drifter buoy – Page 11 – NOAA Teacher at Sea Blog

October 5, 2005March 18, 2021

Eric Heltzel, October 5, 2005

NOAA Teacher at Sea
Eric Heltzel
Onboard NOAA Ship Ronald H. Brown
September 25 – October 22, 2005

Mission: Climate Observation and Buoy Deployment
Geographical Area: Southeast Pacific
Date: October 5, 2005

Weather Data from Bridge

Temperature: 19.5 degrees C
Sea level Atmospheric pressure: 1010 mb
Relative Humidity: 90.5%
Clouds cover: 8/8, stratocumulus, altostratus
Visibility: 9 nm
Wind direction: 230 degrees
Wind speed: 6kts.
Wave height: 3 – 4’
Swell wave height: 3 – 5’
Seawater Temperature: 19.5 degrees C
Salinity: 34.7 parts per thousand

Science and Technology Log

Notice that the seawater temperature declined from 28.7 to 18.8 degrees C between yesterday and today. We crossed the equator last night so this must have something to do with it. I went to Doctor Weller and asked for an explanation:

At this latitude and at this season we are still under the influence of the southeast Trade Winds. Wave motion generates and moves at 90 degrees to the wind direction. Now the Coriolis Effect comes into play causing waves to deflect to the left in the southern hemisphere. That means that the prevailing wave direction is from northeast to southwest south of the equator.

As the winds move into the northern hemisphere wave movement is still at 90 degrees. However, now the Coriolis Effect causes waves to deflect to the right, from southwest to northeast. So this time of year the wave motion in the two hemispheres is 180 degrees to one another. As the surface waters move apart, deeper ocean water comes to the surface to fill the area evacuated by the surface wave motion. This water is coming from greater depths and is colder. This accounts for the lowering of the seawater temperature. Dr. Weller suggests that this action brings nutrients to the surface which should enhance feeding opportunities for marine life.

Vertical and horizontal motion of ocean water causes constant exchanges of heat energy. These exchanges are between water of different temperatures and also the atmosphere. Currents, waves, upwelling, evaporation, and winds are just some of the factors that influence heat exchanges on planet earth. These processes are critical to maintaining global climates. Dr. Weller’s Upper Ocean Processes Group seeks to better understand these relationships.

Ship Crew Activity

I went to the Bridge this morning to gather weather and sea condition data. The Officer of the Deck was LTJG Silas Ayers and the Watch Stander was Ordinary Seaman Phil Pokorski. The Bridge Officer always has a crewmember with them whose job it is to be lookout to scan the ocean and report what can be seen. This could be another ship, debris, or whales. The crewmember takes a sighting and determines the distance and bearing. Avoiding collision is an important job for the Officer of the Deck.

While there, the three of us engaged in a discussion of nautical measurements and their equivalencies. LTJG Ayers went to the Chart Room and extracted a reference book. Here are the values we found:

Fathom = 6 feet, 2 yards, 1.8288 meters

Cable = 720 feet, 240 yards, 219.4560 meters

Statute Mile = 5280 feet, 1760 yards, 1609.344 meters

Nautical Mile = 6,076.11548556 feet, 1852 meters, 1.150779448 statute miles

League = 3 statute miles, 4830 meters

(As in 20,000 Leagues under the Sea)

Being a Jules Verne fan, I’ve often wondered how far 20,000 leagues really is. Now I know that it is 60,000 statute miles. But nowhere is the ocean nearly that deep. Phil then pointed out that Verne was referring to horizontal distance traveled while submerged in the Nautilus. Finally the title of his tale makes sense to me.

Personal Note

Starting last evening I was hearing a squeaking sound. At first I thought it was my deck shoes squeaking on the tile deck floors. Then I notice that even when I wasn’t moving the sound persisted. I was beginning to wonder if being at sea and wearing a motion sickness patch wasn’t causing me to be hallucinatory. I looked and looked for the source of the sound. I finally asked Dr. Weller if he could hear it and fortunately he said yes. It is the sound generated by the Sea Beam, the ocean floor profiler. I was relieved to know that if wasn’t just me hearing this sound.

