, and Depth meter – usually in the middle of the mapped area.  The CTD is used to estimate sound speed in the location she is mapping.  This is important because ocean depth is measured by the amount of time it takes for a sound wave to leave the ship, bounce off the ocean floor, and return back to the ship.

This is a photograph of a halibut on the uncharted pinnacle discovered by Dr. Pirtle, similar to what I saw real-time on the camera late at night.

She then selects three to five areas to conduct camera drops.  The camera travels to the bottom of the ocean where she can see if the area is untrawlable or trawlable based on what the camera shows her.  I, on the other hand, get to see deep ocean critters in their habitats, which is also very cool.   There are two types of camera drops – ones that record the information and then get played back later, and real-time camera drops where we can literally watch the camera make the trek to the bottom of the ocean in real-time.  Dr. Pirtle uses the camera data to “groundtruth” or check the seafloor type against her acoustic map, to identify fish and other animals in the area, and to observe how species use the seafloor habitat.

As my shift was coming to a close, I could barely keep my eyes open, but I didn’t want to miss this.  Tonight, we dropped the live camera into the depths.  I stayed awake for the first drop so I could see what these operations looked like.  Dr. Pirtle expertly maneuvered the camera into the deep using something that looked much like an old-school Atari controller.

slide o' fun

This photograph shows Dr. Pirtle's work in combination - the area she surveyed is in the bottom right corner. The other three photos are snapshots of the surveyed area.

As the camera dropped, we saw a few pollock and some other unidentified neritic creatures, but the real fun started when we got to the bottom.  It was intense as Dr. Pirtle relayed information back to the bridge about the direction in which to travel, holding the ship still in the waves and currents when she wanted to examine an area more closely, and communicate with the technicians on the hero deck to relay the height that she wanted the camera held at.  We saw all sorts of interesting creatures on the ocean floor – some arrowtooth flounder, a halibut, and Pacific Ocean Perch.  We also observed beautiful cold-water corals and sponges that form a living component of seafloor habitat for many marine animals, including our target – rockfish.   We even saw a shark!  It was completely worth getting to bed a little bit later to see this incredible work in real-time.

unmapped pinnacle

This is the unmapped pinnacle discovered by Dr. Pirtle and her colleague! Now, seafloor maps have been updated to include this potentially dangerous sea hazard.

On a side note, in a previous leg of the survey, Dr. Pirtle and her colleague from UNH CCOM, Glen Rice,  found an underwater pinnacle that was later determined to be a navigational hazard!  This pinnacle came so close to the surface of the water that in a “perfect storm” of low tide and a large enough ship with a deep enough hull, it could have unknowingly collided with this unmapped pinnacle – which could have potentially been disastrous.  Glen, a NOAA hydrographer, was able to update the navigational charts in the area, alerting ships to the pinnacle’s presence.  It just further supports the idea that the our oceans are so vastly unexplored – there is so much we don’t know about the feature that takes up the biggest portion of our Earth!   I asked her if she named it because she discovered it – I quickly learned that just because you find something in the Ocean, it doesn’t mean you get to keep it.  Apparently, you can’t name it, either.  But I still called it Pirtle’s Pinnacle.  I think it has a nice ring.

Personal Log

It was a sad day today watching the scientists pack up and box and tag the lab equipment and computers.  As everyone bustled about, I spent some time hanging out for the last time on the bridge, in the galley, and in the fish lab thinking about my journey coming to its close.  Although we spent the majority of it tied to the dock, I am so grateful for the opportunities we experienced that we otherwise would not have – it was a blessing in disguise, because we really got to experience all of Kodiak, and much of the bays and inlets around the island from the ship.  The pictures will bring no justice to the beauty I’ve experienced in the last three weeks, whether it was walking along a beach with wild horses or staring in all directions to find nothing but water for as far as the eye could see.  I spent an hour one night on the bridge watching the Leonids streak across the sky – a front row and first class seat, in my opinion.  I never though that dodging whales would be an area of concern in my small life until we sailed through pods of them every day.  If you would have told me three years ago I’d be petting an octopus three weeks ago, I would have called you a fool.  If you would have told me three hours ago that this experience would be coming to a close three minutes from now, I would believe you even less.  In the last three weeks, I have never laughed harder, worked more eagerly, or learned more with and from these incredible individuals who call this ship Home.  As I quietly stood on the bridge watching the fast rescue boat dart off to the docks, I remembered the last time it was in the water watching carefully over us as we swam around the ship in our gumby suits.  As we drove silently through the still waters to the city docks, we bade farewell to the animals that accompanied us on our trips – otters, eagles, puffins, and even sea lions gathered around to see us off to our homes and families.  Or, they just so happened to be there looking for food and doing other instinctual things, but I do really think I saw an otter wave me goodbye.

whale!

