Mooring – NOAA Teacher at Sea Blog

July 25, 2019

Catherine Fuller: National Mooring Day, July 11, 2019

NOAA Teacher at Sea

Catherine Fuller

Aboard R/V Sikuliaq

June 29 – July 18, 2019

Mission: Northern Gulf of Alaska (NGA) Long-Term Ecological Research (LTER)

Geographic Area of Cruise: Northern Gulf of Alaska

Date: July 11, 2019

Weather Data from the Bridge

Latitude: 59° 00.823 N
Longitude: 148° 40.079 W
Wave Height: 1 ft, ground swell 3-4 ft
Wind Speed: 5.4 knots
Wind Direction: 241 degrees
Visibility: 5 nm
Air Temperature: 13.3 °C
Barometric Pressure: 1014.6 mb
Sky: Overcast

Science and Technology Log

At home, I regularly check information from the buoys that literally surround our islands. They give me real time, relevant data on ocean conditions and weather so that I am informed about storm or surf events. We also have buoys that track tsunami data, and the accuracy and timeliness of their data can save lives. Deploying and monitoring these buoys is a job that requires knowledge of ocean conditions, electronics, rigging and computer programming.

preparing buoy system — Pete (foreground) and Seth set up the buoy system in preparation for deployment

buoy anchors — The anchors for the buoys were made of train wheels

Pete Shipton is onboard as the mooring technician from UAF’s Seward Marine Center. This morning, he, Dr. Danielson and the crew deployed three moorings near oceanographic station GAK6i (about 60 miles offshore in the Northern Gulf of Alaska) at a depth of 230 meters. The search for the right depth required that R/V Sikuliaq do an acoustic survey of the area last night to find a kilometer-long area of the right depth and bottom slope. The three moorings will be situated close enough to each other that for all purposes they are collecting a co-located set of readings representative of this site, yet far enough apart, with small watch circles, that they don’t overlap and foul each other. The set of three is designed to have one surface buoy on either side with sensors at the surface and through the water column and a third buoy in the middle with sensors also distributed across all depths.

The first buoy, GEO-1, gives information on physics, optics, nutrient
chemistry and has a profiling instrument that will “walk” up and down the mooring wire from about 25 m above the seafloor to 25 m below the surface, collecting profiles four times a day. The mooring has many of the sensors that the ship’s CTD has, including an ADCP (Acoustic Doppler Current Profiler), a weather station with a GPS that measures wind speed, relative humidity, sea level pressure, and air temperature. The buoy system was designed to withstand and operate in 8 m waves; in larger waves the surface buoy is expected to become submerged. At one meter of depth, GEO-1 measures the temperature, salinity, chlorophyll fluorescence and photosynthetically available radiation.

On GEO-2 (the center buoy), similar data is recorded at 22 m below the surface. There will also be a sediment trap, mammal acoustics recorder, particle camera, and an AZFP (acoustic zooplankton fish profiler), which has four frequencies that can detect sea life from the size of fish down to the size of zooplankton. It records sound reflections from all sizes of creatures and can see fish migrations during day or night within a range of 100m (from 100m depth to the surface).

Buoy GEO-3 is the primary “guard” buoy, or marker for the whole set. It also has a real-time transmitting weather station and near-surface measurements.

Linking the mooring lines and the anchors are acoustic releases,
which are remotely controlled tethers whole sole function to listen for a “release” command that will tell them to let go of the anchor. Since the limiting factor on the instruments is the life of the batteries, they will be picked up in a year and the acoustic release will allow the instruments to be brought back aboard Sikuliaq. These buoys will be providing real time information for groups such as the Alaska Ocean Observing System (www.aoos.org) about weather and ocean conditions, while also collecting
information about sea life in the area.

Pete and Seth on buoy — Pete (left) and Seth (right) test the stability of the buoy

Deploying the buoys was a lengthy process that required careful
coordination of parts, lines, chains and personnel. Luckily everything
went off perfectly! As the anchor weights for the two surface buoys deployed, they briefly pulled the buoys under, causing a bit of joking about whether the line length was calculated correctly. The brief “dunk test” was an excellent first trial for submergence during this coming winter’s storm conditions.

The second buoy briefly scares us by going under!

MarTechs:

There are opportunities for careers at sea in a wide variety of positions on board a research vessel. One of the most interesting is the MarTech (Marine Technician), because of their dual role during a scientific cruise.

The Marine Technicians are technically assigned to the science team although they are a part of the ship’s crew. Bern and Ethan are the MarTechs on this cruise and both work specifically with R/V Sikuliaq. They are considered a part of whatever science team is on board at the time. The MarTechs are on 12-hour shifts, from 8:00 to 8:00. Ethan is on at night, and Bern is on during the day, although there is some overlap. The two men help to deploy and recover instruments for the science team and as well as helping the crew with any deck operations. They also are responsible for the computer lab and overseeing the data displays and production from the various sensors, as well as maintaining the instruments on the ship that provide information. Although they are always at hand to help when we need it, you will often find them also repairing and upgrading ship’s equipment and helping with engineering tasks.

Bern sets up camera — Bern setting up one of his cameras.

Bern has been a MarTech on R/V Sikuliaq since 2013, and had previous experience on other research vessels, both American and international. Bern is also the ship’s unofficial documentation guy; he has a number of small cameras that he regularly uses to capture the action on board, whether from the vantage point of one of the cranes or on top of his own helmet. You can find examples of Bern’s camera work on R/V Sikuliaq’s Instagram site (@rvsikuliaq).

Ethan and Ana — Ethan helps Ana with the iron fish.

Like Bern, Ethan has also worked on other research vessels but has been on R/V Sikuliaq since it was built. This is the only ship he’s been a MarTech on. His interest in oceanography, especially marine acoustics, led him to this career. Marine acoustics is more than just listening for large species such as whales. There are acoustic sensors that “listen” to the ship and help ensure that it is functioning normally. Other acoustic sensors, such as the ones based in the open keel of the ship use sound technology to map the ocean floor as we progress on our path. Ethan was kind enough to show me the keel and explain the instrumentation. In addition, there are instruments that constantly record salinity, temperature, current strength, solar radiation and other measurements along the path we travel to provide a more complete picture of the environmental conditions existing at every point.

The ship’s acoustic instruments are mounted in the open keel; it’s open to the sea!

The marine technicians manage the computer lab when they are not needed for operations. This lab is the nerve center of the ship and allows the science team to work closely with the bridge to coordinate the movement of instruments and the speed of the vessel through the water to achieve optimum results. You can find information on meteorology, navigation, engine performance, depth sounders, closed circuit monitors, ship acoustics and deck winch statistics by looking at specific screens. In addition, the staterooms have monitors that also allow viewing of certain screens.

By far the two displays that are followed most closely are the CTD cast screens and the AIS screen. The AIS screen gives our course on a map, and shows our progress as well as future waypoints. It also shows our speed and bearing to our next point as well as ocean depth and wind speed and direction. The CTD screen shows real-time results in a number of categories such as salinity, oxygen, chlorophyll, temperature, nitrates and light as the CTD descends and ascends through the water column. Based on the results of the down cast, the teams determine the depths from which they’d like water samples collected as the CTD rises.

The CTD screen looks like spaghetti until you understand the color code for each line.

The Bridge:

The equipment on the bridge represents the pinnacle of technology as far as ship operations go. The captain’s chair has been described by some members of the science team as the “Battlestar Galactica” or “Star Trek” chair, and it really does look like it fits in a science fiction movie. Displays on the bridge show performance of the engines, radar returns and our bearing and range from them, and any other pertinent information to vessel performance. Ship movement and waypoints are hand plotted by the second mate, who also oversees ship movement along with the captain, chief mate and third mate. The ship’s officers work the bridge on a rotating watch schedule. One of the cool features of this ship is that it operates two Z-drives, similar to what is used on tugboats. These are propellers that can move independently of each other and turn in any direction. They allow the ship to be maneuvered precisely, which is a great help when we need to stay on a station through multiple operations. Various views of the bridge and the navigational instruments used by the ship’s crew are shown in the gallery below.

View of the bridge
View of the bridge
View out the bridge
The Captain’s Chair

Captain Eric Piper shows off his new jacket

Personal Log

Happy Mooring Day! It’s our self-declared “national holiday”! Because the process of deploying the moorings and buoys took up all of the morning and a part of the afternoon, most of the rest of the science team took the morning off and slept in. So many of them ran on the treadmill that running might become a part of our “holiday” tradition. My roommate even took bacon back to her room to eat in bed. Gwenn brought out her Twizzlers…somewhat appropriate because they look like steel cable (even though the moorings did not use cable). It was a nice breather for the science team, who have been working very hard to collect samples and run experiments. Somewhere along the line, the idea of making Mooring Day a “holiday” caught on, and it’s become a bit of a joke amongst the team. We’re down to a week to go, and everyone is beginning to think about what happens when we get in and when we all go home. But… we’re not quite there yet, and there’s a lot of work left to do.

Animals Seen Today

We apparently have a stowaway…a small finch-like bird that flits about the ship. It must have joined us when we were near land, and now we ARE the land.

August 19, 2018August 19, 2018

Roy Moffitt: Life on a LEGO, August 14-15, 2018

NOAA Teacher at Sea

Roy Moffitt

Aboard USCGC Healy

August 7 – 25, 2018

Mission: Healy 1801 – Arctic Distributed Biological Observatory

Geographic Area: Arctic Ocean (Bering Sea, Chukchi Sea, Beaufort Sea)

Date: August 14-15, 2018

Current location/conditions:

Evening August 15 – North- Northwest of Wainwright, Alaska

Air temp 35F, sea depth 47m , surface sea water temp 32.2F

Life on a LEGO

The LEGO is a nickname given to the large green plastic pallet-like mooring. Their retrieval from the sea floor is pictured here. This equipment was retrieved after being deployed for a year on the sea floor in about 40 meters of water. The mooring is called a DAFT (Direction Acoustic Fish Tracker). On the DAFT there are instruments that measure ocean temperature, salinity, and pressure. The primary instrument is an echo sounder that records any schools of fish that may pass overhead.

Lego Retrieval — Retrieval of the “Lego,” a large plastic mooring that has spent the past year collecting data at the ocean bottom

What the DAFT was not designed to do, but does well, is catch sea life. The fiberglass pallet has 1 1/2″ square holes in it that allow water to pass through on retrieval and it also catches sea life as if it were a net. Yesterday we pulled two of these “Legos” from the sea and they were covered with marine life. The most remarkable sight were the large blue king crabs, (around half dozen on one pallet). Here I am holding one of the bigger ones– such awesome looking creatures!

Roy and crab — TAS Roy Moffitt holding a blue king crab

On the smaller size, we found a hermit crab (shown here hiding in a shell).

Also on board were many sea stars. Most were the Brittle Stars. This is the picture of the sea star with the small legs. I think they are called the Brittle Stars because when I tried to gently remove them from the mooring, sadly their legs kept breaking off. There were dozens of these on the mooring.

There was another sea star with nine legs. It was very pretty and looks like a drawing of the sun. Not surprising, I found out this one is called the “Sun Star.”

Some not-so-pretty items on the moorings I like to call “mooring acne” are called tunicates. These are filter feeders and come in many different forms.

Tunicate

Sea Squirt

The one on my hand looks like a giant pimple and when you try to take it off the mooring it squirts you in the face. Not surprisingly this tunicate is called the “Sea Squirt.”

Think about it…

All of the life on the Lego mooring was sent back to the sea to hopefully find a new home. The Lego pallet mooring mentioned above is not large, about 4 ft by 6ft. The mooring in this story was only in the ocean one year and became the home of the above mentioned marine animals – crabs, sea stars, tunicates, and also thousands of barnacles! One tiny piece of the sea floor contained all this life! Imagine how rich in life the entire unseen ecosystem is in the Chukchi Sea!

Today’s Wildlife Sightings

For the last two days, I saw several walruses. Pictured below is one that popped up by a piece of ice. Teaser – look for a future blog focusing on walrus and their habitat.

Walrus by ice — A walrus pops its head up above water near a piece of ice

Now and Looking forward

We are now seeing small bands of pack ice and individual pieces of ice called “growlers”. Sea ice has not interrupted science operations, as of today. There is plenty of open water so far. We should see ice of different concentrations for the rest of the trip as we continue to head north. Look for future pictures and some of the science on sea ice coming soon. For now here are a couple pictures from August 15.