October 4, 2005March 18, 2021

Eric Heltzel, October 4, 2005

NOAA Teacher at Sea
Eric Heltzel
Onboard NOAA Ship Ronald H. Brown
September 25 – October 22, 2005

Mission: Climate Observation and Buoy Deployment
Geographical Area: Southeast Pacific
Date: October 4, 2005

Weather Data from Bridge

Temperature: 25.5 degrees C
Clouds cover: 6/8, stratus, altocumulus
Visibility: 12 nm
Wind direction: 245 degrees
Wind speed: 13kts.
Wave height: 3 – 5’
Swell wave height: 3 – 5’
Seawater Temperature: 28.7 degrees C
Sea level Atmospheric pressure: 1005 mb
Relative Humidity: 82%

Science and Technology Log

Today Senior Scientist Bob Weller and Senior Engineer Assistant Paul Bouchard showed me the acoustic releases. These are devices that are placed on the tether that holds the Stratus Buoy to its anchor on the ocean floor. At the deployment location the ocean depth is 4425 meters (14,518 feet). The acoustic release will be placed 30 meters from the anchor. Attached to the tether will be 35 instruments placed at a particular distance from the buoy. Their attachment distance will determine the depth at which they are located and will allow scientists to gather data about conditions at these particular depths of the water column.

The job of the acoustic release is to detach the buoy and tether from the anchor. When we arrive at the currently deployed buoy a digitized acoustic signal will be sent through the water. The acoustic release will “turn loose” of the anchor and allow our team to retrieve the buoy and the instruments attached to the tether. This is important because some of the instruments contain a year’s worth of data that must be downloaded and analyzed. Another reason is the cost of the buoy itself, all of the instruments, and the cable and line that have held it to the anchor. These things are worth about $500,000 dollars and would be difficult to replace. All of the instruments can be refurbished and used again.

When we arrive at the currently deployed Stratus Buoy the acoustic release that was put in place last year will be activated. This should allow us to retrieve the system and replace it with the one we are carrying on board the ship. The acoustic releases we are carrying will be placed in the tether holding the new buoy and will not be activated until next year when that system is recovered. Acoustic releases are also used on drilling platforms and other objects tethered to the sea floor. These machines allow the objects tethered to be freed without the need to dive into the water and cut the line. These are an ingenious piece of technology that improves the safety and convenience of oceanographic research teams.

Ship Crew Activity

I had the opportunity to watch Boatswain Group Leader Cornell Hill making a line splice. He took the end of the line around a metal eye that is built with a groove on the outside. The line comes back on itself and Cornell braids the strands into the main part of the line. He has a knife with a spike on it to help lift the strands so he can braid it together. What results is a closed loop with metal lining at the end of the line. It’s very strong and is used as an attachment point. I have long wondered how this was done so it was very interesting to see the skillful way Cornell accomplished this feat.

Terms

Acoustic signal – a particular blend of frequency and pattern of sounds that sends a message through the water to instruct a device to perform its operation. Example is the signal sent to activate the acoustic release.

Acoustic Release – a device that releases a line when given the proper sound signal. Used in the tether system of the Stratus buoy.

Bosun – crew member in charge of deck operations

Line – rope Line Splice – Braiding stands of a line back into itself.

Tether – attachment to a fixed object. This may be a combination of cable, chain, line, or wire. Example is the attachment of the Stratus Buoy so that it doesn’t drift away.

