Valerie Bogan: First Days at Sea, June 9, 2012

NOAA Teacher at Sea
Valerie Bogan
Aboard NOAA ship Oregon II
June 7 – 20, 2012

Mission: Southeast Fisheries Science Center Summer Groundfish (SEAMAP) Survey
Geographical area of cruise: Gulf of Mexico
Date: Saturday, June 9, 2012

Weather Data from the bridge:  Sea temperature 27.5 degrees celsius, Air temperature 24.2 degrees celsius, calm seas with thunderstorms in the area.

Science and Technology Log

As I mentioned in the previous entry the Oregon II is conducting a groundfish survey.  During this research cruise we are studying many aspects of the Gulf’s ecosystem.  We start by collecting general information about the water chemistry.  To do this we use a piece of equipment called a CTD which stands for Conductivity/temperature/depth.  This piece of equipment collects information on the temperature, salinity, fluorescence and turbidity.

CTD

This is the instrument used to measure salinity, called a CTD.

I am going to briefly explain what each of these readings are and why they are important to the scientific community.  Everyone knows what temperature is but you may not be aware of its importance to the health of our planet.  The phrases global warming and climate change have become very popular in the last few years. By collecting temperature data in the same spot year after year scientists can determine if the oceans really are getting warmer.

sea surface temperature map

Map of the surface temperatures around the world. The highest temperatures are found in the red areas the lowest temperatures are found in the blue areas. (photo courtesy of bprc.osu.edu)

The oceans contain salt water which  is the most important difference between oceans and lakes.  The measurement of the amount of salt in an ocean is called salinity.  And the amount of salt in an ocean can reflect the workings of the water cycle.  If there is an excessive amount of evaporation due to high temperatures, the ocean will become more salty due to the fact that there is more salt in less water.  On the other hand  if there is a lot of rain or melt waters from glaciers and mountains then the water will become less salty because now the same amount of salt is dissolved in more water.

salt

The amount of salt in the water determines the salinity.

Fluorescence is the measurement of light which is connected to the photosynthesis rate of algae.  The health of the algae has a direct connection to the amount of carbon dioxide that can be absorbed by the ocean.  Algae produces its own food just like a tree so if the algae is healthy,  more carbon dioxide will be necessary  to carry out photosynthesis  and then ocean can absorb more natural and man-made carbon dioxide.   These readings can also tell us how well the oceans are responding to climate change.

algae

These algae make their own food through the process of photosynthesis.(photo courtesy of swr.nmfs.noaa.gov

Turbidity is the measure of water clarity.  If the turbidity is high it means that light isn’t getting through to the organisms below which in turn means that the algae and seaweed can’t get the light they need to make their own food.  High turbidity can also cause the water temperature to go up due to the excessive amount of silt and particles floating and absorbing energy from the sun.  High turbidity can also cause small animals on the bottom  of the ocean to be buried alive as the particles settle out the water column.

muddy Mississippi river

This is an example of the silt and particulate matter which is flowing into the ocean everyday.(photo courtesy of http://www.motherjones.com)

Personal log

Greetings from the Gulf of Mexico.  I have now been onboard  the Oregon II for one complete day and am slowly but surely becoming accustomed to the layout of the ship.  It has all the comforts of home even if they have different names and  look different from the parts of your home.  The place I sleep and keep my belongings in  is called a stateroom.  It is a small space but honestly the only thing I use it for is sleeping .  One other difference from your room at home is that the cabinets have latches which keep them closed even when the ship is rolling with the waves.  Given the fact that large waves may come up at any time it is important that all personal belonging are securely stored so that they don’t become flying projectiles which can hurt someone.

stateroom

This is where I am bunking for the voyage.

cabinets

The ship also contains restrooms but they are called the heads.   Fresh water is an important resource on the ship as we only brought so much with us so the toilets are flushed using  seawater which is very easy to come by out here on the gulf.  There are also a couple of showers something which is very important given the fact that our work has the ability to make us very dirty and nobody wants to be stuck on a boat with a bunch of dirty stinky people.

shower

This is where we clean off all the dirt that accumulates during sampling runs.

Safety is very important on ship so we have drills to practice what to do in case of emergency, just like the drills we do at Maple Crest middle school.  Today we had a fire drill during which the scientists were to muster (that means to report) in the lounge and stay out-of-the-way of the crew members who are actually trained to put out a fire if one should occur on the ship.  Following that we had an abandoned ship drill during which we had to put on long pants and shirts and a survival suit.  The purpose of all this clothing is to keep you protected from the elements if you have to float in the water for an extended time while waiting on a rescue ship to come

Survival suit

This is the suit you must wear during abandon ship drills.

Sue Oltman: Salinity and Seamount Sleuths, May 24, 2012

NOAA Teacher at Sea
Sue Oltman
Aboard R/V Melville
May 22 – June 6, 2012

Mission: STRATUS Mooring Maintenance
Geographical Area: Southeastern Pacific Ocean, off the coast of Chile and Ecuador
Date: May 24, 2012

Weather Data from the Bridge:
Air temperature: 18.3 C / 64.9 F
Humidity: 70.3%
Precipitation: 0
Barometric pressure: 1011 mB
Wind speed: 2.3 NNW
Sea temperature: 19.16 C

Personal Log

The weather has been terrific – clear, in the 60’s with a little wind, nice sailing with the current helping us along. We are in the trade winds region. The view from the bridge (Captain’s pilot house) is excellent.  Everyone is terrific and very patient in showing us the ropes. There’s plenty of time to get to know people.  I’m getting to practice my Spanish a bit with our 2 students from the University of Concepcion (Chile) and two more Spanish speakers, from Chile and Ecuador. The two others on watch with me are Seb Bigorre (WHOI) and Ursula Cifuentes, a grad student from Chile, so we speak some Spanish during the watches. Life on a ship is different, but some of the comforts of home are here, too. Thank goodness there is a laundry, otherwise I would have had to bring 3 weeks worth of clothes! The food has really been fantastic!

Mark serving up some great food

Mark is one of our friendly cooks who keeps everyone on the ship happy!

Mess deck

The mess deck is where we eat our meals, grab a snack, or sit to read or chat at off times.

The dinner tonight is carne asada (fajitas) and you can smell it cooking. Bob and Mark, our cooks, have also served us white bean chili, salads, cheeseburger sliders, roasted chicken, fish, pork roast and vegetables, seasoned hash browns, bacon and eggs, all kinds of fresh fruit, not to mention the desserts like blueberry cobbler and cinnamon rolls. 

With all this great food, I was thankful to find that the crew makes places on the ship to work out! Some do “laps” by walking the ship a few dozen times around. There is an exercise room with weights and bikes and more equipment can be found in other places around the ship.

Science and Technology Log

The Woods Hole UOP (Upper Ocean Processes group) and rest of the team is now in a rhythm of deploying probes and gathering data. Like super sleuths, we are tracking a cold, relatively fresh water mass which originates inValparaiso and moves northwest. This water mass lies under the warm, salty surface layer.  At 50 meters depth, there is a clear distinction in the water masses since we began deploying the UCTDs. Just like a detective matches fingerprints, we have a “fingerprint” of the cold, fresh water.  A seasonal thermocline has been identified! Nan Galbraith, a programmer from WHOI, is processing all of the numerical data into useful images.  The surface water layer (graph) has a temperature about 20º C and salinity > 35 ppt (parts per thousand). At 50 meters depth, the temperature abruptly drops to 17º C and falls to 7.5º C at 400 m which is the bottom depth we are testing; similarly the salinity drops to 34.1 ppt. Although we are traveling through water about 4,000 m deep, we are interested in tracking this water mass. I’m still having trouble remembering approximate Celsius to Fahrenheit conversions: here’s a link to help.

http://www.wbuf.noaa.gov/tempfc.htm

However, another factor has come into play which we must consider. We are nearing a tectonically active area – the Nazca Ridge, a fracture zone. There are many seamounts, some of which have not been previously mapped. Whoever is on watch must look at the ever-changing multi-beam sonar display to look for seamounts – we don’t want the instrument to slam into an underwater volcanic mountain! The closer we get to the Nazca Ridge, the higher the likelihood of seamounts.

Seamounts

We constantly monitor the multi beam sonar display for bathymetry and sea floor features. The red or yellow circular areas are seamounts.

All in all, we will cover about 2,268 miles until we reach the Galapagos, so the multibeam sonar is a critical piece of navigation equipment.

