sediment core – NOAA Teacher at Sea Blog

July 1, 2019July 2, 2019

Betsy Petrick: Core Sampling in the Lab, June 30, 2019

NOAA Teacher at Sea

Betsy Petrick

Aboard R/V Point Sur

June 24 – July 3, 2019

Mission: Microbial Stowaways: Exploring Shipwreck Microbiomes in the deep Gulf of Mexico

Geographic Area: Gulf of Mexico

Date: June 30, 2019

Science Log

When the ROV returns to the ship, the scientists jump into action. The sediment cores are brought into the lab for sampling.

Core samples are loaded on the ROV in crates and with luck they all come back the same way.

Dr. Justyna Hampel, an aquatic biogeochemist and postdoctoral research assistant at the University of Southern Mississippi, is researching how microorganisms colonize on and around deep sea shipwrecks. She is taking sediment samples for DNA testing, and identifying nutrients in sediment pore water, the water trapped inside the sediment. Her study will help us learn about the relationship between microbes and shipwreck biomes. It took many hands to process the core sediments for her research.

As assistant to graduate student Rachel Mugge, I felt a bit like a nurse in an operating room. Every sample was taken carefully to ensure it was not contaminated.

Here’s how it went: Carefully remove the plug from the bottom of the core sample tube. Slide the core onto the extruder quickly so as not to lose any sediment. (An extruder is a wheel on a threaded bolt. It is precisely calibrated to measure 2 cm increments as you turn the wheel 4 2/3 times. )

Remove the lid and use a siphon hose to remove the sea water on the surface. Rachel does this by placing one end of the hose in the core tube and the other end in her mouth and sucking gently to get the flow of water going. Once it is moving she lets the water drain into a basin. Try this at home! You can get water to flow up and over an obstacle with this technique.

Next Rachel turns the extruder wheel until the mud is exposed at the top of the tube. She describes the mud to lab manager Anirban Ray, who writes it down next to the sample number. (“S 54, brown, unconsolidated, black streaks, tube worm burrows.”) I snap the paper wrapping off a wooden tongue depressor and hand it to her. She uses it to dig a sample out of the center of a sediment core. I hand her an open vial and she fills it. I cap it. Next she puts some sediment into a petri dish and Anirban seals and labels it. Then I hand her an open sterile whirl-pak for a final blob of sediment. I whirl this little baggy and twist tie it closed. Vials and whirl-paks go in the deep freezer. We do these three steps 40 times for 120 samples. The challenge I find in this kind of repetitive task is how quick and efficient can I be while still being careful and precise? Let me tell you. Pretty fast and efficient.

Putting a sediment sample into a vial. The core is on the extruder, which pushes the sediment upward when you turn the wheel.

At the same time this was going on, Justyna was extracting pore water (water that comes from inside the sediment) to analyze it for nutrients.

Personal Log

While we worked, I had a porthole at my station to keep an eye on the ocean as we cruised out to our third and final shipwreck. Dolphins raced with our ship this evening. Silvery flying fish skittered over the water reminding me of hummingbirds, the way their fins were a blur of movement. The color of the ocean now can best be described in terms of watercolors. Ultramarine. That says it all.

Calm sea — Clouds are reflected in a calm sea.

August 27, 2018August 27, 2018

Roy Moffitt: Headed Home, Cruise Summary, August 25-26, 2018

NOAA Teacher at Sea

Roy Moffitt

Aboard USCGC Healy

August 7 – 25, 2018

Mission: Healy 1801 – Arctic Distributed Biological Observatory

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

Date: August 25-26, 2018

Past – Current – Future locations/conditions:

72.5 North latitude: This past week we had 3-4 days of below freezing temperatures (27) with snow showers

Nome, Alaska: (8/25/18) Departing temperature 51 and cloudy

Contoocook/Hopkinton, NH: First day of school Tuesday (8/28/18)- Forecast 94 degrees Mostly Sunny (did I mention we don’t have air conditioning in New Hampshire?)

