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.

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!