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Wesley Struble, 23 July, 2010

NOAA Teacher at Sea
Wes Struble
Onboard NOAA Ship Ka’imimoana
July 8 – August 10, 2010

Mission: Tropical Atmosphere Ocean (TAO) Cruise
Geographical area of cruise: Equatorial Pacific from 110 degrees W Longitude to 95 degrees W Longitude
Date: Friday, 23 July 2010

Weather Data from the Bridge

Current location: 4 degrees South Latitude & 110 degrees West Longitude
Cloud Cover: 5/8
Cloud Type: Stratocumulus
Visibility: 10 nautical miles
Wind Bearing: 100 degrees
Wind Speed: 20 Kt
Wave Height: 2 feet
Swell Height: 5 – 7 feet
Barometric Pressure: 1015.5 mb
Temperature: 24.8 degrees C (76.6 degrees F)

Science and Technology Log

There are a variety of buoys used by NOAA in the Pacific Ocean. One of the more interesting is the ADCP buoy. ADCP stands for Acoustic Doppler Current Profiler. This buoy is anchored to the sea floor like most of the other buoys deployed on this cruise. The major difference is that the ADCP buoy does not float at the surface but rather is tethered with a line short enough to keep it submerged approximately 300 meters below the surface of the sea. In addition, it is only deployed with the TAO buoys at the equator and not at any of the other TAO buoy locations. The buoy’s name defines its function – current profiling – using acoustic signals (similar to sonar) the buoy provides a profile (or vertical map) of the ocean currents from the depth at which the buoy is tethered to the surface. The ADCP is able to measure both the speed of the current and the direction in which it is moving. Even though the TAO buoy at the same latitude is generally visited more often, the ADCP buoy is visited only once per year. During the visit the buoy is retrieved, cleaned, damaged parts replaced or repaired, data downloaded, batteries replaced, and sensors upgraded (if necessary).

Buoy with newly attached ADCP unit – A
KA skiff at the ADCP buoy

The flotation component of the buoy is a large orange sphere just over four feet in diameter. This float is made of syntactic foam. In general, foam is a mixture of two substances: a gas phase in a solid or liquid phase. Syntactic foam should not be confused with the common foam with which we are all familiar (like the typical Styrofoam coffee cup). Most of these foams are generally composed of expanded polystyrene (a thermoplastic polymer) where the gas phase is air and the solid phase is polystyrene. Syntactic foams on the other hand use other substances for the components.

The ADCP acoustic transmitters & receivers

One of the more common syntactic foams uses small glass spheres 10 – 200 micrometers (millionths of a meter) in diameter. These glass spheres are filled with air during the manufacturing process. The spheres are then mixed in with some type of epoxy resin and allowed to cure to produce the foam. The buoyancy of the foam is affected by the size, number, and wall thickness of the glass spheres. Some of the applications that typically utilize syntactic foams are the manufacture of radar transparent materials, acoustic attenuating materials, and more specifically deep sea buoyancy floats. Our float is anchored to the sea floor with a large (several thousand pound) weight that prevents it from drifting. The material used to attach it to the anchor is very stable and exhibits little elongation under tension, thus keeping the buoy consistently at the same depth. The payload (the ADCP itself) is approximately 1 meter long and about 20 centimeters in diameter and is mounted in a circular well that is bored vertically through the center of the float. The ADCP has four sending/receiving units mounted at the top of the main body. One can see these in the photographs. These units send and receive a 75 kHz signal that reflects (echoes) off the sea/air boundary and returns to the buoy.

When we were close to the location of the ADCP buoy one of the scientists activated an acoustic trigger that released the buoy from its sea floor mooring anchor. Since it was almost 1000 feet under water it took a few minutes for the float to reach the surface. When the buoy was spotted the ship made a slow pass to visually inspect the float and to launch the skiff. The skiff towed a long and very strong line from the ship which was then attached to the top of the buoy. At this point the skiff was brought back aboard. The ship then came about so that the buoy was directly a stern. When all was ready the winch began to retrieve the line and slowly bring the buoy on board. When it reached the deck of the fantail it was made secure and the tether line (that attached the buoy to the anchor) was tied off to a chain on the ship’s deck.

Working on the ADCP buoy on the fantail of the      KA – B

The buoy was then disconnected from its tether line and the line was attached to a large winch and all several thousand meters of it was rolled onto a number of large empty spools and stored on board. While the anchor line was being retrieved the science crew downloaded the stored data from the ADCP and prepared the buoy for redeployment. When the deck hands were ready the process was reversed. First, the tether line was attached to the buoy and it was lowered over the fantail. Then the line was slowly played out. When the ship was in the appropriate position she began to move forward as the crew played out line. When they reached the end of the line a large (several thousand pound) anchor was attached, lowered, and released. This entire process took the better part of a day.