Ashore and I am headed back to NH

After completing our work in our most Northern point stop, we steamed back to Nome with just one more set of measurements on the way back, then had one final day of travel. It was sunny on the first day back but rougher seas than we had experienced thus far.

There were estimated 8-12 ft waves and some even larger that crashed over the Healy. To the right is a picture that I captured of the bow during this portion of our trip and the rocky seas. Keep in mind that for most of the day we were lucky enough to be on the front deck of the boat! After the waves calmed we were in the fog for most of the way home so spotting more whales and seals was difficult.

Cruise Summary

In short, the trip was a success with the tremendous amount of data collected. This data will now be analyzed by scientists and students and I hope to see some scientific papers on this research in the future. Here is a list of what was done on this trip:

31 mooring deployments and 24 mooring recoveries

(To review what the work involved in this see my blog: Moorings all day

142 CTDs (that’s a lot of up and downs!)

(To review what a CTD see my blog: Measuring Ocean Properties with the CTD)

51 Bongo samples

(To review what a bongo see my blog: Bring in the Bongos)

There were several Methot net tows.

To review what a Methot net tow is see my blog: Catching the Tiny Fish in the Big Sea

There was constant monitoring for birds and marine mammals with all sightings recorded. This experience was my personal favorite of the trip.

To review, see my blog: Walrus and Polar Bears on Ice

In addition to the above, there were many (I don’t have the exact count) Van Veen Grabs. I did not get to explain these in a blog so here is a quick overview. Scientists that study the sea floor, including the top layer of soil called the benthic zone, use a VanVeen Grab Sampler pictured below. It is lowered to the sea floor and then the scissor-like arms close the catch capturing a hunk of the sea floor and everything that was living on it. Once on shore the catch is rinsed through a sieve until all the clay is rinsed away leaving just the organisms that were living there (such as mollusks, clams, starfish, worms and more) and a few stones.

van veen process — Van Veen Grab Sampler process

The scientists on the team also took HAPS core samples. I did not get to explain these in a blog so here is a quick overview. The HAPS corer, pictured below, is a gravity corer. This is a device that is lowered to the sea floor and then the weight of the device settles into the sea floor. When the HAPS corer is lifted, the bottom of the tube containing the cut into sediment closes, trapping the sample. These samples are then stored in clear tubes as shown in the picture. Scientists can examine sentiment layers to gain a better understanding of the sea floor at that location by studying the sedimentary layers.

HAPS corer

HAPS core samples stored in tubes

All this above data has been copied and specimens are stored. The primary focus of this trip was to gather data and now the long process of analyzing and communicating the results will begin.

Cruise Reflections

This was such a great opportunity for me to meet so many different scientists and to both observe and assist the varied scientific studies occurring all at once. I needed all three weeks to get a handle on it all. I am looking forward to sharing what I have learned with my Maple Street School students back in New Hampshire and following the scientific studies as they move forward. Thanks to NOAA, Maple Street School, everyone else that allowed this learning opportunity to happen. It was a summer I will not forget experiencing a ship crash through ice in August! I leave you with some of the reflections of the birds I captured on those calmer days at sea.

The tufted puffin is not all that graceful at taking off. (below)

tufted puffin take off — The tufted puffin is not all that graceful at taking off.

The Common Murre (below)

Three male Eider Ducks

June 24, 2009April 5, 2021

Mark McKay, June 24, 2009

NOAA Teacher at Sea
Mark McKay
Onboard Research Vessel Knorr
June 10 – July 1, 2005

Mission: Ecosystem Survey
Geographical Area: Bering Sea, Alaska
Date: June 24, 2009

Science Log

It has been a very busy couple of days here on the Knorr. I haven’t received very much sleep. But then again, none of the science team has either. We have been a little ahead of schedule so it was decided that we could stay on station at a pretty interesting site for a longer period of time and due some diurnal studies, meaning, how are the organisms and ecosystems we are studying changing as we cycle through daytime to night. I am working on a project on phytoplankton so this was especially interesting for my work. So I was up several time thorough out the night collecting water samples and analyzing them. We headed to a particularly productive area right between the Pribilof Islands. As you can see from the photographs you can just barely make out St. Paul Island. As usual everyone scrambles to get his or her experiments in the water. A familiar face on the deck is Ebett Siddon who is a graduate student working on zooplankton and juvenile fish on this trip.