Here is a whale "waving goodbye" with his fluke in the Gulf of Alaska - I will never forget the journey I had here!

Thank you so much to the crew and scientists of the Oscar Dyson - you fed my soul this summer and rejuvenated me in a way I never could have imagined.  I am more revived today than I was on the first day of my second year of teaching (because, let’s face it, the first day of your first year you spend most of your time trying not to vomit) and I owe it completely to the Teacher at Sea Program and to all of the fine people I got to work with.  To my partner in crime, Cat Fox – I’ll see you when we’re landlocked again!  It was a total blast working with you.  Thanks for always being there for a good laugh and for finding me so many salmon berries!  If you are wondering whether or not you should apply for this program in the 2012 season - this is the advice I will give to you:  JUST APPLY!  It will change your life - promise.

Until our next adventure,

Staci DeSchryver

Did you know…

While I was working my night shift, I got the opportunity to help Dr. Pirtle “log the turns” of the ship as it was “mowing the lawn” in the zigzag pattern.  This meant that I got to communicate with the bridge via radio every time they ended a transect and began turning in the opposite direction.  I’m sure you may have predicted that this was most certainly a highlight of my work.  It took great restraint on my part to behave myself with the radio, as everyone knows that radios can be a lot of fun.  I did, however, let a few nautical words fly on the airwaves up to the bridge, one of them being “Roger, Willco.”

I had no clue where the origin of the word “Roger” came from.  But now I do…

Roger, which starts with the letter R, means “Received”, which means, “I received your last transmission.”  A long time ago, the radio alphabet (you know, Alpha, Bravo, Charlie, Foxtrot, Whiskey, etc.) used Roger to represent the letter R.  It has since been changed to “Romeo.”  Adding Willco to the end, means “I received your transmission, and I WILL COmply.”   So saying that I received a message from the bridge and I was going to comply with it really made me look like a navigational moron – because they weren’t asking me to comply with anything.  But I still had fun.

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.

Cathrine Fox: Issue Thirteen: Walleye Pollock Status Page

NOAA TEACHER AT SEA
CATHRINE PRENOT FOX
NOAA SHIP OSCAR DYSON
JULY 24 – AUGUST 14, 2011


Personal Log:
I have not always had the best morals when it came to eating seafood. I discovered the joys of sushi in San Francisco after I graduated college. There was one place that I would frequent so often that the sushi chefs would would create something for me when I walked through the door. I later learned from Ruth Reichl in her book Garlic and Sapphires that the phrase I was looking for was “Omakase.” Literally: I am in your hands. In their capable hands I tried unagi (eel), hon maguro (bluefin tuna), and hamachi (yellowtail) for the first time. And I fell in love.

A few years later, a friend mentioned to me that I might want to moderate my adoration of some fish. Never one to take someone else’s word, I did my own research. I read, with growing horror, that my delicious eel farms were not sustainable, and that bluefin tuna was declining worldwide. Evidently, there were so many others that shared my love of the cool simple taste of hon maguro that we were loving these and other species to death. I know, you probably don’t want to take my word for it. Do your own research and then come back: FishWatch and SeaFoodWatch.

Back? Did you see that Yellowfin tuna are being sustainably harvested? Yes, me too. One order of hamachi sashimi, please.

What is my point with all of this? I want to show you what data are used to make these determinations about sustainability. I assure you, it is not random or haphazard. In fact, the purpose of my time in Alaska was to provide data to fisheries managers (composed of teams of fishermen, scientists, and officials) to let them make educated decisions on the health of walleye pollock populations in the Gulf of Alaska. What data do we collect? How do we know what the fish are doing, and how many there are? It isn’t an easy job… there is no Walleye Pollock Facebook Status Page that you can just check… (Cartoon citations 1, 2, and 3). You have to get dirty and do some real science.

Adventures in a Blue World, Issue 13

Adventures in a Blue World, Issue 13

Until our next adventure,

Cat

Walleye Pollock age classes.

Walleye Pollock age classes.

p.s. Although my “real job” has severely impacted the amount of time I have to cartoon, I am still working on at least two more (and up to seven, if I find a way to get a hold of a Time-Turnerlike Hermione Granger) cartoons. Thank you for being patient!

Lindsay Knippenberg: Oceanography Day! September 11, 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 11, 2011

Weather Data from the Bridge
Latitude: 58.00 N
Longitude: -166.91 W
Wind Speed: 23.91 kts with gusts over 30 kts
Wave Height: 10 – 13ft with some bigger swells rolling through
Surface Water Temperature: 6.3 C
Air Temperature: 8.0 C

Science and Technology Log

On a calm day letting out the CTD is easy.

On a calm day letting out the CTD is easy.

