CTD – Page 21 – NOAA Teacher at Sea Blog

July 7, 2014August 21, 2021

Crystal Davis, When Science Goes Wrong, July 6 2014

NOAA Teacher at Sea

Crystal Davis

Aboard NOAA Ship Oregon II

June 23 – July 7, 2014

Mission: SEAMAP Groundfish Survey

Geographical area of cruise: Gulf of Mexico

Date: Sunday July 6, 2014

Weather: Clear and Sunny

Waves: 1-2 feet

Science and Technology Log:

The title of this post should actually be, “when science doesn’t go exactly as planned,” but that doesn’t sound quite as dramatic.

If you have ever written a lab report, you know that there is a section for procedures (what you did). The procedures need to be explicit so that they can be replicated by another individual who will obtain the same results. If your experiment cannot be replicated, your experiment is not valid and is useless. While it is okay for your hypothesis to be different than your expected outcomes, you always have to follow your procedure.

But . . . what if you’re in the middle of the ocean potentially hundreds of miles away from shore and on a deadline? You can’t go back to shore. There are at least thirty people on your boat and a lot of money invested in this data collection. Yet you still have to come up with a way to complete your survey. The events that follow are incidents that occurred on the Oregon II from July 26-July 6 and how the scientists coped with these situations.

Sharks

Juvenile Hammerhead Shark — Hammerhead Shark, Courtesy of Robin Gropp

In August, NOAA conducts a Longline Survey surveying sharks. Sharks are captured, identified and many are tagged with tracking devices to monitor the location and population density of sharks. Other sharks are sampled to determine age, analyze growth, sexual maturity and study stomach contents.

When sharks are captured in the trawl net on the Groundfish Survey, Robin (the intern) has been releasing them back into the Gulf after collecting data. However, not all of the sharks survive being pulled up in the net. The picture to the left is of a juvenile Hammerhead that did not survive. While this saddens me, he has been frozen and will be used to educate students in the outreach programs that NOAA participates in.

Nature vs Science

Waves crashing on the bow of the Oregon II. This picture was not taken on my survey, but this is what the weather felt like to me.

Sometimes mother nature interferes with the survey and things don’t go exactly as planned. For the first week of my trip we ran into some bad weather. There was a series of storms that came off the coast bringing rain, thunder, lightning and waves that were five to seven feet high. The weather conditions were so bad that the day shift couldn’t immediately collect data at a number of stations. They spent a lot of time waiting for the squalls to pass until it was safe to collect data. In fact, the weather in the Fall Groundfish Survey is so bad that there are a few extra days built in to run from hurricanes.

This morning we were trawling off the mouth of the Mississippi River and brought up a net full of sargassum (seaweed). The entire net, all 42 feet of it, was completely full of sargassum and very little marine life. No one on the boat had seen this much sargassum in the net before. This catch had to be thrown back overboard because the data is not usable. Basically, with that much sargassum in the net, the scientists are not sure if the trawl was fished properly. There is the possibility that because the net was so heavy, it was bogged down, uneven or not scraping the bottom of the ocean floor evenly.

The beginning of a squall courtesy of Andre DeBose

Squall moving the doors on the trawl net courtesy of Andre DeBose

Trawl Net filled with Sargassum

Warren and Mike checking to see if we are keeping the trawl

Mike and Eloy checking out the Sargassum

Formalin

On the Oregon II, plankton samples are preserved in Formalin (40% Formaldehyde). Formalin is a clear substance that stops cells from breaking down. A few days ago we noticed that the Formalin was no longer clear, it was in fact opaque. You can see this in the picture on the left. My night shift crew was worried that it was no longer useful and that we could not bring planktons samples back to the lab in Pascagoula. However, our chief scientist assured us that we could still use the Formalin and that it would be effective. The color change indicated that the base in the mixture was breaking down but since we only have a couple more days of plankton sampling, that it will be fine.

