2015 – Page 32 – NOAA Teacher at Sea Blog

March 20, 2015August 21, 2021

Julia West: It’s the Small Things in Life… March 20, 2015

NOAA Teacher at Sea
Julia West
Aboard NOAA ship Gordon Gunter
March 17 – April 2, 2015

Mission: Winter Plankton Survey
Geographic area of cruise: Gulf of Mexico
Date: March 20, 2015

Weather Data from the Bridge, 0800, 3/20/15
Temperature: 25.5°C (78°F)
Wind direction: 90° (E)
Wind speed: 6 knots
Sky condition: cumulus (cu), 15% cloud cover

First:

Sunrise, Gulf of Mexico — Sunrise on our first morning at sea – a nice way to start a new adventure!

I’m really excited to see everyone commenting and asking questions, and I hope I do a good job answering them. If you don’t get your answer right away, remember that I am learning too! I will be answering lots of them in the blog posts, and others in the comments, and hopefully I’ll get to most or all of them! The internet out here is marginal at best, so when the satellite connection is good, I try to run with it. That’s why there might be gaps in our communication.

Science and Technology Log

If you haven’t guessed by now, there are several methods of sampling plankton. Each one is used several times a day, when we get to one of the sampling stations. Since the whole point of these research cruises are… well… doing research, it is fascinating to see the communication between the scientists and the NOAA Corps crew who run the ship. At the beginning of the cruise, Pam, the FPC (Field Party Chief, or chief scientist), discussed the stations we need to get to with LT Marc Weekley, the operations officer (OPS), and ENS Dave Wang, the navigations officer (NAV). Together they made a plan. Some of the decision is based on weather; for example, in the first leg of the cruise, which ended just before I got here, there was bad weather coming in, so they decided to work south, to skirt most of the weather coming from the northwest, and then work back northward. Here is a map of the entire sampling area:

These are the winter plankton sampling stations. Most of the stations to the east of Pascagoula were covered in the previous leg of the research cruise. The dots are about 30 miles apart. The light solid lines show the edge of the continental shelf and the dotted line is the edge of U.S. waters. Credit: Pamela Bond/NOAA

On our leg, we are doing a little zigzagging south, and then will be zigzagging west all the way toward Texas. There is constant communication between the officers on the bridge, the scientists in the lab, and the deck crew, especially as we get toward the sampling station. There is a navigation chart on the monitor on the bridge, and a video feed of the chart to the lab and every TV monitor on the ship, so everyone knows exactly where we are and how close we are to the next station. There are also closed circuit video cameras in various places around the boat that can be viewed on the lab and bridge monitors. The scientists and crew can see everything that is going on as equipment gets deployed over the side. The bridge has to give the OK for anything to be deployed or recovered, even a plankton net.

Our plankton sampling stations — These are the stations we are sampling. The X’s are stations we have completed as of early on 3/20, and the lines that connect the dots are how we have traveled.

There’s also a camera on the bow of the boat, looking down at the water. With that camera you can sometimes see dolphins “bow surfing.” The bow of the boat pushes a wave ahead of it, something you’ve probably seen if you’ve been in any boat with a motor. Imagine a permanent, amazing surfing wave – one that you can ride for miles! If you fall off the wave, just a few tail strokes and you’re back on it. That’s life as a dolphin!

OK, now back to plankton:

Today I want to introduce CUFES, or “Continuous Underwater Fish Egg Sampler.” This unit is pumping in seawater continuously, agitating it to funnel any plankton and fish eggs into the collecting device. This device was first used on the west coast, where the fish eggs are larger. Here in the Gulf, eggs are very, very small, and not the priority, so the CUFES is used to collect whatever plankton are pulled into it. The intake is 3 meters below the surface.