Growlers in fog — “Growlers” – the view looking from the deck of USCGC Healy down into the fog

Walrus broken ice — Another view of the walrus, swimming near broken up ice

August 13, 2018

Roy Moffitt: Moorings All Day, August 12, 2018

NOAA Teacher at Sea

Roy Moffitt

Aboard USCGC Healy

August 7 – 25, 2018

Mission: Healy 1801 – Arctic Distributed Biological Observatory

Geographic Area: Arctic Ocean (Bering Sea, Chukchi Sea, Beaufort Sea)

Date: August 12, 2018

Current location/conditions: mid day August 12 Northwest of Icy Point Alaska

Air temp 34F, sea depth 43 m , surface sea water temp 43F

Moorings all day

Moorings are essentially anything left tied to an anchor at sea. In this case, moorings hold many different types of scientific instruments that have been anchored at sea for a year. We are only here in the Arctic for a couple weeks. In order to monitor the ocean when people are not here, many different kinds of underwater instruments that have been designed to record ocean conditions are left under the ocean attached to moorings. To service these moorings they must be retrieved. This is one of the main tasks of this trip. When we arrive at a mooring station, one would not know it as the mooring is underneath the ocean, hidden from sight. A audio signal is sent to the underwater release and a buoy (a large yellow float) is deployed. Then, the Coast Guard steps into action. This picture below shows a Coast Guard crew fishing for a buoy in a not-so-calm sea. When they hook the buoy they will tie it to a rope that is hooked into the Healy‘s on board winch. The winch will pull in the buoy as the rope is wrapped around a turning spool.

Moffitt_Mooring Retrieval_small — The Coast Guard crew fish for a buoy in a not-so-calm sea

When the buoys and attached instruments come out of the ocean they can be covered with sea life, such as barnacles which you may be able to see as small white shell looking creatures in the picture below. The buoy in the picture is mostly covered in bryozoans. Although it looks like seaweed, bryozoans are not plants, but tiny sea filtering animals chained together. Either way it has got to go. This was my job today. I washed all the buoys and cleaned the instruments. For the sensitive parts on the instruments, this meant using a sponge and toothbrush. For the rest of the instrument, I used a power washer.

Mooring retrieved from the ocean — A mooring retrieved from the ocean, covered in marine life – mainly bryozoans.

cleaned instrument — A close-up of the mooring instrument, post-cleaning

Once this instrument is in the science lab, the sound recorder (as mentioned in the August 8th blog post) was taken apart and thoroughly cleaned. It will be reused at another station during this trip if all is functioning well. In the next picture, this equipment is now shown cleaned and sitting in the lab. Much of the cleaning was done with toothbrushes and a wire brush. So another important role for a scientist is spending a lot of time cleaning equipment! Not exactly glorious!

The Mustang Suit

In my life, I have power washed many things, but aboard the Healy in the Arctic, for safety reasons, I have to wear a Mustang suit. Essentially the Mustang is an oversized orange snowsuit designed to save a life if anyone falls overboard into the near freezing Arctic waters. It has a light beacon and a whistle attached for rescuers to find you and it is designed to keep body heat in for a longer amount of time than plain clothes. This is to try to keep anyone from immediately getting hypothermia and hopefully provide the additional few minutes it would take to rescue a man overboard. I prefer to call the Mustang a big fluffy orange sweat suit– even though it was 34 degrees out I was sweating in it!

NH dudes — Teacher at Sea Roy Moffitt (left) and UNH researcher Anthony Lyons (right) wearing Mustang Suits

Here I am, in this picture, looking like an orange Pillsbury doughboy with fellow New Hampshire resident Anthony Lyons. Anthony is from the University of New Hampshire (UNH) and is a Research Professor at the Center for Coastal and Ocean Mapping, School of Marine Science and Ocean Engineering. Anthony is retrieving and deploying moorings with passive acoustic devices that record animal sounds and rain from under the ice. The instruments also measure the density of plankton and fish in the water, both food sources for marine animals. With data over time, changes in density of these populations with changes of ice cover can be found.

Today’s Wildlife Sightings

Sometimes life clings on to the moorings. These basking starfish were attached to a mooring we pulled in yesterday. Then, the next picture is an Anemone curled up in a ball that was also attached to another mooring.

Basking Starfish

Anemone

Now and Looking Forward

Air temperature has dropped to 34 degrees F, and although the surface sea temperature is 43, lower in the water column the temperatures are actually near or below freezing. It looks like we may see some pieces of ice as soon as next mooring stations tomorrow. Those changing conditions will have to be monitored for mooring retrieval, as a buoy cannot pop up through ice!

June 28, 2016March 12, 2021

Julia Harvey: More to a Mooring than meets the Eye, June 26, 2016

NOAA Teacher at Sea

Julia Harvey

Aboard NOAA Ship Hi’ialakai

June 25 – July 3, 2016

Mission: WHOI Hawaii Ocean Timeseries Station (WHOTS)

Geographical Area of Cruise: Pacific Ocean, north of Hawaii

Date: June 26^th, 2016

Weather Data from the Bridge

Wind Speed: 15 knots

Wind Direction: 100 degrees (slightly east southeast)

Temperature: 24.5 degrees C

Barometric Pressure: 1014.7 mb

Science and Technology Log

One of the primary objectives of this WHOTS project is to deploy WHOTS-13 mooring. This will be accomplished on our second day at sea.

Site of Mooring-13 courtesy of WHOTS Project Instructions — Site of Mooring-13
(courtesy of WHOTS Project Instructions)

The mooring site was chosen because it is far enough away from Hawaii so that it is not influenced by the landmasses. Mooring 13 will be located near mooring 12 in the North Pacific Ocean where the Northeast Trade Winds blow. Data collected from the moorings will be used to better understand the interactions between the atmosphere and the ocean. Instruments on the buoy record atmospheric conditions and instruments attached to the mooring line record oceanic conditions.

A look at interactions between the atmosphere and the ocean. [R. Weller, WHOI]

There is a lot more going on than just plopping a mooring in the sea. Chief Scientist Al Plueddemann from Woods Hole Oceanographic Institution and his team began in-port prep work on June 16^th. This included loading, positioning and securing the scientific equipment on the ship. A meteorological system needed to be installed on the Hi’ialakai to collect data critical to the mission. And then there was the assembly of the buoy which had been shipped to Hawaii in pieces. Once assembled, the sensors on the buoy were tested.

Meteorological Station on the Bow — Meteorological Station

As we left Oahu, we stopped to perform a CTD (conductivity/temperature/depth) cast. This allowed for the testing of the equipment and once water samples were collected, the calibration of the conductivity sensors occurred.

Sunday, June 26^th, was the day of deployment. Beginning very early in the morning, equipment was arranged on deck to make deployment efficient as possible. And the science team mentally prepared for the day’s task.

Predeployment — The deck before deployment began. The buoy is the blue item on the left.

Promptly at 7:30 am, deployment began. The first stage was to deploy the top 47 meters of the mooring with sensing instruments called microcats attached at 5 meter intervals. A microcats has a memory card and will collect temperature, conductivity and pressure data about every three minutes until the mooring is removed next year.

Sensing instruments for the morring — Microcats for recording oceanic conditions

readied microcats — Microcats readied for deployment. They are lined up on the deck based on their deployment depth.

This portion of the mooring is then attached to the surface buoy, which is lifted by a crane and lowered overboard. More of the mooring with instruments is lowered over the stern.

The remainder of the mooring is composed of wire, nylon, 68 glass balls and an anchor. At one point, the mooring wire became damaged. To solve this problem, marine technicians and crew removed the damaged portions and replaced the section with wire from a new spool. This process delayed the completion of mooring deployment but it showed how problems can be solved even when far out at sea.

After dinner, the nylon section of the rope was deployed. Amazingly, this section is more than 2000 meters long and will be hand deployed followed by a section of 1500 m colmega line. It was dark by the time this portion was in the water. 68 glass floats were then attached and moved into the water. These floats will help in the recovery of the mooring next year. The attachment to the anchor was readied.

glass floats for recovery — These glass floats will help when the mooring is recovered next year.

The anchor weighs 9300 pounds on deck and will sit at a depth of 4756 meters. That is nearly 3 miles below the ocean surface. The crane is used to lift the anchor overboard. The anchor will drop at 1.6 m/s and may take about 50 minutes to reach the bottom. As the anchor sinks, the wire, nylon and the rest of the mooring will be pulled down. Once it reaches the bottom, the mooring will be roughly vertical from the buoy to the anchor.

Personal Log

I sailed aboard NOAA ship Oscar Dyson in 2013 so I already had a general idea of what life aboard a ship would be. Both ships have workout areas, laundry facilities, lounges, and of course messes where we all eat. But on the Hi’ialakai, I am less likely to get lost because of the layout. A door that goes up is near a door that goes down.

On our first day aboard, we held two safety drills. The first was the abandon ship drill. As soon as we heard 6 short and 1 long whistles, we grabbed our life jacket, survival suit and a hat. We reported to our muster stations. I am assigned to lifeboat #1 and I report the starboard side of 0-3 deck ( 2 levels up from my room). Once I arrived, a NOAA officer began taking role and told us to don the survival suit. This being my first time putting the suit on, I was excited. But that didn’t last long. Getting the legs on after taking off shoes was easy as was putting one arm in. After that, it was challenging. It was about 84 F outside. The suit is made of neoprene. And my hands were the shapes of mittens so imagine trying to zip it up. I finally was successful and suffered a bit to get a few photos. This was followed by a lesson for how to release the lifeboats. There are enough lifeboats on each side of the ship, to hold 150% of the capacity on board.

Survival Suit & Julia — Abandon Ship drill with Survival Suit

Safety is an important aspect of living aboard a NOAA ship. It is critical to practice drills just like we do at school. So when something does happen, everyone knows what to do. A long whistle signals a fire. All of the scientists report to the Dry Lab for a head count and to wait for further instruction.

I am reminded of how small our world really is. At dinner Saturday, I discovered one of the new NOAA officers was from Cottage Grove, Oregon. Cottage Grove is just a short drive south of Eugene. She had a friend of mine as her calculus teacher. Then a research associate asked me if I knew a kid, who had graduated from South Eugene High School and swam in Virginia. I did. He had not only been in my class but also swam with my oldest son on a number of relay teams growing up. Small world indeed.

Did You Know?

The Hi’ialakai was once a Navy surveillance ship (USNS Vindicator) during the Cold War. NOAA acquired it in 2001 and converted it to support oceanic research.

May 24, 2012August 11, 2021

Sue Oltman: Getting My Sea Legs, May 22, 2012

NOAA Teacher at Sea
Sue Oltman
Aboard R/V Melville
May 22 – June 6, 2012

Mission: STRATUS Mooring Maintenance
Geographical Area: Southeastern Pacific Ocean, off the coast of Chile and Ecuador
Date: May 22, 2012

Science and Technology Log

It’s finally the day we will leave port! I’m awakened by the feeling of my bed shaking and a crash of something falling, this could have been an earthquake. The science party boards the boat after breakfast and spends a lot of time fastening all equipment down and securing it to shelving; even my laptop needs to be affixed to my desk with Velcro.

My stateroom is on the 02 deck, which is one floor below the main deck. I’m in 02-50-2 with a private “head.” Everything is made of steel (even the toilet and shower) and is bolted down, too.

As we move out towards open ocean, the R/V Melville – all 278 feet of it – is moving northwest at about 11-12 knots and all seasoned hands comment on how calm the seas are. However, there are factors such as pitch, roll and heave which I am not accustomed to! Ocean conditions affect the ship with roll of about 3° to 5° – swaying back and forth to the left (port) and right (starboard.) Pitch is the hull tilting forwards or backwards and is about 1 ° or less. Heave is vertical displacement of the ship and is a meter or less. The roll starts getting to me after dinner, despite the sea-sick medicine! Fortunately, after lying down for a while, the sickness passes.

Next, I went up to the lab where all the monitors are to see what I can learn about our course. Watching the multi-beam sonar display (from the Bathymetry XTD) as the ocean floor drops out from below us is fascinating. An array of 191 SONAR beams maps it out. The colors appear like the depth color key on classroom maps we use of the ocean floor – dark blue where deepest and yellow or even red where it is shallower.

The monitors showed the ocean floor depth as it dropped from 2500 m to about 4700 m in an hour or so. The ship was beginning to sail over the trench!

In the lab — This monitor shows the bathymetry or depth of the ocean in real time as we sail.