Personal Log:

I arrived back home last night and let me tell you it is strange to be back on land. I was never seasick on the Oregon II, but I am 100% landsick now. I find myself swaying from side to side anytime I’m standing still (Dock Rock is the official term). And when I woke up last night to get a glass of water, I fell over because I was swaying so much. It’s actually pretty funny but I will be glad once this goes away.

I’m still taking in my experience from the last two weeks but I am so grateful for the people I met and was able to work with. Everyone on the Oregon II was helpful, accommodating, friendly and made me feel at home. They took time out of their day to answer my questions, give me tours, tell me stories about their history and adventures on board, go over their research and they were genuinely interested in what I do in my classroom. XO (Executive Officer) LCDR Eric Johnson spent a good chunk of his time telling me about the NOAA Corps and made me want to sign up. Although I’m not too old to apply, (I have too many attachments at home to do so) if I could do the last ten years over I would apply to their program. I will definitely make sure my students know that the NOAA Corps is an option for them and am hoping to make a trip down to San Diego to take them on one of the boats next year.

I’m particularly grateful to the Chief Scientist Andre DeBose and Watch Leader Taniya Wallace who made sure I knew I was not going to die at sea. As the boat was leaving Galveston I could not stop crying because I was 100% certain I was never coming back ( I may have watched The Perfect Storm too many times). Andre and Taniya were so reassuring and comforting and I can never thank them enough for that.

I’m looking forward to using the knowledge, pictures and data from this trip in my classroom next year. I’m also excited because I heard that I can apply to be a volunteer on a NOAA cruise and am looking forward to this in the future.

July 2, 2014August 21, 2021

Dana Clark : Alaska in 3D, June 30, 2014

NOAA Teacher at Sea

Dana Clark

Onboard NOAA Ship Fairweather

June 23 – July 3, 2014

Mission: Hydrographic Survey

Geographical area of cruise: South Coast of Kodiak Island

Date: June 30, 2014

Weather Data: Latitude – 56° 34.74′ N, Longitude – 154° 02.21′ W, Sky Condition – 1/2 clouds, Present Weather – clear, Visibility – 10+ nautical miles, Wind – 15 knots, Temperature – 10° C

Science and Technology Log

I had a great day yesterday on the launch gathering more hydrographic survey data. We had a pretty, sunny day with calmer waves until the afternoon. Then the wind and waves picked up and we were tossed around a bit. It didn’t help that we had to survey an area called Whirlpool Point that is nicknamed “the washing machine”! Here is an 18 second clip as we entered the washing machine until I had to turn off the camera so I could hold on with both hands. Note that at the beginning, she says she’s stopping logging the data and you’ll see why!

Dana Clark and CTD — Dana Clark getting ready to deploy the CTD

In this top picture you can see me getting ready to lower the CTD (Conductivity, Temperature, and Depth) into the water. After about 5-7 minutes the CTD is raised and then connected to the launch’s onboard computer which uses special software to download the data from the cast. In the picture below you can see Pat Berube showing me how to connect it to the computer. Once we gather this along with the multi-beam sonar data, the day’s work is saved to a hard drive and turned in to the evening processing crew.

Pat Berube showing Dana Clark CTD connection — Pat Berube showing Dana Clark how to connect the CTD for data download

They take the raw data from the launches hard drive, copy it to the ship’s network, and convert it to a format that is readable by the mapping software. They apply correctors like sound velocity from the CTD, tide, and the vessel’s motion data to correct the multi-beam soundings in processing. Let me show you what some of their digital terrain models (DTM) look like. When you have a DTM of the seafloor, it shows the morphology of the seafloor in a range of colors and shows features like rocky areas, sand waves, and seismic faulting. These are statistical representations of all the multi-beam sonar soundings.

