Richard Jones & Art Banger

January 11, 2010April 6, 2021

Richard Jones & Art Bangert, January 11, 2010

NOAA Teacher at Sea
Richard Jones
Onboard NOAA Ship KA‘IMIMOANA
January 4 – 22, 2010

Mission: Survey
Geographical Area: Hawaiian Islands
Date: January 11, 2010

Science Log

“Science isn’t pretty…” Dexter from the cartoon Dexter’s Laboratory tells his sister. What he really needs to say is that science is hard work, work that takes a team of scientists, technical specialists, and in this case the dedicated crew from the NOAA ship Ka’Imimoana. Yesterday was our first real taste of what it takes to get the data needed to understand the role of the tropical ocean in modifying the world’s climate. We began out day with a shallow cast of the CTD at 6N:155W that ended around 7AM. A shallow cast still goes to a depth of 1000 meters (how many feet is that?) and takes about two to three hours to complete. The Survey Technician, a couple of the deck crew and several officers worked though heavy winds (35knots) and seas of around 18 feet and intermittent downpours of rain to make the data from the TAO Buoy array more solid.

Once the CTD was back on the ship and secured we headed toward our first recovery/deploy at 5N:155W. Our next task was to recover a TAO buoy that had been sending climate data for the past 8 months. The recovery began with a pass by the buoy to make sure that everything was still attached and that the buoy would be safe to “hop” and then come aboard. During these “fly-bys” or passes to view the condition of the old buoy the crew had an opportunity to fish. The Doc caught a nice Mahi Mahi as you can see in the image. Two Ahi (Yellow fin tuna…fresh poke and sashimi…yum) were caught, a Wahoo or Ono, and a small Galapagos shark that was released back in to the ocean.

After our successful fishing the RHIB was sent over to the buoy to secure the ‘bird’ (how we refer to the anemometer) and attach a line for hauling in the buoy to the ship. Once the winch line is attached the RHIB was brought back onboard and we started the recovery.Retrieving the buoy produced a steady rhythm of line in, filling spools, and switching to empty spools.Even the Ensign’s got in on the deck action running in a spool and scraping the barnacles off the old buoy.

Once the buoy was completely recovered (about 4 hours) we set the deck for deployment of the new buoy and broke for dinner. After dinner we began the deployment which took about 3 hours and ended in the dark around 8PM. Deployment of buoys is basically the opposite of the recovery process: Nielspin, plastic coated steel cable, with its sensors attached are then attached to the buoy with its electronics.

This line along with thousands of meters of braided line feed out into the water until the buoy’s anchor position is reached.Once the buoy was anchored in the water we waited for about a half an hour then swung by the buoy to check that it was operational. Once the buoy was confirmed as successful, the crew began to prepare for the 5N CTD and our first drifter buoy deployment.

Rick helped with this CTD to continue his training for his solo CTD’s coming in a day or so.The 5N CTD, like the 6N was a shallow cast and took about 2 hours and once the CTD was stowed Rick, the Survey Technician and two Ensign’s bid farewell to the first drifter and the day was pau (“done”) as the Hawaiians say.

Today was our opportunity to take it a little easier as compared to yesterday’s long day of buoy recovery and deployment that did not end until after dark. We had an opportunity to catch-up on some email and work on an article that is due on the 15^th of January. Nothing like being under a time crunch to get you motivated. The day is filled with sun and winds are “fresh” as it is called by some. The first order of business was to help with the 3N: 155W shallow cast CTD. It is still had to grasp that shallow is over 3000 feet down into the ocean. When the pressure of the water increases the equivalent of 1 atmosphere each 10 meters that is a lot of pressure when something goes down 1000 meters like the shallow CTD does. When we make our deep cast (3000 meters) at the equator the pressure on the instruments is staggering. What would it be in pounds per square inch? Once the CTD was back on the ship and we resumed our course south along the 155W longitude line we worked on getting the Atlantic Oceanographic and Meteorological Laboratory (AOML) drifter prepared for its deployment as the Bronc Buoy at the Equator along the 155W line.

If followers look back to a post from October they can see the stickers that the students at Billings Senior High Freshman Academy prepared for the drifter they were adopting through NOAA’s Adopt-A-Drifter Program. If you are interested in adopting a drifter you can find information about the program in the “links to learning a little more” area of this Blog. After lunch we helped the Brian, Jim and Alan to put together a specialized TAO buoy that collects information about the amount of dissolved Carbon Dioxide in the ocean in addition to the typical temperature, salinity, humidity and rain data that is gathered. These buoys appear to be easy to build.