Two safety drills were conducted – a fire drill and an abandon ship drill. There was also training on the scientific equipment we will deploy, the UCTDs (underway conductivity, temperature and depth probes), and ARGO drifter buoys. Sean Whelan led the class on UCTD training and Jeff Lord prepped us on the drifters. These smaller buoys will be released and will float freely, carried by the currents.

The UCTDs will be deployed hourly around the clock on the aft deck (back of the ship.) Salinity and density are derived from these values. The probe is dropped into the water, will sample for about 2 minutes to 400 m or so and then be retrieved. The casting line is then rewound onto the spool to be ready for the next deployment like a sewing machine bobbin being wound. The data is transmitted to the computer via Bluetooth when a magnetic key is inserted to activate it.

Everyone was trained how to use the winch as they will need to use it on watch. Each watch has 3 people and is 4 hours long, and then you have 8 hours off. My assigned watches are 0400 – 0800 hours and 1600-2000 hours (4 to 8) so I will need to alter my sleeping schedule! Those on watch must stay in the downstairs lab and conduct UCTD releases during those hours. The instruments inside the UCTD are very sensitive and costly and must be handled very deliberately.

There is one more session. Keith – the ship’s “res tech” or resident technician – conducts a CTD handling class. The “rosette: is the circular frame in which water sampling devices called CTDs are placed to take water sampled in international waters. These are different from the UCTDs because deep zone water is sampled for salinity and temperature. This will be done about 7 times on this cruise. It is large and the instruments are housed in a sturdier casing so it is heavier and the winch operator must lower this into the ocean with a crane.

We are looking forward to be seeing some great sunrises and sunsets from our research vessel during watches!

May 21, 2012August 11, 2021

Sue Oltman: Greetings from the Ring of Fire! May 20, 2012

NOAA Teacher at Sea
Sue Oltman
Aboard R/V Melville
May 22 – June 6, 2012

Mission: STRATUS Mooring Maintenance
Geographical Area: Vina del Mar, Chile
Date: May 20, 2012

Personal Log

I’m staying in the town of Vina del Mar, about 90 minutes from Santiago and close to the busy port city of Valparaiso. Learning a bit more about the culture of this country. Once again, I’m reminded how useful it is to know other languages. The science team from WHOI (affectionately called by its acronym, pronounced hooey) is led by Dr. Robert Weller, the chief scientist, a renowned oceanographer whose expertise is moorings. The mooring for STRATUS 11 will be recovered and STRATUS 12 will be deployed. Another significant science contribution of WHOI is the Alvin submersible. Alvin has explored the mid-ocean ridge in the Atlantic Ocean extensively.

Last time, I shared that earthquakes are almost expected here, so there is a common concern about tsunami preparedness. In 2010, many Chileans lost their lives due to a tsunami they did not know how to react to. The country’s leaders are trying to implement better evacuation plans, so there is a large public drill planned in about a week here. There are banners in the street announcing the upcoming drill! Think of the school fire drills we have…a whole country will practice in a coordinated earthquake and tsunami drill to ensure that lives will be spared in the future.

Valparaiso colorful street — Many of the steep hills of Valparaiso were colorful – the homes and artistic graffiti.

The port of Valparaiso is very colorful and busy, with a lot of commerce taking place. New cars enter South America here, as does steel for construction and other goods. The U.S. oceanographic research ship R/V Melville arrived and the team has been getting equipment ready for the mission ahead. The new buoy and instruments have been shipped here separately, and the technician, Val Cannon, has been checking them out before they are deployed.It’s not an everyday event that a US Navy ship enters Chile, so local government will take the opportunity to somehow enrich their citizens. A school group visited for a tour of the ship as well as an overview of the scientific research happening aboard the vessel. The Melville science crew prepared to give a presentation to the group of high school students on Saturday morning. The research vessel Melville had come into port on the heels of 2 weeks of earthquake research by Oregon State University scientists. This scientist gave a presentation about her work first.

Scientists present to Chilean students — Dr. Sebastian Bigorre, WHOI, and Elsie Denton, translator, and I speaking to the students.

Next, Dr. Sebastien Bigorre (Seb) gave a talk about the atmospheric research in the Stratus project which I will elaborate more about in upcoming blogs. He showed them the location of the stratus mooring and why that location is chosen – it is in the area of persistent stratus cloud cover in the lower atmosphere. Did you know that some ocean water masses have a specific “fingerprint? ” This allows scientists to determine where that water mass travels to, and this reveals more information about winds and currents in the region.I gave the students an overview of the Teacher at Sea program and how NOAA provides resources for science instruction, and invites teachers to experience cutting edge science in the oceans. Teachers at Sea create new lessons and curriculum related to their cruises which are then shared on the NOAA website. The Chilean science teachers asked if these materials were available to them as well, and were happy to find out that they were.

Today was also a busy day of shipboard work inValparaiso, heavy work and long hours of getting the project’s equipment aboard. Crates and crates of equipment and gear was unloaded, involving cranes and heavy lifting by all. Even the top scientists are not exempt from the gritty hard labor! In the video clip, you will see Dr. Weller and other hardworking, versatile scientists assembling the mooring on deck. The ocean is all around us, but no one is swimming in it.

The water is pretty cool here, due to the Peru current which bring Antarctic water masses northward. There is continuous upwelling from about 1,000 meters where the thermocline is.

The coastline is on the edge of the Peru-Chile trench, part of the network of tectonic plate boundaries surrounding the Pacific. While on land, we are on the South American plate, and when we put out to sea, we will be above the Nazca plate. This is a subduction zone where the trench descends to as deep as 6,000 meters in places! The Nazca plate is subducting under the continent. The R/V Melville will mostly be sailing in water in the 4,000-4,500 meter range. This teacher is ready to set sail! Comment below to let me know your questions about the ship.

Answers to previous polls:

The KMS hat won! Upwelling is the movement of deep,cold, nutrient rich water to the surface. The cables can be over 4000 meters long.

May 10, 2012August 11, 2021

Sue Oltman: Moorings and More, May 10, 2012

NOAA Teacher at Sea
Sue Oltman
Aboard R/V Melville
May 22 – June 6, 2012

Personal Log:

In a few days, I will be en route to Santiago, Chile and meet up with the Stratus research team that I will spend about 3 weeks with. The scientists are from the Woods Hole Oceanographic Institute in Massachusetts. After some preparation, the Melville will depart from the port of Valparaiso.

Moorings will be referenced many times, I expect – and that’s not something we often encounter in landlocked Atlanta, GA. When something is “moored” it is fastened or secured in place by a cable, rope or anchor. So a boat can be moored as an alternative to being tied to a dock in a marina. Obviously, there will not be any docks and marinas in the middle of the eastern tropical Pacific!

Stratus surface mooring — One of the moorings we will recover during this mission (photo courtesy of WHOI)

The scientific instruments involved in the Stratus project are integrated into buoys and into the cable that secures them to the ocean floor. These surface data buoys are moored and are sometimes just called moorings. There are buoys in the ocean that collect all kinds of data way beyond just temperature – wind direction and speed, salinity, conductivity, dissolved oxygen, and more. Some provide early detection of potential tsunamis, a concern in this area – last month,Valparaiso experienced a 6.8 magnitude earthquake, and in Chile, earthquakes are no surprise.

Location map of Stratus project — The Stratus project focuses on a specific area in the open ocean. (image courtesy of WHOI)

Speaking of earthquakes, the largest earthquake ever recorded occurred in Chile in 1960. Technology and our ability to predict and warn has come a long way in the last 50 years! Stratus is using data to predict climate change – this cruise will be the 11th mission of the team to collect more data for this project. It is exciting to think of the potential this holds for us!
[polldaddy poll=6211066]

Personal log:

Here I am with the NOAA survival suit – in a San Diego museum!

Ship life is going to be different for me! I’ve learned that there are some similarities in rules to the Rock Eagle and Jekyll Island field trips I’ve taken with students! First of all, I will sleep in a bunk bed; next, I am only allowed to wear flip flops in my cabin – no open toed shoes on the deck of the ship. I’ll be expected to clean my room and my own bathroom before I leave the ship. Absolutely no swimming is permitted! One thing that will be different is that there will always be someone working around the clock – and that means someone will always be sleeping. Safety is of the utmost importance – one of the first things we will do is conduct a safety drill. Instead of a PFD, NOAA uses survival suits in case of emergency.
What do you want to know about the ship? Send me your question by leaving a comment.

July 16, 2009April 5, 2021

Scott Sperber, July 16, 2009

NOAA Teacher at Sea
Scott Sperber
Onboard Research Vessel Kilo Moana
July 9-17, 2009

Mission:Woods Hole Oceanographic Institution Hawaii Ocean Time series Station; Albert J. Plueddemann, Chief Scientist
Geographical area of cruise: Central Pacific, north of O’ahu
Date: July 16, 2009

Weather Data from the Bridge
Temperature: 22.64 C
Humidity: 80.6%

Science and Technology Log

I am up very early today, 0530, the last full day at sea. I did not make a log entry yesterday it was a very busy day. The day totaled a full 12 hour hard work day for me. The day started out a about 0545 with the initial recovery of the old buoy. The acoustic (sound) release mechanism was triggered and the glass balls cam up to the surface with the rope attached. The glass balls were in a large cluster once onboard and had to be untangled.

Glass balls coming onboard (left) and popped glass ball (right).

Five of the glass balls have imploded at some time and the glass that had remained had turned into a fine white powder. After the glass balls were brought onboard and untangled and put into their boxes the chore of bringing the 5 miles of line and cable began. I started out in the box to flake (lay the rope down) the line as it came in. After quite a while and a lot of rope the capstan (the vertical winch) broke. It was the only break I had since we began. A break when the brake broke. LOL. The line was cut and placed on the main winch to complete the process. This slowed the whole procedure down because once the rope was on the winch; we had to unwind it all into its storage boxes. This had to be down 2 times and it set the whole recovery procedure behind about 2 hours. If you remember the procedure of deploying the new buoy, one chain link section at a time with the sensors attached, this procedure was now reversed for the recovery.

Scott in the box (left) and Scott on deck (right).

When the sensors came up each one was taken into the lab, photographed, videoed and a narrative was taken on to the condition of the sensor including what type of marine (ocean) growth had taken place over the year. I was given the task of taking the sensors into the lab, hanging them for photographic purposes and then bring them back outside. A dirty job but some one had to do it. This process from start to finish, recovery of the buoy to the end of documenting the condition of the sensors took 10 hours. After this the real fun started, cleaning the sensors. Now we are talking dirty. We had to clean off all marine growth from the sensors so Jeff could then start recovering data.

Personal Log

Well today I was able to put on my new steel toed boots. I should have broken them in a couple of times before this; my feet ached at the end of the day, wore a hard hat all day, a safety vest, got to climb into a box with miles of rope, got to smell like an old aquarium. All and all a great day. Sure didn’t need to ride the bike, Carly passed on it too.

Jeff and the sensors in the lab (left) and dirty sensor with goose barnacles (right).

All this said and done I would really like to take the time to thank all the people who made this possible. I have done many things in my professional career to broaden my professional knowledge and this has got to be one of the best experiences of all. First and utmost I would like to thank the NOAA Organization. Without their desire to stress the importance of Science education through increasing the knowledge base of the educators of the world this would not have been possible. Thank you to Dr. Al Plueddemann, Chief Scientist, Dr. Roger Lukas and Dr. Fernando Santiago, both of the University of Hawaii. Not only did they share their wealth of knowledge with me but guided me through the practices of this WHOTS project and confirmed in me my beliefs of the importance of long term research in science. Thank you to the rest of the Science Party. You all put up with me and showed me how to do what you needed. Thank you to the Captain and the crew of the R/V Kilo Moana.

The R/V Kilo Moana (left) and Dr. Plueddeman, Paul Lethaby, Sean Whelan and Dr. Roger Lukas (right).

What a great experience. Thank you to my principal, Robert Weinberg, at Sherman Oaks Center for Enriched Studies and to my students. Keep it up kids, it is you that make SOCES number one. I would also like to thank my wife. Without her encouragement and enthusiasm towards our profession, she is also a teacher, I don’t know if I would have applied. She is my inspiration. Thank you one and all for allowing me to participate in this career and life enriching experience.