On the watches, as we deploy the UCTD probe, which looks like a 2 foot long bullet, weighing about 10 lbs., and good teamwork is the hallmark of a successful launch and recovery. Sometimes we are working in the dark with only the ship’s lights and a flashlight. I have learned how to make a splice in the line – the cord is only about 1 mm in diameter! This line and any splice must be strong enough to hold onto a 10 pound instrument being dragged though 400 m of water at 12 knots. Picture 3 people at 4 a.m. on a moving ship, using tiny instruments to sew a splice in a 1mm line, all while the line is attached to the winch. Like a surgical team, we are all focused and know what tool the splicer needs next. Sometimes quick thinking and a problem solving mindset is needed. There was a foam “bumper” that we had been attaching to the line to cover the probe when it got close to the boat. The probe is expensive and this was protection from it slamming into the steel fantail. When it was lost in the water, the team on watch used a nearby mop to protect the probe while reeling it in. On the next watch, Seb figured out a different solution.

Why does it smell like diapers in here?

Back in the lab a different bit of problem solving with the scientific method is going on! Often when buoys are recovered, they are fouled — covered with barnacles and all kinds of organisms, fishing line, etc. that get caught in them. Jeff Lord – mechanical whiz – has hypothesized that applying a better “anti-fouling” substance can keep these from affixing themselves to the equipment. He has liberally applied Desitin, a zinc oxide ointment, to the instruments. This is the same treatment for diaper rash on babies’ bottoms!  So therefore, the odor in the lab reminds us of diapers. It will be a year before we know if Jeff’s hypothesis is correct, because after the STRATUS 12 buoy is moored, it will be a year before it is recovered.  What do you think will happen?

Some of the science party was given a tour of the ships technical equipment behind the scenes. Bud Hale explained not only all of the monitors and ship terminology, but took us down into the equipment rooms where we encountered a gravimeter (measures gravity variations), modern gyros with optics and GPS (measures pitch, roll and heave).

Bud Hale

Bud is an expert on all things technical on the ship. He is more than happy to tell you how any of it works!

Tomorrow, we hope to see the desalination plant on the ship which gives us our fresh drinking water.

UCTD files

After each deployment of a UCTD, data is uploaded into the computer. I’m starting to get the hang of it!

Wes Struble: Analysis of Water Samples, March 4, 2012

NOAA Teacher at Sea
Wes Struble
Aboard NOAA Ship Ronald H. Brown
February 15 – March 5, 2012

Mission: Western Boundary Time Series
Geographical Area: Sub-Tropical Atlantic, off the Coast of the Bahamas
Date: March 4, 2012

Weather Data from the Bridge

Position:30 deg 37 min North Latitude & 79 deg 29 min West Longitude
Windspeed: 30 knots
Wind Direction: North
Air Temperature: 14.1 deg C / 57.4 deg F
Water Temperature: 25.6 deg C / 78.4 deg F
Atm Pressure: 1007.2 mb
Water Depth:740 meters / 2428 feet
Cloud Cover: 85%
Cloud Type: Cumulonimbus and Stratus

Science/Technology Log:

In the previous log I described a CTD cast in detail from start to finish. Now that the CTD platform is on the deck of the Ron Brown the actual sampling process can begin. The CTD has a number of Niskin bottles holding a little more than 10 liters of water each. Water samples from each bottle must be collected and analyzed for various parameters which could include: Salinity, Oxygen content, Inorganic carbon, and others. On this cruise most of the CTD casts were sampled for both salinity and dissolved oxygen.

The first step in measuring salinity involves a careful rinsing of the sample bottles. After a standard three rinses, the bottle is filled and the depth from which the water was sampled is recorded for each bottle.

As a beautiful western Atlantic sunset falls on the Ron Brown another night of CTD's begins

I prepare a water sample for dissolved oxygen analysis after a CTD Cast at 2:00 am

The dissolved oxygen analysis lab station in one of the science labs on the Ron Brown

The full sample bottles are then either taken to the dissolved oxygen lab station or the Salinity lab station for analysis.

A close-up of the amperometric titration apparatus for analysis of dissolved oxygen in one of the science labs on the Ron Brown. A solution of Manganese Chloride and a combination of Sodium Hydroxide/Sodium Iodide is added to the water sample to sequester the oxygen and then when the temperature is stable the solution is amperometrically titrated with thiosulfate.

The Ron Brown off the starboard stern from the workboat

The "climate airlock" leading to the salinity analysis lab. The airlock helps keep the water samples under constant temperature and humidity conditions.

The two Autosals in the Salinity lab. These are precision instruments for measuring the salinity of seawater

A east-west cross-section across the eastern Atlantic Ocean. The eastern US coast is at left. The diagram illustrates north (reds)-south (blues) movement of the Antilles and Deep Western Boundary Current. Vertical scale in meters horizontal scale in 100,000 meter units (100 kilometers)

Dave Grant: The Straits of Florida, March 3, 2012

NOAA Teacher at Sea
Dave Grant
Aboard NOAA Ship Ronald H. Brown
February 15 – March 5, 2012

Mission: Western Boundary Time Series
Geographical Area: Sub-Tropical Atlantic, off the Coast of the Bahamas
Date: March 3, 2012

Weather Data from the Bridge

Position:30 deg 37 min North Latitude & 79 deg 29 min West Longitude
Windspeed: 30 knots
Wind Direction: North
Air Temperature: 14.1 deg C / 57.4 deg F
Water Temperature: 25.6 deg C / 78.4 deg F
Atm Pressure: 1007.2 mb
Water Depth:740 meters / 2428 feet
Cloud Cover: 85%
Cloud Type: Cumulonimbus and Stratus

Science/Technology Log:

Entering the  Gulf Stream and Straits of Florida

“There is in the world no other such majestic flow of waters.
Its current is more rapid than the Mississippi or the Amazon.
Its waters, as far out from the Gulf as the Carolina coasts, are of an indigo blue.
They are so distinctly marked that their line of junction with the common sea-water
may be traced by the eye.”

Matthew Maury – The Physical Geography of the Sea

 While our cruise could hardly be called leisurely, most sampling has been spread out between sites, sometimes involving day-long periods on station while the CTD and moorings are recovered from great depths (5,000 meters). However, Chief Scientist Dr. Baringer regularly reminds us that west of the Bahamas in the Gulf Stream transect, our stations are in much shallower water (≤800 meters) and close together (The Florida Straits are only about 50 miles wide), so we should anticipate increased activity on deck and in the lab. In addition to the hydrology measurements, we will deploy a specialized net to sample those minute creatures that live at the surface film of the water – the neuston.

The Neuston net is deployed for a 10-minute tow.

The Neuston net is deployed for a 10-minute tow.

Now that we have crossed the Bahama Banks and are on-station, the routine is, as expected, very condensed, and there is little time to rest. What I did not anticipate was the great flow of the Gulf Stream and the challenge to the crew to keep the Brown on our East-West transect line as the current forces us north.  Additionally, as Wordsworth wrote, “with ships the sea was sprinkled far and wide”  and  we had to avoid many other craft, including another research ship sampling in the same area.

Ben Franklin is famous for having produced the first chart of this great Western Boundary Current, but naval officer Matthew Maury – America’s Scientist of the Sea – and author of what is recognized as the first oceanography text, best described it.  Remarkably, in The Physical Geography of the Sea, first published in 1855, he anticipates the significance of this major climate study project and summarizes it in a short and often-quoted paragraph:

“There is a river in the ocean. In the severest of droughts it never fails,
and in the mightiest floods it never overflows.
Its banks and its bottom are of cold water, while its current is of warm.
The Gulf of Mexico is its fountain, and its mouth is the Arctic seas.
It is the Gulf Stream.”

 

Gulf Stream water

CTD data from the Straits of Florida
1. Note that temperature (Red) decreases steadily with depth from about 26-degrees C at the surface,
to less than 10-degrees C at 700 meters. (Most of the ocean’s waters are cool where not warmed by sunlight).
2. Dissolved Oxygen (Green) varies considerably from a maximum at the surface, with a sharp decline at about 100 meters, and a more gradual decline to about 700 meters. (Phytoplankton in surface water produce excess oxygen through photosynthesis during daylight hours. At night and below about 100 meters, respiration predominates and organisms reduce the level of dissolved oxygen.)
3. Salinity (Blue) is related to atmospheric processes (Precipitation and Evaporation) and also varies according to depth, being saltiest at about 150 meters.