Below you will see two examples of the the seafloor generated by Pat Berube, a NOAA hydrographer, that show a 3D base surface. The first one just has the 3D multi-beam base surface. The second one is the same but it also has a chart draped over it. The chart ends up being the final product with the new soundings shown on it. Look at the bottom left model and you will see a reef in the bottom right, a green trench with rocks in it in the middle and at the top yellow area are sand ripples. The large round black spot in the middle is an island and the smaller black circle to the right of it is a small group of rocks. There is also another trench on the left in blue. The colors are added to see the features better. The numbers on the chart on the right are fathoms, which show the depth. Click on each to bring up a larger high resolution picture.

3D model of the seafloor, NW of Aiaktalik Island, Alaska. Photo courtesy of Pat Berube and NOAA

3D model of seafloor with chart overlay, NW of Aiaktalik Island, Alaska. Photo courtesy of Pat Berube and NOAA

In the two pictures below it shows the actual land features of the island that is the black circle in the 3D map above and the rock outcropping that is represented by the small black circle to the right. These pictures show how what we see when surveying transfers to what we see on the charts.

Small island NW of Aiaktalik Island, Alaska

Scientist of the Day

Today I would like you to meet Cathleen Barry, a Cartographer for NOAA who is currently aboard the Fairweather. Cathleen is someone who makes maps, more specifically, navigational charts. And she fell into this field of work in the most unusual way. She was a recent graduate of California State University, Northridge, with a BS in Earth Science. She has loved maps since she was a child, but little did she know then that she would end up drawing maps for a living! Working as a beginning Cartographer in the Marine Geophysics department on campus, her professor tasked her with making a poster to advertise a NOAA expedition to the Arctic.

Cathleen Barry, NOAA Cartographer — Cathleen Barry, NOAA Cartogropher aboard the Fairweather, 2012. Photo courtesy of Cathleen Barry

The Marine Geophysics department was looking for graduate students to participate in a geophysical cruise to the Bering Sea aboard the NOAA Ship Discoverer, a 100 meter oceanographic research vessel. When the poster was complete she drew ten lines on it for sign-ups, and after thinking about it, she decided to put her name on the first line. They needed a cartographer to map during this trip and a career was born!

This career has sure evolved over the years. When Cathleen started out, cartographers drew with pen and ink on drafting paper and now it’s all computer generated. Her job is to use the bathymetric and features data collected to update America’s nautical charts. Earth’s crust is very dynamic and the seafloor changes all the time! When she retires, maybe around 2020, she will say goodbye to a field she has loved for over 30 years.

Personal Log

I have to tell you, typing a blog while my body gently sways from one side to the other is very strange. My abdominal muscles, gluteus maximus, and quadriceps are getting a workout as my muscles tighten to help me to to stay put! I do need the mini workout since the cooks here keep us well fed!

The weather here is so variable. The temperature on my last blog was 21° C and today it was 10° C with cold winds. I was glad I was not out on the launches today and was interested in working with the mapping on the ship until I heard and saw video of what was in the water today. The launches saw a large pod of about 40 orca whales playing about right by their boats! I was so bummed I missed it. Maybe tomorrow?! Then again, tomorrow I will be in a launch that is going to survey a section of the seafloor that has a possible shipwreck in it. Sunken treasure anyone?

Question: Which picture do you like better, the daytime picture of Joe and me on the crest of Cape Kaguyak (note the orange Ambar boat to the left and the white ship Fairweather anchored to the right) or the nighttime picture of the sunset from the flybridge of the Fairweather? You can click on pictures in my blogs to see them full size. Vote in the poll below!

Dana Clark, Cape Kaguyak, Alaska — Dana Clark and ENS Joe Brinkley atop Cape Kaguyak, Alaska

Sunset from the Fairweather — Sunset from the NOAA ship Fairweather, June 28, 2014

June 30, 2014August 21, 2021

Kainoa Higgins: Mantas and Megalopae, June 28, 2014

NOAA Teacher at Sea
Kainoa Higgins
Aboard R/V Ocean Starr
June 18 – July 3, 2014

Mission: Juvenile Rockfish Survey
Geographical Area of Cruise: Northern California Current
Date: Saturday, June 28, 2014

Weather Data from the Bridge: Current Latitude: 45° 59.5’ N Current Longitude: 125° 02.1’ W Air Temperature: 12.7° Celsius Wind Speed: 15 knots Wind Direction: WSW Surface Water Temperature: 15.5 Celsius Weather conditions: Partly cloudy

Find our location in real time HERE!