Crew member Nemo McKay & Scientist Will Thompson retrieving the ADCP buoy

Personal Log

I have enjoyed getting to see the crew work together. One can tell that they clearly get along well and appear to enjoy working together because of all the friendly banter that passes between them. I have been impressed with how conscious they are about safety. I have been able to begin participating in some of the work deck activity during the buoy operations and it has helped in my understanding of what actually takes place. It has also helped me to get to know a number of the crew members better.

“Did You Know?”

Did you know that the greatest buoy equipment problem that occurs in this area of the ocean is vandalism? Many of the buoys are damaged, stolen/cut loose, or destroyed. This might be done either out of anger and frustration, for financial gain (the buoys have quite a large mass of aluminum framing and electronic equipment), or by accident. Regardless of the reason, much time, data, and financial resources are lost and consumed in maintaining TAO array in the Pacific Ocean.

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Kathy Schroeder, May 13, 2010

NOAA Teacher at Sea
Kathy Schroeder
Aboard NOAA Ship Oscar Dyson
May 5 – May 18, 2010

Mission: Fisheries Surveys
Geographical Area: Eastern Bering Sea
Date: May 13, 2010

5/13 My boat ride!

Getting on the rescue boat
Getting on the rescue boat

After the ship made it’s way through the ice we made it to our destination, which was about 2 miles off the island of St. Paul. We were supposed to arrive around noon, but it wasalready almost 3. We were there because the scientist (Bill) who was in charge of releasing the Mooring buoy had to get to the airport for a flight at 4. Bill was supposed to get off the ship when it came into port on May 3, but due to ice he was unable to release the buoy on the last trip, so he stayed onboard and was able to release it on this trip.

On the rescue boat
On the rescue boat

While on the bridge the CO (Commanding Officer) asked who wanted to go on the rescue boat to take Bill, and I smiled and raised my hand. He asked if I really wanted to go—of course I said yes! Next think I knew I was putting on my foul weather gear (the orange jacket and pants), gloves and boots. The boat can only hold 4 people so Dennis, Amber, Bill and I got ready to leave. As we were waiting I got to see Grey whales off in the distance. I would guess about 4 of them. They lowered the boat, with Dennis and Amber aboard, into the water with a crane. The boat then came around the starboard side to pick up Bill and me. We had to climb down the Jacob’s ladder (about 9 meters from the ship to the boat) to get onboard.

Being pulled back up onto the Dyson
Being pulled back up onto the Dyson

I was the last one in. We were on our way. Or so we thought. Dennis started yelling to the ship that he lost throttle. Could only go forward-not reverse. We came back to the ship and tied up. The waves were really pushing us into the ship. They told Bill and I to get out. An engineer climbed down, and 5 minutes later the problem was solved. It was just a pin that had come loose inside the gearbox.Time to board again! And we were off to St. Paul. The waves were nice and rolling so we didn’t get a lot of splash. We went past a red metal buoy that was really dented. Look like a boat ran it over, but they said it was from the ice. The dock where we were supposed to drop off Bill had been taken out of the water because of all the ice.

We went to a boat ramp and let him off there. Amber and I took our picture on St. Paul. Back in the boat—time to get back to the ship.The ship looked so little and far away, but we made it back in about 15 minutes. It was much rougher going this direction. This time I got to say on the boat as they attached the crane and brought us up. I was nothing but smiles for the rest of the day. This has to go down as the best day so far. Started off with sea ice, found my chapstick I lost about 4 days ago, went in the rescue boat, saw a Grey whale, filet mignon and au gratin potatoes for dinner, and played Apples to Apples for the first time. Wow! What a day!

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Christine Hedge, September 13, 2009

NOAA Teacher at Sea
Christine Hedge
Onboard USCGC Healy
August 7 – September 16, 2009 

Mission: U.S.-Canada 2009 Arctic Seafloor Continental Shelf Survey
Location: Chukchi Sea, north of the arctic circle
Date: September 13, 2009

Weather Data from the Bridge 
Latitude: 720 44’N
Longitude: 1560 59’W
Temperature: 350F

A Seasonal Ice buoy with a thermistor chain is deployed from the Healy. This buoy starts in open water and later may
A Seasonal Ice buoy with a thermistor chain is deployed from the Healy. This buoy starts in open water and later may freeze into the ice. This instrument collects ocean and air temperature data, barometric pressure data, and location data.