Today Jeanette and Florence took me under their wing to teach me about the oceanographic research they are conducting onboard the Dyson. At every station there is a specific order to how we sample. First the transducer, then the CTD, then numerous types of plankton nets, and then we end with the fishing trawl. The majority of the oceanographic data that they collect comes from the CTD (Conductivity, Temperature, Depth). The CTD is lowered over the side of the ship and as it slowly descends to about 100 meters it takes conductivity, temperature, and depth readings. Those readings go to a computer inside the dry lab where Jeanette is watching to record where the pycnocline is located.

The results from the CTD. Can you spot where the pycnocline is?

The results from the CTD. Can you spot where the pycnocline is?

The pycnocline is a sharp boundary layer where the density of the water rapidly changes. The density changes because cold water is more dense than warm water and water with a higher salinity is more dense than water that is lower in salinity. So as the CTD travels down towards the bottom it  measures warmer, less salty water near the surface, a dramatic change of temperature and salinity at the pycnocline, and then colder, saltier water below the pycnocline. Once Jeanette knows where the pycnocline is, she tells the CTD to collect water at depths below, above, and at the pycnocline boundary. The water is collected in niskin bottles and when the CTD is back on deck Florence and Jeanette take samples of the water to examine in the wet lab.

Filtering out the chlorophyll from the CTD water samples.

Filtering out the chlorophyll from the CTD water samples.

Back in the lab, Jeanette and Florence run several tests on the water that they collected. The first test that I watched them do was for chlorophyll. They used a vacuum to draw the water through two filters that filtered out the chlorophyll from the water. As the water from the CTD passed through the filters, the different sizes of chlorophyll would get stuck on the filter paper. Jeanette and Florence then collected the filter paper, placed them in labeled tubes, and stored them in a cold, dark freezer where the chlorophyll would not degrade. In the next couple of days the chlorophyll samples that they collected will be ran through a fluorometer which will quantify how much chlorophyll is actually in their samples.

Jeanette collecting water from the CTD.

Jeanette collecting water from the CTD.

Besides chlorophyll, Jeanette and Florence also tested the water for dissolved oxygen and nutrients like nitrates and phosphates. All of these tests will give the scientists a snapshot of the physical and biological characteristics of the Eastern Bering Sea at this time of year. This is very important to the fisheries research because it can help to determine the health of the ecosystem and return of the fish in the following year.

Personal Log

One of the high points for me so far on the cruise has been seeing and learning about all the new fish that we catch in the net. We have caught lots of salmon, pollock, and capelin. The capelin are funny because they smell exactly like cucumbers. When we get a big catch of capelin the entire fish lab smells like cucumbers…it’s so weird. We have also caught wolffish, yellow fin sole, herring, and a lot of different types of jellyfish. The jellies are fun because they come in all different shapes and sizes. We had a catch today that had some hug ones and everyone was taking their pictures with them.

Now that is a big jelly fish.

Now that is a big jelly fish.

Today we also caught three large Chinook or king salmon. Ellen taught me how to fillet a fish and I practiced on a smaller fish and then filleted the salmon for the cook. What is even cooler was that at dinner we had salmon and it was the fish that we had caught and I had filleted. Fresh salmon is so good and I think the crew was happy to get to enjoy our catch.

The catch of the day was a 8.5 kg Chinook salmon.

The catch of the day was a 8.5 kg Chinook salmon.

Salmon for dinner, filleted by Lindsay.

Salmon for dinner, filleted by Lindsay.


What else did we catch?
Walleye Pollock

Walleye Pollock

A juvenile Wolffish

A juvenile Wolffish

Yellow Fin Sole

Yellowfin Sole

 A squid

A squid

Herring

Herring

Lots of little Capelin

Lots of little Capelin

Lindsay Knippenberg: A Tour of the Oscar Dyson, September 8, 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 8, 2011

Weather Data from the Bridge
Latitude: 54.14 N
Longitude: -166.57 W
Wind Speed: 27.33kts
Wave Height: up to 17 ft
Surface Water Temperature: 8.4 °C
Air Temperature: 7.7 °C

While hiding from the storm in Dutch Harbor for the past two days, I had plenty of time to explore my new home onboard the Oscar Dyson. The Dyson is 209 ft in length and is like a small city. Everything that I would need during my two-week cruise, including a laundry room, would be available to me onboard. To show you what life is like onboard a ship, I decided to go on a little tour of the Dyson and take some pictures of the different areas of the ship. If you are interested in  more in-depth specifications of the ship, check out the Oscar Dyson’s website.

Science and Technology Log

Let’s start in the scientific areas of the ship. I have been spending most of my time working with the fisheries team in the fish lab. When we are done trawling and the fishermen bring in the net, they dump our catch onto a large conveyor belt. As the conveyor belt slowly moves, we sort our catch by species. Once we are done sorting, we also process the catch by weighing, measuring, and taking samples of the organisms. To learn more about this process, see my blog post from September 4th.