Science and Technology Log:

Neuston Net and Manta Tow Today, the weather is pleasant but the sea seems more than restless. The show must go on! I step onto the open deck behind the wet lab just as Dr. Curtis Roegner, a fisheries biologist with NOAA, is placing a GoPro onto the end of an extensive net system.

Dungeness Crab – A Pacific Northwest Delight Photo Credit: http://www.smokeybay.com

While Curtis specializes in the biological aspects of oceanography, he is especially interested in the synthesis of the ocean system and how bio aspects relate to other physical and chemical parameters. He joins this cruise on the Ocean Starr as he continues a long-term study of distribution patterns of larval crabs. The species of focus: Cancer magister, the Dungeness crab; a table favorite throughout the Pacific Northwest.

While I have been known to eat my weight in “Dungies”, I realize that I know very little about their complex life cycle. We begin with “baby crabs”, or crab larvae. Once they hatch from their eggs, they quickly join the planktonic community and spend much of their 3-4 month developmental process adrift – at the mercy of the environmental forces that dictate the movement of the water and therefore, govern the journey of these young crustaceans. It has been generally assumed that all planktonic participants float wherever the waters take them. In that context, it makes sense that we have been finding large numbers of larvae miles offshore during our nighttime trawl sorting. Still, not all are swept out to sea. Every year millions make their way back into the shallows as they take their more familiar, benthic form which eventually grows large enough to find its way to a supermarket near you. The question is: How? How do these tiny critters avoid being carried beyond the point of no return? Is it luck? Or is there something in the evolutionary history of the Dungeness crab that has allowed it to adapt to such trying conditions?

Dungeness Crab Megalopae — “Dungie” babies

Curtis tells me about recent research that suggests that seeming “passive” plankton may actually have a lot more control of their fate than previously supposed. By maneuvering vertically throughout the column they can quite dynamically affect their dispersal. Behavioral adaptation may trigger vertical migration events that keep them within a particular region, playing the varied movement of the water to their advantage. Curtis believes the answer to what determines Dungie abundance lies with with the Megalops, the final stage of the larva just prior to true “crab-hood”. By the end of this stage they will have made their way out of the planktonic community and into estuaries of the near shore zone.

Kainoa and Curtis — Dr. Curtis Roegner explains the importance of his study

This continued study is important in predictably marking the success or failure of a year’s class of crab recruitment. That is to say, the more Megalopae that return to a region, the better the promise of a strong catches for the crabbing industry – and a better chance for you and me to harvest a crab or two for our own table!

As Curtis and I discuss his research, he continues preparing his sampling equipment. The instrument looks similar to the plankton nets we use in marine science at SAMI only it’s about ten times longer and its “mouth” is entirely rectangular, unlike the circular nets I am used to using. I’ve heard the terms “manta”, “bongo” and “neuston” being tossed around lab and yet I am unable to discern one from the other. It’s time I got some answers!

Curtis explains that the Megalopae he wants to catch are members of the neuston, the collective term given to the community of organisms that inhabit the most surface layer of the water column. The Neuston net is named simply for its target. It occurs to me that a “plankton net” is a very general term and that they can come in all shapes and sizes. In addition, the mesh of the net can vary drastically in size; the mesh on our nets at school is roughly 80µm, while the mesh of this net is upwards of 300μm (1 µm or micrometre is equivalent to one millionth of a metre).

Manta tow & Neuston net — The manta body design for neuston sampling. A specialized plankton tow.