***************************
“Ron Brown: Phone Home!”

At Midnight, just within sight of the beam of the Jupiter Inlet Lighthouse (And to the relief of the home-sick sailors on board – “Finally -  after  more than two weeks, we are within the range of cell phone towers!”) we began our studies of the Straits of Florida and the Gulf Stream. Nine stations in rapid order – standing-by for a CTD cast, and then turning into the current to set the neuston net for a ten-minute tow.

The purpose of the net is to sample creatures that live on or visit the interface between air and water, so the mouth of the net is only half submerged. Neuston comes from the Greek for swimming and in warm waters a variety of invertebrates and even some young mesopelagic fishes rise within a few centimeters of the surface at night to filter phytoplankton and bacteria, and feed upon other zooplankton and even drowned terrestrial insects that have been blown out to sea.

On the upper side of this water/atmosphere interface, a smaller variety of floating invertebrates, notably Physalia  and Velella (Portuguese man-of-war and By-the-wind-sailor) use gas-filled buoyancy chambers or surface tension to ride the winds and currents. This much smaller group of seafarers is further classified by oceanographers as Pleuston.

Prior to this cruise, my experience with such a sampling device was limited – Years ago, spending miserable nights sailing in choppy seas off of Sandy Hook, NJ searching  for fishes eggs and larva rising to the surface after dark; and later, much more enjoyable times studying water striders – peculiar insects that spend their lives utilizing surface tension to skate along the surface of Cape Cod ponds.

Our CTD and net casts are complicated by rising winds and chop, but some great samples were retrieved. Once the net is recovered, we rinse it down with the seawater hose, collect everything from the bottle at the cod end, rinse off and separate the great mass of weed (Sargassum) and pickle the neuston in bottles of alcohol for analysis back at the lab.

Midnight shift: Recovering the net by moonlight.

Midnight shift: Recovering the net by moonlight.

Midnight shift: Recovering the net by moonlight.

Midnight shift: Recovering the net by moonlight.

Since much of the zooplankton community rises closer to the surface at night where phytoplankton is more concentrated and the chances of being preyed upon are slimmer, there are some noticeable differences in the samples taken then and during daylight hours. Unavoidably, both samples contain great quantities of Sargassum but the weed-colored carapaces of the different crustaceans are a clue to which specimens are from the Sargassum community and which are not.

Gulfweed Shrimp - Latreutes

Gulfweed Shrimp – Latreutes

We hit the jackpot early; snaring a variety of invertebrates and fishes, including the extraordinarily well-camouflaged Sargassum fish – a piscatorial phenomenon I’ve hoped to see ever since I was a kid reading William Beebe’s classic The Arcturus Adventure. What a tenuous existence for such a vulnerable and weak swimmer, hugging the Sargassum as it is dashed about in the waves. Even with its weed-like disguise and ability to blend in with the plants, it must lead a challenging life.

A unique member of the otherwise bottom-dwelling frogfishes, the Histrio histrio has smooth skin, and spends its life hitch-hiking along in the gulf-weed forest. Like other members of the family Antennariidae, it is an ambush predator, luring other creatures to their doom by angling with its fleshy fins.

The Sargassum fish (Histrio)

The Sargassum fish (Histrio)

Needlefish and Sargassum fish

Needlefish and Sargassum fish

Another highlight for me is the water striders we found in several samples. These “true bugs” (Hemiptera) are remarkable for several reasons. Most varieties of these “pond-skaters” (Or Jesus Bugs if you are from Texas) are found on calm freshwater lakes and streams, but a few members of this family (Gerridae) are the only true marine insects – representing a tentative Arthropod reinvasion of the sea after their splendid foray onto land hundreds of millions of years ago.

Two great finds: Sygnathus pelagicus– A Sargassum pipefish – a cousin of the sea horse. Halobates – the water strider. An example of the Pleuston community.

Two great finds:
Sygnathus pelagicus– A Sargassum pipefish – a cousin of the sea horse.
Halobates – the water strider. An example of the Pleuston community.

Using surface tension to their advantage, they “skate” along by flicking their middle and hind legs, and can even “communicate” with each other by vibrating the surface of the water with the hair-like setae on their feet. On lakes their prey is other insects like mosquito larvae, confined to the surface. How they manage to find food and communicate at the surface of the raging sea is a mystery, but whatever the means, they are adept at it, and we recovered them in half of the samples.

The ocean's insect: The  remarkable water stride

The ocean’s insect: The remarkable water stride

The scientists who provided the net are generally more interested in ichthyoplankton to monitor fish eggs and larvae to predict population trends, and monitor impacts like oil spills; so this is why samples are preserved to return to the lab in Miami.

Before packing up things after our marathon sampling spree I was able to examine our catch and observed a few things:
1. I am the “High-Hook” on the cruise – catching far more fishes (albeit tiny ones) than the rest of the crew with their fishing poles. (Needlefish, sargassum fish, pipe fish, filefish and several larval species)
2. Depending on the time of day the samples were taken, there is a marked difference in the quantity and composition of organisms that have separated from the Sargassum and settled in the sample jars – (Noticeably more at night than during daylight hours).
3. There appears to be a greater variety of sea grasses present (Turtle grass, etc.) on the eastern (Bahamas side) of the Straits. We observed one seabean - drift seeds and fruits (or disseminules) from terrestrial plants.
4. Plastic bits are present in all samples – particularly plastic ties (Table 1.)

Settled organisms in sample jars.

Settled organisms in sample jars.

Sargassum fauna: Portunid crab – with eggs on her belly.
(Portunus was a Roman god - Protector of harbors and gates,
who supposedly also invented navigation)

Belly view of a Caridean shrimp

Belly view of a Caridean shrimp

A tiny fish egg ready to hatch!

A tiny fish egg ready to hatch!

A larval fish begins its perilous journey in the Gulf Stream.

A larval fish begins its perilous journey in the Gulf Stream.

Site/Local time

Notable Contents*

Biomass Site Depth
8 Day 17:48 Weed, Grasses(3 spp) 3.0 mm 79˚12’ 485 m
7 Day 16:10 Grasses(4 spp) 2.0 mm 79˚17’ 616 m
6 Day 14:30 Grasses(2 spp) Fish eggs and larva Trace 79˚22’ 708 m
5 Day 12:45 Water striders, Grass (1 spp) Trace 79˚30’ 759 m
4 Day 10:13 Crustacean larva, shrimp (large), 7.0 mm 79˚36’ 646 m
3 Dawn 07:53 Crustacean larva, shrimp (large), water striders Trace 79˚41’ 543 m
2 Night 05:10 Crustacean larva, shrimp (small), Pipefish, water striders 7.0 mm 79˚46’ 388 m
1 Night 02:48 Crustacean larva, shrimp, needlefish, Sargassum fish, Herring(?), Portunid crabs, shrimp (large), Copepods 13 mm 79˚51’ 264 m
0 Night 00:37 Crustacean larva, shrimp, Copepods 25 mm 79˚56’ 148 m

*Plastic bits and Sargassum weed and its endemic epibionts are present in all samples.

Table 1.   Contents in sample jars.

There is a marked difference in the quantity and composition of organisms collected at night (Left).

There is a marked difference in the quantity and composition of organisms collected at night (Left).

There is a marked difference in the quantity and composition of organisms collected at night (Left) and during the day (Right).

There is a marked difference in the quantity and composition of organisms collected during the day (Right).

With sampling completed we steer north to ride the Gulf Stream towards the Brown’s home-port,  and turn away from the bright lights of Florida …

“Where the spent lights quiver and gleam;
Where the salt weed sways in the stream;
Where the sea-beasts rang’d all around
Feed in the ooze of their pasture ground:”

Matthew Arnold

"Red sky at morning...sailor take warning!"

“Red sky at morning…sailor take warning!”

Homeward bound:

A storm battering the Midwest will impede our progress back north to Charleston and threatens to bring us the only foul weather of the cruise. Note the location of the cold front over the Florida Straits.

“Now the great winds shoreward blow;
Now the salt tides seaward flow;
Now the wild white horses play,
Champ and chafe and toss the spray.”
Matthew Arnold

As the sailors say: "The sheep are grazing." A gale is brewing and kicking up whitecaps as we sail north to Charleston.

As the sailors say: “The sheep are grazing.”
A gale is brewing and kicking up whitecaps as we sail north to Charleston.