Science and Technology Log 

Buoys and Moorings And Gliders, Oh My!!! 
Exploring the oceans has a lot in common with exploring space.  NASA can send manned or unmanned missions into space.  Sending manned vehicles into space is more complicated than launching a probe or a telescope. The same is true for exploring the Arctic Ocean.  We can collect data on an icebreaker, manned with Coast Guard and science personnel or use instruments that can send back data remotely.  On this mission, many instruments have been deployed to send back data about the conditions in the Arctic. These instruments continue to do their work after the crew and scientists from the Healy have moved on.  Ice buoys, which float or freeze into ice floes, are one example.  The HARP instruments (High-frequency Acoustic Recording Package), which sit on the sea floor, are another.

A United States Navy team, under the supervision of Navy Commander William Sommer, has launched a very interesting instrument from the Healy called the Seaglider. We have been tracking its movements since it was launched on August 8th. The Seaglider collects information about the salinity, temperature, and optical clarity of the ocean. The Navy is interested in how sound travels through the oceans and this glider is an important tool for doing just that.

CDR Bill Sommer, AG1 Richard Lehmkuhl, and MST3 Marshal Chaidez deploy a Seaglider from the Healy in the Chukchi Sea. Data from the Seaglider will improve the performance, and aid in the evaluation, of the effectiveness of the ocean models in the Arctic. Photo courtesy of PA3 Patrick Kelley, USCG.
CDR Bill Sommer, AG1 Richard Lehmkuhl, and MST3 Marshal Chaidez deploy a Seaglider from the Healy in the Chukchi Sea. Data from the Seaglider will improve the performance, and aid in the evaluation, of the effectiveness of the ocean models in the Arctic. Photo courtesy of PA3 Patrick Kelley, USCG.

What makes the Seaglider unique is that instead of just drifting, it can be driven.  In fact, this instrument is directed via satellite from a computer lab in Mississippi!  The glider moves up and down in the water column and like an air glider it uses this up and down motion to move forward. It has a GPS and a radio so that it can communicate its location. The Seaglider deployed from the Healy in August was picked up today.

Final check of the Seaglider before it was launched.
Final check of the Seaglider before it was
launched.
The green dots indicate the path of the Navy Seaglider as it collected data in the Chukchi Sea.
The green dots indicate the path of the Navy Seaglider as it collected data in the Chukchi Sea.
Coast Guard and Navy personnel work together to retrieve the Seaglider on September 13.
Coast Guard and Navy personnel work together to retrieve the Seaglider on September 13.
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Rachel Dane, May 3, 2005

NOAA Teacher at Sea
Rachel Dane
Onboard NOAA Ship Ka’imimoana
April 29 – May 10, 2005

Mission: Oceanographic Survey
Geographical Area: Puerto Ayora, Isla Santa Cruz, Galapagos
Date: May 3, 2005

Plan of the Day
0300: 0.5S CTD
1200: Equatorial mooring repair followed by a deep CTD and an ARGO
1845: 0.5N CTD
2345: 1N CTD

Weather Data
Latitude: 0 degrees N
Longitude: 94 degrees W
Visibility: 12 nautical miles
Wind Direction: 150 degrees
Wind Speed: 12 knots
Sea wave height: < 1 foot
Swell wave height: 2-3 feet
Sea water temperature: 26.5 degrees C
Barometric pressure: 1013.0
Cloud cover: 2/8 cumulus, cirrus

Science and Technology Log 

Today is my first full day on the KA’IMIMOANA (KA).  After sleepily answering my 3:30 AM wake-up call and quickly grabbing a hot cup of caffeine, I met Shawn and Jay on deck to begin the first CTD cast of this second leg of the KA’s journey along the equator. CTD is an acronym for “Conductivity, Temperature, Depth”; it is essentially an analysis of the salinity and chlorophyll levels of a site specific water sample. The casts are performed at each 1 degree change in latitude along the entire TAO array.  The CTD “package” consists of 15 cylinders, each about 1.25m high, attached to a sensing apparatus. Based on commands from the deck, this sensing apparatus will open and close the cylinders and provide real-time data of water conductivity, temperature, density and salinity. For the purposes of this morning’s sample, the package was lowered to a final depth of 1000m for sample collection.  Final depths vary with each cast.  Once the cask is deployed, data analysis of the water sample is displayed graphically on a nearby computer—this morning I was able to view a graphical representation of the thermocline for the first time!

Before lunch, I shadow Doc during her weekly safety inspection.  What a great opportunity for me to see the inner workings of this impressive vessel!  After lunch, the announcement that we have arrived at the site of our first buoy repair comes echoing over the loudspeakers, and it’s buoy time!