However, standing on top of a TAO buoy anchored to the ship’s deck while trying to hold on with one hand and attach electronic sensors with the other can be daunting as the ship pitches to and fro considering the seas we had today. One gains a whole new perspective and respect for the power of the Ocean and the scientists who routinely build these buoys so that good data can be collected to help mankind. One added benefit of working on the buoys is that occasionally we have the chance to do a little personalizing. Art painted MSU CATS on one side since he works at MSU and since I just graduated from Bozeman last May. On the other side Rick put in a plug for Billings Senior Broncs. So now the Broncs and the Cats will be part of the TAO array at 155W at the equator for the next year.

We also had our first fresh sashimi and poke.Rick for one can’t wait! It is great that we have a crew with diverse skills and hobbies. Deck crew who prepare top notch sashimi and a doc who makes poke with his help.

January 9, 2010April 6, 2021

Richard Jones & Art Bangert, January 9, 2010

NOAA Teacher at Sea
Richard Jones
Onboard NOAA Ship KA‘IMIMOANA
January 4 – 22, 2010

Mission: Survey
Geographical Area: Hawaiian Islands
Date: January 9, 2010

Science Log

Today was a busy day. We were up before dawn so we could check on an existing buoy close to the location of our new deployment. We made what was called a ‘fly-by’. The ship closed on the buoy and at about a mile it was vaguely visible in the early dawn. The first buoy deployment of our mission began about 7:30 AM and we had the anchor in the water about 11AM and everything went smooth. The new generation TAO buoy was deployed at 155 W longitude and 8 N latitude in a depth of 5200 meters(about 3.2 miles deep!). The TAO buoys, also called moorings, are anchored to the ocean floor using plastic coated steel cable and heavy rope. We have a drawing of the standard buoy to give you some idea what the whole package looks like, at the surface as well as below. The adjacent image is of the actual buoy that we deployed today.As you can see the color scheme has change to a solid International Yellow above the waterline.

During the initial deployment electronic sensors are placed at specific depths on a special coated steal wire. These sensors are designed to by induction and send information about conductivity (salinity), temperature and sometimes depth to the instrument tube in the buoy.This image shows two of the science team placing one of these sensors on the line.

The information provided by these sensors, and those on the buoy that measure surface conditions, help climate scientists better model the behavior of the ocean atmosphere interface and understand what patterns are more representative of El Nino, La Nina, or Neutral conditions.

In addition to the deploy of this first buoy on our trip, the ship was also engaged in the deployment and recovery of the first deep CTD. This 3000-meter (about 9750 feet or slightly over 1 3/4^thmiles down) cast went fairly smoothly until it was on its way back to the surface. The winch

controller overheated and the CTD had to rest

for about one hour while the instrument package sat at 2000 meters.After the control circuits had a chance to cool we were able to continue the recovery of the CTD and resume or course south on the 155 W to our next station at 7N for a 1000 meter CTD cast. There is a good chance that we will do the CTD later this evening since it will take about six hours for the ship to transit one degree depending on sea conditions.

January 7, 2010April 6, 2021

Richard Jones & Art Bangert, January 7, 2010

NOAA Teacher at Sea
Richard Jones
Onboard NOAA Ship KA‘IMIMOANA
January 4 – 22, 2010

Mission: Oceanographic Survey
Geographical Area: Hawaiian Islands
Date: January 7, 2010

Science Log

Today was a day of transit. We did a lot of work on the buoys, preparing them for deployment and Rick, with the help of Tonya our Chief Survey Technician, got about half of the cups that his students decorated for ‘shrinking’ into the mesh bags to attach to the deep CTD when we do one . The CTD is a rosette of bottles that are sent to depth, in this case 3000 meters (how many feet is that and how many atmospheres of pressure?) where water samples and a record of the Conductivity (salinity), Temperature, and Depth are taken. These CTD’s will help provide a double check for the electronic data that our buoys collect and add to the data used to model El Nino/La Nina. One of the side activities of the CTD is to send down the cups to be squeezed by the pressure. We also have a cup of similar size that will be used as a control so that students will be able to see the changes that the cups undergo. Rick also has brought along a Styrofoam wig head from his daughter Teri to see the effect on a larger scale.

In addition to our work on the buoys we had our first at sea drills including an abandon ship drill.But since we had a similar drill in port we only were required to muster to our stations with our exposure suits, long sleeve shirt, head cover, and long pants and wear our personal flotation device.