I see skies of blue….. clouds of white Bright blessed days….dark sacred nights And I think to myself …..what a wonderful world

~ Louis Armstrong

Folks on the ship take in the beautiful Hawaiian sunset…

July 14, 2009April 5, 2021

Scott Sperber, July 14, 2009

NOAA Teacher at Sea
Scott Sperber
Onboard Research Vessel Kilo Moana
July 9-17, 2009

Weather Data from the Bridge
Temperature: 23.66 C
Humidity: 76.34%

Science and Technology Log

Today is another slow scientific day today. So today I am doing some other type of scientific learning, some local marine biology. Today I am learning about how to fish in the local Hawaiian Islands style. Breeze Simmons, research associate student level 1, is showing me all of his riggings for various types of fish and fishing conditions. He is even rigging up something for me so I might have an opportunity to try to catch something later today or tomorrow. I have learned that Mahi has eyes like humans and they can see up to the surface. They are a very strong food source in the ocean the world record is close 86 pounds and that only took about 18 months of growth. Mahi mahi is also known as the dolphin fish, not to be confused with “Flipper” of dolphin fame, also known as Dorado. Ahi is tuna, Ono is Wahoo. There are also Marlin and Aku, a member of the mackerel family.

I am also sharing the Pacific Ocean with Hurricane Carlos. It’s a big ocean out here and I have not felt any effect from it and we don’t plan to. Carlos is still off the coast of Mexico now. This is so cool to be on board this ship with all these experts and to be adding to my knowledge. The meteorologists on board say that if Carlos comes close to Hawaii its strength will die out (lose its energy). The weather balloon launches are continuing on schedule every 4 hours with Tom and me taking the 0700 and 1100 launches. Tomorrow promises to be a very hectic day aboard ship. We will be recovering the old buoy. Everything will begin at a 0600 and continue all day.

Personal Log

Since today is such a mellow day I have taken this opportunity to catch up on some reading, sun, listening to music and continue by bike riding. It has now become a bit of competition between, Carly, one of the very young interns, 25 years young from the University of Hawaii, and me as to who is riding the most miles each day. Today she rode more.

The ship has an onboard DVD system where movies and such are piped into each berth (room) along with scientific information. I was in my berth and I put on one of the channels and what did I see that someone had put on in the main lounge? It was an episode of National Geographic and who was on the episode but my good friends from UCLAs’ Marine Biology Department, Dr. Bill Hamner and his wife Peggy. Small world, Peggy wrote one of my letters of recommendation for this expedition. They are part of the reason I am so involved in Ocean Sciences.

Today’s Task

Look up and find a picture of all the fish that were mentioned above.

July 13, 2009April 5, 2021

Scott Sperber, July 13, 2009

NOAA Teacher at Sea
Scott Sperber
Onboard Research Vessel Kilo Moana
July 9-17, 2009

Weather Data from the Bridge
Temperature: 24.13 C
Humidity: 72%

Science and Technology Log

The ship moved to the location of the old buoy last night. Visually, what a difference between the two. This one is certainly not the bright yellow color of the new one launched just 3 days ago. Yesterday I mentioned that the two thermometers on the new buoy were not reading identical temperatures and that they were about 0.4 degrees difference. After asking a few questions I came to be informed that the importance of this particular series of expeditions, WHOTS, is that it is the accuracy of this longevity study that gives it its validity. NOAA’s value of this study is that the study is an ongoing study not one that collects data brings it back to a lab and analyzes it and that is the end of it.

Science is not a one shot deal. This is something I have tried to stress with my students over the years. Good science, good data, is done with multiple sampling, either longevity study or many samples over a shorter period of time. Any data can happen once but for it to be valid it needs to be substantiated. For a number of years now the WHOTS study has not only brought back this type of data but has been able to note the small changes in this particular environment. It has shown how these micro changes, shown over time, have an overall affect on a macro scale. This is the credence of this study is. The fact that small changes do over a long period of time do show an effect. The simple fact that the ship stayed on station for 3 days to calibrate the measurements with the new buoy, and then moved to the location of the old buoy shows the effort to make sure that even the most infinitesimal piece of data is made constant and notable.

Today, at this second location, there is being made shallow casts (samplings) with the SEABIRD at depths up to 200m every 4 hours. These depths are the same depths as those of the instruments on the buoys. Sometimes during the course of a years study the sensors will have a tendency to drift (change) or jump in their data. These casts, engineering calibration casts, close to the buoys standardize the CTDs again reading temperature, conductivity, dissolved oxygen and then calculating density. These calibrations of any drifts serve as a comparison over the course of the year and are used to recalibrate the data. With the recovery of the old buoy, one year worth of data will be downloaded and the similarities of all data with past weather conditions will be analyzed. Again the sensors that are on the buoy are; MICROCATS, acoustic Doppler current meters and vector measuring current meters.

Personal Log

Kuhio gave a shot at fishing this morning. Because the old buoy has been in the water for a year it has become a floating reef. So far Kuhio has hooked into and rough aboard 4 Mahi mahi. YUM, fresh fish tonight. I have been told that all over the old buoy and its sensors will be organisms of all types. Jeff has asked be if I would help scrap off the old sensors. OH BOY. Dirty smelly job I am sure.

July 12, 2009April 5, 2021

Scott Sperber, July 11-12, 2009

NOAA Teacher at Sea
Scott Sperber
Onboard Research Vessel Kilo Moana
July 9-17, 2009

Weather Data from the Bridge
Temperature: 24.2 C

Science and Technology Log

Compared to yesterday today is a very slow scientific day. After releasing the WHOTS buoy, things really calmed down. Let me take this opportunity to tell you a bit about some of the instrumentation on the buoy itself. The overall goal of the project is to collect data about the ocean and atmosphere over a long period of time. These data will serve to help answer questions about such things as global warming and its impact in the tropics. On the buoy itself, pictured in a previous log, there are instruments that measure temperature, humidity, solar radiation, wind direction and speed. A GPS unit keeps track of the buoy’s location at all times. On the buoy there is also an antenna which transmits data to satellites. Each of the two buoys [explain why there are two in the ocean for this 4-day comparison period] in the water has enough slack in the lines to allow for an approximate 2-mile radius circle.

Profile of CTD on shallow casts

The weather balloon launching continues every four hours with teams of two or three taking each launch in shifts. Some CTD casts have been done with the small package SEABIRD CTD. This is set over the side, lowered down by crane and yo-yoed up and down for about four hours. During this time, data are sent directly to an onboard computer and collected by the scientists. These data include temperature and salinity. This is important information to assess changes going on in the crucial air/sea interface.

These particular locations, ones where temperature and salinity difference vary worldwide, the thermocline and halocline are dependent on variables such a currents and air temperature. On the final assent collection bottles are closed to collect water samples for further analysis. With all of this sophisticated instrumentation onboard surface water temperature samples are still taken with the old fashioned method of lowering thermometers into the water several times to take an average reading. Some things never change. The information collected by both the oceanographic crew as well as the meteorological crew aboard is truly showing the links, the association between the interaction of the air and sky, in the crucial air/sea interface.

I found out today that the temperatures on the two thermometers on the WHOTS-6 buoy are not matching. They are off by about 0.4 degrees C; that is the level of precision necessary for this research. The scientists are looking into which one is closest to the temperatures read on the ship before we move off to the old buoy’s location tomorrow. Apparently, this is not something that can be reconfigured so the scientists need to know which thermometer they can rely on for information. There are two of just about every instrument on the WHOTS buoys. This serves as a backup and a comparison for the same location and enables the greatest accuracy in the data.

Profile of weather balloon sonde

Personal Log

I’d like to share a bit more about my onboard life. I have gotten acclimated finding my way around the ship (sort of). Well, at least I don’t get lost going to the mess hall anymore. I am in a berth on an upper bunk with Jeffrey Snyder, one of the primary researchers from the University of Hawaii. The berth is quite comfortable as berths can go since it has been years since I was in a bunk bed. Various alarm clocks go off at anytime at night so the crew can go on their watch. There is even a ghost alarm that goes off at 01:15 that Jeff and I cannot locate. Food is not at a shortage. It seems that every time you turn around it is time to eat, and what great food it is too. There is fresh salad lunch and dinner, fresh fruit, at least 3 entries to choose from each mea and desserts. LA Fitness here I come. I received what I consider a gift today from Fernando Santiago, one of the principle scientists, a DVD of the procedures that are used on the Hawaii Ocean Time-series Project.

July 12, 2009

Had some down time today after setting off another weather balloon and a great fruit and yogurt breakfast. Took a 7 mile bike ride. You may ask where in the middle of the ocean you can take a 7 mile bike ride. They have a nice little fitness room on board.

Words of the day: Mahimahi, calibration, dissolved oxygen, interface, thermocline, conductivity, temperature, depth.

July 10, 2009April 5, 2021

Scott Sperber, July 10, 2009

NOAA Teacher at Sea
Scott Sperber
Onboard Research Vessel Kilo Moana
July 9-17, 2009

The crew readying the glass balls for deployment

Weather Data from the Bridge
Temperature: 23.83 C

Science and Technology Log

This morning will be when the WHOTS-6 buoy will be deployed. Via the A-frame on the aft deck, the buoy will be hoisted and placed into the water. This process is done after 40m of chain and MicroCats are lowered into the water. These serve as a keel for the buoy prior to attaching the balance of the chain instruments and then thousands of feet of line which is belayed out by tension and hand over hand from many volunteers, the 80 glass balls that provide for floatation and then the massive anchor weights (air weight of 9300 lbs) to hold the whole thing down to a final depth of 4720m. Each individual section of chain with instrumentation has to me attached prior to releasing the buoy. Note the instrumentation on the top along with the large flat white “tail” to keep the buoy set with the wind.

The WHOTS-6 Buoy. Note the instrumentation on top and the wide white fin.

Along with the oceanographic research and data collecting going on there is also atmospheric data being collected with the use of weather balloons. These helium filled balloons are to be launched every 4 hours for the entire expedition. The balloons are filled to 500 psi (pounds per square inch) of helium, the tanks of which are on board, attached to a calibrated sonde (sensing) device which reads data, temperature, air pressure and humidity and transmits the data back to the ship. Under the careful and watchful eye of Ludovic Bariteau of CIRES and the University of Colorado, at 0730, I was able to successfully set up and launch the fourth balloon of the study. Thomas Dunn and Julie Kelly, also from the University of Hawaii research team aboard, were there to assist.

Preparing the weather balloon for launch

Personal Log

I got to launch a weather balloon. The thrills and new experiences never stop. I am very anxious to take my experiences and new knowledge back to school. I also had to practice putting on a survival suit during our safety drill. Will the fun never end?

Words of the Day: acoustics; Doppler shift; calibrate, psi

Here I am launching a weather balloon! Donning my survival suit

July 9, 2009April 5, 2021

Scott Sperber, July 9, 2009

NOAA Teacher at Sea
Scott Sperber
Onboard Research Vessel Kilo Moana
July 9-17, 2009

Weather Data from the Bridge
Temperature: 23.9 c

The WHOTS-6 buoy getting prepared to be placed on the ship

Science and Technology Log

As a first log I would like to explain a little about this project. Much of what you will be reading will be directly from correspondence I have received from NOAA themselves prior to the expedition. The following is the cruise plan that the chief scientist, Al Plueddemann sent me before the cruise:

Overview

The R/V Kilo Moana (KM) will participate in mooring operations associated with the WHOI Hawaii Ocean Timeseries Station (WHOTS) project. The primary intent of the WHOTS mooring is to provide long-term, high-quality air-sea changes and upper ocean temperature, salinity and velocity at a specific location in the central Pacific Ocean.

Receiving tower for the weather balloon information

The first WHOTS mooring was deployed in August 2004, and the site has been continuously occupied since that time by means of annual mooring service cruises. The KM will depart from the UH Marine Center at Sand Island on 9 July 2009 to the WHOTS site. The cruise will include participants from WHOI, U. Hawaii, NOAA ESRL, U. Colorado CIRES, and possibly a NOAA Teacher at Sea (ME). The WHOTS moorings are a design utilizing wire rope, chain, nylon and polypropylene line. The surface buoy is a 2.7-meter diameter foam buoy with a watertight electronics well and aluminum instrument tower. Instruments are attached to the mooring line in the upper 150 m. An acoustic (sound) release is placed above the 9300 lb anchor, and 80 glass balls above the release provide backup flotation.

These receive information from the sun. The temperature skimmers.