The equator! For me, it’s no longer simply a line around the globe.  Not only does the equator represent the dividing line between the northern and southern hemispheres of the earth, but this is also the region where Pacific ocean currents are being extensively studied by NOAA in order for us to better understand the relationship between the oceans and climate.  Essentially, the TAO buoy array acts as a 6000 mile antennae that scientists use to monitor ocean trends.

Donning hard hat and life jacket, I ran to the third deck clutching my zip locked camera and climbed into one of the orange work rafts attached to the KA’s port side.  We (Dave, Brian, Chris, Matt and I) were gently lowered into the water by attentive crew members, and off we motored to our waiting buoy, about 75m away.  Unfortunately, this buoy had been damaged by a fishing vessel so Dave and Brian had some repairs to make.  Fish prefer to swim in the vicinity of buoys because schools feed on the growth that accumulates on the underside, and it is quite common for large fishing vessels to tie up to TAO buoys; oftentimes damage occurs in the process.  After the repairs were complete, I was enthusiastically invited to jump onto the mooring buoy, and it was the absolute highlight of my day! Since fish like to hang out by the buoys sea birds do too; this was immediately obvious to me once I had hopped onto the platform and was clinging to the rungs of the tower.

The entire apparatus was covered from top to bottom with dried guano, and within minutes of climbing and perching on the tower, so was I!  Kind of gross; however, this did not prevent me from reveling in the experience of being on the equator and bobbing like a cork, completely and utterly surrounded by water.  It felt as though I had stepped into a completely foreign liquid universe.  Other than our work boat, the only object in the panoramic view was the KA’IMIMOANA headed towards the horizon. I believe that I could have very happily floated on that buoy for the rest of the day, reveling in the vastness.

Once back in the orange raft, our expert coxswain Chris kicked it into turbo gear and off we sped on a high speed chase, in hot pursuit of our ocean home.  Although the KA remained in sight for the entire operation today and although I longed for more time bobbing in the serene, blue stillness of the equatorial Pacific, there was a feeling of extreme comfort in riding to port side of the mighty Ocean Seeker.  Looking up, we saw 10 of our crew members peering anxiously over the rails on all decks, ready to work together to bring us home safely.

Personal Log

On a daily basis, I continue to be amazed by this ship.  So many aspects of life aboard the KA’IMIMOANA are extremely refreshing: that it is a floating home that operates so efficiently through the patience, teamwork and cooperation of all hands, that a hallway passing almost always evolves into a friendly conversation, and that crew members are consistently willing to share their knowledge and experience with me and excitedly teach new information.

Despite my best intentions and despite a 4.5 mile run on the treadmill, I was not able to squeeze in a rest this afternoon. Now it’s 10:30pm and I’m feeling exhausted, but too overwhelmed to sleep.  This evening I studied the Southern Cross and surrounding constellations with Don. Although I live at the Grand Canyon and regularly study extremely impressive night skies, the stars here rival what I’ve become accustomed to at home.  Thanks to Jimbo’s call I watched over 100 squid swarming on our starboard side, and kudos to Tony–his expert fishing skills have ensured that we will all enjoy fresh calamari tomorrow night!  Matt was the first person to introduce me to an actual example of bioluminescence tonight, visible in the ship’s wake; thank you, Matt, it was so incredibly cool! I definitely plan on taking him up on his offer for me to borrow the “Blue Planet” series to learn more about deep ocean luminescence.  So, brimming with curiosity and excitement, I look forward to the gentle rocking of the ship once I tumble into my bunk later this evening.

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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 17, 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 17, 2004

Location: Latitude 19°40.26’S, Longitude 89°46.38’W

Weather Data from the Bridge
Air Temperature (Celsius) 19.59
Water Temperature (Celsius) 20.13
Relative Humidity (percent) 73.07
Air Pressure (millibars) 1017.14
Wind Direction (degrees) 101.42
Wind Speed (knots) 15.44
Wind Speed (meters/sec) 7.67

Question of the Day

What are the ship’s three types of motion?

Positive Quote of the Day

“Never say “No” to opportunity.” Melvin G. Marcus

Science and Technology Log

Today, we made the big turn toward the San Felix islands and we’re heading southeastward at 12 knots. We did our last CTD cast of the cruise! Several of us decorated more Styrofoam cups to send down for compression by the pressure of the ocean water at 1000 meters depth. This afternoon and for the remainder of the cruise we will be tossing drifting buoys and Argo floats over board from the fantail. The Argo float has a bladder that inflates and deflates to allow it to go down to 2000 meters, drift in the current for about 10 days, and then record temperature and salinity as it comes back to the surface. It then transmits the data to a satellite where it is then sent to a ground station. The Argo float goes up and down over and over until the battery runs out. These floats are never recovered. It is hoped that there will be 3,000 of them in the oceans by 2006.