The Fish Lab. This is where the fish are brought in and processed.

The Fish Lab. This is where the fish are brought in and processed.

Next to the fish lab is a wet lab. A lot goes on in the wet lab. Some scientists are identifying plankton under microscopes, other scientists are dissecting fish stomachs to see what the fish are eating, and some scientists are filtering water from different depths of the ocean looking for chlorophyll.

The Wet Lab. Scientists study the ocean water, use microscopes, and dissect fish stomachs in this lab.

The Wet Lab. Scientists study the ocean water, use microscopes, and dissect fish stomachs in this lab.

When you pass through yet another door, you end up in another lab called the dry lab. There are several computers and other pieces of machinery that control the instruments that are lowered over the side of the ship at our sampling stations. This room is where a lot of the oceanography data is collected. I will talk about what they do and the data that they are collecting in another blog.

The Dry Lab. Jeanette is watching the data come in from one of the instruments.

The Dry Lab. Jeanette is watching the data come in from one of the instruments.

The last lab is across the hall and it is called the acoustics lab. This room is mostly composed of computers and lots of large screens to track where the fish are underneath the boat. Stay tuned for more on acoustics later.

The Acoustics Lab. Paul is using acoustics to watch the fish swim under the boat.

The Acoustics Lab. Paul is using acoustics to watch the fish swim under the boat.

Personal Log

I know that many of you have been wondering…Where do I sleep? What do I eat? What do I do when I am not playing with fish? And do I get to take a shower after playing with fish all day? Hopefully these pictures will help you to get a better idea of what life is like on the ship. It is no cruise ship, but I’m not “roughing it” by any means.

Let’s start with my room. The rooms are actually a lot larger than I thought that they would be. Everyone has a roommate and I am sharing a room with the Chief Scientist, Ellen Martinson. Each room has two bunks, a desk with an internet connection, two lockers for storing gear, a refrigerator, drawers for more storage, and a bathroom.

Mine and Ellen's room.

Mine and Ellen's room.

Ahh…the bathroom. Each room has its own bathroom with a sink, shower, and toilet. Before I got here I had imagined having one large bathroom for each floor or group of rooms, so this was a pleasant surprise. Even better was that it was much larger than any bathroom I have ever seen on a boat. The shower even has a bar to hold onto when you are trying to shower in rough seas, which I have found quite useful.

My Bathroom...it's so huge for a boat.

My Bathroom...it's so huge for a boat.

So what do I eat? It is more like what have I not eaten. The food has been excellent and there is always a variety of choices to choose from. Breakfast is from 07:00 – 8:00 and consists of eggs, bacon, sausage, pancakes or french toast, oatmeal, and today there was even quiche. I’m not a big breakfast person so I have been eating cereal and fruit for most breakfasts. Lunch is from 11:00 – 12:00 and is my favorite meal of the day. The cook makes amazing soups and there is usually a good sandwich to pair it with. If you don’t want soup and sandwich, there is usually burgers, quesadillas, or chicken fingers to choose from. If you don’t think that you can make it until 17:00 (or 5pm) when dinner is served again, don’t worry. There are usually fresh-baked cookies in the galley at around 15:00. If you still are hungry at dinner time, then you are in for a treat. So far for dinner I have had pork chops, spaghetti, leg of lamb, steak, and chicken ala king. Of course you would have to finish dinner with dessert and coffee. How about homemade chocolate cake and a scoop of ice cream? And you can’t just serve a regular cup of coffee. How about a mocha latte made from the espresso machine in the galley?

The Galley. Lots of good food can be found here.

The Galley. Lots of good food can be found here.

What happens if you eat too much and get sick? Don’t worry, the ship has a medical officer and infirmary if you need medicine. We have had some pretty rough seas during our cruise so it is nice to know that there is somewhere that I can go if I am feeling sick or if I need more medicine.

Not feeling well. Don't worry, the ship has a medical officer and infirmary.

Not feeling well? Don't worry, the ship has a medical officer and infirmary.

What do I do when I’m not playing with fish in the fish lab? Well, there are lots of things to do to keep yourself busy. You could workout in one of two workout rooms. You could choose from over 500 movies to watch in the lounge. You could clean your fish-smelling clothes in the laundry room. My personal favorite is to go up to the bridge and check out what is going on outside. From here you can see for miles and there are usually lots of seabirds to see and if you are lucky you can even see a whale or porpoise passing by.

Wash your dirty clothes at the ship's laundry room.

Wash your dirty clothes at the ship's laundry room.

Relax in the lounge and watch a movie.

Relax in the lounge and watch a movie.

Eat too many cookies today? Work off those extra calories in one of the ships two workout rooms.

Eat too many cookies today? Work off those extra calories in one of the ships two workout rooms.

Check out the bridge to look for sea birds and whales.

Check out the bridge to look for sea birds and whales.