Two meteorological systems will be deployed aboard the KM in addition to the ship’s standard sensors. The first system is one developed at WHOI to meet the need for more accurate meteorological observations from volunteer observing ships. The configuration on Kilo Moana will include five main components: a splash-proof housing with sensors for AT/RH (Atmospheric temperature and relative humidity), SWR (short wave radiation) and LWR (long wave radiation), a second housing with a BP (barometric[atmospheric] pressure sensor and central data logger, a rain gauge, a wind sensor, and a GPS) global positioning system) logger. Data are made available in real-time using a computer kept temporarily in the ship’s chart room.

Cruise Plan

Staging/Destaging: Preparation of the WHOTS-6 buoy and mooring equipment will take place at the UH Marine Center during 1-6 July. Loading and staging of scientific equipment on the KM will be done on 7 July (or earlier as the situation permits). As part of the preparation, the two meteorological systems described above will be mounted on the KM. One will be mounted on the bridge mast. Others will be installed on a 30′ high tower on the port bow, and the instrumentation and computers for theses will be kept on the port (left) side of the ship There will also be an installation along the railing for a boom that will support a sea surface temperature skimmer device and mounted on the port side of the bridge.

Operations: The cruise involves four principal operations, as listed below. These operations are expected to require 9 ship days.

1. Deployment of the WHOTS-6 mooring. The buoy will be deployed through the A-frame, after which the ship will proceed slowly ahead. The remainder of the mooring will be deployed over the stern using the mooring winch, capstan, air tuggers, and crane as necessary. Acoustic ranging from three stations will allow the mooring anchor position, to be determined by triangulation.

2. Sensor comparison period. During a period of approximately 4 days between release of WHOTS-6 and recovery of WHOTS-5, the KM will establish and hold position, with bow into the wind. During the comparison period satellite transmissions from the buoys will be monitored using equipment supplied by the scientists. A series of shallow (200 m) CTD (conductivity, temperature and depth) casts will be done at approximately 4 hr intervals using a CTD and rosette supplied by the science party.

3. Recovery of the WHOTS 5 mooring. The WHOTS-5 mooring is presently on station at another location not far from the new buoy. The WHOTS mooring release will be fired and recovering of the old buoy will begin with the glass balls (lower end) and proceed to about 50 m below the buoy while the ship moves ahead slowly. The work boat will be used tograb the glass balls and pass a leader line to the KM. The work boat will be lowered again and used to connect a line to the buoy and pass the line to the stern of the ship. The buoy will be recovered through the A-frame. Recovery operations will use the A-frame, the mooring winch, capstan, air tuggers, and crane as necessary.

4. Deep CTD casts and CTD Survey. At certain times during operations,several deep (1000 m) CTD casts will be made. The fifth WHOTS WHOI-Hawaii Ocean Timeseries Site (WHOTS) buoy was deployed from the Kilo Moana at 03:24:39 UTC June 5, 2008.

The R/V Kilo Moana will be deploying the WHOTS-6 mooring and will for a number of days be used in the comparison of real time data between the new mooring, the WHOTS-5 mooring and that of the ship. After which the WHOTS-5 mooring will be recovered via the A-frame on the stern.

Real Time Data

Hourly averaged meteorological data for the current deployment of the WHOI Hawaii Ocean Time Series Station are received via Service Argos four times daily. Hourly averages are also being transmitted for an engineering study using the Iridium Satellite service. Preliminary data is displayed in unedited form as time series plots, and is available for download as ASCII files.

Personal Log

Wow. That is a lot of scientific jargon and acronyms which I will try to clear up in the next week. As for my responsibilities they will include but not be limited to:

During this expedition I will try to match the NOAA goals of which are:

Short-term Goals

I will:

Understand how NOAA oceanic and atmospheric research is linked to National Education Science Standards and Ocean Literacy Principles.
Understand the education and training paths that lead to NOAA-related careers.

Mid-term Goals

I will:

Use NOAA data and resources in classroom activities. (oh boy)
Use NOAA-related career information in classroom activities, when mentoring students and when working with colleagues.

Why am out here in the middle of the ocean?

The vision of NOAA’s Teacher at Sea program is to be NOAA’s main provider to teachers of opportunities to participate in real-world scientific research and maritime activities.

Tasks and Responsibilities

I will have a defined set of tasks and responsibilities before, during, and after the mission. During the mission, I will be under the ultimate command of the ship’s Commanding Officer. AYE, AYE CAPTAIN. However, I will also be considered a member of the science party, And will also be under the direction of the mission’s Chief Scientist and will be expected to take part in the tasks assigned by the Chief Scientist.

MICROCat sensor to be located at 155 meters

Everyone here is very accommodating of the new guy. I am going to quietly sit back and observe for a while, there is so much going on I do not want to get in the way. From my berth window, I look directly out on the A-frame, great cautious way to observe the deployment without stepping on anyone’s toes. I am watching the crew assemble the line of MICROCat and other monitoring devices. Lengths of chain, shackles and hitches are laid over the deck in what seems like a chaotic mess but I have been assured that it will all flow out nicely when the deployment of the system begins. You can see how the MicroCATs are labeled with their respective depths.. There is also another device, the Seabird, that will be the one that bobs (yo-yo’s) up and down for daily data regarding, temperature, conductivity and depth.

Words of the day: deployment, winch, capstan, crane, acoustic, triangulation, comparison, bow, stern, A-frame

July 11, 2008March 18, 2021

Jillian Worssam, July 11, 2008

NOAA Teacher at Sea
Jillian Worssam
Onboard U.S. Coast Guard Vessel Healy
July 1 – 30, 2008

Mission: Bering Sea Ecosystem Survey
Geographic Region: Bering Sea, Alaska
Date: July 11, 2008

Meet Kevin, Jimmy, John and Dave, all ready for mooring action on the Bering Sea!

Science Log

They are the men of the back deck, working diligently to prepare and then release their moorings in depth determined locations, where they will settle (literally) for a year. These unsung heroes are the mooring men!

For the past week I have been observing a lot of scientific research and much has been based on living critters, but there is so much more occurring on the HEALY this summer. Under the guidance of Tom Weingartner, the mooring men have been working diligently to not only construct, but then release their moorings which will stay here in the Bering, collect data and then be retrieved, next year!

With various forms of sampling equipment the Spider C40

So what then is a mooring, well this specific example is a bottom mounted instrument, or “Spider C40.” You will notice that the “Spider” is chock full of sampling equipment, there is an: acoustic Doppler current profiler, flurometer, Sea Cat, and transmissometer. Each one of these instruments is designed to collect specific data, which will be saved then interpreted next year.

The “spider” commonly referred to as Helen, is the second of three instruments being placed on what is known as the central ray to the south of Nunivak Island. There are three ” mooring rays,” central, southern and northern, and placed on each will be a series of three mooring. At this time Tom is working on a three year NSF grant. What exactly is Tom learning from this data, well check in tomorrow for a more in-depth look at what scientists learn from moorings? I would though like to go into a bit of detail on the deployment of a “spider” to the bottom of the Bering.

This Spider was deployed in 25 meters of water. Its objective to sit firmly on the bottom.

AS the winch raises the instrument array, the scientists and MST team work in tandem to make sure everyone is safe and the deployment successful.

Not only is this mooring going to the bottom, but it has two acoustic release mechanisms, one to be used in a year to bring the entire mooring back to the surface, and the other to be used, right now. For a controlled fall, the spider is securely placed on the sea floor by the MST team using a 3/8inch winch wire. Kevin will then send a 12 kilohertz signal telling the second release mechanism to let go.

Kevin is setting up the electronics equipment necessary to release the mooring after placement on the sea floor.

Once the signal is sent to the acoustic release, the line to the ship is let loose, and then a GPS bearing taken so that in a year the scientists will be able to retrieve the mooring and all the wonderful data it has collected.

Check in tomorrow for a continuation with the mooring men and the science behind why they are setting these moorings, and what they will do with the data. We will also look at the actual construction of a mooring onboard.

Using the GPS to get an accurate location so that the team can come back for a pinpoint retrieval.

Quote of the Day: What is life? It is the flash of a firefly in the night. It is the breath of a buffalo in the wintertime. It is the little shadow which runs across the grass and looses itself in the sunset. -Crowfoot

FOR MY STUDENTS: Do you think we could construct a simple mooring to record data from the pond?

Those mooring men are working him to exhaustion! Thank goodness for the excellent food on board!

June 24, 2006March 19, 2021

Diana Griffiths, June 24, 2006

NOAA Teacher at Sea
Diana Griffiths
Onboard UNOLS Ship Roger Revelle
June 22 – June 30, 2006

Mission: Hawaiian Ocean Timeseries (WHOTS)
Geographical Area: Hawaiian Pacific
Date: June 24, 2006

Weather Data from Bridge
Visibility: 10 miles to less than 25 miles
Wind direction: 065°
Wind speed: 06 knots
Sea wave height: small
Swell wave height: 4-6 feet
Sea level pressure: 1014.5 millibars
Cloud cover: 3, type: stratocumulus and cumulus

Buoy Technician, Sean Whelan, contacting the Acoustic Releases on WHOTS-2.

Science and Technology Log

Today was very busy because it was the day that WHOTS-2 mooring, which has been sitting out in the ocean for almost a year, was recovered. At around 6:30 a.m., Sean Whelan, the buoy technician, tried to contact the Acoustic Release. (The Acoustic Release is the device that attaches the mooring to the anchor. When it receives the appropriate signal, it disengages from the anchor, freeing the mooring for recovery. There are actually two releases on WHOTS2.) He does this by sending a sound wave at 12 KHz down through the ocean via a transmitter, and when the release “hears” the signal, it returns a frequency at 11 KHz. The attempt failed, so the ship moved closer to the anchor site and the test was repeated. This time it was successful. Based on the amount of time it takes the acoustic signal to return, the transmitter calculates a “slant range” which is the distance from the ship to the anchor. Because the ship is not directly over the anchor, this slant range creates the hypotenuse of a right triangle. Another side of the triangle is the depth of the ocean directly below the ship. Once these two distances are known, the horizontal position of the ship from the anchor can easily be calculated using the Pythagorean theorem.

Recovery of WHOTS-2 buoy aboard the R/V REVELLE.

After breakfast, the buoy recovery began. A small boat was lowered from the ship and driven over to the buoy, as the ship was steamed right near the buoy. A signal was sent down to activate the Acoustic Releases. Ropes were attached from the buoy through a pulley across the A-frame, located on the stern of the ship, to a large winch. With Jeff Lord leading the maneuvering of the 3750-pound buoy, it was disengaged from the mooring and placed safely on deck. This was a bit of a tense moment, but Jeff did a wonderful job of remaining calm and directing each person involved to maneuver their equipment to effectively place the buoy. Once the buoy was recovered and moved to the side of the deck, each instrument on the mooring was recovered. The first to appear was a VMCM, (Vector Measuring Current Meter) located just 10 meters below the buoy.

Jeff Lord, engineering technician, directing the recovery of a Vector Measuring Current Meter (VMCM).

Then two microCATs were pulled up, located 15 and 25 meters below the buoy, followed by a second VMCM. This was followed by a series of eleven microCATs located five or ten meters apart, an RDI ADCP (Acoustic Doppler Current Profiler), and two more microCATs. As each instrument was recovered, the time it was removed from the water was recorded and its serial number was checked against the mooring deployment log. Each instrument was photographed, cleaned off and sent to Jeff Snyder, an electronic technician, for data upload. Each of these instruments has been collecting and storing data at the rate of approximately a reading per minute for a year (this value varies depending on the instrument) and this data now needs to be collected. Jeff placed the instruments in a saltwater bath to simulate the ocean environment and connected each instrument to a computer by way of a USB serial adaptor port. The data from each instrument took approximately three hours to upload. Tomorrow, these instruments will be returned to the ocean alongside a CTD in order to compare their current data collection with that of a calibrated instrument.

Once all of the instruments were recovered, over 4000 feet of wire, nylon rope, and polypropylene rope were drawn up using a winch and a capstan. Polypropylene rope is used near the end of the mooring because it floats to the surface. The last portion of the mooring recovered was the floatation. This consisted of eighty glass balls chained together and individually encased in plastic. The glass balls, filled with air, float the end of the mooring to the surface when the Acoustic Releases disengage from the anchor. It takes them about 40 minutes to reach the surface. Recovering the glass balls was tricky because they are heavy and entangled in one another. Once on deck they were separated and placed in large metal bins. After dinner, a power washer was used to clean the buoy (it is a favorite resting place for seagulls and barnacles) and the cages encasing some of the instruments. The deck was cleaned and organized to prepare for tomorrow.