As we toss the drifters we are doing a promotional video segment to describe what a drifter measures and encourage teachers and their students to adopt a drifting buoy. This is a great way to get real science in the classroom. The Adopt a Drifter Program is sponsored by NOAA’s Office of Climate Observation and can be accessed online at http://osmc.noaa.gov/OSMC/adopt_a_drifter.html.

This afternoon Diane and I toured the ship and recorded it with the video camera. We went to the galley, mess hall, our stateroom and toilet room, the ship’s bow and the bridge. The bridge is where the ship is driven. While on the bridge, we spoke with NOAA Corps officer Silas Ayers and he explained how they record and report the weather observations to the National Oceanic and Atmospheric Administration (NOAA) offices located back in the United States. Tomorrow, he will give us a complete tour of the bridge.

In “6:00 Science on the Fantail”, we interviewed Chris Fairall, a physicist/mathematician who works for the NOAA Environmental Technology Lab (ETL) based in Colorado. Chris explained some of their instrumentation for measuring clouds and precipitation. He said that some of their instruments can individually measure the smallest of mist droplets! They have worked closely with the Woods Hole Oceanographic Institution over the past few years to compile data for the stratus cloud deck over this part of the Pacific Ocean. Chris said that the main reason this particular location was selected for the study was lack of data because it had never been thoroughly studied.

This evening, Diane and I continued the writing of the children’s book documenting this Stratus 2004 cruise.

Personal Log

Today has been another good day at sea. I’ve gotten emails from students, family and friends. I’ve had good food to eat and good conversation and laughter with new friends. I spent some quiet, alone time to ponder and count my blessings. The sun momentarily broke through the stratus clouds like a smile from up above! We tossed some Argo floats and drifters overboard. We’re steaming ahead to new and exciting places! What more could I ask for?

An observation: the Argo float is tossed in the water without removing the biodegradable cardboard box, so it looked to me like a casket as it floated away in the wake of the ship. I guess it really is a burial at sea because the Argo floats are never recovered.

Paul and I are about to deploy another Argo float shortly. This will be my first Argo float where I actually get to do the hands-on tossing! I’ve just been observing up until now. We’ll lower it by a rope over the back of the fantail then release it into the water.

Another observation: As the ship steams along it is rolling and pitching. All that motion causes stuff to shift and creak and rattle. Even if I’m in a room all alone, I still feel like someone else is there, too. It’s an odd sensation to hear a noise, turn expecting to see someone and nobody is there!

I look forward to tomorrow. We have a couple of interviews and will continue working on the book plus tossing a few more drifting buoys and floats along the way.

Until tomorrow,

Mary

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Mary Cook, December 14, 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 14, 2004

Location: Latitude 19°45.13’S, Longitude 85°30.82’W

Weather Data from the Bridge
Wind Direction (degrees) 164.30
Relative Humidity (percent) 75.74
Temperature (Celsius) 18.60
Air Pressure (Millibars) 1016.02
Wind Speed (knots) 15.33
Wind Speed (meters/sec) 8.40

Question of the Day

Why do you think the floaters are made of glass?

Positive Quote for the Day

“Patience is passion tamed.” Lyman Abbott

Science and Technology Log

At about 5:30 this morning the WHOI guys are up early and ready to go! This is the day that the new and improved Stratus 5 surface mooring is deployed! It’s what everyone has been working toward. My understanding is that first, the mooring line and upper 50 meters of instruments will be put in the water and attached to the buoy. Second, the buoy will be deployed with a quick release hook off the port side. Then the ship will move ahead to bring the buoy behind it. Next, the ship will slow down and move ahead as needed to keep the buoy aft while the crew attaches the remaining instruments. The last things to be put on the mooring line are the glass ball floaters, the acoustic release, and then the 9000 pound anchor. We’ll wait around for a couple of hours for the anchor to sink and settle, then, they’ll take a Seabeam (echo-sounding) survey of the ocean floor where the anchor is located. After the survey, we’ll move downwind of the buoy and tomorrow inter-comparison testing will begin.

Now, it’s 5:30 in the afternoon, and all the hard work is completed. Everything went off without a hitch. Well, almost. There were a couple of tense moments throughout the day, but all in all it went very well. The planning and orchestration of the whole process is quite amazing with several people communicating with radios and hand signals, all getting it done just right.

