Tag: drifter buoy

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Mary Cook, December 19, 2004

NOAA Teacher at Sea
Mary Cook
Onboard NOAA Ship Ronald H. Brown
December 5, 2004 – January 7, 2005

Mission: Climate Prediction for the Americas
Geographical Area: Chilean Coast
Date: December 19, 2004

Location: Latitude 25°07.83’S, Longitude 81°54.62’W
Time: 0830

Weather Data from the Bridge
Air Temperature (Celsius) 19.04
Water Temperature (Celsius) 19.42
Relative Humidity (percent) 56.95
Air Pressure (millibars) 1018.17
Wind Direction (degrees) 155.6
Wind Speed (knots) 15.91
Wind Speed (meters/sec) 7.99
Sunrise 0734
Sunset 2116 (9:16 pm)

Questions of the Day

Why is the sunset so late in the day?

Positive Quote for the Day

“The world of achievement has always belonged to the optimist.” J. Harold Wilkins

Science and Technology Log

We tossed the last of fifteen drifting buoys this morning! It’s not the end, but the beginning of a wonderful new program. I’d say the Adopt-a-Drifter program got underway with a big splash! Teachers and their students around the world can adopt a drifting buoy just like my students at Southside Middle School in Batesville, Arkansas. They can map its path as it goes with the flow of the ocean currents. These drifting buoys also provide sea surface temperature and air pressure. This information can be utilized to gain a better understanding of the global oceans. I watched as Jeff and Bob deployed another Argo float. These floats are lowered over the back of the ship and when the quick-release mechanism comes in contact with the water, the powder in a small device dissolves and this releases a spring that unhinges the float from the straps. The straps are pulled back onboard as the ship leaves the Argo float in its wake.

I sat down and had a conversation with Chief Scientist Dr. Robert Weller of Woods Hole Oceanographic Institution about the importance of oceanic/atmospheric studies. He made some very good points that highlighted the fact that when just 1ºC of heat energy is released from the ocean water into the atmosphere it affects the air flows for thousands of miles. This then can be like a domino effect and continue around the globe influencing weather patterns for people everywhere.

At 2:00 we interviewed Richard Whitehead, Chief Steward. Richard is over the food preparation in the galley. Richard shared that he has been working on ships for over 40 years and has had several trainings for the position he now holds. He said that the menus were developed based on nutritional guidelines and availability of produce. Richard shared with us that they keep the produce fresh for weeks by keeping it very cool and placing it in special bags that slows the deterioration. He also said that there are many safety issues that concern food preparation on a moving ship. All the pots and pans are deep, there are railings on the stovetop, and special care must be taken with knives. The countertops must be covered with anti-slip cloths to keep everything from sliding around. He also said that they consider the weather when deciding what to prepare because you wouldn’t want to bake a cake while the ship was moving through rough waters.

We changed “6:00 Science on the Fantail” to “6:00 Science in the Van on the Bow” because we wanted to interview Jason Tomlinson of Texas A & M about his work with aerosols. First of all, Jason explained that an aerosol is not a spray can. It is a small particle in the air. Jason showed us the Tandem Differential Mobility Analyzer (TDMA). It looks like a mad scientist’s invention with wires, tubes, canisters, and radioactive components! It is one of the best devices in the world for analyzing small particles in the air. It draws in air from outside then dries the air. It then separates the particles according to size. Jason said that these particles are too small to see with the naked eye but they have a great influence on cloud formation and cloud life length. The TDMA can determine what the particles are made of by adding moisture or by adding heat. The TDMA costs about $70,000! He also showed us the Aerodynamic Particle Sizer (APS) which analyzes larger particles. They mostly get sea salt and dust out here in the ocean. Jason said that there’s a mystery about the sea salt and its influence on clouds. The APS costs about $35,000. He also said that occasionally they take in the ship’s exhaust and that destroys their data for that particular time. He concluded by saying that it all gets back to climate change and using these data to make better models for predictions.

After our interview with Jason, we ran outside to glimpse San Felix and San Ambrosio Islands! Our first land sighting in over two weeks! These small islands, located about 300 nautical miles from Chile, are volcanic in origin. They are basically huge, desolate rocks protruding up from the ocean floor. As far as I could tell nothing is growing on them. Seafaring birds do nest on the cliffs. Since 1975 the Chilean Navy has had an installation on San Felix Island where they operate a short airstrip, a weather station and a tide station.