She frequently uses the MOCNESS Sampler, which allows the researchers in her team to open and close bottle at specific depths. It’s a pretty good-sized device so it takes a fair amount of skill to operate it. The sediment core people have been just as busy. They pulled up a core with a very cool deep water shrimp. Notice the large reflective eyes on this creature. There is a lot of life around here. When I got up this very early this morning to collect samples there were some porpoises hanging around one of or floating sediment traps. There wasn’t enough light to get any pictures. My bird survey friend have promised me some great pictures of Albatross so stay tuned.

Deep water shrimp with large reflective eyes

June 19, 2009April 5, 2021

Mark McKay, June 19, 2009

NOAA Teacher at Sea
Mark McKay
Onboard Research Vessel Knorr
June 10 – July 1, 2005

Mission: Ecosystem Survey
Geographical Area: Bering Sea, Alaska
Date: June 19, 2009

Science Log

Some very interesting activities have been going happening on board the Knorr the last couple of days. While everyday there is a routine of cruising to a station, stopping and dropping plankton nets and/or other probes, other, more exotic experiments get deployed. For example, yesterday researcher Pat Kelley from the University of Rhode Island and his team retrieved sediment traps that they had set out 24 hours before. Their interest is seeing what is settling to the bottom of the ocean and at what rate this material is settling. To do this, they use a rather ingenious device. They take tubes and fill them with salt water that is many times more concentrated then regular seawater. Because it is so dense, the concentrated saltwater stays in the open toped tube as it is lowered into the ocean. Anything that falls into this liquid stays in the trap and can be recovered for analysis. That’s where it gets interesting. Deploying and then recapturing a drifting probe can be a little tricky. After letting the sediment trap loose for 24 hours, you first have to go back and find it.

Fortunately the trap uses a satellite beacon that broadcasts its position to the ARGOS satellite system. The Argos program is administered under a joint agreement between the National Oceanic and Atmospheric Administration (NOAA) and the French space agency, Centre National d’Etudes Spatiales (CNES). The system consists of in-situ data collection platforms equipped with sensors and transmitters and the Argos instrument aboard the NOAA Polar-orbiting Operational Environmental Satellites (POES). The Argos system will lead you right to your instrument, then you have t get it on board. After they locate the instrument, they bring the ship along side and “lasso” so the deck crew can attach a cable and lift it out of the water using the A-frame crane located on the aft portion of the ship. The sediment traps are attached to a long line comprised of a heavy weight at one end with floats and a buoy at the other. The device is separated and brought up in sections so that they can be brought aboard using one of the ships cranes.

This takes a lot of skill to do, especially when on a deck that is slippery and rocking with the waves. Remember that this is done in between the other experiments and device tows. The deck crew is probably the busiest and hardest working group on this cruise. Another group on the cruise is the U.S. Fish and Wildlife Service “bird people” as they seem to be know as on the ship. They are made up of Elizabeth Labunski and Sophie Webb, both of which position themselves on the ships bridge so that they can survey what birds and marine mammals are present in-between stations. The Eastern Bering Sea is a very productive area and is rich in bird life. I went up to visit them on the bridge.While there they identified a rather unhappy Red-legged Kittiwake (Rissa brevirostris) sitting rather pitifully near the bow of the ship.