Elizabeth Bullock: Introduction, December 8, 2011

NOAA Teacher at Sea
Elizabeth Bullock
Aboard R/V Walton Smith
December 11-15, 2011

Introduction

Hello! My name is Elizabeth (Liz) Bullock and I work for the NOAA Teacher at Sea Program (TAS).  Before I worked at NOAA (the National Oceanic and Atmospheric Administration)  I was in graduate school at Clark University in Worcester, MA studying Environmental Science and Policy.  As my final project, I created an environmental curriculum for the Global Youth Leadership Institute (GYLI).  Through this experience, I realized how much I love both science and educating others about the importance of the natural world.

I have been invited to take part in a research cruise on the R/V Walton Smith.  I will be participating in the Bimonthly Regional Survey / South Florida Program Cruise.  The researchers on this survey are  from NOAA’s Atlantic Oceanography and Meteorological Laboratory (AOML) which is located in Miami, FL.

What will we be studying?  The scientists on this survey are very interested in knowing about the strength and health of the ecosystem.  They can judge how strong it is by looking at various indicators such as water clarity, salinity, and temperature.  They can also record information about the phytoplankton and zooplankton that live in the water.

Question for students: Why do you think it is important to learn about the phytoplankton and zooplankton?  What can they tell us about the ecosystem?  Please leave a reply with your answers below by clicking on “Comments.”

Here is a map of the route the R/V Walton Smith will be taking.

Research Map

The R/V Walton Smith will be leaving Miami, FL and traveling around the Florida Keys into the Gulf of Mexico.

I am so excited and I hope you will follow along with me on this journey of a lifetime!

Caitlin Fine: Introduction, July 26, 2011

NOAA Teacher at Sea
Caitlin Fine
Onboard University of Miami Ship R/V Walton Smith
August 2 – 6, 2011

Mission: South Florida Bimonthly Regional Survey
Geographical Area: South Florida
Date: July 26, 2011

Personal Log

Hola! My name is Caitlin Fine and I teach science at Escuela Key (Francis Scott Key School), a dual-language immersion elementary school in Arlington, VA. I am a Virginia native and my heart is constantly torn between the lively activities of the Washington, D.C. area and the peaceful beauty of the Shenandoah Valley. I left Virginia for college and graduate school, but returned 4 years ago to begin my teaching career for Arlington County Public Schools.

Caitlin Fine

On top of Aspen Mountain during a recent trip to Colorado

Although I majored in Political Science and Spanish Literature and I have graduate degrees in Spanish Literature and Multicultural Education, I have always been interested in science. During college, I worked on an organic farm in Andalucia, Spain that practiced permaculture (this is a way of using the land that is sustainable so that the soil does not use-up all of its nutrients). I also traveled around the Southern Cone of South America (Chile, Argentina, Peru, Bolivia, Brazil) studying the geology of the region. As you can see, I have some experience with farming and the mountains. But I have never really spent an extended time at sea — I have never slept on a boat or studied the marine ecosystems up close and personal over a period of time. I hope that I am not seasick!

My interest in science mixed with my love of cooking has created a current obsession — the health of our national and global food and water supplies. Did you know that every time we take medicine or use pesticides on our plants, a small amount of it enters the water supply and some of it ends up in the rivers and oceans nearby where fish and water plants are trying to live?

The science program at Key is a bit different from traditional elementary schools in that there are three science teachers who teach all 630 students. For the past two years, I have taught the Kindergarteners, the 2nd graders and half of the 5th graders. Key kids are amazing scientists — they are full of questions about how the world works and they are not afraid to get busy trying to figure things out on their own through hands-on inquiry and cooperative learning. I cannot wait to return to Key with new knowledge of oceanography, ocean-related careers and ways to monitor the health of the ocean to share with my students and colleagues!

I am so excited to be a Teacher at Sea for the National Oceanic and Atmospheric Administration‘s 2011 Field Season! Teacher at Sea is a program that provides allows Kindergarten through college-level teachers to live and work alongside scientists on research and survey ships. The goal of the program is to help teachers understand our ocean planet, environmental literacy, and maritime work so that they can return to the classroom and share information with their students about what it is like to be a real scientist who studies the ocean.

I will be on a 5-day cruise on the R/V Walton Smith in south Florida.

R/V Walton Smith

This is the R/V Walton Smith

From what I understand, we will be taking measurements across the south Florida coastal marine ecosystem (the southwest Florida shelf, Biscayne and Florida Bays, and the Florida Keys reef tract). The program is important because the research has helped scientists keep an eye on the sensitive marine habitats, especially when the ecosystem has had to deal with extreme events, such as hurricanes, harmful algal blooms or potential oil spill contaminants. We will test the circulation, salinity, water quality and biology of the ecosystem.

Drainage Basin

The currents might move some of the Mississippi River water toward south Florida

During this cruise, I have been told that we might be able to measure Mississippi River water because it might enter our survey track.

Scientists are also going to be trying out new optical measurement tools! It sounds as though I will have a lot to report back to you about!

Please leave me a comment or any questions you have about the cruise.

Please take a moment to take my poll:

Heather Haberman: Gulf Water Health, July 12, 2011 (post #4)

  • NOAA Teacher at Sea
    Heather Haberman

    Onboard NOAA Ship Oregon II
    July 5 — 17, 2011

Mission:  Groundfish Survey
Geographical Location:  Northern Gulf of Mexico
Date:  Tuesday, July 11, 2011

Weather Data from  NOAA Ship Tracker
Air Temperature: 29.5 C   (85.1 F)
Water Temperature: 29.8 C  (85.6 F)
Relative Humidity: 76%
Wind Speed: 2.09 knots

Preface:  Scroll down the page if you would like to read my blog in chronological order.  If you have any questions leave them for me at the end of the post.

Question of the Day:  Are you seeing any oil rigs on your trip?

Answer:   There are so many oil rigs out here in the Gulf of Mexico that I can’t recall a time when I couldn’t see one.  Some are small and some are enormous.  I never realized that there were so many different engineering designs for oil rigs.  At night they are all lit up and it looks like a city in the sea out here.  All of the bright lights do pose some problems for migrating birds especially during bad weather when the are attracted to the lights.  The birds will often circle the lights to exhaustion or hit the structure so hard that it kills them.

Science and Technology Log

Topic of the Day:  How do researchers determine the health of the Gulf waters?

Science and Technology log:

You wake up in the morning and you don’t feel well.  What do you do?  Some people may stick a thermometer in their mouth to see if they have a fever.  Body temperature is a good indicator of illness or infection.  If you still don’t feel well after a few days you could visit a doctor who may check your eyes, ears, throat, blood pressure, etc.   Doctors can often figure out what’s making you sick by using certain tools and running tests.  Researchers do the same thing with the ocean.  In order to see how “healthy” the ocean is, measurements need to be taken.  Can you tell which trawl was from healthy water and which was from “sick” water?

0.5 kg (1.1 lbs) is all we got from this 30 minute trawl

Over 500 kg (1,100 lbs) of fish were collected in this 30 minute trawl.

Why aren’t we seeing a lot of marine life in certain parts of the Gulf of Mexico?  You don’t have to be a doctor to answer this question, but you do have to have some scientific tools to diagnose the problem.

On the Oregon II, a device called a CTD is used to take measurements such as conductivity (salinity), temperature, chlorophyll concentration, and dissolved oxygen (DO).  These water quality measurements let researches know what’s happening in the water just like a doctor would look at your test results to gage your health status.  Sometimes a doctor may need to do a second test just to confirm the results.  NOAA’s fisheries biologists do the same thing with their water quality assessments.  Winkler titrations and a hand-held Hack Dissolved Oxygen meter are used to confirm the dissolved oxygen readings from the CTD.  Scientists need to make sure the data they collect is accurate and the more tests they perform the better their data will be.

This large piece of equipment is a CTD sensor. The top portion of the machine contains three gray vertical cylinders which are used to collect water samples. Under the machine are sensors that test the water quality while it is submerged. Here I am washing out the sensors once it was brought back on board from a test.

When comparing data from this device to our trawl samples, it’s obvious that water with low levels of dissolved oxygen can not support much life.

Dissolved Oxygen: Marine animals need oxygen to survive just like land animals do.  The main difference is that most marine animals have gills which are able to diffuse oxygen molecules from the water directly into their blood.  Diffusion is the process of a molecule moving from an area of high concentration to low concentration.