At “6:00 Science on the Fantail”, we interviewed Keir Colbo who works for Woods Hole Oceanographic Institution. He shared with us his duties for the day. According to Keir, his job is to stay out of the way and record everything in a logbook. I mean everything. Keir wrote down the deployment time, serial number and order of every instrument that went into the water. He counted every glass ball floater (total 90). He recorded the Global Positioning System (GPS) reading of the anchor as it was dumped into the ocean. GPS uses a receiver to locate an object by detecting a series of satellites. Keir also explained the glass ball floaters. They are 5/8 inch thick glass domes with a diameter of 17 inches. The glass balls are put into bright yellow plastic hulls that protect from breakage and enable them to be chained together. Keir’s job is very important even though at times it may seem monotonous. When the scientists return next, his records will be the first thing they pull for references to make sense of the science.

Personal Log

It’s 5:30 Tuesday morning and I am sitting at my desk thinking about the day that’s before us. The ship is constantly moving with the ocean motions. There’s no way to get away from it – it’s always a presence with me. I can’t help thinking that we’re atop something alive and breathing. Every time there’s a swell it feels like the ocean is taking a deep breath and then slowly exhaling. It reminds me of the rhythmic breathing of someone who is asleep. I must admit, I can more easily understand why some ancient cultures worshipped the ocean or devised amulets for protection from the spirits of the ocean. Well, I don’t worship the ocean but everyday I gain a deeper respect and appreciation for it – for its vastness, and power and how much all of life on Earth is so intricately dependent upon its wellbeing. Even living things that are a long way from the ocean like in Arkansas, or south central Siberia, depend on the ocean.

I enjoyed today. We watched all the guys working in unison to get the work done which has danger lurking around every corner. These guys are safety-minded, too. They do things right and they watch out for each other. It’s also cool to see the Chileans and Americas working together. It’s like it should be. My least favorite part of the day was waiting for all the cable to reel out. I took a nap. My most favorite part of the day was when the 9000 pound anchor was dumped overboard! What a BIG splash! It sounded like someone doing a cannonball at the city swimming pool. Everybody was smiling.

Happy Birthday, Deano.

Until tomorrow…..

Mary

Posted on

Mary Cook, December 13, 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 13, 2004

Location: Latitude 19°45.88’S, Longitude 85°30.36’W

Weather Data from the Bridge
Wind Direction (degrees) 147
Relative Humidity (percent) 72.19
Air Temperature (celsius) 19.34
Water Temperature (celsius) 19.36
Air Pressure (millibars) 1015.75
Wind Speed (knots) 15.71
Wind Speed meters/sec 8.08

Question of the Day

Why aren’t light waves or radio waves used for ocean exploration?

What is a nautical mile?

Positive Quote for the Day

“The Earth is given as common stock for man to labor and live on.” Thomas Jefferson, letter to James Madison, 1785

Science and Technology Log

Today the Woods Hole scientists are making preparations for the new Stratus 5 mooring deployment. Early this morning Paul and Jason were placing the CTD units in ice water to spike the temperature sensors and set the clocks on each unit. Using cranes, winches and ropes, the boatswain and his crew in conjunction with the WHOI scientists moved the old Stratus 4 away from the launch site and put the new Stratus 5 in position for tomorrow. All the instruments are being readied and the ship is making a horseshoe-shaped transit as the Seabeam records echo soundings from the ocean floor. Echo sounding is when sound waves are sent to the bottom and then bounced back to a receiver. This can then be used to show the depth of the ocean at that location. The Seabeam can make an 8 kilometer-wide reading as the ship moves along. The computer display of the ocean floor looks like several parallel ridges. Bob Weller says the ship is also running parallel to those ridges which will aid in the placement of the anchor. If we were going perpendicular to the ridges the anchor deployment would be more difficult and hampered by the ship going against the trade winds.

We had our weekly fire and abandon ship drills and they announced that we are over 800 nautical miles from Chile. The San Felix islands are about 300 nautical miles from here. All of the WHOI guys have turned in early because tomorrow is an even bigger day than yesterday!

Personal Log

OK. I know I wimped out last night. Sorry. So today I’ll try to do better. Besides being really tired last night, it was windy and the ship’s motion tossed me back and forth in the bed. All night long I had the instinctive feeling that I needed to hang on tight to the railing. Even when I was asleep, there was a persistent apprehension in the back of my mind that I was about to be thrown from my bed!

Yesterday, everyone worked outside so much that today we’re all sunburned and have red noses. It doesn’t seem to matter how much sunscreen I use, the sunrays still penetrate and zap me.

I’ve been working on my lesson plans and, boy, do I have some of the greatest resources! Chris and Dan, the meteorologists sat down with me and we brainstormed some radiosonde lesson plan ideas. Diane has given me some great input and is helping it all come together. I want these lesson plans to be useful, practical and interesting all the while meeting or exceeding our state and national education standards.