Personal Log

I’m just beginning to realize that this trip is nearly over. We only have four days left. I knew it wouldn’t go on forever but as the old saying goes “time flies when you’re having fun”. What a superb voyage this has been for me-a voyage that is continuing my personal quest to search out the majesty of Earth. In doing so it is my heart’s desire to absorb the inexplicable magnificence of our Earth. I want to be permeated with awe for the splendor as I soak it in with my eyes and ears and nose and skin. I am amazed. How can I take it all in? Where was I when the Earth was formed and hung in the nothingness of space? From where did this splendor come? Clouds and rain and snow and hail are amazing! Mountains and valleys and canyons and caves are amazing! Oceans and rivers and glaciers and springs are amazing! Rocks and minerals and soil and sand are amazing! People and animals and languages and ideas are amazing! And they all work together in a symphony of overwhelming magnitude. I believe that we’re all an inextricable part of this grand masterpiece. Traveling is not the essential element in a voyage. Life is a voyage no matter where you are. Our voyage is how we perceive our surroundings, how we face our challenges, and how we come to Truth. Actually, none of us ask for this voyage called life. We’ve been thrust into it by forces greater than ourselves. So here we are. We do have some choices, though. Will we make the most of this journey or will we let it sweep us along without ever wondering, and questioning and being amazed?

Until tomorrow,

Mary

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Mary Cook, December 16, 2004

NOAA Teacher at Sea
Mary Cook
Onboard NOAA Ship Ronald H. Brown
December 5, 2004 – January 7, 2005

Mission: Climate Prediction for the Americas
Geographical Area: Chilean Coast
Date: December 16, 2004

Location: Latitude 19°44.39’S, Longitude 86°20.07’ W
Time: 8:00 am

Weather Data from the Bridge
Relative Humidity (percent) 72.50
Air Temperature (Celsius) 19.34
Water Temperature (Celsius) 19.78
Air Pressure (Millibars) 1016.06
Wind Direction (degrees) 97.86
Wind Speed (knots) 20.90
Wind Speed (meters/sec) 10.31

Question of the Day

When is the first day of summer in the Southern Hemisphere?

Positive Quote of the Day

“Most of us miss out on life’s big prizes. The Pulitzer. The Nobel. Oscars. Tonys. Emmys. But we’re all eligible for life’s small pleasures. A pat on the back. A kiss behind the ear. A four-pound bass. A full moon. An empty parking space. A crackling fire. A great meal. Hot soup. A glorious sunset” -Anonymous

Science and Technology Log

Yesterday was probably the last RHIB ride I’ll ever get to go on and last night at midnight, we left the Stratus 5 buoy all alone moored to the Pacific Ocean floor. I felt a little wistful.

So far today has been a quiet day. We’re steaming toward the San Felix islands. We’ve started watch duty again. Alvaro Vera and I have watch duty together from 8:00 am to noon and from 8:00 pm to midnight. This evening we’ll do another CTD cast. All the WHOI guys are dismantling the old buoy and packing up all the components to be sent back to Woods Hole. I finally got tons of email from my students and many of them are tracking the adopted drifting buoy which makes me proud of them. It seems I’ve spent half the day answering them. I’ve enjoyed it though. It’s good to have connection across the miles. We came out from under the stratus cloud deck and what a beautiful day! People are sitting out on the fantail soaking in the sun and warmth.

Personal Log

I’ve just been out on the ship’s bow peering over the edge to watch the ship slice through the water. It’s mesmerizing and clears my mind of thoughts. I think it’s like meditating. It’s especially calming to just look and listen and forget everything else. I see the many hues of blue in the water. I hear the waves splashing and the hum of the ship’s engine. The salty air feels clean in my lungs. Even the greens of the slimy algae growth just below the water line add another dimension to the sights and sounds of life at sea.

With a clear mind and clean lungs,

Until tomorrow,

Mary

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Mary Cook, December 10, 2004

NOAA Teacher at Sea
Mary Cook
Onboard NOAA Ship Ronald H. Brown
December 5, 2004 – January 7, 2005

Mission: Climate Prediction for the Americas
Geographical Area: Chilean Coast
Date: December 10, 2004

Location: Latitude 19°39.97’ S, Longitude 83°40.08’ W
Time: 9:30 a.m.

Weather Data from the Bridge
Wind Direction (degrees) 118.48
Relative Humidity (percent) 70.62
Temperature (Celsius) 18.99
Air Pressure (Millibars) 1015.61
Wind Speed (knots) 12.97
Wind Speed (meters/sec) 7.21
Cloud Type Stratus

Questions of the Day

What does CTD stand for? (answer is found in the previous logs)

What season is it right now in the southern hemisphere?