October 3, 2005March 18, 2021

Eric Heltzel, October 3, 2005

NOAA Teacher at Sea
Eric Heltzel
Onboard NOAA Ship Ronald H. Brown
September 25 – October 22, 2005

Mission: Climate Observation and Buoy Deployment
Geographical Area: Panama Canal
Date: October 3, 2005

Weather Data from Bridge
Clouds cover: 7/8, stratus, cumulus, altocumulus
Wind direction: 250 degrees
Wind speed: 18kts.
Wave height: 3 – 4’
Swell wave height: 5 – 5’
Seawater Temperature: 29.9 degrees C
Sea level Atmospheric pressure: 10.10 mb
Relative Humidity: 82%

Science and Technology Log

Today I worked my first watch from 08:00 to 12:00. I was responsible for being present in the main science lab and monitoring our position and being aware of where the first deployment of instruments will occur. Since we are not yet allowed to deploy any instruments, it was a fairly slow day. We did receive training from Sergio Pezoa on how to calibrate and activate radiosondes. These are the instrument packages that send back information on its position, temperature, atmospheric pressure, and relative humidity. These instrument packages carry a water-activated battery and are attached to a helium balloon. They are released into the atmosphere at prescribed times and send back by radio the information they gather to the receiving unit. This continues until the balloon fails and the instrument package tumbles to earth. Radiosondes are the basis for most of the information about conditions in the upper troposphere. I’ll be working on the team that launches the weather balloons carrying these instrument packages.

October 2, 2005March 18, 2021

Eric Heltzel, October 2, 2005

NOAA Teacher at Sea
Eric Heltzel
Onboard NOAA Ship Ronald H. Brown
September 25 – October 22, 2005

Mission: Climate Observation and Buoy Deployment
Geographical Area: Panama Canal
Date: October 2, 2005

Science and Technology Log

We’ve been in port at Panama City. The whole idea of sailing from the Atlantic basin across part of the continent to the Pacific basin seems rather amazing. Seeing the locks in operation was fascinating. A tug helped us get into the correct position then four cables were attached, two forward and two aft. These cables were each fed out from a winch on railroad switch engines which were on tracks on either side of the lock.

The engines moved with us and kept tension on the cables so our ship stayed in the center of the lock. The locks are 1000 feet long so our 274’ vessel could fit in with another ship. Once we were in, the lower gate closed and water started to flow in from the base of the sidewalls of the lock. I was surprised at how rapidly the lock filled with water. The water largely flows in by gravity so little has to be pumped. Once we finished going through the three locks we were lifted to the level of the natural lake that acts as a critical part of the passage. This lake, which is filled by the abundant rainfall, provides water to fill the locks and has a navigable channel dredged across. On the western side is the infamous cut. Here the canal looks like it is a river going through a canyon although it has no current and the canyon is man-made. The ship descended through locks on the Pacific side and we docked at Panama City.

When I awoke on Saturday the deck crew and engineers were preparing to take on fuel. This is a ticklish business that requires a lot of attention. It’s the same principle as pulling into the local gas station except the hoses are 8” in diameter and get bolted together then bolted to the ship. We took on 80,000 gallons of diesel fuel which we will need for the next leg of our voyage to Arica, Chile. The RON BROWN can hold about 120,000 gallons of fuel. I was pleased that this wasn’t billed to my account.

This morning I went out for a walk around the compound where our ship is docked. This is a military compound with nicely kept grounds but around the edges the indigenous vegetation is showing itself. There were several pathways up into the trees where I got a sense of what the forest in Panama is like. “Green” and “busy” are two operative descriptors. In areas along the edge there were several beautiful plants in bloom. I also got to watch leaf-cutter ants carrying there booty back to their nests. These guys travel back and forth along the same path from the tree they are carving leaves from to their residence. It always reminds me of a safari through the jungle. I also saw an Agouti in an opening. I had only seen photos of this large rodent and I was excited to see one in the field. It was in the 80’s and very humid so I returned to the ship very damp.

We are preparing to depart on the next leg of the cruise. We expect to pull away about 17:30 after the Pilot comes on board. Twelve more members of the scientific team arrived yesterday so we now have our full complement. I have assigned my first “watch” tomorrow from 08:00 to 12:00. We will be trained on deployment of drifters and ARGOS buoys this evening. I also will be helping the meteorological team by launching weather balloons. We’re going to begin the scientific research tomorrow. Wow!