I’m still confused because I am fairly certain I have heard others refer to the tool by another name. Curtis explains that while any net intended to sample the surface layer of the water column may be referred to as a neuston net, this particular net had a modified body design which deserved a name of its own. The “manta” is a twin winged continuous flow surface tow used to sample the neuston while minimizing the wake disturbance associated with other models. The net does seem to eerily resemble the gaping mouth of a manta ray. These enormous rays glide effortlessly through the water filtering massive volumes of water and ingesting anything substantial found within. On calm days, our metallic imposter mimics such gracefulness. Today however, it rides awkwardly in the chop, jaggedly slicing and funneling the surface layer into its gut. It’s all starting to make sense. Not only is this a plankton net designed to sample plankton, it is also a plankton net designed to sample only the neuston layer of the planktonic community. The modified body sitting on buoyed wings designed to cover a wider yet shallower layer at the top of the water column further specified the instrument; a neuston net towed via manta body design for optimized sampling. Got it.

Collected Plankton Sample — A filtered sample of various crustaceans collected from the neuston

After the tow is complete, Curtis dumps the cod end of the net into a sieve, showing me an array of critters including more than a dozen Megalopae! Two samples are frozen to ensure analysis back at the Hammond Lab in Astoria. There, Curtis will examine the developmental progress of the Megalopae in relation to the suite of data provided by the CTD at each testing site. This information, along with various other chemical and physical data will be cross-examined in hopes of finding correlation – and perhaps even causation – that make sense of the Dungeness crabs’ biological and developmental process.

Analysing CTD Data — Dr. Curtis Roegner looks for patterns relating crab Megalopae and CTD data

The CTD

The CTD measures conductivity, temperature and depth among other auxiliary measurements

Fundamentally, a CTD is an oceanographic instrument intended to provide data on the conductivity, temperature and depth of a given body of water. The CTD is one of the most common and essential tools on board a research ship. Whether it’s Jason exploring benthic communities, Sam hunting jellies, or Curtis collecting crab larvae, all can benefit from the information the CTD kit and its ensemble of auxiliary components can provide about the quality of the water at a given test site. In general, the more information we collect with the CTD the better our ability to map various chemical and physical parameters throughout the ocean. Check out the TAScast below as I give a basic overview of and take a dive with the CTD and its accessories.

Personal Log:

Just when I thought I was beginning to get the hang of it…. Hold on, I have to lie down. As I mentioned above, the seas have been a bit rougher and I’ve been going through a phase of not-feeling-so-hot for the first time this trip. It’s odd because we hit some rougher ocean right out of Eureka and it didn’t seem to faze me much. I stopped taking my motion sickness medicine a few days in, and though I’ve picked it back up just in case, I’m not entirely convinced it’s the only contributing factor. I think it has more to do with my transition onto the night shift and all the plankton sorting which requires lots of focus on tiny animals. The night before last was particularly challenging. In the lab, all of the papers, books and anything else not anchored down slid back and forth and my body felt as if it were on a giant swing set and seesaw all at once. In addition, each time I looked out the back door all I could see was water sloshing onto the deck through the very drainage holes through which it was intended to escape. I remember wondering why there were so many rolls of duct tape strapped to the table and why chairs were left on their side when not in use. Well, now I know. Earlier today we made a quick pit stop in Newport, Oregon – home of the Hatfield Marine Science Center as well as NOAA’s Marine Operations Center of the Pacific. In short, this is where NOAA’s Pacific fleet of vessels is housed and the home base to several members of my science team, including Chief Scientist, Ric Brodeur.

The NOAA Pacific Fleet — The NOAA Pacific fleet at rest in Newport, OR.

I remember the anticipation of seeing the R/V Ocean Starr, a former NOAA vessel, for the first time. Growing up in Hawai’i, I remember these enormous ships making cameo appearances offshore, complete with a satellite dome over the bridge, only imagining the importance of the work done aboard. Now here I was, walking amongst the giants I idolized as a kid – the difference being that my view was up close and personal from behind the guard gate, a member of their team. I’m totally psyched even though I attempt to pretend like I’ve been there before. As much as I could have spent all afternoon admiring, I needed to make the most of our two hour layover in the library uploading blog material. Unfortunately the satellite-based internet is incredibly finicky out at sea. It’s a first world problem and understandably a part of life at sea, I realize, but all the same, I apologize to all those anticipating regular updates. I continue to do the best I can. I can say, however, that the Hatfield Marine Science Center boasts a fantastic library. I look forward to exploring the rest of the facility upon my final return in a little over a week. ‘Till then, BACK TO SEA!