Lindsay Knippenberg: Going Fishing! September 4, 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 4, 2011

Weather Data from the Bridge
Latitude: 54.13
Longitude: -166.41
Wind Speed: 24.10kts
Wave Height: 4-6 ft
Surface Water Temperature: 9.0°C
Air Temperature: 8.8°C

Science and Technology Log

The station grid for all of the proposed sampling sites.

The station grid for all of the proposed sampling sites.

Yeah! Today we left Dutch Harbor and began the second leg of the Bering-Aleutian Salmon International Survey (BASIS). The purpose of the BASIS Study is to assess the status of marine species in the Eastern Bering Sea and support the decision making process for commercially important fisheries. The scientists on my team are accomplishing this goal by combining their knowledge of fisheries, oceanography, and acoustics. While I am onboard I will be helping out the scientists in all these different areas to get a broad view of all the science going on during our cruise.

There are specific sampling locations called stations that we will be going to throughout the Eastern Bering Sea. The map on the left shows the locations of these stations. The green dots are the stations that we are sampling during leg 1 and leg 2 of the BASIS survey. Leg 1 is already complete and they sampled at all the stations east of Unalaska. We will be picking up where they left off and sampling at all of the remaining green stations. The black dots are stations that will be sampled by another vessel named the Bristol Explorer.

The trawl net being let out behind the ship.

The trawl net being let out behind the ship.

For the first station I got to help out the fisheries team in the fish lab. We did a surface trawl by letting out a large net out the back of the boat with floats on it to keep it at the surface. By adjusting the floats and weights on the trawl, the fishermen can choose what depth they fish at. While the net is out, the OOD (Officer of the Deck) slowly motors the ship for about 30 minutes and the net catches the fish that are swimming in that area and depth. For this station we want to see the fish that are swimming within the top 30 meters of our sampling area. At later stations we might also do a mid level or deep trawl to see the fish that live at those depths.

We found some Salmon!

We found some Salmon!

After the 30 minutes were up, the fishermen slowly brought in the net and we immediately saw salmon caught in the net. Yeah! We caught something! As more and more net was brought in the fish began to pile up on our sorting table. There were a lot more fish than I had expected and the majority of them were salmon. It was now our job to sort the fish by species and I will admit that I am pretty slow at identifying the species. They may all look like fish, but they each have identifiable features like the color of their gums (black for Chinook Salmon), type of gill rakers, or color patterns on their body or tails. At this station we were lucky enough to pull in four out of the five salmon species in Alaska. We caught Chinook, Sockeye, Chum, and Pink Salmon. We also caught several different species of jellyfish and some squid.

That is a lot of salmon to sort.

That is a lot of salmon to sort.

After we caught the fish, we had to process them. In order to learn about the fish and the health of their population, we took samples and collected data from the fish we caught. Here is a description of the data we collected and what the scientists can learn from that data.

Weight and Length – Weight and length are an index of fitness for the fish. The scientists multiply how fat the fish is by how long it is to determine its lipid (fat) content. In cold waters the fish tend to have a higher lipid content than in warmer waters where the fish have to use more energy to metabolize. Additionally, if a fish has a higher lipid content, it might also mean that it is healthy and finding prey easily.

Gill rakers (white hairs on top of the red gills) from two different salmon. Can you see the difference?

Gill rakers (white hairs on top of the red gills) from two different salmon. Can you see the difference?

Axillary Process – We cut the axillary process off the fish we caught for genetic studies. The scientists know the baseline genetic sequence for the salmon that come from different regions of the world. By looking at the genetics of the fish we caught, we can tell where the fish came from and reconstruct their migration and distribution. For instance, the scientists have used the genetics from the axillary processes to determine that a large percentage of chum salmon caught in the Eastern Bering Sea are from Japan.

Sexual Maturity – By looking at the testes and ovaries of the fish, the scientists can determine if the fish were immature or mature and when they were going to spawn. Using this information along with the results from the axillary process genetics, the scientists can determine migration patterns and growth rates.

Determining the sex, stomach contents, and sexual maturity of the fish we caught.

Determining the sex, stomach contents, and sexual maturity of the fish we caught.

Male vs. Female – The scientists also use the testes and ovaries to determine if the fish was a female or male. This is helpful in looking at the ratio of males to females in their population.

Stomach Contents – By removing the stomach of the fish and analyzing its stomach contents, the scientists can determine what the fish was eating. This is can be very helpful when comparing warm years to cold years and the effect that climate change can have on prey sources and the nutrition of the fish.