Things to pursue: Design of the Panama Canal, History of the Panama Canal, and Plants and animals of Panama

August 19, 2005March 18, 2021

Joan Raybourn, August 19, 2005

NOAA Teacher at Sea
Joan Raybourn
Onboard NOAA Ship Albatross IV
August 14 – 25, 2005

Mission: Ecosystem Productivity Survey
Geographical Area: Northeast U.S.
Date: August 19, 2005

Weather Data from the Bridge

Latitude: 40’ 17” N
Longitude: 70’ 08” W
Wind direction: NNE (29 degrees)
Wind speed: 19.6 knots
Air temperature: 19° C
Sea water temperature: 22.8°C
Sea level pressure: 1018.1 millibars
Cloud cover: cloudy

Question of the Day: Yesterday a goldfinch visited us, but we are far out to sea. When I took the picture above (#6), our position was 41.39 N and 67.11 W. About how far was this little guy from Woods Hole, Massachusetts?

Yesterday’s Answer: Qualitative data is the “what” that your doctor can observe but not necessarily measure. She might look in your ears, eyes, and throat, feel your internal organs through your abdomen, observe your spine, test your reflexes, have you balance on one foot with your eyes closed, and ask general questions about how you feel. Quantitative data is the “how much”; it is something that can be measured. Your doctor will probably measure how tall you are and how much you weigh, and take your temperature and your blood pressure. If she takes blood or urine samples, they will be analyzed for both qualitative and quantitative properties. We are observing and recording similar kinds of data about the ocean, so scientists can get a good picture of the health of this ecosystem.

Science and Technology Log

We are very fortunate on this cruise to be able to deploy a drifter buoy. The NOAA Office of Climate Observation (OCO) established the Adopt-a-Drifter program in December 2004. The program makes buoys available to teachers who are participating on cruises as Teachers at Sea. Our drifter has been adopted by my school, Greenbrier Intermediate School of Chesapeake, Virginia, and by Julie Long’s school, Farnsworth Middle School of Guilderland, New York. We named him (It’s a buoy!) Moose in honor of the fact that he was deployed in the Georges Bank area of the Gulf of Maine, which has a number of GOMOOS (Gulf of Maine Ocean Observing Systems) buoys. Moose is the fourth drifter buoy to be deployed as part of the NOAA program, and joins over 1,000 drifter buoys collecting data worldwide.

The buoy itself is a blue and white sphere about the size of a beach ball. It is attached to a drogue, a long “tail” that hangs below the buoy and ensures that it is drifting with the surface currents and not being pushed along by the wind. The buoy is equipped with a water temperature sensor, and a transmitter so that its position and temperature data can be beamed to a satellite, which relays this information to a ground station that will place it on a website. Julie and I decorated the buoy with our school names and signatures – it even has a Greenbrier Intermediate School sticker and a picture of our panther mascot. Then we deployed the buoy on August 18 by tossing it over the side of the ship while it was moving slowly. It was a little sad to see Moose drifting off without us, so small on the huge ocean, but we can follow his adventures for the next 410 days by checking the Adopt a Drifter website. You can begin tracking it here. You can find Moose by clicking on his WMO number, which is 44902. The website will give you the location of the buoy (latitude and longitude) and the date, time, and temperature of the surface water at that location.

What can scientists do with the data about surface water currents that buoys such as Moose are collecting? Of course it can be used to track major ocean currents. Knowledge of currents is useful for understanding the ocean ecosystem and for navigation. But this data will also be used to build models of climate and weather patterns, predict the movement of pollution spills, and even to assist with forecasting the path of approaching hurricanes.

Personal Log

I finally feel like I am becoming useful as a scientist on this cruise, not just an interested observer. Although I have been busy helping from Day 1, I am gaining confidence about conducting some parts of the work on my own. I have learned to collect and preserve the plankton samples, process water samples for chlorophyll, and operate the CTD (Conductivity, Temperature, and Depth), a computer linked instrument that measures oceanographic data. This morning I was up in time to watch a beautiful sunrise and had time to do a load of laundry during a long steam between stations. We had a raft of seabirds sitting hopefully off the stern while we were stopped for some work, and the weather is cool and sunny. It’s a beautiful day in the neighborhood!