Recovery of mooring floatation on WHOTS-2, consisting of 80 glass balls encased in plastic.

Personal Log

The theme that keeps going through my mind during this trip and today especially, is how much of a cooperative effort this research requires. It begins with the coordination between Dr. Weller and Dr. Lukas to simultaneously collect atmospheric data using the buoy and subsurface data with the mooring instruments. In addition, Dr. Frank Bradley, an Honorary Fellow at the CSIRO Land and Water in Australia, is on the cruise working to create a manual set of data points for relative humidity using an Assman psychrometer to further check the relative humidity data produced on the buoy. Within the science teams, coordination has to occur at all stages, from the collection of data to its analysis. This was very evident in physical form today with numerous people on deck throughout the day working to retrieve the mooring, fix machinery as it broke down (the winch stopped twice), and clean the instruments. In the labs, others were working to upload data and configure computer programs to coordinate all of the data. In addition to all of this is the quiet presence of the ship’s crew who are going about their duties to be sure that the ship is running smoothly. Several of the crew did take a break today just after the instruments were collected in order to put out fishing lines! They caught numerous tuna and beautiful Mahi Mahi that the cook deliciously prepared for dinner.

June 23, 2006March 19, 2021

Diana Griffiths, June 23, 2006

NOAA Teacher at Sea
Diana Griffiths
Onboard UNOLS Ship Roger Revelle
June 22 – June 30, 2006

Mission: Hawaiian Ocean Timeseries (WHOTS)
Geographical Area: Hawaiian Pacific
Date: June 23, 2006

Science and Technology Log / Interview

Dr. Lukas, aboard the REVELLE collecting water samples from the CTD.

Dr. Roger B. Lukas Professor of Oceanography Dept. of Oceanography and Joint Institute for Marine and Atmospheric Research University of Hawaii at Manoa.

After taking a CTD sample earlier this afternoon, I spoke with Dr. Lukas, the research scientist on this cruise who is leading the recovery and replacement of the mooring components below the WHOTS-3 buoy. The following is a summary of our discussion.

Dr. Lukas encouraged to me to communicate to my students how imperative it is to set up means of continually confirming the accuracy of scientific data. The data from the mooring, for example, is compared with six or seven different profiles in order to verify the accuracy of its data and to determine when an abnormal reading has occurred (i.e. a sensor breaks or fishing lines are caught in an instrument).

Organisms both in the sample and in the surrounding water can shift the conductivity calibration in a CTD (Conductivity Temperature Depth) instrument. Therefore, the calibration of these instruments must be constantly checked and monitored. Throughout the day today at two-hour intervals, Dr. Lukas has been sending down CTD’s that provide a continuous profile of the salinity and temperature of the ocean from the surface to the maximum depth of the cast. There are sampling bottles on the rosette of the CTD that close at a depth of 10 and 200 meters. The water from these samples is brought to the surface and is used to calibrate the conductivity of the CTD. The conductivity readings (which are used to determine salinity measurements) are compared to readings taken from the sampled water via an analytical instrument called an Autosal. The Autosal is located in a lab on the ship near the main science lab. This instrument is contained in a water bath for stabilization and is kept in a temperature-controlled room. Any atmospheric pressure variations that might occur during the Autosal conductivity tests do not have enough of an effect on the conductivity determinations to create inaccuracies in salinity readings. The Autosal itself is calibrated against standard seawater which is quite expensive ($55 for a small vial) but whose salinity is known to the nearest part per million (ppm).

Salinity, or the number of grams of dissolved salts in a kg of seawater, is detected in one part per million (ppm) and is not taken as a direct measurement. Instead, both the temperature of the sample and its conductivity are measured. This is because the conductivity of seawater is affected by three variables: temperature, pressure, and salinity. Temperature affects conductivity ten times more than does salinity. Basically this means that temperature measurements must be extremely accurate in order to obtain precise salinity measurements. If a temperature reading were to be off by 1°C this would produce an error in the salinity determination by a factor of ten. This would render the salinity measurement entirely useless. Salinity measurements are related to a scale known as the Practical Salinity Scale where, for example, a reading of 35 units would be equivalent to the conductivity of 35 grams of salt in 1 kg of water. The scale is practical because the ratio of ionic chemical compounds in the ocean remains relatively constant.

Ultimately, the salinity readings produced by the instruments contained in the MicroCATs in the mooring are being compared to numerous measurements taken off of the ship via the CTD’s profiles. The CTD’s readings are being calibrated against water samples taken by closing bottles on the CTD frame at different depths, which are then measured in the Autosal, which is, in turn, calibrated against standard seawater samples. The multiple checks on the temperature measurements taken at sea are not a stringent as those of the salinity readings because the temperature instruments do not have nearly the same rate of calibration drift. Unless they are broken, they will only drift approximately one millidegree per year.

There are different types of oceanographers who study various parameters of the ocean. Dr. Lukas is a physical oceanographer as opposed to one who studies the biological or chemical aspects of the ocean. Physical oceanographers study such factors as current, waves, wind, heat content, temperature, and salinity. However, there is overlap amongst the different areas of science. A chemical determination, such as salinity, can actually be quite pertinent to the physical study of the ocean. Alterations in salinity correlate with changes in density. Variations in density gradients across the ocean cause flow or ocean currents. Other factors that affect the ocean currents include the depth of the water; wind, which drags water along; and the rotational motion of the earth. For example, if a current is moving northward, the rotation of the earth causes an apparent force to affect the water thus drawing it eastward and changing the direction of the current. Additional smaller factors that affect the current include turbulence in both the air and the sea. Turbulence is chaotic eddying motions that cause mixing amongst masses of water at different temperatures and salinities.

Dr. Lukas has a Bachelor’s degree in Mathematics, and a Master’s and PhD in oceanography. The work that he has done in earning his PhD gives him the ability to lead a research project, such as the Hawaii Ocean Time-series (www.soest.hawaii.edu/HOT_WOCE). However, Dr. Lukas noted that one does not need a PhD to be a vital part of a research team. We have people working as part of the science team on this cruise who are at the Master’s, Bachelor’s and Associate’s degree levels.

When asked about what he likes about his work, Dr. Lukas told me that he enjoys several aspects of his job. He enjoys going to sea and the fact that his work leads him to discover new things. He also values the freedom that his occupation affords him. If he is successful in obtaining funding for a proposal, he has the freedom to carry out a project of his own design. His work has taken him to a variety of places including Papua New Guinea, the Philippines and the Bay of Bengal!

It became very evident in talking with Dr. Lukas that he is devoted to this work that he so enjoys. He puts many hours into his profession. As he stated, he and Dr. Weller have continual “time and a half” jobs. His occupation involves many different aspects including being at sea, gathering data and preparing for such science cruises. He spends large chunks of time working with his research group of eight members. This work involves managing and training the members of the group as well as dealing with various personnel issues. Approximately 20% of his time is spent teaching at the graduate level. This is a smaller percentage than many of his colleagues. Dr. Lukas spends time developing projects and proposals and a significant amount of time completing the science for those that are funded. This science includes analyzing data, writing papers, attending meetings, etc. Finally, another large aspect of his job is of a more global, community nature. Like many of his colleagues, he reviews the work of other scientists. He is a member of various committees including those that make recommendations to funding agencies. He has numerous meetings each year, some of which require extensive travel. He travels to Washington D.C. several times a year, and has worked to raise awareness in congress concerning global issues relating to the ocean and our environment.

Finally, I asked Dr. Lukas if he had any advice for students interested in oceanography. He replied that, “There is no such thing as too much math or science!” One of his team members was nearby and commented that although math might seem boring in high school it becomes so important later on. Dr. Lukas confirmed that it is a tool that allows scientists to accomplish a lot. This is clearly evidenced by the work that he is able to complete.

June 22, 2006March 19, 2021

Diana Griffiths, June 22, 2006

NOAA Teacher at Sea
Diana Griffiths
Onboard UNOLS Ship Roger Revelle
June 22 – June 30, 2006

Mission: Hawaiian Ocean Timeseries (WHOTS)
Geographical Area: Hawaiian Pacific
Date: June 22, 2006

Weather Data from Bridge
Visibility: 10 miles to < 25 miles
Wind direction: 080°
Wind speed: 12 knots
Sea wave height: small
Swell wave height: 2-4 feet
Sea level pressure: 1016 millibars
Cloud cover: 5
Cloud type: cumulus, stratocumulus

WHOTS –3 buoy during transfer from 2nd to 1st deck. — WHOTS –3 buoy during transfer from 2nd to 1st deck

The Cruise Mission

The overall mission of this cruise is to replace a mooring anchored north of the Hawaiian island of Oahu. It’s called the WHOTS buoy: The Woods Hole Oceanographic Institution (WHOI) Hawaii Ocean Timeseries (HOT) Site (WHOTS). The mooring consists of a buoy that contains numerous meteorological sensors that collect data on relative humidity, barometric pressure, wind speed and direction, precipitation, short and long wave solar radiation, and sea surface temperature. The buoy serves as a weather station at sea, one of few such stations in the world.

There are two of each type of sensor on the WHOTS-3 buoy to ensure that data collection will continue should a sensor break down. The buoy is equipped with a GPS unit. The buoy also serves as a platform for observing the ocean. Hanging below the buoy are four different types of instruments. These include SeaCATs, MicroCATs, an ADCP and NGVM. The SeaCATs and MicroCATs take salinity and temperature measurements. The MicroCATs, in addition to salinity and temperature, also take depth measurements. There are several of each instrument attached to the mooring and they are located approximately 5 meters apart down to a depth of 155 meters. (The WHOTS-2 mooring only contains MicroCATs). The ADCP or Acoustic Doppler Current Profiler is an instrument that allows the scientists to measure the velocity of the current at a set of specific depths. The NGVM is a New Generation Vector Measuring device that measures the velocity of the current at fixed points using propeller sensors located at 90° to one another. Finally, two Acoustic Release Devices are attached to the anchor that is holding the mooring in place.

These instruments allow the scientists to determine the location of the anchor and will also mechanically release the mooring from the anchor when sent a specific acoustic signal. (More about how these work in a later log). The WHOTS-2 mooring has been sitting in the ocean for a year collecting data. It is powered by 4000 D-cell batteries and is capable of running off of them for about 16 months. I asked Jason Smith, the lead instrument calibration technician, why solar panels weren’t used on the buoy and he told me that they are susceptible to being shot at or stolen. Evidently anything that looks valuable in the middle of the ocean is vulnerable to theft!

Personal and Science Log

R/V REVELLE’s resident technician, Cambria Colt, operating the crane used to move the WHOTS-3 buoy to the main deck of the ship.

After arriving in Hawaii on the afternoon of Monday, June 19^th, it feels good to be at sea on a moving vessel. I spent the remainder of Monday meeting the science crew from WHOI (Woods Hole Oceanographic Institution) led by the Chief Scientist, Dr. Robert Weller, having a nice dinner and falling asleep after a long day of travel.

Tuesday brought my first view of the REVELLE, a working science vessel owned by the SCRIPPS Institution of Oceanography in La Jolla, California. Go here for diagrams, pictures and statistics describing this ship. The ship has two platforms below the main deck and three decks above, not including the bridge. The main deck contains heavy equipment consisting of several winches, a crane, an electric winding cart and other machinery designed to move heavy objects. All of this equipment operation is run or overseen by Cambria Colt, the resident technician, who knows the ship like the back of her hand. It is her primary job to act as a liaison between the ships’ crew and the scientists, making sure that the needs of the science team are met. We were at the ship by 7:30 a.m. and the team started working, preparing for the cruise.

Many of the team members had already been here for a week unloading and working with the instruments. The team works well together – everyone keeps busy and seems to know what to do without a lot of discussion. I helped Jason to string up two GPS units on an upper deck of the stern of the ship as well as an antenna.

GPS units set up by science team on stern of R/V REVELLE.

The antenna is used to transmit all of the data from the mooring and from the ship to a satellite, which then directs it to WHOI. I also recorded measurements as Sean Whelan, the buoy technician, measured the distances from the top of the buoy to all of the instruments located on the buoy. He also wrapped bird wire repellant along the top of the tower of the buoy in an attempt to keep birds from landing on the instruments. The bird wire is spiky wire that jets out in various directions and can be quite treacherous to work with! Along the deck, Jeff Lord, an engineering technician, and Scott Burman, an undergraduate volunteer, worked on bolting down numerous winches to the deck that will be used to pull the buoy out of the water. Several winches are used on all sides to maintain maximum control over whatever is being maneuvered into or out of the water.