Positive Thought for the Day

“Life leaps like a geyser for those willing to drill the rock of inertia” Alexis Carrel

Science and Technology Log

Today Bob Weller and Jeff Lord of Woods Hole Oceanographic Institution (WHOI) helped me deploy two more adopted drifting buoys for Viviana Zamorano’s class at the Escuela America in Arica, Chile and Debra Brice’s class at San Marcos Middle School in San Diego, California! Their classes will be able to electronically access the drifter’s location along with the sea surface temperature and pressure. They can then use this information to study the ocean currents.

Late tonight and early tomorrow we will arrive at 19º45.91’S 85º30.41W , the location very near the Stratus 4 moored buoy that has been in the water for over a year. We will hover here for a day and conduct inter-comparison tests of the old buoy’s instruments with the instruments onboard the ship. This is a very important part of the research and data collection because they must prove that the information gathered is accurate. Accuracy of the data is of the utmost importance. After the testing is complete, they will begin the process of reeling in the old Stratus 4. This will take quite a while because there’s about 3 miles of cable to bring onto the ship. Then the old Stratus 4 will be hoisted onboard. I’ll give more details about the new Stratus 5 deployment as the time draws near.

This evening we interviewed Jeff Lord for “6:00 Science on the Fantail”. Jeff is a senior engineering tech for WHOI. He’s intricately involved in the new design of the Stratus 5. Jeff said that two really big changes in this new design are the construction materials and the modular-style architecture. The buoy is made of Surlyn foam, a tough but soft and buoyant substance. It can withstand wear and tear of whatever the ocean environment throws at it. Also, when taking it in and out of the water, if it bangs into the side of the ship, no problem! The other new design aspect is that the Stratus 5 can be taken apart and shipped in closed containers. The old Stratus design has a big aluminum hull that is one solid piece. It is too big to fit in a closed container, therefore the end of it sticks out about two feet. Jeff said that nowadays, transporting in open containers is very difficult because it limits the stackability and transportation companies find it difficult to deal with. Jeff also told us about the cables and ropes attaching the buoy to the 9000 pound anchor. The upper section is made of strong cable wire that can support the instrument packages and resist being bitten in two by fierce sea creatures. Then there’s lighter nylon rope that goes down nearly to the bottom and the last portion is made of a buoyant material so it doesn’t drag on the seafloor and get tangled. Jeff said to just wait until the old buoy is reeled in and new one deployed because it’s an impressive operation!

Personal Log

Today has been a good day. I like throwing the drifter buoys overboard. It only takes a few seconds but it makes me feel part of something important, something important on a global scale. This evening the sky is overcast but beautiful nonetheless. It’s cool and fresh out on the deck. I smiled to see that Phil has donned his reindeer antlers to set the holiday mood. Diane has been taking pictures of everyone and posting them on the doors. Bruce completed another great illustration for our book. It’s been approved for me to tour the engine room! The WHOI guys are getting excited because time is drawing near for the big buoy.

This afternoon I worked on developing lesson plans based upon the science work being done on the ship. I’m very excited about coming up with some practical and interesting lessons. Tonight during my watch, I am operating the radio as the Chilean university students perform a 3000 meter CTD cast. It takes about 3 hours to complete. Several of us have decorated Styrofoam cups and sent them down with the CTD rosette. Many people put Christmas greetings on them. Some of the Chileans put an American flag and a Chilean flag on their cups. I drew the Ron Brown ship with a “Christmas star” overhead. We are anxiously awaiting their return from the depths of the deep blue sea. I just found out that watch duty is suspended for the next five or six days! My watch times are good because they’re during waking hours but some people have the night shift plus an afternoon shift. So they’ll get a much needed break and get to sleep the night through instead of catching a nap here and there. Like I said, today has been a good day.

Until tomorrow….

Mary

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Mary Cook, December 8, 2004

NOAA Teacher at Sea
Mary Cook
Onboard NOAA Ship Ronald H. Brown
December 5, 2004 – January 7, 2005

Mission: Climate Prediction for the Americas
Geographical Area: Chilean Coast
Date: December 8, 2004

Location: Latitude 19°39.99’S, Longitude 77°07.27’W
Time: 8:30 am

Weather Data from the Bridge
Wind Direction (degrees) 126.27
Relative Humidity (percent) 72.01
Temperature (Celsius) 18.87
Air Pressure (millibars)
Wind Speed (meters/sec) 7.30
Cloud Type Stratus at 2810 feet

TODAY’S BIG NEWS!