June 28, 2014August 21, 2021

Dana Clark: Alaska’s Rocky Seafloor, June 26, 2014

NOAA Teacher at Sea

Dana Clark

Onboard NOAA Ship Fairweather

June 23 – July 3, 2014

Mission: Hydrographic Survey

Geographical area of cruise: South Coast of Kodiak Island

Date: June 26, 2014

Weather Data: Latitude – 56° 45.40′ N, Longitude – 154° 9.99 W, Sky Condition – 7/8 clouds, Present Weather – clear, Visibility – 10 nautical miles, Wind – 3 knots, Temperature – 14° C

Science and Technology Log

Dana Clark on the fantail of the Fairweather

Each morning there is a meeting of the launch crew on the fantail, which is aft, which means the back deck of the boat. You need to wear your hard hat and your PFD which stands for Personal Flotation Device. It is really great that the life-jacket is embedded into the jacket. Wednesday I went out on a launch, a 28 foot boat, and attempted to collect hydrographic data. However, the weather did not cooperate. We were tossed around by winds of 30 knots, which is approximately 34.5 mph, and 5 foot swells and waves. I found out that swells are large scale rollers of water and waves are choppy. Swells have more amplitude, a lot of energy, are larger, and are driven by far off (can be thousands of nautical miles away) weather storms or very high or low pressure systems. Waves are surface wind driven, choppy, smaller, and have more pitch. You can have either one by itself or you can have both together, either going the same direction or cross-ways. Well, we had both swells and waves from different directions at the same time! The waves had whitecaps and the swells were just big! I couldn’t even get out my camera to take a picture because I was holding on to the rail in the cabin with both hands, trying not to fall or get in the way of the scientists as we pitched about. And, can you believe, no seasickness! We were called back to the ship after the current we measured registered at 5 to 5.5 knots, much too fast for us to put our CTD (Conductivity, Temperature, and Depth) into the water. The professionals aboard the Fairweather put a premium on safety and knew it was time to call an inclement weather day and have the launches return. By the way, the picture at the left was taken on another day. How quickly the weather can change!

Mark Bradley NOAA Fairweather — Mark Bradley using multi-beam sonar 3D imaging to confirm uncharted rock in navigational waters

Today, it was wisely decided that I would be exposed to the science on the ship while the launches went out and the weather system finished passing through. I was able to learn from Mark Bradley who is a hydrographic survey technician. Some days he goes on the launches and uses the multi-beam echo sounder to map sections of the seafloor. Other times he works on the ship processing the data that has been collected and preparing the descriptive report. Today he was comparing old charts to the new survey soundings that a launch had previously recorded while they were picking up holidays during a low tide. Remember, holidays are where there are gaps in the data. While resurveying this holiday they saw a rock sticking out of the water so they came back later in the day during high tide and used the multi-beam sonar to get a depth measurement for the top of it. Mark then took this data and compared it to the old charts. The old charts didn’t even have this rock recorded! He used his 3D imaging and measured the rock at 83 meters wide and 30 meters tall. It was huge! At low tide, it stuck a meter out of the water. This rock was in navigational water and easily could have damaged or sunk a boat. Mark confirmed another nearby rock was 3 feet under the surface so if you were in a boat you wouldn’t see it. This second rock was a known rock; however, on the old chart it was at 42 feet below the surface, not 3 feet! So there is a great need to update our navigational charts since the old ones can be over 100 years old. Eventually, this chart he’s updating will be revised and published by NOAA Charting Division.