All of this information can then be extremely useful to fisheries managers who are assessing the stock of the fish that are important to commercial fishermen. One of the species that we hope to collect as we sample at other stations is Pollock. Pollock is the largest US fishery by volume. Each year around 2.9 Billion pounds of Pollock are harvested. To learn more about the Pollock fishery check out this link to NOAA FishWatch. The scientists  on my team are assessing the health of the Pollock fishery by looking at the total lipid content of Age 0 Pollock in late summer. Their lipid content is important at this time of year because winter in coming and they will need lipids to survive the cold winter. By looking at the lipid content of the Age 0 Pollock that we collect, the scientists can predict how many Age 0 Pollock will survive to become Age 1 Pollock and eventually mature to become Age 3 or 4 Pollock that can be harvested.

Personal Log

The fluke of a whale as it dives.

The fluke of a whale as it dives.

Whales! I was hanging out on the bridge getting my last look at land for a couple of weeks when I thought I saw a whale out of the corner of my eye. I couple of minutes later a huge Humpback Whale breached right next to the ship. I have seen whales before, but it was just their dorsal fin of flukes. This was crazy. An entire whale was out of the water and it kept on breaching over and over again like it was playing. I wanted to take a picture, but I was too mesmerized to even take my eyes away from it for a moment. Then as I started to look farther out to sea, I saw even more whales. There were about a dozen whales flapping their tails and rolling on to their sides. It looked like they were having a good time playing on a beautiful day.

The weather forecast for September 4 - 6. It doesn't look good...

The weather forecast for September 4 - 6. It doesn't look good...

That beautiful day, however, did not last very long. We managed to sample at two different stations when the wind started to pick up and the waves began to get a little larger. The forecast was calling for a Gale Warning with gusts of up to 50kts and 20-24 ft seas. Those conditions are far too dangerous to fish in, so we turned around and headed back to Dutch Harbor. Hopefully the storm will pass quickly and we will only have to hide out a couple of days until it is safe to fish again.

Lindsay Knippenberg: I Made It! September 3, 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 3, 2011

Weather/Location Data for Unalaska, AK
Latitude: 53°54’0”N
Longitude: 166° 32′ 36″ W
Wind Speed: Calm
Air Temperature: mid 50’s°F

Personal Log

It was a long day of traveling. I flew from Washington DC to Seattle to Anchorage to Cold Bay to Dutch Harbor.

It was a long day of traveling. I flew from Washington DC to Seattle to Anchorage to Cold Bay to Dutch Harbor.

Whew…I made it to Unalaska. After an entire day of sitting on airplanes and running through airport terminals, I am finally here. I can’t believe how beautiful it is here. The surrounding mountains are a stunning green color and there have even been some sightings of blue sky between the normal grey clouds. I am also amazed at how warm it is. It almost got up to 60°F today, but I was told that the weather can change here pretty quickly. We have already heard of bad weather coming our way next week. The National Weather Service issued a Gale Warning with predictions of wind gusts of up to 50 knots and waves above 20 feet. I had better take my seasickness medications.

The beautiful town of Unalaska.

The beautiful town of Unalaska.

We don’t ship out until tomorrow, so we decided to take advantage of the nice weather and explore Unalaska. Unalaska is much bigger than I thought that it would be. It is a major international fishing port and is one of the larger cities in Alaska with about 4,000 residents. Life in Unalaska revolves around fishing. Most residents are either commercial fishermen, work in the processing facilities, support the fishermen through stores and other services, or work in the ship yards where the seafood is shipped to all parts of the world. The name of the harbor where all of this is going on might be familiar to you. It is called Dutch Harbor and is where the show “Deadliest Catch” is filmed about the commercial crab fishermen. Crab is not the only type of commercial seafood coming out of Dutch Harbor. Pollock, Cod, Halibut, Rock Sole, and Mackerel are just a few of the other commercial fisheries in Dutch Harbor.

A World War II bunker on top of Bunker Hill in Unalaska (Photo Credit: Jillian Worssam).

A World War II bunker on top of Bunker Hill in Unalaska (Photo Credit: Jillian Worssam).

For those of you interested in history, Dutch Harbor also has historical significance from World War II. Dutch Harbor was the only land in North America, besides Pearl Harbor, that was bombed by Japanese Zeros during World War II. In our exploring around the island today, we saw evidence of Armed Forces’ bunkers, Quonset huts, and barracks still visible amongst the green hills of Unalaska. The National Park System opened a WWII National Historic Area and Visitor Center in 2002 in Unalaska and I hope to have time to visit it either before or after my cruise.

Enjoying the beach at Summer Bay in Humpy Cove. In 1997 this was the site of a 47,000 gallon oil spill.