I also met the captain of the ship, Tom Desjardins, in the afternoon. I had no idea he was the captain when I first saw him, he was working hard on deck with the rest of the crew, clad in a T-shirt and shorts. He is quite affable, calm, and willing to put in a hand where it is needed. In a quick discussion with him I learned that security has become much tighter on the ship since 9/11. There are always two people on watch at the entrance to the ship when it is in port making sure that everyone who enters and leaves is accounted for. We all wear badges when we are on ship when it is in port. I also asked him about potable water use on the ship. The ship can hold 12,000 gallons of water and up to 3,000 gallons more can be distilled per day. Heat from the ship’s engines is used to distill the water.

I had Wednesday free to do a bit of sightseeing and that leads me back to today. We packed our clothes onto the ship early this morning and made up our berths (beds). The staterooms (bedrooms) are larger than I had expected. I have my own room and share a head (bathroom) with Terry Smith, another member of the team. Terry is also an undergraduate who won the NOAA Hollings Scholarship to participate on this cruise. Currently working towards a second career, Terry was a chef for 20 years before making the plunge to study science. She is working towards a degree in geo-oceanography. During the day I was able to get a computer set up and mostly watched and asked a few questions as more work was being done. The ship left port at 4:00 p.m. After taking a few pictures and watching the beauty of the coast slip away, I went back inside to attend a meeting led by Cambria and Dr. Weller.

Life Aboard Ship

Cambria talked about safety and reviewed some basics about living on the ship. We wear closed toed shoes at all times (except in our rooms), preferably steel-toed. When we are working on deck during the scientific operations we will wear hard hats and safety vests. Tomorrow there will be a safety drill at some point to be sure we all know where to “muster” and how to proceed should a fire or other problem occur on the ship. We separate our trash here – anything plastic and non-biodegradable has a separate bin. All of the paper and food waste, etc, has its own bin and is eventually tossed into the sea. Meals are at specific times during the day (and they are quite good!) but we are asked to “eat and run”, as the galley crew needs to get on with their work of cleaning up and preparing for the next meal or just getting some time off. The ship is equipped with a laundry and an exercise room. Evidently on long cruises members of the crew can be seen running laps around the main deck.

Vocabulary – Weather Data

Wind direction: Wind direction is measured in degrees, which follow the readings on a compass.

Wind speed: Measured in knots. A knot is 1 nm/hr. A nautical mile is the distance required to travel 1° longitude. It is equivalent to 1.85 km.

Sea wave height: This is the height of waves produced by the wind. This is logged in the ships log as either small or slight. The technical formula for sea wave height is .026 x (speed of wind)².

Swell wave height: This is the height of the swells produced by distant weather patterns. Swells form a wave pattern as opposed to sea waves, which are more random. Swell wave height is measured in feet.

April 14, 2004March 18, 2021

Dr. Laura Brezinsky, April 14, 2004

NOAA Teacher at Sea
Laura Brezinsky
Aboard NOAA Ship Miller Freeman
April 8 – April 22, 2004

Day 6: Wednesday, April 14, 2004

Latitude: 57.40.47N
Longitude: 155 12.38

Weather: continuous clouds
Visibility: 29.5-49.5 ft (Very High)
Wind direction: 220 degrees
Wind speed: 11 (m/s)
Sea level pressure: 26

Science and Technology Log

Last night we sailed south/west and this morning we are off the coast of the Alaska Peninsula in the vicinity of Katmai National Park. According to Carol Dewitt, one of the supervisors on this leg of the project, there have been an inordinate number of lost moorings on the GLOBEC line as compared to other moorings in this area. It has been suggested that this could possibly be due to long-line fishing interference but no definitive cause has been determined as of yet. Today we will recover and deploy another buoy and continue in a south westerly direction.

Personal log

Last night during my nightly visit to the bridge I discovered that the crew was closely observing 2 lights that were directly in our path. The concern was that they could possible be marker buoys for a long line and if we were to cross the line it could become entangled in our propeller. Fortunately the lights turned out to be a small boat and a marker for some rocks called “latex rocks”. There is only one captain (John Herring) on this boat and he cannot be on watch 24 hours a day. Often the driving of the boat is turned over to the other crew members including the XO (Executive office) as well as other less senior personnel such as the ensigns. After watching them all work I have complete confidence in their abilities, dedication and attention to detail.

Question of the day: What is long-line fishing and how is it impacting our fisheries? What regulations have been put in place to try and reduce negative impacts of long-liners?

Laura

April 12, 2004March 18, 2021

Dr. Laura Brezinsky, April 12, 2004

NOAA Teacher at Sea
Laura Brezinsky
Aboard NOAA Ship Miller Freeman
April 8 – April 22, 2004

Day 4: Monday, April 12, 2004

Latitude: 59.31.830N
Longitude: 149 10.28’W

Weather: clear Visibility: 29.5-49.5 ft (very high)
Wind direction: 355 degrees
Wind speed: 6 (m/s)
Sea wave height: virtually flat
Sea level pressure: 143mb
Cloud cover: Nimbostratus

Science and Technology Log

This morning we are off the coast of Seward. We have been having difficulty retrieving a mooring because it is not vertical in the water. At the base of the mooring there is a switch that releases the mooring from the anchor by remote control. The switch also has a sensor that tells the ship what the position of the mooring is. Apparently the mooring is horizontal in the water rather than vertical and that is likely the reason why we cannot
find it. The boat will return with a remote rover that will find and retrieve the mooring.

For now, we will continue on and get the next mooring which is closer in to the coast.

Personal Log

The seas are flat, the sun is shining and the coast is stunningly beautiful. We are close enough to land that I can see individual features. There is a very large coastal glacier directly inshore from us. I will try and look up the name of that glacier and report tomorrow on that.

Question of the day: What is the definition of a glacier? How are glaciers being used to track global change over geologic time?

Laura

August 28, 2002March 18, 2021

Diane Stanitski: Day 18, August 28, 2002

NOAA Teacher at Sea

Diane Stanitski

Aboard NOAA Ship Ka’imimoana

August 16-30, 2002

Day 18: Wednesday, August 28, 2002

The FOO (Field Operations Officer)’s quote of the day:

“Better three hours too soon than a minute too late.”
– William Shakespeare

Weather Log:
Here are our observations at 0900 today:
Latitude: 3°39.88’S (into the Southern Hemisphere!)
Longitude: 140°00.36’W
Visibility: 12 nautical miles (nm)
Wind direction: 100°
Wind speed: 13 kts
Sea wave height: 4-5′
Swell wave height: 6-8′
Sea water temperature: 27.1°C
Sea level pressure: 1011.7 mb
Cloud cover: 2/8, Cumulus, Cirrus

Hurricane Genevieve lives!

Science and Technology Log:

I stayed up until I couldn’t keep my eyes open anymore last night. I finished the script and lesson plan for today’s broadcast with my graduate students in the Atmospheric Environment class. When I awoke at 0600, I realized that the fish bite test was already in progress on the fantail of the ship. I quickly prepared for my morning broadcast and then went outside to see if I could help place fish heads (mostly red snapper) on the lines that were being tested. The objective of the test was to qualitatively determine the fish-bite protection of a new armored mooring cable. The current cable that is used, nilspin, is very heavy while the cable to be tested is much lighter, but has a greater diameter. The test cable consists of a polyester core wrapped with electrical wires with up to two layers of special cloth armoring with a PE jacket. The cable diameter is ~221 mm. The test consisted of towing three 100 m cables (no armor, single, and double) simultaneously from the stern while the boat moved at 1-2 kts. Fish heads were attached every 3 meters to each cable. I was asked to take notes on the procedure since it was a new experiment and to use a multimeter to ensure that the lines were actually measuring electrical conductivity in case of a fish bite. Occasionally, I managed to assist with the deployment of the lines by helping place mesh bags alongside the line, opening the bag and inserting a partially frozen and slimy head of a fish, attaching the bag to the cable with wire ties, and then placing electrical tape over the wire tie and ends of the bags to keep them attached. It took approximately 2-1/2 hours to prepare the fish lines and deploy them. I really enjoyed it. There’s something exciting about having a group of people working together toward a common goal, especially when science is involved.

We started the broadcast soon after the fish bite test was running and I had the opportunity to interview a number of people on board who hadn’t been highlighted in a past broadcast. They were great! This was a more scientific webcast mostly focused on El Nino and the research conducted on the ship. I loved every minute and learned a great deal in the process. The video is 51 minutes long and can be accessed at on our videos page. Check it out when you have time.

I asked Lobo, our Chief Engineer, how portable water is created on the ship. He provided a great overview of the process. Seawater is converted into fresh water by vacuum distillation. In the end, the water is used for drinking, as process water, and for domestic purposes. The seawater to be distilled evaporates at a temperature of about 40°C (very low temperature for evaporation to occur) as it passes between the hot plates in an evaporator on board. The evaporating temperature corresponds to a vacuum of approximately 93%, which is maintained by the brine/air ejector. The vacuum serves to lower the evaporation temperature of the feed water. Having reach boiling temperature – which is lower than at atmospheric pressure – the feed water undergoes a partial evaporation, and the mixture of generated vapor and brine enters the separator vessel, where the brine is separated from the vapor and extracted by the combined brine/air ejector. The vapors that are generated pass through a demister where any drops of seawater that are entrained are removed and fall to the bottom of the distiller chamber. The vapors continue to the condenser where they condense to fresh water as they pass between cold plates. The freshwater that is produced is extracted by the freshwater pump and led to the freshwater tank. We can store approximately 3000 gallons of water on board.

I conducted a CTD test by myself for the first time tonight at 7:30 PM. Everything worked and we decided to test zucchini, a green pepper, a potato, and a round loaf of bread to see what happens to it when it’s submerged to the extreme pressure at 1000 meters below the water surface. When we finished the CTD cast where we sampled water at 1000m, 800 m, 600 m, 400 m, 200 m, 150, 100 m, 60 m, 40 m, 25 m, 10 m, and the surface, we brought the sampling cylinders up with the food. The potato looked and felt the same, the zucchini was squishy, the green pepper looked exactly the same but it had a crack on the side and was full of water. It must have burst on the way down and filled with water. In this case, the pressure would have been the same from the inside to the outside so no change in size took place. The bread looked like pita bread. It had been placed in plastic wrap, 2 zip-lock bags, and another plastic sleeve, but still managed to get wet. Interesting experiment.

Just after the CTD returned to the surface, I went to the starboard side of the ship to throw in an AOML, a device that measures water currents across the ocean surface (more on this tomorrow). AOMLs float away into the distance but transmit their data on a realtime basis. They are occasionally retrieved, but usually remain in the Pacific forever.

Personal Log:

I am receiving all of your emails – thank you! It’s great to hear that your first week of classes is going well. I will highlight several of your questions in tomorrow’s log!

Congratulations to Steve Osmanski who knew that the term “knot(s)” is a unit of maritime speed goes back to the days of sailing ships, when speed was measured by throwing a wooden device called a “chip log” over the stern of the ship. The chip log had a line attached with knots spaced along it. When the log was thrown overboard, a timing device (usually a 30-second sandglass) was turned and the number of knots that passed through the user’s hand as the line unreeled during the 30 seconds was the ship’s speed in nautical miles per hour. It was reported to the officer of the deck as so many “knots.” The distance between knots in a log line is calculated at 1.688 feet for every second in your timing interval; so a 30-second log line would have knots 50.64 feet (50 feet, 7 and 2/3rds inches, just about). Many of you answered this correctly, but Steve was first!

John and I played Yahtzee tonight in the third round of the match. I managed to win again so I move into the semi-final round.

Question of the day: How long is the Ka’imimoana? Check out Teacher at Sea web site for all the details.

Closer to land, but wishing I was further out to sea…
Diane

October 19, 2001March 18, 2021

Jane Temoshok, October 19, 2001

NOAA Teacher at Sea
Jane Temoshok
Onboard NOAA Ship Ronald H. Brown
October 2 – 24, 2001

Mission: Eastern Pacific Investigation of Climate Processes
Geographical Area: Eastern Pacific
Date: October 19, 2001

Latitude: 20º S
Longitude: 85º W
Air Temp. 18.8º C
Sea Temp. 18.4º C
Sea Wave: 3 – 5 ft.
Swell Wave: 3 – 5 ft.
Visibility: 10 miles
Cloud cover: 7/8

Science Log

It’s done! Everyone was up early and out on the fantail (the aft deck) right after breakfast. Although the waves were a bit higher today the sun was bright and the temperature mild. In the complete reverse order of how the old mooring was brought in on Wednesday the new mooring was deployed. People worked from 7 this morning ’till 4 in the afternoon to get this put out properly and safely. Near the very end, after paying out close to 4000 meters of rope, the glass balls were attached, next the release valve, and lastly the anchor. The anchor consists of 3 large solid steel wheels that weigh close to 10,000 pounds! What a splash it made when it hit the water! Now there is a sense of relaxation and success. Tomorrow the onboard computers will check for signals from the mooring and then we will be on our way.