I tossed the first adopted drifting buoy overboard with the help of Dr. Bob Weller of Woods Hole Oceanographic Institution! My eighth graders and I at Southside Middle School in Batesville are proud to be the first school to adopt a drifting buoy. We will periodically access the buoy’s coordinates online and track it as it moves with the ocean currents. It’s a great feeling to be a part of this important scientific endeavor!

Question of the Day

How do you think I can determine the exact elevation of the clouds?

Positive Quote for the Day

To be capable of steady friendship or lasting love, are the two greatest proofs, not only of goodness of heart, but of strength of mind. William Hazlitt (1778-1830) English essayist

Science Log

Yesterday evening, we had our first interview with a scientist. We’re going to try and schedule one every evening and call the session “6:00 Science on the Fantail”. The fantail is the back of the ship. It’s flat and open with an A-frame used to hoist and guide objects off of the ship. Alvaro Vera is an engineer with a Master’s degree in oceanography and is from the Chilean Armada (Navy). Alvaro and his team have been working for over a year preparing to deploy the first tsunami buoy in the Southern Hemisphere. They have trained in Seattle and gotten the buoy ready for this moment. A tsunami is a wave generated by an undersea earthquake. The instruments for this buoy can detect changes in pressure at the bottom of the ocean as small as 2 centimeters and will give the coastal areas about one hour warning. He said that about 100 years ago a tsunami devastated Arica on the coast of Chile. For this reason and continued threat, it is important that the Chilean population living along the coastal areas have ample warning of an impending tsunami.

Today, we sent several Styrofoam cups down to 1500 meters depth in the ocean. We decorated the cups with drawings, the date and location, then put them in mesh bags. When the cups were brought back to the surface they were miniatures! Styrofoam has air between the particles and as the water pressure builds during the descent the air is forced out and the cup is compressed.

This afternoon, two acoustic releases were tested. An acoustic release is used to release the buoy from the anchor at the bottom of the ocean by using a signal from the surface. One worked. The other did not. The working acoustic release will be used with the Stratus 5 moored buoy that is scheduled to be deployed this weekend. The acoustic release will sit at the bottom of the ocean with the anchor until this time next year. When the scientists come back to replace the Stratus 5 buoy with the Stratus 6 buoy, they’ll signal the release and it will separate the anchor from the buoy. The anchor is then left on the ocean floor.

Personal Log

This evening I went out on the ship’s bow and took a deep breath. My, the ocean is big. And blue. And deep. And always moving. Who can comprehend it? I know I’m just a little speck floating along the surface, but for some reason I don’t feel insignificant. I feel satisfied. And curious. I wonder how the early seafaring explorers felt? It doesn’t seem to matter whether I’m working in the lab, answering emails, wearing a hard hat and life vest on the fantail, or just sitting on the bow looking over the shimmering water, I really like what I’m doing. I’m getting to know some of the other people on board. As we waited for the acoustic releases to be pulled up from a depth of 1500 meters, I had the opportunity to just hang out with Bruce, Bob, and Paul. Bruce did his pirate’s “Aarrrgh” and told a bit about the true story of Moby Dick. Bruce Cowden is the ship’s boatswain. He and his crew keep the ship in working order. He’s also an artist and is illustrating a book about our cruise. His artistic talent is impressive. Everyday, I eagerly await his next illustration. Bruce designed the tattoos around his ankles which resemble Tahitian tiki idols. He said there’s one for each of his two sons. Bruce let me operate the A-frame hoist on the back of the ship as they were lowering the acoustic releases into the water. I felt like “Bob the Builder”! I have to say it is fun operating big machinery!

Today, I learned that both Jonathan Shannahoff who is the man in charge of all the CTD launches, and I have been to Lake Baikal near Irkutsk, Russia. I enjoyed sharing and looking at the pictures of his trip.

It seems to me that the people on this ship have been everywhere in the world. They’re just amazingly intelligent and adventurous individuals.