These birds are interesting because as opposed to their Black-legged cousins, they have a very narrow distribution. According to the Audubon Society, Red-legged Kittiwake’s breeding distribution is limited to just four localities in the Bering Sea: Alaska’s Pribilof Islands, Bogoslof Islands, and Buldir Island, and Russia’s Commander Islands. More than 75% of the species’ known population breeds on St. George Island in the Pribilofs, which were about 40 miles from where we were cruising. The weakened bird was captured so that it could be warmed up and released when it regained its strength.

Elizabeth Labunsk and Third Mate Alison Paz surveying Bering Sea birdlife

Sophia Webb holding Red-legged Kittiwake

June 17, 2009April 5, 2021

Mark McKay, June 17, 2009

NOAA Teacher at Sea
Mark McKay
Onboard Research Vessel Knorr
June 10 – July 1, 2005

Mission: Ecosystem Survey
Geographical Area: Bering Sea, Alaska
Date: June 17, 2009

Science Log

During the night the Knorr turned south westward to start it’s collecting along the CN (Cape Newenhan) line. We had skirted the edge of Bristol Bay before heading back out to into the Bering Sea. The expedition is following a plan that lets it stop at locations they have stopped at in previous years. This allows the scientists to compare data from multiple years so they can get a more accurate picture of what’s happening in the Bering Sea.

When I got up this morning I had to double check to make sure we were still on the Bering Sea and not something more temperate. The sky has been clear and the air temperature has been a “balmy” 45º F. May be I’m getting used to the weather but I had to take my jacket off to stay comfortable. The weather change quickly up here and may be totally different, and more severe later today. Best to be prepared for anything! So far the trip has been surprisingly pleasant. The one thing I’m not used to is the fact that the sun is always up. At 10 o’clock at night I step outside and it’s just like noon back at home.

Today is going pretty much like previous days. Everybody knows their job and goes about it in a efficient manner, meaning don’t get in the way, you are likely to get bowled over. They sent down the Multicore Apparatus again this morning. Hit a pretty sandy bottom but this time they had an unexpected hitchhiker. One of the cores came up with a Echiuran worm. Interesting creature. It has the consistency of a full water balloon, and is similar to the “innkeeper worms” which are common back home in California. Makes is living eating detritus in sediments that it pushes to its mouth with its proboscis (snout). Some types of Echiurans feed by making a “net” of mucus that captures detritus in the water. They then pull in the mucus and eat the captured detritus.

The zooplankton people are having fun with their collecting with one exception. Apparently the waters we have been sailing are fairly heavily populated with Jellyfish. The “Jelly’s” apparently gum up the collection bottles making collection little more difficult. I was watching as they tried to clean them out of their nets and it is a sticky mess. More on that later. For now, dinner! The food on the Knorr is great by the way.

June 15, 2009April 5, 2021

Mark McKay, June 15, 2009

NOAA Teacher at Sea
Mark McKay
Onboard Research Vessel Knorr
June 10 – July 1, 2005

Mission: Ecosystem Survey
Geographical Area: Bering Sea, Alaska
Date: June 15, 2009

Science Log

We are underway!!! Got up this morning to a flurry of activity as the Knorr was preparing to get underway. I hooked up with my researcher Dr. Ray Sambrotto from Columbia University. His interests are in phytoplankton and the different chlorophylls they produce. There is a lot of plankton work happening on this cruise, as well as some benthic (seafloor) studies and surveying of seabirds. It’s amazing how much science they squeeze into a cruise. One of the things I saw as we were heading out was a very cool example of a Hanging Valley. This geological feature is formed by glaciers. I saw it when we flew into Dutch Harbor but I didnt get a chance to get a picture of it. As we set out on the Knorr we passed right by it so I got my chance.

The day before we departed was spent storing equipment, testing instruments, and getting settled in our quarters. Problems with equipment not arriving on time wont prevent the start of the mission. We got underway right about 11 am Alaska time and headed for our first station over the Bering Canyon. Safety is everything onboard the Knorr so before anything really gets started we are required to undergo safety training. The ships crew is very concerned with making sure everyone is safe so they go through procedures in detail.