The water is agitated, and then funneled into a sieve. The water is piped right back into the ocean, and the plankton collect on the sieve. Every 30 minutes (yes, they have a timer), the sieve is removed, and the sample is rinsed and transferred to a small bottle. The bottle is filled with ethanol as a preservative. This sampling method provides a continuous record of plankton, in contrast to the isolated stations that are used for the rest of the sampling, which are about 30 miles apart. In addition, the ship has another device that continuously records temperature and salinity. This unit is called the……..wait for it……. thermosalinograph! Every 30 minutes, when the CUFES sample is taken, the minimum, maximum, and average temperature and salinity for that half hour gets imported right into the CUFES “event” (the computer data sheet). Also recorded are the start and end positions of the ship, as well as the water depth. There is no shortage of data, and this is just one of the plankton sampling methods!

CUFES sieve — The water then gets funneled into this sieve, where the plankton collect.

Chrissy and the CUFES — Here is Chrissy in the “wet lab,” ready to stop the water flow to the sieve, so she can collect the sample.

Andy and CUFES — Andy is collecting the sample, picking any stragglers from the sieve with tweezers.

Personal Log

Now that I’ve been on the ship for 3 days, life is falling into a routine. The scientists work 12 hour shifts – noon to midnight, and midnight to noon. There are two scientists on each shift, and Pam works long days overseeing both shifts. Chrissy, pictured above, is one of the midnight-noon workers. I wasn’t required to stand a particular shift; I float between both shifts as well, so I can work with everyone and get to know them all. Also, this way I don’t have to ask the same questions over and over again to the same people – I can spread out my repetition and drive them all less crazy! I’m kidding, because they are all incredibly patient. One thing about scientists is that they invite questions. Science is all about questions. And you can bet I’ve asked a few that had them scratching their head a bit, but we always find the answers!

More about the ship – you can find out a lot on the Gordon Gunter’s web page. That’s where I go to find out when meal times are! The ship is 224′ long. My stateroom is on the port side of the 01 deck (the first deck with windows that you can walk around, if you’re looking at the picture), toward the forward end. Above that is the 02 deck, which has a smaller interior. The 02 deck is where the life rafts are kept. Above that is the bridge deck, smaller still, but fun to be up there at the control center of the ship’s world! And the very top is the fly bridge – a cool place to hang out and see far and wide. Below the 01 deck is the main deck (also known as 1 deck), where the galley (mess deck) and lounges are. Below that is the 2 deck, where the engine and generators are, as well as the laundry room and a gym. This is the heart of the ship.

Johns on the bridge — ENS Kristin Johns at the controls on the bridge

One last picture (next time I’ll have more pics) – we had our first fire and abandon ship drills. These are extremely important, and everyone takes them seriously. I forgot to bring my camera to the fire drill, but I’ll try to remember next time. I had to put on my “gumby” suit, which is the survival suit we all need if we have to abandon ship. It’s an incredibly thick neoprene dry suit, and I felt rather silly in it, but it’s serious business! Cute, don’t you think?

Did You Know?

In the Gulf of Mexico, the continental shelf extends about 60-100 miles from shore. The average depth of the Gulf is 1615 meters, with a maximum of about 4000 meters.

Challenge yourself: Where is the “Sigsbee Deep?” Are we going there?

New Term for the Day

Thalassophilia – love of the sea!

March 19, 2015August 21, 2021

Theresa Paulsen: Intriguing Deployments, March 19, 2015

NOAA Teacher at Sea
Theresa Paulsen
Aboard NOAA Ship Okeanos Explorer
March 16-April 3rd

Mission: Caribbean Exploration (Mapping)
Geographical Area of Cruise: Puerto Rico Trench
Date: March 19, 2015

Weather Data from the Bridge: Partly Cloudy, 26.7˚C, waves 1-3ft, swells 2-4ft.