It’s a beautiful sunshiny day (which is rare here) and the white capped waves skipped across the indigo-colored waters as far as the eye could see. Very picturesque. I wanted to go out to the ship’s bow but the wind was whipping around too strongly. I enjoyed watching the guys move the two buoys into position. It’s fascinating to watch big machinery work. My stomach got a little tense when the buoy was suspended by ropes in midair and the ship’s motion caused it to swing. There’s just not much room for error on the fantail because there’s equipment stored everywhere. But the guys did a great job and made it look easy. “All in a day’s work” is what they say. I’m still impressed.

“Chester”, one of the young men in the Chilean navy, just showed us his CD photos of Antarctica, when he was there for research and training. His research was with whales. He said that he took biopsies of whales. That sounds dangerous to me, but the photos were so cool! (pun intended)

I got more emails today from school and family. It always makes me smile to open the messages and read what’s happening back home. It’s an encouragement to know that out of sight doesn’t mean out of mind. I have to say, I’m missing my students. I’ve never realized how much energy they give me. I think about them often. I’ll be glad to see them again in January.

Well, this has been another great day for this Teacher at Sea!

Until tomorrow…

Mary

Posted on

Mary Cook, December 12, 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 12, 2004

Location: Latitude 19°46.24’S, Longitude 85°30.89’W
Time: 7:00 am

Weather Data from the Bridge
Wind Direction (degrees) 145.06
Relative Humidity (percent) 80.68
Air Temperature (Celsius) 19.22
Water Temperature (Celsius) 19.32
Air Pressure (Millibars) 1014.64
Wind (knots) 13.76
Wind Speed (meters/sec) 6.53

Question of the Day

Why are the water and the air temperatures nearly the same?

Positive Quote for the Day

Physical concepts are free creations of the human mind, and are not, however it may seem, uniquely determined by the external world. Albert Einstein, Evolution of Physics

Science and Technology Log

Today’s the big day! The Woods Hole Oceanographic Institution scientists will begin bringing the old Stratus 4 buoy onboard the RONALD H. BROWN. They’ve enlisted the help of just about everyone on the ship. At 6:00 this morning, the sky was dark blue and overcast. As daylight began to creep in, we all gathered in the main lab to prepare for the day’s work. First of all, the scientists triggered the acoustic release at the bottom of the ocean which is about 4400 meters deep. This released the buoy and array of instruments underneath it from the anchor. The 9000 pound anchor was left on the ocean floor. Then we waited.

And waited. And waited some more. It was about 45 minutes in all. We were waiting for the floats to come to the surface. The floats are big glass balls covered in yellow plastic hulls. They’re about the size of a medicine ball. And they are heavy, too. Wouldn’t you think a float would be lightweight? After the floats popped up out of the water, David, Phil, Jason and I went out on the RHIB to hook onto them and tow them to the ship. Once again the RHIB ride was awesome!

Pulling the floats onto the ship began the whole process of reeling in the old Stratus 4 mooring. This took all day. First they reeled in all the cable connecting the surface buoy to the anchor. At the beginning the buoy was a little speck near the horizon but as the cable got shorter, the buoy got closer and bigger until it was just behind the ship. That alone took several hours. When the instruments began coming in, we had to log and photograph each one. Then another RHIB ride was in order!

This was the RHIB ride of my life! Jeff, Diane, Jason, Phil and I went barreling across the swells and hit a wave that bounced Jason into midair for a second or two! I was hanging on with all my might and waves came over the edge right into my face. When we arrived at the buoy the guys hooked onto it and we towed it back to the ship. Then the crew on the ship hauled it aboard with a crane. While they were hauling it in we stayed out in the RHIB and pitched and rolled. That’s when I started to feel a little bit green. Fortunately, we were soon retrieved but on the starboard side of the ship…home, sweet home. We then watched the final removal of subsurface instrumentation. Wow! The Stratus 4 buoy was covered in amazing barnacles! Big ones and little ones. Long-necked barnacles are bizarre looking creatures. They attach themselves to anything in the water, just like suction cups. It’s like they’re stuck on with Super Glue. Once everything and everyone was safely onboard we had a barnacle scraping party. All available hands scraped those little rascals off and threw them back into the ocean. It was a mess but with everyone pitching in things got nicely cleaned. Tomorrow, we get everything ready for the deployment of the new and improved Stratus 5 buoy!

Personal Log

I am so tired.