Enjoying the beach at Summer Bay in Humpy Cove. In 1997 this was the site of a 47,000 gallon oil spill

What’s the best place to go on a beautiful, sunny day in Unalaska? The beach, of course. We didn’t go to the beach to get sun tans or to go for a swim. We went to check out the tide pools. I love tide pools! It is amazing how resilient the little creatures are that live in the tide pools. When the tide is in they are completely submerged under water and then six hours later they are above the water level when the tide goes out. To make life even harder, they are also smashed by huge waves crashing on them as the tide goes in and out. It is a tough life, but there was such a diversity of life that they must be pretty tough and have some helpful adaptations. As I explored amongst the rocks, I found sea anemones, barnacles, mussels, and lots of different types of seaweeds. On our way back to the van, we also found a stream leading back to a brackish lake and the salmon were running. They are amazing creatures to watch too. The amount of energy that they exert and the sacrifice that they make to reproduce is incredible.

I am now a member of the female dominated science team onboard the Oscar Dyson.

I am now a member of the female dominated science team onboard the Oscar Dyson.

Unfortunately we couldn’t spend our entire day exploring. The plan for the rest of the day is to get settled onboard the Dyson, have a science team meeting to discuss the science that we will be doing and the logistics associated with the different stations and sample sites, and have a safety meeting with the crew of Dyson to discuss life onboard the ship and emergency situations. I am so excited to go out to sea tomorrow and actually start fishing.

Kevin Sullivan: Zooplankton, September 1-5, 2011

NOAA Teacher at Sea
Kevin C. Sullivan
Aboard NOAA Ship Oscar Dyson
August 17 — September 2, 2011

Mission: Bering-Aleutian Salmon International Survey (BASIS)
Geographical Area:  Bering Sea
Date:  September 1-5, 2011

Weather Data from the Bridge 

Leg 1 has concluded.  Oscar Dyson is currently at port in Dutch Harbor.  Please use link (NOAA Ship locator) to follow ship in future research cruises and current location/conditions.


Science and Technology Log

I am back home and my expedition aboard the Oscar Dyson has come to a conclusion.  My travels home had me leaving Dutch Harbor at 7:30 PM and arriving into Newark, NJ the following day at 2:30 pm EST, an incredibly long, red-eye flight back home.  Although my involvement aboard the ship has come and gone, the ship is currently in port at Dutch Harbor taking on more fuel and supplies and readying to do a “turnaround trip”.  For Leg II they will be heading back out into the Bering Sea to obtain further data.  The following is a map that depicts the stations for Leg 1 and 2.  For Leg 1, all of the green stations (40#) represents the areas where we conducted our research.  For Leg II, they will be focusing on the black circle stations.  When all of this field work is complete, and the numbers are “crunched” they can be extrapolated out to get a better idea of the overall health of the Bering Sea ecosystem as detailed in prior blogs.

BASIS 2011 Station Grids

BASIS 2011 Station Grid

So, before I left Alaska, I was discussing a bloom and readying the blog platform for a discussion of zooplankton and other higher-ordered interactions of the Bering.  Ok, so moving on…the next feeding level in the marine world would be the primary consumers….the zooplankton.  Zooplankton, although a very simplified explanation, are essentially animals that drift (planktonic) while consuming phytoplankton (for the most part).  These zooplankton in turn, are a resource for consumers on higher trophic levels such as the Pacific Cod, salmon,  and Walleye Pollock (which are a primary focus on this survey).  Zooplankton are typically small and in order to obtain samples from the sea, we have been utilizing specialized nets (information and pictures to follow) to extract, analyze and collect them for further investigations back at the lab.

The following picture is a good visual to represent this flow of energy that we have been discussing since the first Blog Entry.  An important observation is that the sun is the “engine” that initiates all of these interactions.  The exchange of carbon dioxide compliments of Photosynthesis and respiration, the abundance of phytoplankton in the photic zone (see last blog entry), which are food for the zooplankton, which in turn, become food for higher-order carnivores.

Marine Food Chain
Marine Food Chain

One of the more important zooplankton species out in the Bering are the euphasiids.  These are small invertebrates found in all of worlds oceans.  The common name is Krill.  These species are considered a huge part of the trophic level connection, feeding on the phytoplankton and converting this energy into a form suitable for the larger animals.  In the last blog, I put in some pictures of euphasiids that we caught.  These euphasiids have a very high lipid content (fat) and in turn, are what is responsible for getting salmon their richness in oily flesh, the Omega Fatty acids, and there natural, pink-fleshed color.  I have read before about the differences between farm-raised vs. wild salmon from a nutritional standpoint.  Farm-raised salmon often lack the abundant Omega oils that are found in the wild species.  Also, it is true that in order for the farm-raised salmon to get their pinkish color to the flesh, they are fed a nutritional supplement to give the color….essentially, like adding a food dye.  So, in class this year, we will have to be very careful when analyzing the pros and cons of aquaculture/fish-farming.