Have you ever sprayed air freshener and noticed how the smell moves from where you sprayed it (high concentration) throughout the entire room (low concentration) until the smell is equally distributed throughout the room (equilibrium)?  That’s how diffusion works.

It’s very important to understand that the amount of dissolved oxygen MUST be higher in the water then inside of the animal’s body or diffusion of oxygen into the blood won’t take place.  This means the animals will either have to move or die.  This is what’s happening in the “Dead Zone” in the Gulf of Mexico.

The reason levels of oxygen are so low in the Gulf of Mexico are due in part to human actions.  The overuse of fertilizers that are high in nitrates and phosphates are one of the major problems.  When it rains or floods, these extra nutrients wash off of our lawns and into storm drains which then drain into the rivers.  Most of the Mississippi watershed consists of agricultural land in the breadbasket of the Midwest where a lot of fertilization takes place during the spring and summer months. All of the nutrients from the rivers in the Mississippi watershed eventually empty out into the Gulf of Mexico.

Mississippi Watershed: The area of land that drains into the Mississippi River and out into the Gulf of Mexico.

These nutrients help the aquatic plants grow, just as they helped our lawns and crops grow.  Now you may be thinking “In the last blog you talked about how important aquatic plants are when it comes to oxygen production.”  Indeed they do make oxygen, but as all of these plants die and sink to the bottom of the sea, bacteria feed on (decompose) their remains and use up the available oxygen in the process.  More oxygen is consumed by these aerobic bacteria than was made by the plants which is why oxygen levels can get so low.

Hypoxia is the term used when dissolved oxygen is below 2 mg/l or 2 parts per million.  That means for every one million molecules, only two of them are oxygen molecules.  Most marine life try to avoid water that’s this low in oxygen because they will become stressed or die.  The hypoxic zone in the Gulf occurs in one of the most important commercial fishery zones in the United States during the spring and summer months.  Why during the spring and summer?  There are a couple of answers to this question.  One is because of the fertilizer runoff which I mentioned earlier.  The other has to do with water temperature.

As water temperature increases, it naturally looses it's ability to hold gas molecules like oxygen. Cooler water naturally holds more oxygen. Source: Koi Club of San Diego

This is a map of the data we have been collecting during the Groundfish Survey. Our data gets sent in everyday and the maps are updated weekly. Check back at http://www.ncddc.noaa.gov/hypoxia/products/ for a complete map of Bottom Dissolved Oxygen after July 17th 2011.

When the data collection is complete you will notice that the “dead zone” is larger than the state of New Jersey.  It is bigger this year than in previous years due to the flooding that’s occurred in the Great Plains and Midwest this spring and summer.

Salinity (salt level):  This measurement is extremely important to the fish that live in the ocean because each species has an optimal salinity level that it requires.  Remember osmosis?  Osmosis is how cells move water in or out depending upon their environment.  If a fish ends up in an environment that’s too saline (salty), the water will begin to leave the cells of the fish through osmosis and they could “dehydrate”.  If they are in water that’s too fresh, then their cells will start to fill with water and they could “bloat”.  All of this cellular work is done by the body in order to maintain homeostasis.  Homeostasis refers to the ability of a living thing to keep its body in balance with the ever-changing environment in which it lives.

Salinity also affects the levels of dissolved oxygen in the water.  The saltier the water, the lower the oxygen levels will be.  It also creates a problem with waters ability to “mix”.

Notice how the heavier salt water settles to the bottom of the sea. The red dots represent the amount of dissolved oxygen during a hypoxia event. Notice that due to a lack of water mixing, the concentration of oxygen is much lower in the saltier bottom layer of water.

Chlorophyll Concentrations:  As the last blog mentioned, chlorophyll is a green pigment that phytoplankton and other aquatic plants have.  By calculating the concentration of chlorophyll in an a region, researchers can determine how productive the area may be for fishing.  Remember that zooplankton eat phytoplankton and bigger fish eat zooplankton, which are then eaten by bigger fish. A good general rule of thumb is that if the water is clear and blue then there won’t be as much living in it as green cloudy (turbid) water. Areas of hypoxia can also be predicted if the levels of chlorophyll get too high.

Now that you know some of the basics about ocean health, try to do your part.

*   If you must use fertilizer, do so sparingly.

*  Purchase soaps and detergents that are labeled phosphate free.

*  Be sure to make sustainable choices when purchasing seafood (visit Seafood Watch)

Personal Log

Today I found out why fishermen do not like dolphins.  A pod of dolphins were following us on a trawl and when we brought up the catch there were holes in the net.  We had to dump the sample back into the sea and try again after the holes were patched.  We went back to do a second trawl in the same area and the dolphins did the same thing.  We decided to try to “outrun” the dolphins on our way to the next station.

The reason we can’t collect data on the trawls with net holes is because we won’t get an accurate representation of the actual number of species living in that area.  In science it’s very important to make sure we collect good data.

A pod of dolphins following our ship.

Kathleen Brown: Sea Science, June 11, 2011

NOAA Teacher at Sea
Kathleen Brown
Aboard R/V Hugh R. Sharp
June 7 – 18, 2011

Mission: Sea Scallop Survey
Geographical area of cruise: North Atlantic
Date: June 11, 2011

June 11, 2011

Weather Data from the Bridge
Time: 12:50 PM
Winds 12.9 KTs
Air Temperature: 11.94 C
Latitude 41 05.84N
Longitude 067 25.88 W

Science and Technology Log

Lowering the CTD

Lowering the CTD

Every third station along the journey, the crew takes a CTD reading. CTD stands for conductivity, temperature, and depth. Using a submersible set of probes, the characteristics of the ocean water are measured at set intervals, from the surface to the sea bottom, and then again from the sea bottom to the surface. Wynn, the marine technician, takes the time to explain to me that on this cruise the equipment is set to measure temperature, salinity, oxygen and phosphorescence. The probe is extremely heavy and must be lowered with a winch. The capability of the equipment is quite sophisticated and can take a water sample at any depth. A canister can be programmed to shut quickly, capturing approximately ten liters of water. The timing of the data collection process depends upon the depth of the water, but today it takes about five minutes. The data is collected for the NOAA team back on land.

Our journey will circle the outer edges of George’s Bank. We are on the eastern leg of the trip, somewhere between 80 and 100 miles from land. As far as the eye can see, it is ocean. Once in a while, we can see a fishing vessel off in the distance and we have seen dolphins and sunfish swimming near the ship. This afternoon I heard Mary, the First Mate, announce over the radio that she spotted a whale. I ran up to the bridge to see if I could get a look, but I was too late!

I have been eager to learn the stories of the scientists and crew, and to find out what has drawn them to the work at sea. The backgrounds of the people on the ship are varied, and they are both men and women of all ages. One person reports, “ I knew that I wanted to be a marine biologist since fifth grade.” Another says, “I grew up around boats.” Yet another speaks about wanting a hands-on career that could last a lifetime. There are several students on this leg of the cruise. I have learned there are many paths to the career at sea: experience in the military, technical school, college and university, and hands on experience over the years It seems that if you are attracted to the sea, you have a place on a scientific research vessel.

Personal Log
Toward the end of the day, the boat starts to roll a bit more than it has. We have been informed that the wave heights tomorrow may increase to 5 to 8 feet. Taking a shower while the boat rocks from side to side is challenging. I grip my flip flops to the floor of the shower and hang on!

Question of the Day
What do you think the level of salt in the water can tell scientists?

Margaret Stephens, May 28, 2011

NOAA Teacher at Sea: Margaret Stephens
NOAA Ship: Pisces
Mission: Fisheries, bathymetric data collection for habitat mapping
Geographical Area of Cruise: SE United States continental shelf waters from Cape Hatteras, NC to St. Lucie Inlet, FL
Date:  May 28, 2011 (Last day!)

NOAA Ship Pisces. Photo credit: Richard Hall

NOAA Ship Pisces. Photo credit: Richard Hall

Weather Data from the Bridge
As of 06:43, 28 May
Latitude 30.15
Longitude 80.87
Speed 7.60 knots
Course 285.00
Wind Speed 10.77 knots
Wind Direction 143.91 º
Surface Water Temperature 25.53 ºC
Surface Water Salinity 36.38 PSU
Air Temperature 24.70 ºC
Relative Humidity 92.00 %
Barometric Pressure 1011.10 millibars
Water Depth 30.17 m
Skies: clear

r at Sea Margaret Stephens and Scientist David Hoke in Pisces attire.