After the safety briefings and getting some of Dr. Sambrotto’s equipment running, I had a chance to play in the mud. Dr. Shull’s group from Western Washington University is looking at cores of sediment taken from the ocean bottom. Their interest is in how nutrients are cycled through deep-water sediments. They drop the sampling device, called a Multicore, which has specialized sampling bottles to the ocean bottom. The device pulls cores from the seafloor and when the sampling device is retrieved, the scientists have a sample of the sea floor. My job came after the bottles were retrieved. The process was to slice through the cores at specific depths and save the samples for further analysis. Good way to get really dirty.

January 3, 2005March 18, 2021

Mary Cook, January 3, 2005

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: January 3, 2005

Location: Latitude 45°49.53’S, Longitude 75°03.22’W
Time: 0930

Weather Data from the Bridge
Air Temperature (Celsius) 11.90
Water Temperature (Celsius) 13.55
Wind Direction (degrees) 343.52
Wind Speed (knots) 5.85
Relative Humidity (percent) 66.50
Air Pressure (millibars) 1016.06
Cloud Cover 6/8 Altocumulus
Sunrise 0615
Sunset 2152

Question of the Day

What is phytoplankton?

Quote of the Day

“Dream no small dreams for they have no power to move men.” Johann Wolfgang von Goethe

Science Log

This afternoon I interviewed Co-chief Scientist, Julio Sepúlveda, an oceanography graduate student from the University of Concepción. Julio did his Master’s thesis work for eight months at Woods Hole Oceanographic Institution in Massachusetts. In April, he’s leaving for Germany to spend three years continuing his education toward a PhD. in marine organic geochemistry. Julio has been kind enough to further explain the work they’ve been doing onboard the RONALD H. BROWN. The Chilean group of scientists include Pamela Rossel, Sergio Contreras, Rodrigo Castro, Alejandro Avila, and Luis Bravo. He says that their work has two parts: the water column process and the sedimentary record. The water samples and the sediment traps give a “picture of the moment”. They conducted the transect of samples starting at the shallow coastal waters and moving into the deeper offshore waters. These samples will provide a gradient of the nutrient concentrations at the Bay of Concepción which is part of an active upwelling location. To put it simply, they are looking at how the phytoplankton (plant-like microscopic organisms) uses the nutrients in the water. In particular they are looking at the nitrogen stable isotopes (nitrogen atoms with different masses) and their concentrations. They are trying to see how this is related to El Niño which greatly affects Chile and many places around the world. Julio explained that normally the upwelling brings cooler water containing nutrient-rich materials up to the surface. During El Niño events, the upwelling brings warmer, less nutrient-rich waters to the surface. This changes many things including the weather. The causes of El Niño are multi-varied air-sea fluxes that are not fully understood. In the last ten years the scientific community has been especially interested in knowing the possible influence of global warming in the El Niño variability. It seems that its frequency is changing and several articles indicate that El Niño is occurring more often. So their research provides a few “pixels” for capturing the entire “picture” of El Niño.

The second part of their research involves the core samples. The purpose of the core sampling is to collect the layers of sediments on the ocean floor. Julio described the layers to be like pages in a history book. Each layer tells the “story” of what was going on in the water at that location during that time. They are also looking at the degradation of the organic matter in the core samples. So, Julio says the water samples tell us about the present and the core samples tell us about the past. Using these methods of research, it is their intention to better understand the history of El Niño and better predict future El Niño events.

Personal Log

This morning we entered the fjords! Several of us were up and outside on the deck at 0630, “ooohing” and “aaahing”, taking pictures even though it’s very cold and windy out there. It is an irresistible attraction. We’re passing by the peninsula Tres Montes and we’re headed for the Bay of Tarn. All morning we’ve been sailing by emerald forest-covered mountains and black craggy rocks that have been eroded into peculiar shapes by the waves relentlessly smashing against them. The clouds are ominous and hanging low. The albatross are soaring with wings spread wide. An occasional whale sends a plume of spray into the air. I want these scenes to be indelibly saturated into my mind’s eye. I never want to forget this. No dwellings. No other ships. It’s just us. Just us and the birds and the whales. It’s good. It’s all good.