A wee bit rocky today.We have a swell that seems to be coming from the starboard (right) aft quarter, which gives the ship a strange movement that has made some of the folks a little queasy.Ships tend to roll (movement around an imaginary line running bow to stern) pitch (movement up and down around an imaginary line running 90 degrees to the direction of roll) and yaw (movement left or right of the imaginary line running bow to stern).Today the KA is doing all three at the same time which is why we are encouraged to take Meclizine HCL (Dramamine) for a few days prior to the trip and for the first few days at sea. Taking this makes it easier for the crew to function in an environment that has un-natural motion without getting ‘seasick’. Even with the weird motion of the ship, we still have work to do and for us “newbies” things to learn before we are allowed to do them, like learn how to set the ‘painter line’ for the RHIB so that we will stay attached to the ship in the advent that the engine of the RIHB doesn’t start or other various bad things that can happen to a little boat in a big ocean. We didn’t actually ride in the RHIB today, we simply learned how to enter the boat, where to sit , where the emergency items are located, and how to start and steer the boat.

One of the tasks that needs to be done prior to the deployment of our first Buoy at 8N:155W is to determine (as close as possible) the ideal position for the buoy’s anchor. To do this it is essential to know the true depth of the ocean and the topography (collectively called bathymetry) of the area within a few miles of the target latitude and longitude for the buoy.Brian, our Chief Scientist, will determine the depth and location for the anchor by using both satellite sea surface heights and actual sonar depth data from ships that have been in the area. In reality, there really isn’t much hard data, physical sonar tracks, for much of the ocean and much of the depth is determined by the actually height of the sea surface as measured by satellite. These measurements take into account variables, such as orbit of the satellite, atmospheric effects on radar, and tides and compare the computer result to a mathematical ellipsoid model of the Earth’s shape. Sounds pretty complicated, and it is, but we can use this calculated sea surface to help determine the depth of the ocean since the surface mirrors the actual topography of the ocean floor. For Academy students, you will have the opportunity to do two activities from the American Meteorological Society (AMS) that will help you understand what it is that we are attempting to do.

January 6, 2010April 6, 2021

Richard Jones & Art Bangert, January 6, 2010

NOAA Teacher at Sea
Richard Jones
Onboard NOAA Ship KA‘IMIMOANA
January 4 – 22, 2010

Mission: Survey
Geographical Area: Hawaiian Islands
Date: January 6, 2010

Science Log

The KA is under her own steam, well actually diesel and electric, and we are making 10 knots (you should figure out how fast that is in miles per hour) at a heading of 173 degrees. The KA uses diesel generators to create the current to drive here electric propulsion motors. She is a vey quit ship because of this configuration which was part of her original deign…to be quite. The KA is a former Navy antisubmarine warfare ship and needed to be quiet to play her role listening for submarines that might have been lurking around the oceans. Now that quiet nature makes it nice for those of us about to have our first night at sea.

Our current position was 157degrees 51 minutes and 7 seconds west longitude (157:51:07 W) and 22 degrees 55 minutes and 8 seconds north latitude (22:55:09N) at 19:30 lcl on the 5^th of January. At that time we had been at sea for about five hours and have many more to go on our way to work the 155 W Buoy line. Sunset was fantastic, but very short. It seems to take almost no time to go from day to night here in the tropics. You can see how it looks behind some of the “birds” (anemometers) that will measure windspeed and direction on the buoys. We are now (09:10 lcl) about 40 nautical miles south of the Big Island and can just see it in the distance. It will be some time before we see land again.

Since we are running a little slow on the internet I will simply post a few images from our first day rather than a video. I will attempt to post a video or two later on but currently we are limited on our bandwidth to about 128K.

For two days I have been overwhelmed as I observed all of the aspects of the crew’s preparation for the TAO mission to Samoa. I am fascinated with everything about this operation – watching the crew load the ship, observing the ship being fueled, viewing the massive nuclear submarines located in Pearl Harbor, and assembling the sensors that collect climate data from each of the buoys we will deploy. Yesterday, in preparation for our voyage, we continued to calibrate instruments and assemble sensors.Last night was our first night at sea, I slept like a baby -the gentle rocking of the boat was like being in a giant cradle.

January 5, 2010April 6, 2021

Richard Jones & Art Bangert, January 5, 2010

NOAA Teacher at Sea
Richard Jones
Onboard NOAA Ship KA‘IMIMOANA
January 4 – 22, 2010

Mission: Survey
Geographical Area: Hawaiian Islands
Date: January 5, 2010

Science Log

The ship has been in port at Pearl Harbor most of the day. We got underway about ten to ten this morning to transit to the fuel pier. We have been loading fuel and getting the various instruments ready for deployment. One of the more memorable things for me was passing by the USS Arizona Memorial and thinking about all the history that has gone on here. It makes one pause and think of the value of our freedom and the price paid for that freedom.

One of the more mundane, but important tasks today has been to check all the sensors and to make sure that the electrical connections are all correct. I even had the opportunity to crawl under the test bench to make sure the connections for the long wave and short wave UV sensors were connected to the correct test leads.