NOAA Teacher at Sea Margaret Stephens and Scientist David Hoke in Pisces attire.

Science and Technology Log

These scientists are not only smart, but they are neat and clean, too! After completing final mapping and fish sampling on the second-to-last day, we spent the remainder of the time cleaning the wet (fish) lab, packing all the instruments and equipment, and carefully labeling each item for transport. We hosed down all surfaces and used non-toxic cleaners to leave the stainless steel lab tables and instruments gleaming, ready for the next research project. The Pisces, like other NOAA fisheries ships, is designed as a mobile lab platform that each research team adapts to conform to its particular needs. The lab facilities, major instruments and heavy equipment are permanent, but since research teams have different objectives and protocols, they bring aboard their own science personnel, specialized equipment, and consumable supplies. The primary mission of NOAA’s fisheries survey vessels, like Pisces, is to conduct scientific studies, so the ship’s officers and crew adjust and coordinate their operations to meet the requirements of each research project. The ship’s Operations Officer and the Chief Scientist communicate regularly, well before the project begins and throughout the time at sea, to facilitate planning and smooth conduct of the mission.

Gag grouper (top, Mycteroperca microlepis) and red snapper (Lutjanus campechanus) specimens, labeled for further study Photo credit: David Berrane

Gag grouper (top, Mycteroperca microlepis) and red snapper (Lutjanus campechanus) specimens, labeled for further study Photo credit: David Berrane

“Wet” (fish) lab aboard Pisces, cleaned and ready for next research team

“Wet” (fish) lab aboard Pisces, cleaned and ready for next research team

We made up for the two days’ delay in our initial departure (caused by mechanical troubles and re-routing to stay clear of the Endeavor space shuttle launch, described in the May 18 log), thanks to nearly ideal sea conditions and the sheer hard work of the ship’s and science crews. The painstaking work enabled the science team to fine tune their seafloor mapping equipment and protocols, set traps, and accumulate data on fish populations in this important commercial fishing area off the southeastern coast of the United States. The acoustics team toiled every night to conduct survey mapping and produce three dimensional images of the sea floor. They met before sunrise each morning with Chief Scientist Nate Bacheler to plan the daytime fish survey routes, and the fish lab team collected two to three sets of six traps every day. The videographers worked long hours, backing up data and adjusting the camera arrays so that excellent footage was obtained.  In all, we obtained ten days’ worth of samples, brought in a substantial number of target species, red snapper and grouper, recorded hours of underwater video, and collected tissue and otolith samples for follow-up analysis back at the labs on land.

Models

Scientists and engineers often use models to help visualize, represent, or test phenomena they are studying. Models are especially helpful when it is too risky, logistically difficult, or expensive to conduct extensive work under “live” or real-time conditions.

Divers exploring hardbottom habitat Photo Credit: Douglas E. Kesling, UNCWilmington, CIOERT

Divers exploring hardbottom habitat Photo Credit: Douglas E. Kesling, UNCWilmington, CIOERT

As described in previous logs, this fisheries work aboard Pisces involves surveying and trapping fish to analyze population changes among commercially valuable species, principally red snapper and grouper, which tend to aggregate in particular types of hardbottom habitats.  Hardbottom, in contrast to sandy, flat areas, consists of rocky ledges, coral, or artificial reef structures, all hard substrates. By locating hardbottom areas on the sea floor, scientists can focus their trapping efforts in places most likely to yield samples of the target fish species, thus conserving valuable time and resources. So, part of the challenge is finding efficient ways to locate hardbottom. That’s where models can be helpful.

The scientific models rely on information known about the relationships between marine biodiversity and habitat types, because the varieties and distribution of marine life found in an area are related to the type of physical features present. Not surprisingly, this kind of connection often holds true in terrestrial (land) environments, too. For example, since water-conserving succulents and cacti are generally found in dry, desert areas, aerial or satellite images of land masses showing dry environments can serve as proxies to identify areas where those types of plants would be prevalent. In contrast, one would expect to find very different types of plant and animal life in wetter areas with richer soils.

Recovering ROV aboard Pisces Photo source: http://www.moc.noaa.gov/pc/visitor/photos‐a.html

Recovering ROV aboard Pisces Photo source: http://www.moc.noaa.gov/pc/visitor/photos‐a.html

Traditional methods used to map hardbottom and identify fish habitat include direct sampling by towing underwater video cameras, sonar, aerial photography, satellite imaging, using remotely operating vehicles (ROV’s), or even setting many traps in extensive areas. While they have some advantages, all those methods are labor and time-intensive and expensive, and are therefore impractical for mapping extensive areas.

This Pisces team has made use of a computer and statistical model developed by other scientists that incorporates information from previous mapping (bathymetry) work to predict where hardbottom habitat is likely to be found. The Pisces scientists have employed the “Dunn” model to predict potential hardbottom areas likely to attract fish populations, and then they have conducted more detailed mapping of the areas highlighted by the model. (That has been the principal job of the overnight acoustics team.) Using those more refined maps, the day work has involved trapping and recording video to determine if fish are, indeed, found in the locations predicted. By testing the model repeatedly, scientists can refine it further. To the extent that the model proves accurate, it can guide future work, making use of known physical characteristics of the sea floor to identify more areas where fish aggregate, and helping scientists study large areas and develop improved methods for conservation and management of marine resources.

Deploying CTD. Photo credit: David Hoke

Deploying CTD. Photo credit: David Hoke

Deploying CTD. Photo credit: David Hoke

Deploying CTD. Photo credit: David Hoke

Conductivity, Temperature and Depth (CTD) Measurements

Another aspect of the data collection aboard Pisces involves measuring key physical properties of seawater, including temperature and salinity (saltiness, or concentration of salts) at various depths using a Conductivity, Temperature and Depth (CTD)  device.

Salinity and temperature affect how sound travels in water; therefore, CTD data can be used to help calibrate the sonar equipment used to map the sea floor. In other instances, the data are used to help scientists study changes in sea conditions that may affect climate. Increases in sea surface temperatures, for example, can speed evaporation, moisture and heat transfer to the atmosphere, feeding or intensifying storm systems such as hurricanes and cyclones.

Pisces shipboard CTD, containing a set of probes attached to a cylindrical housing, is lowered from the side deck to a specified depth. A remote controller closes the water collection bottles at the desired place in the water column to extract samples, and the CTD takes the physical measurements in real time.

Fresh Catch

Of all the many species collected, only the red snapper and grouper specimens were kept for further study; most of the other fish were released after they were weighed and measured. A small quantity was set aside for Chief Steward Jesse Stiggens to prepare for the all the ship’s occupants to enjoy, but the bulk of the catch was saved for charitable purposes. The fish (“wet” lab) team worked well into overtime hours each night to fillet the catch and package it for donation. They cut, wrapped, labeled and fresh froze each fillet as carefully as any gourmet fish vendor would. Once we disembarked on the last day, Scientist Warren Mitchell, who had made all the arrangements, delivered over one hundred pounds of fresh frozen fish to a local food bank, Second Harvest of Northern Florida. It was heartening to know that local people would benefit from this high-quality, tasty protein.

Careers at Sea

Crewmen Joe Flora and Vic Pinones

Crewmen Joe Flora and Vic Pinones

Many crew members gave generously of their time to share with me their experiences as mariners and how they embarked upon and developed their careers. I found out about many, many career paths for women and men who are drawn to the special life at sea. Ship’s officers, deck crew, mechanics, electricians, computer systems specialists, chefs and scientists are among the many possibilities.

Chief Steward Jesse Stiggens worked as a cook in the U.S. Navy and as a chef in private restaurants before starting work with NOAA. He truly loves cooking, managing all the inventory, storage and food preparation in order to meet the needs and preferences of nearly forty people, three meals a day, every day. He even cooks for family and friends during his “off” time!

First Engineer Brett Jones

First Engineer Brett Jones

Electronics specialist Bob Carter, also a Navy veteran, is responsible for the operations and security of all the computer-based equipment on board. He designed and set up the ship’s network and continually expands his skills and certifications by taking online courses. He relishes the challenges, responsibilities and autonomy that come along with protecting the integrity of the computer systems aboard ship.

First Engineer Brent Jones has worked for many years in the commercial and government sectors, maintaining engines, refrigeration, water and waste management, and environmental control systems. He gave me a guided tour of the innards of Pisces, including four huge engines, heating and air conditioning units, thrusters and rudders, hoists and lifts, fresh water condenser and ionizers, trash incinerator, and fire and safety equipment. The engineering department is responsible for making sure everything operates safely, all day and night, every day. Brent and the other engineers are constantly learning, updating and sharpening their skills by taking specialized courses throughout their careers.