Until tomorrow,

Mary

January 1, 2005March 18, 2021

Mary Cook, January 1, 2005

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: January 1, 2005

Happy New Year!!
Feliz Años Nuevos!!!!

Location: Latitude 37°47.97’S, Longitude 74°02.84 W
Time: 1000

Weather Data from the Bridge
Relative Humidity (percent) 91.44
Air Pressure (millibars) 1015.72
Air Temperature (Celsius) 17.28
Water Temperature (Celsius) 17.58
Wind Direction (degrees) 212.20
Wind Speed (knots) 12.20
Cloud Cover 8/8 Stratus
Sunrise 0638
Sunset 2120

Question of the Day

What causes seasickness?

Quote of the Day

“The best portion of a good man’s life is the little, nameless, unremembered acts of kindness and love.” William Wordsworth

Science Log

All the Chilean scientists plus Jordan Watson from Scripps and the ship’s wage crew are all sleeping soundly after their 48 hour marathon project of collecting water and sediments. They will continue collecting surface water every 30 minutes of latitude but the ship will not stop for these collections.

Sometime tonight we will meet up with the pilots who will safely guide the RONALD H. BROWN through the inside passages. There will be two pilots so that one will be on the bridge at all times.

Today, Les Cruise shared with me that it is a seafaring tradition that the first log entry of the year for the ship should rhyme. So I want to share with you the first log entry of 2005 for the NOAA ship the RONALD H. BROWN.

Underway in the South Pacific 2004 was terrific.
Collecting mud on station six, all three thrusters in the mix.
Punta Tumbes, bearing 119º, at 34 nautical miles away is the closest point of land, in accordance with the Ronald Brown science plan.
All our lights are burning fine and our bow thruster is on line.
Main Power Diesel Generator Two keeps us going through and through.
Ship Service Diesel Generator Five gives us power to survive.
Auto-Positioning is how she sits, on a heading of 206°.
The sky is clear, I will not lie, Watch-Stander Melton is standing by.
Engineer-on-Watch Jacobson is down below, making sure the engines go.
Maneuvering various courses and speeds for sediment trap recovery, maybe there will be a new discovery!
Multiple personnel working in accord have brought the sediment trap aboard. Main Power Diesel Generator Three on line to help us make good time.
Increase speed 700 rpm, Auto track mode now as then.
190° is the way we go. Bow thruster power taken to zero.
Security round complete. That Jim Melton, he’s pretty neat.
Lt. Jones has the deck and conn ensuring the ship carry on.
13.3 nautical miles is our distance run. Hope 2005 will be fun! ”

Personal Log

This evening, my seasick queasiness is much better. I took the medics advice which was, “Stop looking at the computer and go to bed in a dark room. And stay there!” He was right.

But as a consequence of taking his advice my personal log is severely lacking. Most of the time, I’ve been in my stateroom, snuggled under a blanket looking at the backside of my eyelids.

Until tomorrow,

Mary

December 31, 2004March 18, 2021

Mary Cook, December 31, 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 31, 2004

Location: Latitude 36°13.8’S, Longitude 73°31.25’W
Time: 0830

Weather Data from the Bridge
Wind Direction (degrees) 206.36
Wind Speed (knots) 3.94
Air Temperature (Celsius) 15.50
Water Temperature (Celsius) 14.58
Relative Humidity (percent) 96.10
Air Pressure (millibars) 1015.21
Cloud Cover 3/8 Altocumulus and Cirrus
Sunrise 0639
Sunset 2114

Question of the Day

Why are the daylight hours getting longer as we travel southward?