Science and Technology Log:

This morning at breakfast Commanding Officer Mark Wetzler, or CO, explained that we would be deploying instruments today. The first one was a glider for the Navy. The Slocum electric glider is like a tiny, unmanned submarine built like a non-explosive torpedo with small wings. It has the ability to be remote-controlled for weeks to months at sea operating 24 hours a day even in the worst weather. They can be programmed to travel back and forth, dive, and rise periodically to communicate data back to the mainland and accept new missions. These autonomous underwater vehicles (AUVs) can collect many different types of data such as temperature, conductivity, or audio recordings, depending on the sensors attached. Gliders like this one can help detect tsunamis or other changes in the ocean.

Our vessel also records data 24 hours a day but is limited in its duration at sea by the needs of the people and fuel onboard. Have you wondered how we can stay out at sea for nearly 3 weeks at a time without hitting the grocery store or service station? I’ll explain more about that in a future blog.

Deploying the Navy Glider — Navy Glider Deployment

The next deployment was a test run of a “free vehicle.” Dr. Wilford “Bill” Schmidt, and his assistants, Rolf-Martin Vieten and Zamara Fuentes from the University of Puerto Rico, Mayguez (UPRM) are testing the design of vehicles that can be deployed from a vessel like the Okeanos Explorer or a smaller ship. These vehicles are inexpensive to make, easy to deploy, and do not need to be tethered to the ship. They can be programmed to dive to the deepest parts of the ocean, or whatever depth desired, in order to take samples or record data. Once the vehicle has completed data collection or sampling, it releases its anchor and rises the surface where it is retrieved. Meanwhile the deployment vessel can continue other operations such as mapping. Time is not wasted on a research vessel! On this cruise they will use the device to sample the conductivity, temperature and depth of the water column. This will help them learn more about the interaction between different water masses in the Puerto Rico Trench.

Bill's Team — Wilford “Bill” Schmidt, Zamara Fuentes, and Rolf-Martin Vieten with the Free Vehicle

Water masses in the trench are of particular interest to Bill, a professor of physical oceanography, because they could hold a key to understanding the flow of different ocean currents. He explained that water masses form at the surface at a particular temperature and with a certain salinity corresponding to the surface conditions at the time. Temperature and salinity are conservative properties, meaning they don’t change as the water mass moves. So as a water mass formed in Antarctica sinks and moves toward the deepest parts of the ocean due to its density, its cold temperature and salinity don’t vary significantly. So temperature and salinity can serve as fingerprints of water masses. Therefore as he measures these factors through the entire water column in the trench, we would expect to see the values change as we move from the North Atlantic Deep Water to the Antarctic Bottom Water. The image below shows a generalized representation of the typical flow pattern of large water masses.

Ocean Circulation — The ocean circulation system. Image courtesy of NASA.

Bill’s work is supported by NOAA and the National Science Foundation. The NOAA Office of Exploration and Research recently provided him with an award to produce 5 free vehicles with his university team. The fact that Bill’s vehicles are able to travel untethered into the hadal zone at a very low cost makes them uniquely valuable to researchers. Data from the hadal zone is virtually non-existant because only enormous vessels would be able to support winches that could handle the 10,000+ meters of cable that would be required for the tethered vehicles currently used. Since the average depth of the ocean is only 4000m, there is not a large enough demand to make manufacturing such large winches economically feasible.

Also, Bill’s free vehicles are small and can be deployed on very short notice, allowing them to capture data as major events occur. The vehicles can carry interchangeable payloads that could be used in all scientific disciplines. A biologist could request water or bottom substrate samples to examine life forms in the hadal zone that may not exist elsewhere. A geologist might also like to sample the bottom substrate or might wish to record seismic activity at the bottom of the trench to better understand plate interactions. A chemist interested in oceanography could examine the water for trace elements or compounds that were emitted into the air at one point in time, such as chloroflourocarbons (CFCs) that were once used but are now illegal in the US due to their impact on the ozone layer, or tritium (H-3) remnants from nuclear bombs used in WWII. This could provide us with an estimate of how long ago the water mass was at the surface and help us determine the rate of flow into the trench. The research possibilities are endless.

