Patricia Kassis, June 5, 2008

NOAA Teacher at Sea
Patricia Kassis
Onboard Research Vessel Kilo Moana
May 23 – June 10, 2009

Glass balls
Glass balls

Mission: Woods Hole and Hawaii Ocean Time Series
Geographic Region: Hawaiian Islands
Date: June 5, 2008

Science Log

The old buoy came back on board today. First, an acoustic signal was sent to a device located just above the anchor, which released, severing the connection between the anchor and the 80 glass balls above. These glass balls (encased in yellow plastic) are buoyant, but they live deep underwater. They keep the bottom of the rope off of the sea floor and the anchor, and they aid in recovery. The balls come speeding up, but since they have such a long trip, it takes them 40 minutes or so. I guess sometimes balls get crushed on descent, and others on ascent, so the pile of recovered glass balls includes some that are destroyed. One is shown here. Then came miles of nylon and synthetic line, enough to refill those empty boxes, and then the instruments began coming aboard (CTDs and current meters). First came the deepest instruments, looking shiny and new. At slightly shallower depths, we began to see some biology – some nice clean mussel-ish thingies as big as your thumb.

Things growing on the buoy
Things growing on the buoy

Then the buoy itself came aboard. While it is floating, you can’t remove all the instruments below it or it becomes unstable, without that weight pulling it down. So before the last submerged instruments came up, the buoy came aboard. This was a rocking, dangerous, awkward event, with the buoy slamming against the ship. When I asked if this buoy recovery was typical, I was told, in the nautical style of curt understatements, that this was “not a good one”. The buoy itself was covered with barnacle-like things, crabs, slime and, on top, bird droppings. If you got sick in the zoo’s bird house, cleaning this baby is not a job for you. (Cleaning this baby was, by the way, a job for pretty much every science person on board, from chief scientists and technicians on down to lowly observers like me.)

After the buoy was on deck, we recovered the shallowest, and thereby most biologically covered instruments. These had critters and slime. The sticker on this one says “25 meters”. Can you read it? Can you find it? I was on watch until 4 am this morning, so I actually slept through the early stages of buoy recovery, specifically the glass balls ascending. I woke up for lunch (beef pot pie – the beef bearing significant resemblance to last night’s prime rib. I’m not complaining, leftover prime rib is a-okay with me!)

The area around the old buoy was fertile fishing ground, but the scientists require everyone to wait until everything is recovered before casting. This is to avoid tangling fishing lines around science tools. During the nearly daylong recovery operation, the fishermen aboard were salivating over the mahimahi and ahi they saw circling. Finally, they got two lines in and quickly caught two small ahi. Here’s Paul, who gets the award for catching the first.

He was a little embarrassed to strike a pose with a relatively small fish, so I promised him I’d throw this picture away once he catches a bigger one. As of press time, he’s had no such luck.

Buoy comes aboard
Buoy comes aboard
Barnacles!
Barnacles!
Shallow instruments have the most growth
Shallow instruments have the most growth
Catch of the day!
Catch of the day!

Patricia Kassis, June 4, 2008

NOAA Teacher at Sea
Patricia Kassis
Onboard Research Vessel Kilo Moana
May 23 – June 10, 2009

Mission: Woods Hole and Hawaii Ocean Time Series
Geographic Region: Hawaiian Islands
Date: June 4, 2008

Spools
Spools

Science Log

The deployment of the buoy went fine yesterday, and now we’re monitoring data from both buoys while we take some extra measurements of the water in the neighborhood of the buoy. The new buoy has two of everything, and for the most part duplicate pairs agree. The only exception is wind direction, where the two devices disagree by 45 degrees or so. It is thought that a rope got caught slightly for a second on the little spinning instrument during deployment. At present, the planned solution for that is to send Sean out in a boat to climb aboard and replace it. This sounds rough for Sean but might make a good photo op for you and me. Stay tuned. The extra measurements I mentioned involve lowering a rosette with a CTD (remember? it determines salinity and temperature at different depths) and some bottles for collecting water directly. Here’s me in front of the suite of instruments.

The gray vertical cylinders on top are the bottles, and the black and silver cylinder strapped on lower is the CTD. The whole contraption is lowered by a crane, with me providing some sloppy assistance in steadying it, and it then yo-yos (scientific term) up and down through the top of the water column collecting CTD data, which we can see in real time on a computer inside. On its last trip up, the bottles are closed by a technician’s command, and my awkward self helps get the thing back on board. The operation is very controlled (despite my involvement and unlike my yo-yoing experiences) and takes perhaps 45 minutes.