Chief Boatswain James Walker

Chief Boatswain James Walker

Chief Boatswain James Walker is responsible for safe, efficient operations on deck, including training and supervising all members of the deck crew. He entered NOAA after a career in the U.S. Navy.  The Chief Boatswain must be diplomatic, gentle but firm, and a good communicator and people manager. He coordinates safe deck operations with the ship’s officers, crew, and scientific party and guests.

NOAA officers are a special breed. To enter the NOAA Commissioned Officer Corps, applicants must have completed a bachelor’s degree with extensive coursework in mathematics or sciences. They need not have experience at sea, although many do. They undergo an intensive officers’ training program at a marine academy before beginning shipboard work as junior officers, where they train under more experienced officers to learn ship’s systems and operations, protocols, navigation, safety, personnel management, budgeting and administrative details. After years of hard work and satisfactory performance, NOAA officers may advance through the ranks and eventually take command of a ship.

Operations Officer, Lt. Tracy Hamburger

Operations Officer, Lt. Tracy Hamburger

Junior Officer Michael Doig

Junior Officer Michael Doig

All the officers and crew aboard Pisces seem to truly enjoy the challenges, variety of experiences and camaraderie of life at sea. They are dedicated to NOAA’s mission and take pride in the scientific and ship operations work. To be successful and satisfied with this life, one needs an understanding family and friends, as crew can be away at sea up to 260 days a year, for two to four weeks at a time. There are few personal expenses while at sea, since room and board are provided, so prudent mariners can accumulate savings. There are sacrifices, as long periods away can mean missing important events at home. But there are some benefits: As one crewman told me, every visit home is like another honeymoon!

Personal Log

One size fits all?

One size fits all?

Navy Showers

I had expected that life aboard Pisces would include marine toilets and salt water showers with limited fresh water just for rinsing off.  I was surprised to find regular water-conserving flush toilets and fresh water showers. Still, the supply of fresh water is limited, as all of it is produced from a condensation system using heat from the engines. During our ship orientation and safety session on the first day, Operations Officer Tracy Hamburger and Officer Mike Doig cautioned us to conserve water.  They explained (but did not demonstrate!) a “Navy” shower, which involves turning the water on just long enough to get wet, off while soaping up, and on again for a quick rinse. It is quite efficient – more of us should adopt the practice on land. Who really needs twenty minute showers with fully potable water, especially when more than one billion people on our “water planet” lack safe drinking water and basic sanitation?

One size fits all?

One size fits all?

“Abandon Ship!”

One size fits all?

One size fits all?

The drill I had anticipated since the first pre-departure NOAA Teacher at Sea instructions arrived in my inbox finally happened. I had just emerged from a refreshing “Navy” shower at the end of a fishy day when the ship’s horn blasted, signaling “Abandon ship!” We’d have to don survival suits immediately to be ready to float on our own in the sea for an indefinite time. Fortunately, I had finished dressing seconds before the alarm sounded. I grabbed the survival suit, strategically positioned for ready access near my bunk, and walked briskly (never run aboard ship!) to the muster station on the side deck. There, all the ship’s occupants jostled for space enough on deck to flatten out the stiff, rubbery garment and attempt to put it on.  That’s much easier said than done; it was not a graceful picture. “One size fits all”, I learned, is a figment of some manufacturer’s imagination. My petite five foot four frame was engulfed, lost in the suit, while the burly six- foot-five crewman alongside me struggled to squeeze himself into the same sized suit. The outfit, affectionately known as a Gumby, is truly designed for survival, though, as neoprene gaskets seal wrists, leaving body parts covered, with only a small part of one’s face exposed. The suit serves as a flotation device, and features a flashing light, sound alarm, and other warning instruments to facilitate locating those unfortunate enough to be floating at sea.

Thankfully, this was only a test run on deck. We were spared the indignity of going overboard to test our true survival skills. I took advantage of the opportunity to try a few jumping jacks and pushups while encased in my Gumby.

Fish bet ‐‐ Rigged results? Photo credit: Jen Weaver

Fish bet ‐‐ Rigged results? Photo credit: Jen Weaver

Bets Are On!

These scientists are fun-loving and slightly superstitious, if not downright mischievous. On the last day, Chief Scientist Nate Bacheler announced a contest: whoever came closest to predicting the number of fish caught in the last set of traps would win a Pisces t-shirt that Nate promised to purchase with his personal funds. In true scientific fashion, the predictions were carefully noted and posted for all to see.  As each trap was hauled in, Nate recorded the tallies on the white board in the dry lab. Ever the optimist, basing my estimate on previous days’ tallies, I predicted a whopping number: 239.

I should have been more astute and paid more attention to the fact that the day’s survey was planned for a region that featured less desirable habitats for fish than previous days. Nate, of course, having set the route, knew much more about the conditions than the rest of us did. His prediction: a measly 47 fish. Sure enough, the total tally was 38, and the winner was………Nate!   Our loud protests that the contest was fixed were to no avail. He declared himself the winner. Next time, we’ll know enough to demand that the Chief Scientist remove himself from the contest.

 

Chief Scientist Nate Bacheler and red snapper, Lutjanus campechanus Photo credit: David Hoke

Chief Scientist Nate Bacheler and red snapper, Lutjanus campechanus Photo credit: David Hoke

 

Crewman Kirk Perry with Mahi‐mahi

Crewman Kirk Perry with Mahi‐mahi

Catching Mahi-mahi

Once the day’s deck work was over, a fish call came over the ship’s public address system. Kirk Perry, one of the avid fishermen among the crew, attached a line baited with squid from the stern guard rail and let it troll along unattended, since a fishing pole was unnecessary. Before long, someone else noticed that the line had hooked a fish. It turned out to be a beautiful mahi-mahi, with sleek, streamlined, iridescent scales in an array of rainbow colors, and quite a fighter. I learned that the mahi quickly lose their color once they are removed from the water, and turn to a pale gray-white once lifeless. If only I were a painter, I would have stopped everything to try to capture the lovely colors on canvas.

Goodbyes

We entered Mayport under early morning light. An official port pilot is required to come aboard to guide all ships into port, so the port pilot joined Commander Jeremy Adams and the rest of the officer on the bridge as we made our way through busy Mayport, home of a United States Naval base. Unfortunately, the pier space reserved for Pisces was occupied by a British naval vessel that had encountered mechanical problems and was held up for repairs, so she could not be moved. That created a logistical challenge for us, as it meant that Pisces had to tie up alongside a larger United States naval ship whose deck was higher than ours.  Once again, the crew and scientists showed their true colors, as they braved the hot Florida sun, trekking most of the gear and luggage by hand over two gangplanks, across the Navy ship, onto the pier, and loading it into the waiting vehicles.

The delay gave me a chance to say farewell and thank the crew and science team for their patience and kindness during my entire time at sea.

These eleven days sailed by. The Pisces crew had only a short breather of a day and a half before heading out with a new group of scientists for another research project. To sea again….NOAA’s work continues.

All aboard!

A big “Thank you!” to all the scientists and crew who made my time aboard Pisces so educational and memorable!

 

Science team. Photo credit: NOAA Officer Michael Doig

Science team. Photo credit: NOAA Officer Michael Doig

Links & Resources

http://www.marinecareers.net/links_degrees.php

Literature cited:

Dunn, D, Halpin, P (2009) Rugosity-based regional modeling of hard-bottom habitat. Marine Ecology Progress Series 377:1-11

Safety! I hope I never have to use that fire axe!

Safety! I hope I never have to use that fire axe!