FV Test — The first free vehicle test of the voyage

Initial tests looked good. During our 19 day voyage, Bill’s team and the crew will deploy the vehicle up to 11 more times with up to 6 locations strategically placed in the Puerto Rico Trench.

Personal Log:

Are you interested to know what the accommodations are like aboard the Okeanos? They are comfortable enough for a work boat. Take a look for yourself!

I love the curtain around my bottom bunk. It reminds me of the forts my brothers and sisters and I built as kids. I have slept like a baby ever since arriving. The rocking of the boat is very calming.

There are a couple of nice spots to relax and chat, and write in my blog. Here are the library and the lounge.

I am surprised that I really haven’t been seasick. Motion sickness medication really helps. If you really get sick, there is a medical officer on board and sick bay.

I showed you the galley in the last post. We eat in the Mess Hall. The Chief Steward puts tennis balls on the bottom of the chairs to avoid scratching the finish on the floor. Good thinking!

And when I have eaten too much, there is the fitness room! There is a scale in the fitness room, but when you stand on it, the action of the boat rocking causes the scale to oscillate by 30-40 pounds. It is a great demonstration of the difference between mass and weight!

The best place to hang out is outside, of course, where you can possibly see a spouting whale or swimming dolphin. I have seen both on this trip already but I need to be quicker with the camera! Maybe next time!!

View from the bow — The view from the bow of the ship

Question of the Day:

March 18, 2015March 12, 2021

Sarah Raskin: Teacher at Sea Day 6, March 18, 2015

NOAA Teacher at Sea

Sarah Raskin

Aboard NOAA Ship Bell M. Shimada

March 13-18, 2015

Mission: Channel Islands Deep-Sea Coral Study

Geographic Area: Channel Islands, California

Date: March 18, 2015

Day 6: 3/18/15

7th and 8th grade students from Haydock Academy of Arts and Sciences in Oxnard, California, along with elementary students from South Carolina, decorated Styrofoam cups that Peter and I took with us on the Shimada. We brought these cups to show our students the amazing power of underwater pressure. The depths at which the ROV and CTD Niskin Rosette traveled during the voyage were much further than a human body could physically handle without being in some sort of pressurized submersible. Human bodies currently experience air pressure when we are at sea level, though we don’t feel the pressure because the fluids in our bodies are pressing outwards with the equal amount of force. However, once you start traveling underwater, the greater the pressure of the water pushing down on your being. As one NOAA website states: “For every 33 feet (10.06 meters) you go down, the pressure increases by 14.5 psi. In the deepest ocean, the pressure is equivalent to the weight of an elephant balanced on a postage stamp, or the equivalent of one person trying to support 50 jumbo jets!” (http://oceanservice.noaa.gov/facts/pressure.html)

cups on CTD rosette — Peter and I with the students’ cups tied to the CTD Niskin Rosette

To illustrate how powerful the water pressure is in the deep ocean, Peter and I used Styrofoam cups to demonstrate this concept. First, we stuffed paper towels into the cups so that they would retain their shapes during a dive down to the bottom of the ocean floor. Next, we attached the cups to the CTD Niskin rosette. The crew launched the CTD into the ocean and it plunged downwards to a depth of 550 meters. As the cups descended deeper and deeper, the increasing water pressure compressed the air out from between the Styrofoam beads that make up the cup. What was left was a significantly shrunken version of our cups. Here are the before and after pictures:

cups before dive — The cups before the dive

More cups post-dive — The cups post-dive

The CTD Niskin rosette also collected data as it traveled downwards. Water filtered through the machine and sensors gathered information about temperature, salinity, chlorophyll, and dissolved oxygen levels. The tubes on the CTD could also be programmed to collect water samples at certain depths, which they did on the return trip to the surface. This allowed the scientists to collect the water to test for different water quality factors at a later date.

rosette and cups ready to go — The cups and CTD Niskin Rosette prepare to go overboard

reviewing the data — Peter and ST Gunter review the data that is being uploaded from CTD Niskin Rosette during its dive.