I’m involved in a couple more data collection projects, too. One is taking humidity measurements on the bow with an old fashioned psychrometer (Did I spell that right, Proofreader Jim?), and the other is taking water samples from an indoor tap that they assure me draws directly from the ocean. Do you think they are making up chores to keep me busy?

CTDme

Personal Log
Remember yesterday’s question? Where do you store 7 miles of rope and cable? Most of it lives in these boxes and on these spools. I helped drag it out of the boxes, which was tedious and tiring, and I’m assured putting the old buoy line back in the boxes is no picnic. Breeze, an incoming UH student and a guy on my CDT team, is in one for scale. We’ve got a Massachusetts contingency here rooting for the Celtics and coveting a cable connection.

Technician Kuhio has started fishing, but reports no bites yet.
Technician Kuhio has started fishing, but reports no bites yet.

Patricia Kassis, June 1, 2008

NOAA Teacher at Sea
Patricia Kassis
Onboard Research Vessel Kilo Moana
May 23 – June 10, 2009

Mission: Woods Hole and Hawaii Ocean Time Series
Geographic Region: Hawaiian Islands
Date: June 1, 2008

buoy_on_deckScience Log

We just got underway yesterday, and today is very exciting. We’re deploying a new buoy a few miles from an old one, and we intend to leave both in for some days, and finally remove the old one before departing the area. The overall concept here is to get a really good dataset about the ocean and the atmosphere in one location over a long period of time. This program has been ongoing since 2004. These data will serve as a piece of the puzzle in the larger question of how global warming works, and what roles the tropical ocean and atmosphere play. The buoy, shown here sitting at the stern of the ship, is loaded with scientific instruments, distributed in three layers.

On top are the meteorological gadgets, which measure air temperature, humidity, solar radiation, wind speed and direction, and barometric pressure. A GPS unit there keeps track of the buoy’s location, elevation and orientation. There’s a fin to keep the buoy facing into the wind (preventing, for example, temperature sensors from being in contact with air that has already passed over other instruments or surfaces), and on the fin is a white capsule-looking object containing instruments to reflect radar from ships to avoid collisions, and a metal box which contains an antenna. With this antenna, all the meteorological instruments can send data to a satellite at regular intervals. You can see this data, graphed in nearly real time, at the website http://uop.whoi.edu/projects/WHOTS/whotsdata.html. On the buoy’s top you can also see bird wire, and I’m told I’ll understand fully the importance of this component when I see how guano-covered the old buoy will be.

buoy_co2A few instruments are located at sea level: carbon dioxide sensors (not shown) and sea surface temperature (SST) sensors. One SST sensor is embedded in foam and moves freely on a vertical rail, going up and down as the buoy bobs, trying to stay just at the surface of the water, and the second is fixed in place and is there for redundancy. The carbon dioxide sensors are important, especially to us in Hawaii. As you probably know, the earth’s carbon budget is intimately tied to questions about global warming, and since a great deal of carbon is in carbon dioxide molecules, and since carbon dioxide dissolves so readily in ocean water, any measured changes in carbon dioxide levels in the surface water are interesting to climate scientists. The carbon dioxide also contributes to carbonic acid, lowering the pH of the ocean water to potentially damage anything that dissolves in acid – like coral reefs and shells. Chief Scientist Bob Weller thinks this rising pH is actually a bigger concern than global warming. Very early data about climate change came from a long term data set of atmospheric carbonic dioxide collected here on Mauna Loa. If you’ve seen Al Gore’s movie, you recall this jagged sawtoothed graph depicting the rising carbon dioxide levels. It is a prime example of how useful a long term dataset from one spot on earth can be. This WHOTS project hopes to create an analogous dataset, but one about ocean conditions instead of about atmospheric conditions, and in this study (as in the Mauna Loa one) carbon dioxide is likely to play a key role.

The third layer consists of instruments hanging below the buoy: CTDs (the bread and butter of physical oceanography) tell us about the temperature and salinity at different depths; and two types of current meters measure how the water moves, one uses little propellers, the other bounces sound off of plankton in the water. These are connected to the buoy and to one another by a segmented strand – including metal chain and cable at depths where sharks would bite through anything weaker, and nylon and synthetic lines to allow some elasticity at depths where sharks aren’t a concern. Nowhere in this length is a communication wire of any kind, and electromagnetic radiation won’t travel through water, so these gadgets can’t communicate with the above water world. Instead, they hoard their data. When we pull up the old buoy, we’ll be able to download a year’s worth of data from each instrument (after we clean off the gunk). We’ll also get to look for shark bites on the chains, cables and lines.

buoy_launchI have the bottom bunk in a stateroom that I share with another observer. She’s a college student interning with Woods Hole. Our room and the one next to it (housing two University of Hawaii students) connect to a shared bathroom. The ship has a wide stance so it is very stable but a little unpredictable. It doesn’t rock much at all, but still you can’t predict in which direction the next rock will tip you. I have no feelings of seasickness yet (the seas are very calm and I don’t know of anyone on board feeling queasy yet), but keep your fingers crossed because I know I’m prone to it.