Quote of the Day

“Information is the commodity of science.” Kevin Sullivan

Science and Technology Log

No stargazing last night due to cloudiness. So I’ll try again some other night.

Today we’ve been hovering in one place for six hours waiting on the drifting sediment trap to do its thing, which is to trap sediment.

We’re farther from land and in deeper water so it takes longer for the trap to collect a sufficient amount of sediment. They’ve just gotten it out of the water so now we’ll transit for about two hours to the next station and hover there for about eight hours. At this station they will deploy the bigger, heavier core sampler that looks like a 4 meter-long hollow rocket. It will go down to about 1000 meters depth and gravity will ram it into the mud. The layers of sediment will fill the hollow tube then it will close under the pressure as it is brought back to the surface by the winch.

This afternoon as we hovered in one place, the seagulls gathered around the ship for a siesta. There were hundreds of them just sitting in the water like ducks. It was almost like they were waiting to see what we were up to. It was interesting to watch them take to flight from the water. They’d spread their wings and begin flapping. But that wasn’t providing enough lift so they’d start paddling with their feet. It looked they were walking on water!

Finally, up they’d go, soaring through the air and then swooping down, gliding just above the water’s surface.

Personal Log

Today, I’ve been moderately seasick. I think it was the 10-12 feet swells passing under the ship as we hovered at station. The seasick medicine made me drowsy so I’ve spent time lying down in my stateroom off and on all day.

At 0230 in the morning we are supposed to make the turn due south and steam toward the inside passages! I’m ready to move on.

I eagerly anticipate traveling the same paths as the great explorers of Ferdinand Magellan and Sir Francis Drake. We’ll meet up with the pilot who will board the ship and take us safely through the narrow straits.

This is the last day of 2004. As I reflect back on my life during the past year I can’t help but know I’m blessed. With a wonderful family and circle of friends that love me, a good job and great co-workers, good health and great opportunities to live life abundantly. And for all this I am deeply thankful. Of course, we all know that life isn’t always smooth sailing. We all have struggles. Some are life and death struggles, some are relational struggles, some are financial struggles, and some are spiritual struggles. This journey in the Pacific has been more than an adventure for me. Being removed from my comfort zone has compelled me to contemplate. Contemplate just about everything. There’s one phrase that keeps coming to my thoughts over and over again. “It is more blessed to give than to receive.” And I don’t think this means money or other material possessions. I think it means giving of self. This is a much greater challenge, for me anyway. I want to absorb this into my life philosophy for the coming year and for always. I fully realize that I do not know the depth to which I may be called upon to live out this truth, but I have confidence that the future is brighter with this mind set.

Happy New Year!!

Until tomorrow,

Mary

p.s. Happy Birthday, Diane!

December 30, 2004March 18, 2021

Mary Cook, December 30, 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 30, 2004

Location: Latitude 36°21.31’S, Longitude 72°59.65’W
Time: 9:15

Weather Data from the Bridge
Air Temperature (Celsius) 14.33
Water Temperature (Celsius) 14.81
Air Pressure (millibars) 1015.24
Cloud Cover 3/8
Cloud Type: Stratus
Wind Direction (degrees) 325.6
True Wind Speed (knots) 1.26
Sunrise 636
Sunset 2112

Question of the Day

What is a light year?

Positive Quote of the Day

“The influence of each human being on others in this life is a kind of immortality.” John Quincy Adams

Science Log

Last night I went up to the bridge at about 2300 hours. Vickie, Jeff, and Jackie were stargazing in search of the Southern Cross. There it was, almost directly in front of the ship! It had just risen over the horizon and looked more like a baseball diamond than a cross. We also spotted Alpha and Beta Centauri. At about 4.3 light years away, these are among the closest stars to Earth other than our Sun. Vickie also pointed out Orion with his belt of stars and the seven sisters called Pleiades. I’m going to get out my textbook and read up on the Magellanic Clouds because I’m wondering if we can see those from here. Then Jackie looked over the edge of the ship in the wake and caught a glimpse of some momentary flashes of light! Bioluminescence! I stood there pressing my face against the window staring at the darkened waters waiting patiently for some more microorganisms to glow. Sure enough it happened. They looked like little sparks of lightening in a cloud. It happened several times. I’ll definitely be back on the bridge again in search of more wonders of the sea at night.