Media Day

Today, the scientists and Shimada team were joined by media crews from the LA times and the Santa Barbara Independent, along with some of NOAA’s education outreach specialists. The reporters took a tour around the Shimada and they interviewed the scientists about their important work. From Peter Etnoyer, and his team’s work on Lophelia and ocean acidification, Branwen Williams’ research on deep-sea coral, Laura Kracker and team’s mapping of uncharted Sanctuary regions, to the MARE team’s innovative ROV technology, the media had quite a bit to report about!

The reporters were even able to watch the ROV take its final dive of the trip to collect one last acanthogoria sample. One of Branwen’s and Peter’s goals is to be able to determine the ages of these beautiful organisms through the work they do. If they are able to create baseline data for how old an acanthogoria is, based on size and height, then there will be less of a need to collect these specimens in the future. Instead, they will be able to determine age based on looking at the footage during an ROV dive and using the laser measurements on the ROV camera to decide how old the coral is.

Chris Caldow, NOAA research coordinator and organizer of our expedition, speaks with the media.

media watching dive — The media crew watches the ROV’s final dive of the trip

Acanthagoria sample — Gathering around the Acanthogoria sample

Until next time….

My journey on the Shimada finally came to a close today. NOAA sent out their local research vessel, the Shearwater, to meet us in the waters off Santa Cruz Island. Many of the scientists, along with the MARE team and myself boarded the Shearwater and watched as the Shimada became smaller and smaller in the distance. It was very sad to say goodbye, but Chris Caldow and the sonar team will continue on the Shimada with their important mapping of the Sanctuary for the next several days.

Shearwater approach — The *Shearwater* makes its approach to bring us back to shore

Our Backyard

Being able to explore the seldom-visited parts of our sanctuary with the scientists and NOAA crew was a once in a lifetime experience. The research these scientists are doing to uncover the hidden depths of the sanctuary is also helping to illustrate how our actions on land have a direct impact on our oceans.

When we learn more about these rarely seen regions of our Sanctuary and about the deep-sea organisms that make their home there, these places and creatures become something that we grow to love and care about. This exploratory research is so important, because as someone on the trip said; “we cannot protect what we don’t know is there.” This is especially relevant for myself and the students from Haydock, because the Channel Islands truly are our backyard; we can see the Islands and Sanctuary from the shores of our city of Oxnard. When we feel a greater connection to a place such as the Channel Islands National Marine Sanctuary, we are more likely to take part in the stewardship and protection of it for our future generations.

“Treat the earth well: it was not given to you by your parents, it was loaned to you by your children. We do not inherit the Earth from our Ancestors, we borrow it from our Children” (unknown)

To learn more about the Channel Islands National Marine Sanctuary, click on the following link:

http://channelislands.noaa.gov/welcome.html

To learn more about MARE and the ROVs check out their website: http://www.maregroup.org/

For more information about Peter Etnoyer’s work, click the following link:

http://oceanexplorer.noaa.gov/edu/oceanage/03etnoyer/welcome.html

For more information about Branwen Williams work, use the following link:

https://sites.google.com/site/branwenw/home

sunset in Channel Islands NMS — Sunset in the Channel Islands National Marine Sanctuary

March 18, 2015August 21, 2021

Julia West: In Port in Pascagoula, MS, March 17, 2015

NOAA Teacher at Sea
Julia West
Aboard NOAA ship Gordon Gunter
March 17 – April 2, 2015

Mission: Winter Plankton Survey
Geographic area of cruise: Gulf of Mexico
Date: March 17, 2015

Personal Log

I made it! A smooth flight down to Mississippi (which is a new state for me – I’ve never been here). I arrived to sunshine and warm temperatures – OK, downright hot to me, but I’ll get used to it quickly I’m sure. Pamela Bond, the chief scientist on this cruise, met me at the airport and brought me out to the Gordon Gunter. I quickly learned that it is not only Pam who is super nice and welcoming, but the entire crew. I’ll be introducing them more in future posts.