The food is remarkably good. The cook is fantastic and a hard worker. In fact, the ship seems to be divided between people working really hard (from seamen and cook on up to chief scientist and captain) and people looking for something to do (like me and other observers). I’m hoping to get connected with the guy in charge of CTD stations and water sampling so I can contribute a little more. That type of work will get underway after the new buoy is finished launching. I’m told there is sometimes fishing off the stern, especially when we get near the old buoy, with all its accumulated fish food. No poles yet, but I’ll keep you posted. I have good internet connection, so feel free to write to me at mrskassis@hotmail.com or post a comment on the blog. I’ll answer your questions as quickly as I can.

Picture this:
In total, the ropes, chains and cables connecting the anchor to the buoy is about 7 miles long. How would you store that much thick rope? I’ll show you the empties tomorrow…

Brett Hoyt, October 25, 2006

NOAA Teacher at Sea
Brett Hoyt
Onboard NOAA Ship Ronald H. Brown
October 8 – 28, 2006

Mission: Recovery and maintenance of buoy moorings
Geographical Area: Southeast Pacific, off the coast of Chile
Date: October 25, 2006

Weather Data from Bridge 
Visibility:  12nm (nautical miles)
Wind direction:  150º
Wind speed:  5 knots
Sea wave height: 1-2ft
Swell wave height: 4-6 ft
Sea level pressure: 1017.1 millibars
Sea temperature:  16.7ºC or ºF
Air temperature:  17.9ºC or ºF
Cloud type: Stratus

Reggie Glover – Engine Utility Man (“Oilier”) helping keep the ship running smooth. Thanks Reggie!
Reggie Glover – Engine Utility Man (“Oilier”) helping keep the ship running smooth. Thanks Reggie!

The Crew 

For the past 3 weeks we have been highlighting the scientists and their work.  The other unsung heroes of this cruise are the ship’s crew.  These tireless workers work 7 days a week and are on call 24 hours a day. They are up before dawn and go to bed well after sunset. They feed us three square meals a day (they are excellent chefs) and provide us even with the water we drink and bath with.  Without our crew the research does not happen. For this we thank you.

Being a crewmember on a research vessel such as the RONALD BROWN has many hardships. You can’t go to the movies (they show two every night—not always your choice but you can request a movie to be played) or head to the mall (they do have a ship’s store—by the way I’ve seen bigger closets), but it’s our mall, and for this Dave, we thank you for running it. You can’t go for a walk in the park or even stroll down a neighborhood street. Your work place is also your home and you can’t leave either.  But ………………for all these sacrifices how many of you can say you have really seen the world?  For most of us, our “world” may only be the country we live in or perhaps the neighborhood we played in as a child.  To you I ask, have you ever seen the sunset in Fiji or the glaciers in the Straits of Magellan?  Have you ever visited a land that has not seen any rainfall in over 150 years?  Have you ever gazed upon the heads of Easter Island or experienced 45ft waves in the Bearing Sea?  If not, then you have not seen the world.  It is because of this unique attraction for the world and all that is in it, that many people choose the life of a sailor.

Any one like big diesel engines?  Jim Reed inspects the heart of the ship. The RON BROWN has six of these huge diesel engines connected to very large electric generators that in turn feed enough electricity to power the two 3000 horsepower engines that turn the propellers.
Any one like big diesel engines? Jim Reed inspects the heart of the ship, which has six of these huge diesel engines connected to very large electric generators that feed enough electricity to power the two engines that turn the propellers.

Today we will visit with Reggie Glover on board the RONALD H. BROWN.  Reggie is a friendly, always there with a smile, genuinely kind man of 34 years of age.  He has been a seaman for the past 3 years and has served on numerous ships.  He got his start washing dishes for the Military Sealift Command.  He was a civilian who worked on ships that supplied U.S. Naval ships. In only 2 and a half years he has worked his way up to “wiper.” Upon leaving the Sealift Command and joining NOAA, he changed jobs to become an “Engine Utility Man.”  His past jobs have included truck driver, hotel employee, and fast food worker.  When I asked Reggie why he decided to go to sea he replied, “College isn’t for everyone” and his career at sea provided an excellent opportunity to achieve financial freedom. “Money is good, there is tons of overtime, you don’t have to pay rent, and meals are provided. Your paycheck is all yours to save or to spend.”