For this leg of the journey, I’ve been moved to a different stateroom. I’m now down below in the science quarters. The sounds are different down here. I can hear the water splashing up against the ship’s hull. It sounds like I’m in a perpetual carwash!

It’s a soothing sound, though. I slept like a bear in hibernation.

Today begins the science operations. Right now, the scientists are on the fantail preparing the drifting sediment trap with its radar-reflector, floaters and nighttime strobe light. We’ll deploy the instrument then leave it while we make a short transit to the next station for CTD casts and core sampling. Afterwards, we’ll return and retrieve the sediment trap. According to the work plan, we’ll do this same thing at six different locations across the continental shelf and slope off Concepción, Chile. Most of the CTD casts are in fairly shallow water with the deepest one going down to 980 meters. These scientists will be working 48 hours non-stop.

It’s beautiful here in the Bay of Concepción. The water is so smooth and glistening in the sunshine. We’re nearly surrounded by a crescent-shaped coastline and we can see houses, forests, and other ships. This afternoon, we saw several ghostly-white jellyfish pumping their way through the water. Jim pointed out little anchovies swimming nearby. Yum!

I spoke with Kevin Sullivan of the NOAA research branch in Miami and Jordan Watson from the Scripps Institution of Oceanography. They patiently explained some of the science to me. And I really appreciate that.

This is how the drifting sediment trap works. After the instrument collects the sediments from the water near the surface and is retrieved, it will be set aside for a few hours to allow the sediments to settle to the bottom of the tubes. Then a lever is turned that empties the sediments into bottles containing a preservative. Sediments can be particles from the air like dust or particles from the ocean such as little deceased sea creatures called diatoms.

The Rhumor gravity core sampler is basically a one meter long hollow tube with heavy weights attached to the top. After being lifted by the winch, it is slowly lowered into the water. When the tube gets about 10 meters from the ocean floor it is lowered very quickly and gravity rams it into the mud. In this process, the mud layers fill the hollow tube and as the core sampler is raised the pressure closes a valve that keeps the mud from coming out.

I’ve noticed on the SeaBeam readout that the depth here is only about 100 meters. That’s a huge contrast to a couple of weeks ago when we were in waters with a depth of 5000 meters!

It is my understanding that the rationale for their research is to explore the effects of nitrogen distribution and how that affects the marine algae nutrient usage in the present day water column. They are conducting the sampling in this location because of the upwelling that occurs which brings nutrients to the surface and because there are algae present that utilize the nutrients in these upwelling plumes. Likewise, they are interested in evaluating the amount of nitrogen left in the sedimentary record. This will help scientists better understand the history of the oceans.

Personal Log

Today has been a quiet but interesting day. All the science was new to me so I had to pay attention and ask lots of questions. It’s very rewarding to have people around who are eager to share with me what they are doing and the significance of it all in the whole scheme of things. I’ve learned a tremendous lot and my brain is kind of tired. Plus, I miss my mentor. She’s got enough energy for two people! I did take some time to go to the ship’s bow and watch the water skim by and look around for animals. I saw lots of birds and jellyfish. I like watching jellyfish because I never see jellyfish in Arkansas. To me they are intriguing critters because they are transparent. I can see right through them!

Well, I’m headed for the exercise room to rest my brain and work off that cake with chocolate icing that I ate for dessert. Then, after dark, up to the bridge for more stargazing in the Southern Hemisphere!

Until tomorrow,

Mary

p.s. Congratulations Brandon and Becky!