Kristin Golmon NOAA Fairweather — Kristin Golmon on the bridge of the Fairweather

Scientist of the Day

Today I would like you to meet Kristin Golmon, a Junior Officer for NOAA who is currently aboard the Fairweather. This Texan is a woman who is in charge! She is an ODD which stands for Officer of the Deck. Because the CO, the Commanding Officer cannot be on the bridge (the space that you command the ship from) all the time, an OOD directs the bridge when he is below, and is the direct representative of the CO. She drives the ship, does survey work, does administrative duties and currently she’s also working towards her coxswain qualification. Today she is in charge of the bridge, working on charts, communicating with the hydrographic survey launches, and recording the weather. Kristin has always been curious about how stuff works. In elementary school she invented a t-shirt folding machine out of cardboard. You would put a t-shirt on it and it would fold the shirt and you would pull the cardboard out! She always did well in math and science and had her parents, a geologist mom and a mathematician dad, as her role models. She attended Trinity University in San Antonio, Texas and earned a BS in Engineering Science, a minor in Mathematics and another minor in Environmental Studies. She was a senior in college when she heard about NOAA Corps and liked their science mission. She also liked the idea of serving her country in a uniformed service.

Casey Marwine polar bear — Polar bear mom and her two cubs, Artic Ocean, 2012.
Photo courtesy of Casey Marwine.

Being a woman in charge has its challenges when working in a male dominated field but she has the respect of her peers and the CO. Currently, the head of NOAA is Dr. Kathryn Sullivan, a geologist and an astronaut who was the first American woman to walk in space. When asked what she liked best about her job, Kristin said that it’s a pretty cool experience being in charge of a ship, especially when going through narrow passages that take a lot of planning like the Inside Passage in Alaska. She also loved seeing polar bears, a mom and two cubs, while doing the Arctic Reconnaissance Survey!

Personal Log

Dana Clark Fairweather room — Dana Clark working in her stateroom on the Fairweather

Check out where I live on the ship. This is my room, or as we call it aboard ship, my stateroom. Notice the hard hat and survival suit above the bed and the life jacket above the television! I also have a desk that folds up when I don’t need it. It was a treat to have my own room. The shower and the head (what they call the bathroom) is across from my room. Also on the ceiling of the hallway outside my bedroom is an escape hatch! Then in the floor above is another hatch. This way I can safely get up to the upper decks if my hallway gets blocked or flooded.

Dana Clark Escape Hatch — Escape hatch in the hallway ceiling on the Fairweather

Question (or Answers): Today’s question will actually be answers! And speaking of polar bears, remember my question from my first blog when I asked you the question of what were the odds that I would see a polar bear? Well, the answer is none. The polar bears are much farther north and are found in the Artic region of Alaska, Canada, Greenland, and Russia. Unfortunately, I will not be seeing any polar bears. My poll last blog asked you to identify a picture as plant or animal. Many of you voted and it was a pretty split vote between the two! The picture is of bull kelp, a plant, and its scientific name is nereocystis. It can grow huge and I have seen some big ones here in Alaskan waters.

I will leave you with this shot of beautiful Kodiak, Alaska that I took from the ship. This is where we are anchored this week.

June 26, 2014August 21, 2021

Carol Schnaiter, Home Again! June 25, 2014

NOAA Teacher at Sea

Carol Schnaiter

Aboard NOAA Ship Oregon II

June 7 – 21, 2014

Mission: I am back home in Amboy, IL, now so my mission is getting back to a “normal” schedule and getting my land legs back!

Weather: Partly sunny, 82 degrees

Date: June 25, 2014

Science and Technology:

Hypoxia or low oxygen levels in the water is my final topic. The “dead zone” may seem like it does not relate to me being home, but in reality it really does.

This “dead zone” is affected by many things such as the oceanographic conditions, but a major cause is excessive nutrient pollution from agriculture and waste water. Being from a rural agricultural area I wonder how much of what we are doing here in the north affects the ocean waters far away?