Temoshok 10-19-01 whoiglassballsdeploy4 — The glass balls being deployed. The large objects by the A-frame are anchors. The left side is for the IMET Buoy and he right side is for the TAO Buoys.

Temoshok 10-19-01 whoijaneinribbest — TAS Jane Temoshok in the small boat going out to the buoy.

Temoshok 10-19-01 peoplegirlsinhardhats4 — Women in hard hats on the deck: Claudia (Chile), Charlotte (France), Jane (U.S.), and Olga (U.S.) are ready to work on deck.

Travel Log

Wildlife on board

Gordy Gardipe from the engineering crew says that oftentimes seabirds fly onto deck during the night. They are attracted to the lights on the ship and they fly directly into it. Sometimes they die but sometimes they just get disoriented. Gordy has a special box that he uses to capture the bird. He waits until daylight and then sets them free. He said he used to release them right away but often they would just fly right back and do it again. That’s why he waits for sunlight.

Question of the day: What does a petral (type of sea bird) eat?

Keep in touch,
Jane

October 18, 2001March 18, 2021

Jane Temoshok, October 18, 2001

NOAA Teacher at Sea
Jane Temoshok
Onboard NOAA Ship Ronald H. Brown
October 2 – 24, 2001

Mission: Eastern Pacific Investigation of Climate Processes
Geographical Area: Eastern Pacific
Date: October 18, 2001

Latitude: 20º S
Longitude: 85º W
Air Temp. 21.0º C
Sea Temp. 19.0º C
Sea Wave: 2 – 3 ft.
Swell Wave: 3 – 4 ft.
Visibility: 10 miles
Cloud cover: 5/8

Science Log

What lies beneath?

This is our third day “on station” at 85 W. Since successfully retrieving the mooring yesterday most of the scientists on board have been taking apart all the scientific instruments that came up with it. Their hope is that data was recorded all year long and that now they can transfer it to their onboard computers to bring home.

Along with that many people are preparing for tomorrow’s deployment of the new buoy. There are many things to consider, such as the length of rope (4400 meters!) and the depth order in which the instruments are to be attached. Each instrument must be placed along the rope so that it hangs precisely at a certain depth. Furthermore, the barnacles that were attached to the instruments that were brought in yesterday really made it difficult to get at the sensors. So today many of us are painting the instruments with a special paint that barnacles and other sea life don’t like. It’s called “anti-foul” paint. It’s used a lot on the bottoms of boats and such and it smells really bad! Hopefully it will make the buoy unattractive to barnacles.

The most important thing to consider though is where to put the mooring. X may mark the spot on a map, but it doesn’t work in the ocean. Just like the land around you has hills and mountains and valleys and plains the ocean floor is not smooth. In general the depth of the ocean in this part of the world is 4000 to 5000 meters. But if you needed to sink something to the bottom it would be important to know that it’s not going to land on an underwater mountaintop or be pulled down into a deep valley. The Ron Brown has a type of radar called the “sea beam” that looks straight down to the bottom of the sea and sends out acoustic signals. It measures how quickly those signals bounce off the bottom and return to the ship. This tells the computer how deep it is right there. It keeps doing this so the computer can form a picture of the bottom of the sea. It actually forms a map so the scientists can “see” where to drop the anchor.

Travel Log

MYSTERY PACKAGE

Shortly after completing our “web cast” while I was still on the bridge, the ensign on duty reported seeing an object in the water. We all took up binoculars and sighted a bright orange rectangular shaped object, about the size of a shoebox, that was floating off the starboard side. The captain quickly called the crew on deck and told them to prepare to retrieve the item as the ship approached. Of coarse everyone crowded around to see it being brought on board and was speculating as to what it might be. Drugs! Money! Perhaps a love letter! Because of its bright orange wrapping it was obviously meant to be discovered. Some speculated that it was just a piece of safety equipment that had fallen off a ship. The first thing we all noticed when it was lifted on to the deck was the barnacles attached to its underside. From this we inferred it had been in the water for several months, but because of the small size of the barnacles, probably less than a year. The captain came down and used a knife to cut it open. Alas, nothing but Styrofoam inside. We felt so let down!

In my broadcast today, I said I would give a t-shirt to the first student who could identify the signal flags on the back of the shirt. Look at the photo carefully, and if you think you know the answer, send me an e-mail. Be sure to include your name and teacher’s name so I know how to contact you! Good luck.

Question of the day: Is it necessary to paint all the instruments that will hang along the rope with anti-foul. Should the ones hanging at 50 meters get the same amount as those that hang at 500 meters or 1500 meters? Why or why not?

Photo descriptions: This is my roommate Claudia and a scientist from Ecuador helping paint the instruments with Anti-Foul Paint.

This is a photo of the Sea Beam Radar that is mapping the floor of the ocean underneath the ship.

Here are 2 photos of the mystery package that turned out to be nothing!

Look carefully at the signal flags on the T-shirt. Do you know what letter each flag signals?

Keep in touch,
Jane

October 17, 2001March 18, 2021

Jane Temoshok, October 17, 2001

NOAA Teacher at Sea
Jane Temoshok
Onboard NOAA Ship Ronald H. Brown
October 2 – 24, 2001

Mission: Eastern Pacific Investigation of Climate Processes
Geographical Area: Eastern Pacific
Date: October 17, 2001

Latitude: 10º S
Longitude: 85º W
Air Temp. 19.2º C
Sea Temp. 18.6º C
Sea Wave: 2 – 3 ft.
Swell Wave: 3 – 4 ft.
Visibility: 10 miles
Cloud cover: 5/8

Science Log

Mooring Retrieval Day

Did you know that glass floats? Well it does when it’s round like a balloon and full of air. Try putting a holiday ornament in a bowl of water. Did you know that glass can be stronger than steel? Well it is. That’s why 80 air filled glass balls, each 17 inches in diameter, were attached to the anchor that was holding the mooring in place at 10S, 85W. They had to be strong enough to withstand the incredible pressure at 4000 m. below the surface. But when an acoustic signal was sent out to the hook that was holding the rope to the anchor, the hook released the anchor to the bottom of the sea and the balls floated to the surface in one big group. That was the first step in retrieving the mooring.

The big deal with getting the mooring on board the ship is that it all weighs so much. Just imagine the thick rope leading from the surface all the way down to the anchor. The rope alone weighs thousands of pounds! All along the rope there are science instruments that have been collecting and storing data about things like current, temperature, and salinity. So when the glass balls floated the bottom end of the rope, it allowed us to pull it in from the bottom up. A small orange boat called a RHIB (rigid hull inflatable boat) was sent out to hook onto the balls and guide them to the ship. They were hoisted onto the deck of the ship using a big winch. Take a look at all the simple machines in the photos! Pulleys, levers, inclined planes, wheels with axels, and so much more. Slowly the rope was brought in and wrapped along a big spool. Each instrument was carefully detached and catalogued. They will be carefully transported back to Dr. Weller’s laboratory in Massachusetts where the information will be studied. The instruments from lower end of the rope came up nice and clean. The instruments that were attached to the middle part of the rope had a few creatures stuck on to them. But the instruments near the surface were covered with crabs and mussels and barnacles! How did they get there? Remember that the food chain often starts off quite small. The barnacles that you see in the photo started off as really tiny “plankton” that drift around until it finds something to attach itself to (like the rope!). Then they start to grow, attracting other sea creatures to feed off of them. In no time at all there is a complete food chain living on and around the buoy.

When most of the rope was onboard the RHIB went back out to secure the mooring. This time I got to ride along! It was thrilling to be in such a little boat so far away from the RON BROWN. Even though the sea wave height was only 3 – 4 feet, the little boat got really knocked around! It was like an amusement park ride! You can see that I’m wearing my safety vest and hardhat and I’m holding on tight! We guided the mooring to the ship and then a big crane took hold of it and lifted it onto the deck. Finally the mooring was on board.

TAS Jane Temoshok rides in the Rigid Hull Inflatable Boat (RHIB)– she’s the last blue hard hat in the back.

The RHIB heads out to retrieve 80 air-filled glass balls that were attached to the mooring’s anchor.

The floating glass balls ensure scientists can retrieve the instruments on the cable linking the anchor to the mooring buoy.

The mooring buoy brought on board.

Travel log:

Today was a big day on board the RON BROWN. The mooring that was set out here a year ago was located and retrieved. To the uninitiated that may not sound like the biggest deal, but it really is an unbelievable undertaking that requires a lot of forethought, communication, equipment, and muscle. The safety aspects alone require so much preparation. Fortunately it was a successful retrieval and no one was hurt. Now we get to look forward to cleaning the instruments of all those barnacles!

Science fact: The “glue” by which a barnacle sticks (adheres) to something is one of the strongest adhesives known to man!

Keep in touch,
Jane

October 15, 2001March 18, 2021

Jane Temoshok, October 15, 2001

NOAA Teacher at Sea
Jane Temoshok
Onboard NOAA Ship Ronald H. Brown
October 2 – 24, 2001

Mission: Eastern Pacific Investigation of Climate Processes
Geographical Area: Eastern Pacific
Date: October 15, 2001

Latitude: 19º S
Longitude: 85º W
Air Temp. 18.4º C
Sea Temp. 18.6º C
Sea Wave: 2 – 3 ft.
Swell Wave: 3 – 4 ft.
Visibility: 10 miles
Cloud cover: 8/8

Science Log

Moorings

The overall purpose of this cruise called EPIC on NOAA Ship BROWN is to collect data in a variety of forms that will allow scientists a better understanding of the science of climate change. In charge of this leg of the trip is a scientist from Woods Hole Oceanographic Institution in Massachusetts named Bob Weller. Although there is science going on all the time onboard, a major event of the cruise will be to retrieve and replace a mooring at 85W. A mooring is a type of buoy, something that is set into the ocean with a long rope that leads down to an anchor. Hopefully it stays put for a year and up to 4 years. Attached to the mooring are many, many scientific instruments that will collect data over a long time. This particular mooring is very large and has been in the ocean for a year. We expect to reach it sometime this afternoon and we will stay “on station” for 5 or 6 days until the job is done.

Much of the large equipment on board the ship is here solely for the purpose of retrieving this mooring. It weighs thousands of pounds and is extremely expensive. It is also a dangerous procedure when being lifted out of the water. Imagine the biggest crane you have ever seen at a construction site moving big things around. Now imagine that the crane and the items being moved are both bobbing on the water. That gives you an idea of what will be going on. Bob brought 3 men who are experts in this type of mooring operation along, Jeff, Willy and Paul. They have been training us on how to handle the ropes and the winches and some other equipment to make it go smoothly. It will take about a day just to lift it on board safely (several hours just to reel in the rope!). Then we spend the next day cleaning it and putting it away. I wonder what kinds of things will be stuck on it?

On board, there is a brand new mooring ready to be put into the same spot. That will take another whole day! Following that the scientists spend time making sure that all the instruments are working properly before we continue on our cruise.

During these days “on station” the other scientific groups will be launching balloons, studying clouds, taking water samples, and measuring wind speeds. The crew is hoping to go fishing near the mooring and have a bar-b-que! I’m just hoping for continued good weather.

Travel Log

As we travel east and change longitude we change time zones. So this morning, we “lost” an hour, which means we are now only 1 hour different that east coast time. Some people on board forgot to set their clocks and missed breakfast!

Question of the day: Sea life (mussels, barnacles, little fish) can be a problem for the scientists. They often attach themselves to the ropes and instruments and can interfere with the data being collected. Sharks may even bite into the cables and poke holes in them. Scientists are looking for ways to prevent this. Can you think of ways that might help?

Keep in touch,
Jane

NOAA Teacher at Sea Sue Oltman Aboard R/V Melville May 22 – June 6, 2012

NOAA Teacher at Sea
Sue Oltman
Aboard R/V Melville
May 22 – June 6, 2012