Until tomorrow,

Mary

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Mary Cook, December 6, 2004

NOAA Teacher at Sea
Mary Cook
Onboard NOAA Ship Ronald H. Brown
December 5, 2004 – January 7, 2005

Mission: Climate Prediction for the Americas
Geographical Area: Chilean Coast
Date: December 6, 2004

Location: Latitude 19° 50.49` S, Longitude 73° 22.51`W
Time: 8:30 am

Weather Data from the Bridge
Wind Direction (degrees) 144.45
Relative Humidity (percent) 68.72
Temperature (Celsius) 18.65
Barometric Pressure (Millibars) 1012.77
Wind Speed (knots) 11.36
Wind Speed (meters/sec) 5.51

Question of Day

Based on the name, what do you think a thermosalinograph measures?

Personal Log

Good morning, everyone! Wow! What a great way to get a good night’s sleep, in a gently rocking ship. It’s like sleeping on a waterbed. The morning shower was a challenge, though. Being wet and soapy even on a gently rocking ship could be very dangerous. After breakfast, we met with Dan Wolfe and Chris Fairall for radiosonde deployment training. A radiosonde is a really cool giant helium filled balloon with instruments attached to a cord dangling beneath it. The radiosonde must be assembled and calibrated before launching. As the instruments detect the relative humidity, wind speed, wind direction, and temperature readings they transmit these data back to the computer onboard the ship. A radiosonde lasts for about one and a half hours and goes about 20 kilometers (12.4 miles) high. Dan actually deployed a radiosonde and we watched it go up, up and away! Then we went back into the lab and observed the data coming into the computer. I can’t wait until it is mine turn to deploy a radiosonde!

Our next training session was led by Jeff Lord and he showed us how to deploy the drifter buoys and the Argo floats. These are fairly simple to get into the water. Just record their identification numbers, fill in the log sheet for time, date, GMT, latitude and longitude, then toss them overboard. The drifting buoys are small and they measure surface temperature and pressure. The drifters have a long caterpillar-shaped drogue extending far down into the water that ensures the buoy will drift with the ocean currents and not the wind. In a few days we will deploy the first of fifteen drifter buoys and my students at Southside School will adopt this one and keep track of it online. I am amazed at the designs of all these instruments. It’s almost unbelievable what ingenuity has gone into these designs. Some are high-tech and some are low-tech but they all work together to obtain the necessary data for the scientists.

The Argo floats sink down to 2000 meters then float to the surface. On their way up they measure temperature and salinity. When the float reaches the surface, it then sends the information to a satellite. The float has a bladder that deflates and it sinks again to repeat the process. The Argo floats can keep on going for two to four years depending on their battery life.

After our training sessions, Diane and I sat down with Bruce Cowden, the ship’s boatswain, who’s also an artist, to brainstorm for a children’s book about the science work of this cruise.

At 1415, we had our “surprise” safety drills: a fire drill and an abandon ship drill. The fire drill was pretty simple. Upon hearing the alarm, we reported to our muster stations. Then the chief scientist called the bridge and said that all persons were present.

The abandon ship drill was quite another story. When we heard the alarm, we had to go to our staterooms to get our life vests and emergency bag containing the big red “gumby suit”. Then we went to our lifeboat station and put on the suit. Its purpose is to keep you dry and afloat in the event you were forced to abandon the ship.

Diane and I are taking water surface temperature readings every thirty minutes. This is really kind of fun. There’s a thermometer in a tube-shaped “bucket”. The bucket is attached to a long cord. We then swing it over the edge of the ship into the water until the bucket fills up. We raise the bucket and read the temperature immediately. This is compared to the temperature reading on an instrument mounted underneath the ship called a thermosalinograph.

Later this afternoon, we finally arrived at the deployment site for the Chilean Armada tsunami buoy. We are about 200 miles off the coast of Chile. The ship hovered over the location while the buoy was hoisted by a crane then swung over the edge and lowered into the water. At this time the men are unrolling over 5000 meters of cable to attach to the anchors which happen to old railroad wheels. It will take about one hour for the anchors to sink to the bottom of the ocean. The bottom pressure recorder will then be lowered. It detects the slightest changes in pressure as small as two centimeters and sends messages back to the surface buoy which then relays that to a satellite which has direct ground communications. The ship will stay in this position for a few hours to make sure the tsunami buoy and ground pressure recorder are communicating with each other. A RHIB ride is in the near future!

And I hope I’m on it. RHIB stands for rigid hull inflatable boat and they go really fast! Some of the workers will be riding out to the tsumani buoy to check everything out before we leave it.

I’ve just found out that I will have morning watch each day from 0800 until 1200. Everyone on board is assigned a daily four hour watch duty. My duty will be in the main lab and I will stay in contact with the bridge and help out when needed.

So tune tomorrow for more on our exciting adventure!

Mary.