The ship is not at the usual port near the NOAA lab, but at the former naval station, on an island at the mouth of the Pascagoula River. This yard has multiple uses now, as you can see from the pictures below. So not only is the Gunter here, but it has the company of a Coast Guard vessel, and both are dwarfed by a massive oil rig. On the other side of the pier (not pictured) is a USGS vessel and others. There’s a lot going on here!

Gunter, CG vessel, and oil rig — The Gordon Gunter (right) and Coast Guard vessel dwarfed by the huge Sovereign Explorer (oil rig), an old rig that has been docked here for about a year, waiting for bids to take it apart for scrap .

Across the way is Pascagoula’s largest employer, and Mississippi’s largest manufacturing employer, Ingalls Shipbuilding, with 11,000 employees right here in Pascagoula! I can see ships in various stages of construction.

Ingalls 1 — Ingalls shipyard, 1-4 from left to right

Ingalls 4 — That’s a lot of ship building!

I have learned a lot about this area in the one day here at port. Two major events have happened here in recent years – Hurricane Katrina (2005) and the BP oil spill (2010). Both events simply ravaged this area. Everywhere we have been in the last day – the naval station, the NOAA lab, the highway – was under several feet of water during Katrina. You’ve seen the pictures. To hear about it from the folks here is profound. The BP oil spill (also known as Deepwater Horizon oil spill), another devastating event, changed the whole NOAA season (as it did for the fishermen and just about everyone else here). All the NOAA ships on the east coast, and one from the west coast, had to cancel their season’s research and congregate down here to be involved as needed, looking for oil, looking for marine mammals, etc. Today we visited the NOAA lab, where several employees are analyzing plankton samples taken from the affected waters. This is five years later, and still very relevant and ongoing data collection! (sorry, forgot to bring my camera to the lab, but I got to check out lots of plankton under the microscope).

Backing up now, to my arrival: Pam showed me to my room – I’m surprised that I have my own room! It has a refrigerator, closet, desk, comfy chair, my very own sink, and a shared bathroom with the room next door. And it has a TV – I barely know how to use a TV!

And then Tony, the ET (electronics technician) gave me a tour of the boat. Since then, I have been wandering around, sometimes in circles, trying to figure out the layout. I can tell right away that the food is going to be amazing.

My head is already spinning with some of the details about the equipment and technology. Pam was not sure if we would be launching on time – everything has to be just perfect for a research cruise to start, and if there are any issues, we don’t go. There were two repairs that needed to be made since the ship came to port just two days ago: one had to do with the unit that makes our water, by distilling seawater (very important!), and the other had to do with a malfunctioning gyro, or gyrocompass, needed for navigation (also important!). I wanted to know more about how a gyrocompass works, so I first looked it up on Wikipedia, and then talked to Dave Wang, the NAV (navigations officer). It’s so fascinating – a compass that points true north partly by using the rotation of the Earth. The good news is that both of the repairs are done and we will be launching on time!

I just want to share one bit info about a simple piece of equipment on the aft deck. It’s a water tank. I asked Tony what it’s for, when we have the technology to make fresh water. Well, after the oil spill, getting fresh water was a problem, so the tank was added. It was decided that it was convenient to have after it was no longer needed, and is now used for things that need a freshwater wash.

I am wrapping up this blog post now, a day after I started it. I’ve had my safety and ship protocol briefing, and we are underway. We’ve passed the barrier islands, and the ship is starting to rock a bit. Here we go! We have another 5 hours or so to go to get to our first sampling station, so the science work will start tonight. One final photo – to get out of the tight spot we were docked in, a tugboat was necessary:

Tugboat — The tug getting ready to help us leave the dock. At first it held the stern of the ship in place while our bow thrusters pivoted the front, and then it pulled us out.