Sky view from Pisces. Photo credit: David Hoke

Sky view from Pisces. Photo credit: David Hoke

View from Pisces: United States Navy’s Littoral Combat Ship

View from Pisces: United States Navy’s Littoral Combat Ship

Engineers Abe Goldberg and Bob Carroll

Engineers Abe Goldberg and Bob Carroll

Loading gear with crane & hoist

Loading gear with crane & hoist

Loading gear with crane & hoist

Loading gear with crane & hoist

Commander Jeremy Adams looks out from Pisces’ bridge Photo credit: Richard Hall

Commander Jeremy Adams looks out from Pisces’ bridge Photo credit: Richard Hall

Obed Fulcar, July 24, 2010

NOAA Teacher at Sea Obed Fulcar
NOAA Ship Oscar Dyson
July 27, 2010 – August 8, 2010

Mission:Summer Pollock survey III
Geograpical Area:Bering Sea, Alaska
Date: July 24, 2010

Science & Technology Log:
Thursday, July 22: After a night of swinging and swaying from the waves at high seas, I am somewhat used to it already. Today is the start of my new shift from 0400 in the morning until 4:00 pm in the afternoon, 12 hours on, 12 hours off. Since yesterday we left the continental shelf and we are heading to deeper waters. There was a scheduled trawl to be done early this morning, but the Acoustic Lab reported no fish at all on the screens. As part of the survey it is necessary to perform a CTD launch every morning at sunrise. CTD stands for Conductivity, Temperature, and Depth, explained Darin Jones, one of the young scientists in charge of the Pollock survey.
CTD

CTD

The CTD unit is made up of a series of bottles used to collect water samples at different depths, and also includes remote sensors to collect data such as sea temperature, salinity, depth, water pressure, and fluorescence. Fluorescence is the presence of Chlorophyll in the water which depends on the amount of sunlight that penetrates the ocean, indicating the presence of Phytoplankton (algae and other microscopic plants). They rely on sunlight to produce the energy that zooplankton growth is dependent upon. Zooplankton is the foundation of the Bering Sea food chain,since is made up of krill, small shrimp like crustaceans that are the primary source of food for commercial fish such as Pollock, Cod, Salmon, and pretty much any other fish in the North Pacific Ocean.
CTD

CTD

As the CTD is dropped the ship needs to stop in order lower the unit, which is attached by cables to an A-Frame crane, including one to transmit data. The CTD can only be used to depths of 600 meters, so another device called the XBT for Expendable Bathy-Thermograph (for depth and temperature) is used for depths up to 700 meters. It can also be launched manually while the ship is in motion, and data is transmitted through a thin copper wire that splits, hence the name “Expendable”. Once the CTD is hauled back onto deck, the water bottles are drained and samples taken for dissolved oxygen (DO)analysis. DO is sequestered using chemicals that react with the oxygen taking a solid form that preserves it for lab analysis.
XBT

XBT

Personal Log:
Last night I took motion sickness pills to keep me from getting seasick. After breakfast weather got really bad, with waves up to 6 feet, battering the Oscar Dyson. These conditions, combined with a heavy breakfast, made feel really dizzy, and next I know I was throwing up. My roommate, Vince Welton, who is also the ship’s tech guy, got me some very tasty saltine crackers, and medication, that help me feel better. I laid down on my bunk bed and doze off while listening to some Jazz by Michel Camilo.
While trying to rest the waves were crashing into the hull of the ship with a loud noise, while the ship kept going up and down. I was thinking about how seafarers of the past and the conditions aboard were so much different than today. Ocean going trips now are made much easier by the technology and modern amenities commonly found on board. Staterooms with bath, galleys or kitchens fully equipped with fridge, microwave oven, and entertainment rooms with flat TVs and DVD players are the norm. I kept thinking that the next 2 weeks on board the Oscar Dyson will be a lot like space travel, will all the walking up and down stairs from deck to deck, closing of hatches, and not been able to step outside the ship for a walk until reaching port.
The connection I can make about the CTD is that it reminds me a lot of the citizen science data collection and water quality monitoring I conduct with my students after school on the Harlem River, as part of “A Day in the Life of the Hudson River” a yearly event sponsored by NYSDEC (NY State Dept of environmental Conservation) and Columbia University Lamont-Doherty Laboratory. just like in the CTD we collect samples of water from the river to test for Dissolved Oxygen, Chlorophyll, PH, Salinity, Nitrates, plus soil samples from the mudflats.
When we collect the chlorophyll samples we use the same methods just as it’s done on the Oscar Dyson, squirting the water through a circular paper filter until it turns brownish. I am planning a lesson for next school year called “NOAA in the Classroom:Student CTD Activity” where using a student water sampling bottle my Environmental Science Club class will collect water from the Harlem River at different depths with the help of our wooden boat “Boca Chica” built after school. We test the samples for DO, Salinity, PH and other protocols using a LaMotte water quality test kit to monitor the health of the Harlem/Hudson River Estuary. This data will be reported to the GLOBE.gov Program website to be used by scientists and schools all over the world. My middle schoolMS319 is a GLOBE Program partner school, and also we will be reporting data from our new Wireless Weather Station. I strongly believe that students learn science by doing science!
Boca Chica

Boca Chica

“Navegando en Alta Mar”
Jueves, 22 de Julio: Hoy comence my primera guardia de las 0400 am a las 4pm. Desde que zarpamos del puerto de Dutch Harbor hacia aguas profundas me habia librado del mareo, pero finalmente me agarro.
El mal tiempo de hoy temprano, con violetas olas que golpeaban la nave de hasta 18 metros, mas un desayuno muy pesado me provocaron unas nauseas que termine en mi camarote vomitando y tirado en la cama. Despues de tomarme una medicina y de comerme unas galletitas de soda, me tome una siesta y me levante mucho mejor. El Sonar Acustico de la nave no detecto presencia de peces por lo que fui a ver el lanzamiento de un CTD o unidad de Conductividad y Profundidad Termal. El CTD contiene botellas para recoger muestras de agua y sensores para medir la temperatura y salinidad del mar hasta 600 metros.
Para medidas mas profundas de hasta 700 metros se usa una unidad manual desechable llamada XBT. Ambas unidades son usadas para obtener datos cientificos como el nivel de Oxygeno disuelto, Salinidad, Profundidad, y Florescencia (nivel de clorofila), la ultima es muy importante pues refleja la abundancia de algas microscopicas de las que depende elZooplankton. El zooplankton esta compuesto de minusculos crustaceos que son la base del ecosistema alimenticio del Estrecho de Bering, del cual dependen especies comerciales como el Bacallao, Salmon y Arenque, asi como casi toda especie de pez en el Oceano Pacifico Norte. El uso del CTD es muy parecido al trabajo que hago con mis estudiantes analizando las aguas del Rio Harlem. Estos jovenes cientificos tambien toman muestras de agua y practican analisis de campo para Oxygeno disuelto, PH, Nitratos, Salinidad e incluso pruebas de Clorofila, como parte de un evento anual llamado “Un dia en la Vida del Rio Hudson” .
En este evento organizado por el Laboratotio Lamont-Doherty de la Universidad Columbia, y el Depto de Conservacion del Estado de NY, participan escuelas a todo lo largo del Rio Hudson, recaudando datos cientificos sobre el rio. Pensamos usar a “BOCA CHICA”,un bote de madera que armamos de tarde, para una practica de CTD tomando muestras de agua del rio, analizarlas, y reportar los datos en el internet. Tambien mis estudiantes de la Escuela Intermedia Maria Teresa Mirabal Ms319, de origen dominicano en su mayoria, aprenden ciencia ambiental al tomar datos de la Estacion Metereologica ubicada en el techo de la escuela. Ellos reportan los datos via internet en la pagina web del Programa GLOBE.gov, para ser usados por cientificos y estudiantes por todo el mundo.

Kathy Schroeder, May 12, 2010

NOAA Teacher at Sea
Kathy Schroeder
Aboard NOAA Ship Oscar Dyson
May 5 – May 18, 2010

Mission: Fisheries Surveys
Geographical Area: Eastern Bering Sea
Date: May 12, 2010

5/12 Mooring Buoy

Launching a mooring buoy

Launching a mooring buoy

Today we launched another type of buoy. It is called a Mooring Buoy. Its height is 5 meters above the surface (pictured on left) and 72 meters below the surface, which ends with a concrete dome that weighs 4110 (pictured on right). You can see the mooring being towed by the ship to get it into the right position. It has a barometer (measures atmospheric pressure), an anemometer (measures wind speed) and a thermometer on the top. There are sensors at different depths that measure salinity, chlorophyll, temperature, pressure, and nitrates.The information is transmitted to satellite Pacific Marine Environmental Lab (NOAA) that monitors the surface and subsurface of the Bering Sea. This piece of equipment costs $250,000. There are two other moorings already in this location. One measures ocean currents the other measures acoustic plankton. On one it has an underwater rain gauge. Can you figure out what that means? Headed to the Pribilof Islands today. On the way some crew saw sea ice. I’ll be looking! I love reading everyone’s comments. Keep them coming!