Until tomorrow,

Mary

Posted on

Mary Cook, December 11, 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 11, 2004

Location: Latitude 19°44.43’ S, Longitude 85°32.17’ W
Time: 9:30 pm

Weather Data from the Bridge
Wind Direction (degree) 134.18
Relative Humidity (percent) 74.66
Temperature (Celsius) 19.46
Air Pressure (Millibars) 1014.06
Wind Speed (knots) 15.04
Wind Speed (meters/sec) 8.14

Question of the Day

When we send the Styrofoam cups down to 3000 meters in the ocean, what will happen to them and why?

Positive Thought of the Day

“I think laughter may be a form of courage. As humans we sometimes stand tall and look into the sun and laugh, and I think we are never more brave than when we do that.” Linda Ellerbee

Science and Technology Log

This morning we arrived at the Stratus 4 buoy site! The buoy looked so small bobbing out there all alone on the ocean. David Owen took Jeff Lord, Phil Pokorski and I for a boat ride in the RHIB (rigid hull inflatable boat). The RHIB is an orange raft-looking motor boat. The RHIB is raised and lowered into the water on a lever lifting device called a small boat launch. We went out to make a quick inspection and to see if the temperature sensors were working. Jeff said it all looked pretty good and there weren’t as many barnacles as he’d expected. He took pictures then we returned to the ship. Today, all the scientists are quietly working on inter-comparison testing with the ship’s sensors and the buoy.

At “6:00 Science in the Main Lab”, we interviewed Jason Smith, an engineering technician for Woods Hole Oceanographic Institution. Jason explained the instrumentation that will be attached to the bottom of the Stratus 5 moored buoy. The first instrument is a temperature sensor, which is an electronic device. It has a resistance that changes with temperature and that resistance can be measured with an electronic circuit. These instruments can also measure conductivity which is an indicator of salinity. In addition, there are various styles of current meters used. Some are mechanical and some use acoustics. All these instruments will be suspended at different depths with most of them concentrated from the surface down to 300 meters. One problem that they encounter is marine animals adhering to the instruments and fouling up their functions. Different types and colors of anti-fouling paints are being tested to see which one inhibits the marine life from sticking to the machinery. Jason emphasized that it was very important to develop an anti-fouling paint that is both environmentally safe and keeps the marine life from setting up housekeeping on the instruments.

This evening, Diane and I sat down to begin writing the children’s book about the cruise. Don’t let anyone ever tell you this is easy. But we’re progressing nicely and I can see an interesting book emerging.

Personal Log

Well, the last thing my mentor, Diane, said to me last night was “Tomorrow will be a more relaxing day”. So I thought, “I’ll sleep in and take my sweet time getting out and about in the morning.” You know, do some of those personal hygiene things we often take for granted like blowing our hair dry and trimming our toenails.

And so there I am peacefully sleeping like a baby being rocked when Diane comes in and says, “Mary, Bob said the RHIB is leaving in about 30 minutes!” At first, I thought I was dreaming, but then I realized, “This is for real!” Anyway, I jumped up and threw on some clothes and ran out to the small boat launch deck. Sure enough, they were getting ready to leave. I made it in just the nick of time! Yeah! Diane and Bob had my life vest, hard hat and radio ready. I grabbed them and climbed in.

The RHIB ride was awesome! It’s funny how the ocean swells look a whole lot bigger when you’re in a little boat than from the ship’s deck. As the boat zipped up and down across the surface, I was hanging on for dear life and ocean spray was splashing me in the face and running down my back to make a puddle right where I was seated. The buoy would disappear then reappear time and again.

Even in all this excitement and adrenaline rush, my mind was thinking about those early explorers like the Polynesians who launched out in small thatched boats. For a moment, I felt a cosmic connection across time and cultures. And then it hit me, “What were they thinking? This is nuts!” I mean they had to be daring and bold of personage to cast their lives onto the rolling, endless waters in search of the unknown. Then, I gazed back on the RONALD H. BROWN, my temporary home, floating like a little toy ship in a great big tub. I like that ship. It’s like my whole universe for the next 2.5 weeks. Then what happens? My universe will disappear and everyone will go to their own real world lives. I’m still trying to wrap my mind around that thought.

After we did a visual inspection of the buoy, we posed for pictures and zoomed back to the mother ship. As David pulled alongside the ship, Phil and Jeff grabbed the ropes and hooked us up to the small boat launch, then, the operator lifted the RHIB aboard. We banged against the boat launch so hard it knocked my hat off! It went tumbling around in the bottom of the RHIB. I felt like one of those persons who loses their hat in the wind and keeps chasing after it.

We were all wet but with great big smiles on our faces. Riding the RHIB was as good as the Zippin’ Pippin’ rollercoaster in Libertyland! I’m ready to go again!

Until tomorrow,

Mary