Word of the Day (time to start learning the terminology):

Neuston – the organisms that are found on the very top of the water, in the surface film. Contrast that with plankton, which can be said to be found within the water, not always right at the surface.

March 17, 2015August 21, 2021

Theresa Paulsen: And We’re Off! March 17, 2015

NOAA Teacher at Sea
Theresa Paulsen
Aboard NOAA Ship Okeanos Explorer
March 16 – April 3, 2015

Mission: Caribbean Exploration (Mapping)
Geographical Area of Cruise: Puerto Rico Trench
Date: March 17, 2015

Weather Data from the Bridge: Partly Cloudy, 26 C, Wind speed 12 knots, Wave height 1-2ft, Swells 2-4ft.

Science and Technology Log

Elizabeth “Meme” Lobecker, Physical Scientist Hydrographer with the NOAA Office of Ocean Exploration and Research and our Expedition Coordinator, gave the science team aboard the vessel an overview of our expedition on Sunday after an evening of becoming acquainted with the ship and other members of the science team.

She explained how oceanic exploration research is different from the rest of the scientific community and even other projects within NOAA, because it focuses purely on exploration and discovery that can generate hypotheses. In other areas, a scientist has a hypothesis first and sets out to test it through research and experimentation.

The information gained on our mission could generate hypotheses in all kinds of areas of research such as geology, fisheries, oceanography, marine archeology, and hydrography. It could help us identify areas that need protection, such as spawning grounds for commercial fish populations. Meme and her team will turn the data over to the National Coastal Data Development Center within three weeks. From there, it goes to the National Geophysical Data Center and the National Oceanographic Data Center, where it is freely accessible through public archives within 60-90 days of the end of the cruise. From there, any entity, public or private, can access the data for use in their work. Have you ever wondered how Google Earth and Arc View GIS get the background data for their ocean floor layer? This data contributes to those layers. Now you know! Public data access is through www.ngdc.noaa.gov and www.nodc.noaa.gov.

While we currently have low resolution data from satellites, less than 5% of the oceans have high-resolution images. We have better data now about the features of Mars than we do about our oceans on earth. Why? Because ocean surveying is difficult and time-consuming. High resolution maps cannot be made of the ocean floor with current technology on satellites. The technology is getting better and better, though. The image below shows the progression from a leadsman dropping a 10 pound weight attached to a line in the water to the multibeam sonar being used as I type.

Developing Hydrographic Survey Techniques.

Learn more about the history here.

The multibeam sonar aboard the Okeanos Explorer sends out a ping at 30 kHz that bounces off the seafloor and returns to the transducer that is equipped with sensors oriented in 432 different directions receiving up to 864 beams per swath. This method has been tested in depths of up to 8000 meters. It can give us not only bathymetry data, but also water column backscatter and bottom backscatter data. This allows us to know if there are features in the water column like gaseous seeps escaping from the ocean floor. We can also tell something about the surface features, whether they are soft sediments or hard rock, from the bottom back scatter.

Meme has a crew of mappers working with her including Scott Allen, Senior Survey Technician; Melody Ovard and Jason Meyer, Mapping Watch Leads; and several interns. Another important part of the mission is to train a new generation of ocean explorers. These interns, Chelsea Wegner, Kristin Mello, and Josue Millan, come from colleges all over the country. Their main job is to make sure the data is good and to create logs to document data collection. They have to correct the multibeam sonar data by deploying XBTs (Expendable Bathythermographs) that determine the temperature changes within the water column because sound speed increases as water temperature increases. They also use sensors on the ship to measure the conductivity and therefore determine the salinity of the water. Since sound waves penetrate saltier water more easily, the salinity affects the sound intensity measurements. Pressure must also be calculated into the equation because sound speed also increases with increasing pressure.