Reggie has not always had it “easy.” Just before going to sea he was temporarily homeless.  The sea provided a new career and a fresh start. When I asked Reggie what message he wanted to tell students he replied, “Come out to sea with a goal in mind, stick with it, and enjoy the feeling of accomplishment.  If your life isn’t going the way you want, perhaps a job at sea would be an alternative to jail, homelessness, or even college.”  Reggie goes on to say that joining NOAA’s workforce provides many opportunities to advance your skills and education.  NOAA has sent Reggie to Engine Utility School and Refrigeration School and he is planning on taking welding school this fall. He is currently working towards his 3AE (third assistant engineer).

One of the benefits he has enjoyed the most has been the free travel in seeing the world and meeting different people in it.  After visiting with Reggie I can sense he has his goals and will achieve them through his persistence and dedication to a job well done.

If you like to know more about a career at sea, check out the NOAA Fleet and Marine operations website, Automated commerce employment, and Vessel employment opportunities.

Please contact the Marine Operations Center – Atlantic at (757) 441-6206, or Marine Operations Center – Pacific at (206) 553-4548, if you have any questions.

The Teacher 

This is my final log and I would like to thank all those folks at NOAA who saw fit to send me half way around the world for the journey of a lifetime and a chance to participate in one of the most worthwhile projects any teacher could hope to imagine.  I would also like to thank Dr. Bob Weller and all the crew from Woods Hole who took time to answer my questions and make me feel like one of the team.  (Love to scrape those barnacles!) I would like to thank the captain and his crew for keeping us safe and making me feel very much at home 5,000miles from home.  And, I would like to personally thank Lt. (JG) Jackie Almeida for her input and edits on my Teacher at Sea logs and for her help in making my job easier.  If you are a teacher and would like the experience of a lifetime, go to the Teacher at Sea website and apply today.

Brett Hoyt, October 24, 2006

NOAA Teacher at Sea
Brett Hoyt
Onboard NOAA Ship Ronald H. Brown
October 8 – 28, 2006

Mission: Recovery and maintenance of buoy moorings
Geographical Area: Southeast Pacific, off the coast of Chile
Date: October 24, 2006

Data from Bridge 

Visibility:  12nm (nautical miles)
Wind direction:  140º
Wind speed:  4 knots
Sea wave height: 0-1ft
Swell wave height: 6-8 ft
Sea level pressure:  1018.5 millibars
Sea temperature:  18.1ºC or 64 ºF
Air temperature:  18.7ºC or 65 ºF
Cloud type: stratus

Deployment of the new tsunami buoy began at 6am on October 23.  The scientists deployed the buoy first and then plan to deploy the Bottom Pressure Recorder (BPR).  The reason for this is that the BPR must be located close enough to the buoy for the acoustic communication from the BPR to reach the surface buoy.  As there are only a few instruments from the Woods Hole Oceanographic Institution on the buoy, this deployment process only took a few hours instead of most of the day.  They plan on letting the buoy settle for many hours before they deploy the BPR.  One of the challenges for the tsunami buoy is that unlike the Stratus 7 buoy which had a “watch circle” (the distance the buoy could wander) of over 3 miles, the tsunami buoy has a watch circle of no more than 1,500 meters.  This difference is that you don’t want the buoy wandering out of range of the Bottom Pressure Recorder transmitter.  To achieve this, the scientists must make the mooring line exactly the right length.  The day before they deployed the buoy the scientists measured the contours of the ocean floor and knew precisely how deep the water was. At the last minute, the scientists from the Chilean Navy cut and spliced a piece of mooring line to exactly the right length.  (See photo)

The Scientists 

Here a scientist from the Chilean Navy is seen splicing in an eye into the line after it was cut to length.  This process ensures that the buoy stays in the right location and does not wander too far.
Here a scientist from the Chilean Navy is seen splicing in an eye into the line after it was cut to length. This process ensures that the buoy stays in the right location and does not wander too far.

The Machine 

The Chilean Government's tsunami buoy on station in the South Pacific.  This is only one half of the warning equation.
The Chilean Government’s tsunami buoy in the South Pacific. This is only half of the warning equation.
The Bottom Pressure Recorder (BPR) with its anchor attached.
The Bottom Pressure Recorder (BPR) with its anchor attached.

The Experiment 

There was no experiment.

Classroom Activities 

There is no classroom activity, as creating your own tsunami in the classroom would be way too messy.