So how does this all start? The nitrogen and phosphorus that flows into the water fuels the growth of algae, later when the algae dies and decays, it sinks to the bottom. At the bottom the bacteria will devour the dissolved oxygen from the water. With little or no oxygen the organisms living there must either move, if they can, or they will die.

Where does this nitrogen and phosphorus come from? Most of this can be found in fertilizers from agriculture, golf courses and suburban lawns, discharges from sewage treatment plants, and even from erosion of soil full of nutrients. Since past spring was very rainy and there were floods near the Mississippi River much of this was taken from the soil into the water. The flood waters then drained back into the river and into the gulf carrying many of these nutrients.

How do we know this is happening and that it is getting worse? On the NOAA Ship Oregon II and other ships there are daily checks of the water oxygen levels. Tests similar to these have been conducted for many years. The results are compared and they show that changes in the oxygen levels are happening and not for the better.

While on the ship the scientist performed these tests using the CTD. Water taken from the CTD is handled very carefully so no oxygen is added by accident. As chemicals are added, you can see the changes where the oxygen in the water bonds to the chemicals. The results of these tests are compared to the results collected by the computer. Having both tests generate similar results show more proof of the oxygen levels.

I noticed that when the ship was closer to land, the oxygen levels would be lower and Lead Scientist Kim Johnson said as the ship traveled closer to the mouth of the Mississippi River, the levels would drop even more. (I plan on watching the results as they are posted.)

Can anything be done to stop this? Some scientist say one of the solutions would be to use fewer fertilizers another would be to maybe watch when the chemicals were added, so there would be less runoff.

Of course checking septic systems and sewage treatment plants to be sure they are up to code and working correctly would help. These solutions sound simple, but maybe people do not even realize what happens up north and how it really does affect what is going on at the bottom of the ocean.

Maybe our Amboy Marsh is the beginning, a place where the water can be filtered.

Here is a map showing the levels of oxygen in the water.

http://noaateacheratsea.blog/wp-content/uploads/2014/06/20140625_051938-1.jpg

Personal Log:

I have been home now for four days. My land legs are back and I only feel dizzy when closing my eyes while washing my hair in the shower. I want to thank everyone for reading my blogs, I hope you enjoyed my adventure and learned something new.

As I look through my pictures, memories of the sixteen days I spent at sea flood my mind. I look at the safety precautions that were taken to make sure everyone on the ship stayed safe. The drills, the posting of where everyone was to go and what they were suppose to do in case of an emergency, and the sign stating how many days the ship had gone without a problem. I always felt safe, everyone was very careful and followed rules to ensure the safety of everyone….just like we do at school!

Accident free days — 525 Days without an accident!

Ship's emergency bullets — Emergency bullets

I also think about how what seemed like a tiny space became my home away from home. Everything you need to survive on a mere 178 ft ship! Two showers for everyone to share, three heads (toilets) and one washing machine and one dryer. I thought it would be impossible, but it just proved my husband’s theory that we have too much in our home!

Shower room — Two showers to share with everyone!

I want to tell you how thankful I am that NOAA has this wonderful program and allowed me to participate. I know many teachers applied for this and I am honored that I was selected. Thank you to the scientists aboard the ship: Kim, for EVERYTHING, the Night Shift: Taniya, Andre, Lee, Chrissy, and Rebeca for all of their guidance and help.

The deck crew: Chris, Chuck and Mike-thanks for your support and for making the night go by so quickly! Master Dave Nelson and ALL the members of his crew for their help in explaining everything and the tours on the ship!

This survey opened my eyes to what is happening under the water and how fragile life in the deep blue sea really is. It confirmed my thinking that we (the human race) need to look closely at what we are doing everyday and how it affects others. I plan on following the NOAA Ship Oregon II during the rest of the summer groundfish survey and during the fall groundfish survey. I want to see how the oxygen level changes, how the data collected affects the shrimp season, and follow the members of the ship!

Day One — Our first day together! (Photo by Karen Mitchell)

I cannot wait to share with my students and with anyone that will listen! Would I do this again? YES, I would go back to sea in a minute if I had the chance!