XBTS launch — Josue Millan launching an XBT

The vessel’s attitude also has to be factored into the sonar (like teachers need to factor in student attitudes when planning a lesson!) Similar to an airplane, a boat can pivot on its center of gravity in all three-dimensional axes: Pitch, Yaw, and Roll. Think about your own head. Pitch is like nodding your head in agreement, yaw is like shaking your head to say no, and roll would be like putting your ear to your shoulder. Gives new meaning to the phrase “Heads are going to roll,” doesn’t it? Boats also heave, or move up and down as swells pass beneath them.

Mapping Data Collection Screen — This screen shows the data being collected by the mappers.

The screen shot above shows the data as it is being collected by the mappers. In the main window in the upper right is the bathymetry data. Below that is the water column backscatter. In the bottom left is the attitude of the vessel on all axes. The center left gray image shows the bottom backscatter while the number 421 above is the current depth beneath the vessel. Finally, the display on the top left indicates the quality and intensity of each of the 432 beams.

We also have a team of researchers from the University of Puerto Rico that are deploying free vehicles to study water masses within the Puerto Rico Trench. More about them in the next blog!

Safety First! On Monday, we had our first drills as part of our safety training. We practiced the “Abandon Ship” and “Fire” drills. We tested the fire hoses and donned our gumby suits. Mrs. Paulsen is looking pretty good, eh? It is comforting to know I’ll be well-protected by good equipment and a great crew in the event of an emergency.

Kristin Mello and Theresa Paulsen in their gumby suits during the first "Abandon Ship" drill. — Kristin Mello and I are trying out our gumby suits during the first “Abandon Ship” drill.

Fire hose test — Chelsea Wegner testing a fire hose.

After mapping all morning, we learned we had to return to port due to a medical issue. I discovered that engineers are vital to the operation. Without them, we don’t sail – and they are hard to come by. All of my students interested in marine engine repair should consider NOAA in the future. The pay is good and the adventure is awesome!

I took the time in port to work in the galley helping to make lunch with the chefs. They are a friendly bunch. We made fajitas of all kinds and swordfish. Delicious! I also learned how to garnish a buffet line and even washed dishes afterward. In my high school and college days I worked in many restaurants, but they never let me work in the back. They said I was too much of a “people person” and so I was always waiting on customers. Today I got to cook on one of those large grills I see on cooking shows. Fun to cook on, but not fun to clean. The Chief Steward, Dave Fare, said he brought 5000 lbs of food on board for our trip! We’ll be eating well! Good thing there is a fitness room on board too!

Ranier Capati, Chief Cook showed my how to garnish a line. — Ranier Capati, Chief Cook showed me how to garnish a line.

Personal Log

After training on Sunday I had some time to take in a little of the history and culture of San Juan, Puerto Rico. It is a lovely place filled with beautifully colored buildings and fun music. The history is fascinating. According the National Park Service, this is where Chrisotopher Columbus landed on his 2nd voyage and laid claim to the land for Spain. Under Juan Ponce de Leon, Spain took control of the island, displacing the Taíno Indians in 1508. An enormous wall of defense was built to keep hold of the island. Trade winds and ocean currents allowed ships to easily sail here from the east. The fortifications on the island took 10 generations to build.

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Spain kept control of the island against invaders until the Spanish-American war in 1898 when Puerto Rico became a US Territory. The fortress including the Castillo de Felipe del Morro and the Castillo San Cristobal are now historical sites managed by the National Park Service. You can learn more here.

After touring the city, I found my way to the sea! I watched children running from the waves. This reminded me of my childhood. My father used to take us to the coast when we lived in California and Oregon. That is where my love of the sea began. Both of my parents have adventurous spirits and strong work ethics. They taught me that anything is possible if you are willing to take the chance and put in the effort. This is a belief I hope I pass on to my students.

Question of the Day

Can you identify this crustacean I found along a beach in San Juan?

Crab on the beach of Sn Juan. Can you classify it? — Crab on the beach of San Juan. Can you classify it?