Personal Log

Although my official involvement with the Oscar Dyson has come to an end, I will take with me the experiences and knowledge for a lifetime.  It was everything I was hoping it would be and then so much more.  These blogs, the pictures, the video…… all do the expedition no justice.  However, I have pledged to make every effort possible to spread the word about NOAA and its mission and this is exactly what I will do.  I have several more decades of career in front of me and I know that between now and that date, I will use this recent expedition countless times and will hopefully convince the general public about the overall importance of government agencies like NOAA and how common resources must be valued and protected to ensure the health of all of Earth’s inhabitants.

There are so many people who I would like to thank for providing and delivering such an extraordinary experience.  All of the crew aboard the Oscar Dyson, from the engineers, to the chef,  and captain……Thank You.  Your professionalism and ability were truly inspiring.

To the Scientists, You were really the “teachers at sea”.  May you always continue your motivated path to revealing the beautiful secrets this planet has to offer.  Also, my hope that it continues to be done in a fashion that I saw while during my time on the water…..In a professional, unbiased, non-political fashion.  You have reassured my passion for the sciences and have given me fuel to disprove any “non-believers” who claim that the sciences have become corrupted.  In the end, you have shown me the most universal and balanced approach at reaching the truth.

Thanks for reading.

Kevin Sullivan: Bering Sea Bloom, August 28 – September 2, 2011

NOAA Teacher at Sea
Kevin C. Sullivan
Aboard NOAA Ship Oscar Dyson
August 17 — September 2, 2011

Mission: Bering-Aleutian Salmon International Survey (BASIS)
Geographical Area:  Bering Sea
Date:  August 28 – September 2, 2011

Weather Data from the Bridge
Latitude:  56.95N
Longitude: 162.93 W
Wind Speed:  10 Knots
Surface Water Temperature: 10.5 C
Air Temperature:  55F
Relative Humidity: 97%

Science and Technology Log:

Well, at this time tomorrow, the Oscar Dyson will be tied up in port at Dutch Harbor.  This is our end destination for Leg I of the BASIS survey.  I will write-up a summary/conclusion either at that time or shortly after getting back into town.  For now, I will fill you in on some material that I promised.  As noted in earlier blogs…I have been intentionally writing in a trophic bottom up approach.  That is, I started my first blog entries with descriptions of the primary producers, the Phytoplankton.  I covered this extensively and correlated it to the oceanographic work that has been going on aboard this ship.  It seemed logical to work from the base of the food chain and work my way up the trophic levels to the more complex consumers.

However, before I close the chapter on Phytoplankton take a look at the picture I took below.  When I stepped outside and saw this, I thought I had been transported to the Caribbean.  Clear skies, calm seas, tropical blue waters are not typical descriptions for the Bering Sea.  If you look closely enough, you can even see the shadow of the clouds on the surface of the sea.   Science is the field of making observations, forming hypothesis, designing and conducting experiments and drawing conclusions about the natural world we live in.  So…what would you make of this observation?  What has caused this temporary “mirage” of tropics?  Clearly something is going on here.

Coccolithophores

Coccolithophores 08-28-11

Well, although not 100% certain, the most likely explanation is what would be called a Coccolithophore bloom.  These are single-celled algae which are characterised by special calcium carbonate plates as seen in photo below under magnification.

Coccolithophore

Coccolithophore

Under certain conditions, (some speculate that wind pattern changes fail to mix the water column favoring cocolithophore blooms as opposed to other plankton) coccolithophores can create large blooms turning the water brilliant shades of blue pending on the species of coccolithophore blooming at the time.  Ed (Chief Scientist) was telling me of a major bloom that had occurred back in the late 90′s.  I researched it a bit and the following picture is of this bloom in the same general vicinity where we are now.  Amazing to think of how microscopic plants can influence a region on the scale of an entire sea and be seen from space. *Note: this is not a false colored Image

Coccolithophore Bloom 98 Bering Sea

Coccolithophore Bloom 98 Bering Sea

There is also some speculation that these types of blooms may be linked to sub-average runs of salmon (and even impact seabirds negatively in the area).  Some hypothesize that this may be due to the idea that salmon prey heavily upon euphausiids (see picture I took below on 08-28-11 and the one centered beneath for a closer look taken from NOAA) and the euphausiids have difficulty subsiding on the extremely small coccolithophores.  Remember what I was saying about visualizing the flow of energy as a pyramid and the effects of taking out a few or many blocks that make up the base of the food chain.

euphausiids 08-28-11

euphausiids 08-28-11

Euphasiid

Euphasiid

Ok, to make this easier for the reader, I am going to stop this blog here and start a new one dedicated to the zooplankton…..I got a little sidetracked with the whole coccolithophore bloom event…….

Personal Log

Earlier this morning we were greeted with some higher winds and consequently some larger seas.  As my friend back East says conditions got “Sporty.”  Here is a picture from where we launch the CTD.  Winds were out of the SW gusting to 30 knots and seas were in the 10′ range with some larger swells thrown into the mix to keep things interesting.

Bering 09-01-11

Bering 09-01-11