Elizabeth Bullock: Day 5, December 15, 2011

NOAA Teacher at Sea
Elizabeth Bullock
Aboard R/V Walton Smith
December 11-15, 2011

Mission: South Florida Bimonthly Regional Survey
Geographical Area: South Florida Coast and Gulf of Mexico
Date: December 15, 2011

Weather Data from the Bridge
Time: 3:15pm
Air Temperature: 23.6 degrees C
Wind Speed: 15.8 knots
Relative Humidity: 56%

Science and Technology Log

Liz takes a water sample
Here I am taking a water sample from the CTD.

Let’s talk about the flurometer!  The flurometer is  a piece of equipment attached to the CTD which is being used on this cruise to measure the amount of chlorophyll (specifically chlorophyll_a) in the water being sampled.  It works by emitting different wavelengths of light into a water sample.  The phytoplankton in the sample absorb some of this light and reemit some of it.  The flurometer measures the fluorescence (or light that is emitted by the phytoplankton) and the computer attached to the CTD records the voltage of the fluorescence.

The flurometer can be used to measure other characteristics of water, but for this research cruise, we are measuring chlorophyll.  As you know, chlorophyll is an indicator of how much phytoplankton is in the water.  Phytoplankton makes up the base of the marine food web and it is an important indicator of the health of the surrounding ecosystem.

At the same time that our cruise is collecting this information, satellites are also examining these components of water quality.  The measurements taken by the scientific party can be compared to the measurements being taken by the satellite.  By making this comparison, the scientists can check their work.  They can also calibrate the satellite, constantly improving the data they receive.

Combined with all the other research I’ve written about in previous blogs, the scientists can make a comprehensive picture of the ecosystem with the flurometer.  They can ask: Is the water quality improving?  Degrading?  Are the organisms that live in this area thriving?  Suffering?

Nelson records data from the CTD
Nelson records data from the CTD.

Collecting data can help us make decisions about how better to protect our environment.  For example, this particular scientific party, led by Nelson Melo, was able to inform the government of Florida to allow more freshwater to flow into Florida Bay.  Nelson and his team observed extremely high salinity in Florida Bay, and they used the data they collected to inform policy makers.

Personal Log

Today is my last full day on the Walton Smith.  The week went by so fast!  I had an amazing time and I want to say thank you to the crew and scientific party on board.  They welcomed me and taught me so much in such a short time!

Thank you also to everyone who read my blog.  I hope you enjoyed catching a glimpse of science in action!

Answers to Poll Questions:

1)      In order to apply to the Teacher at Sea program, you must be currently employed, full-time, and employed in the same or similar capacity next year as

a. a K-12 teacher or administrator

b. a community college, college, or university teacher

c. a museum or aquarium educator

d. an adult education teacher

2)      The R/V Walton Smith holds 10,000 gallons of fuel.  By the way, the ship also holds 3,000 gallons of water (although the ship desalinates an additional 20-40 gallons of water an hour).

Jacquelyn Hams: 3 December 2011

NOAA Teacher at Sea
Jackie Hams
Aboard R/V Roger Revelle
November 6 — December 10, 2011

Mission: Project DYNAMO
Geographical area of cruise: Leg 3, Eastern Indian Ocean

Date: December 3, 2011

Weather Data from the R/V Revelle Meteorological Stations

Time: 0930
Wind Direction: 232.10
Wind Speed (m/s): 3.4
Air Temperature (C): 27.7
Relative Humidity: 77%
Dew Point: (C): 23.7
Precipitation (mm): 42.2

PAR (Photosynthetically Active Radiation (microeinsteins): 1942.5

Long Wave Radiation (w/m2): 409.3
Short Wave Radiation (w/m2): 373.1

Surface Water Temperature (C): 28.70
Sound Velocity: 1541.5
Salinity (ppm): 33.7
Fluorometer (micrograms/l): 0.3
Dissolved Oxygen (mg/l): 2.4
Water Depth (m): 4422

Wave Data from WAMOS Xband radar

Wave Height (m) 0.5
Wave Period (s): 7.4
Wavelength (m): 86
Wave Direction: 1140

Science and Technology Log

Surface Fluxes Group

The Surface Fluxes group consists of James Edson, University of Connecticut, Ludovic Bariteau, University of Colorado Cooperative Institute for Research in Environmental Sciences (CIRES), and June Marion, Oregon State University. This group measures the amount of radiation and heat into and out of the ocean and was covered in the November 12, 2011 blog posting.

The purpose of this posting is to highlight the work of Ludovic Bariteau who is measuring the carbon dioxide flux between the atmosphere and ocean. For redundancy and testing, the carbon dioxide in the atmosphere is measured with several infrared instruments pictured below. Two of the instruments are in the pilot stage and were developed for this research cruise. The equipment used for measuring carbon dioxide in seawater is done in collaboration with Wade McGillis from Lamont-Doherty-Earth Observatory (LDEO). Ludovic plans to refine the instrumentation based on the pilot test. The carbon dioxide data will be correlated with surface flux data to present a complete picture of ocean atmosphere fluxes.

Photograph of flux instruments.
Photograph of flux instruments on the mast. The instruments measuring air CO2 are indicated by the black arrows. Image credit: James Edson.
Ludovic Bariteau in front of instrument to measure carbon dioxide fluxes.
Ludovic Bariteau in front of the specialized instrument to measure carbon dioxide fluxes between the ocean and atmosphere.
Closeup of carbon dioxide flux instrument.
The above photograph is a close-up of the apparatus used to measure the carbon dioxide content in the ocean water.
Ludovic Bariteau pointing to CO2 measurement device.
Photograph of Ludovic Bariteau pointing to one of the air CO2 measurement devices in the pilot stage.

        

Data printout of Carbon dioxide values of air and water measured from instrumentation aboard the Revelle provided courtesy of Ludovic Bariteau
Data printout of Carbon dioxide values of air and water measured from instrumentation aboard the Revelle provided courtesy of Ludovic Bariteau

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What about the MJO?

Previous postings described the work being done by the 7 science groups and the instrumentation being used to measure the various characteristics of the ocean-atmosphere interaction that may be part of the active phase of the MJO. Readers of this blog may be asking the same question that some of my students are now asking, “Did you experience the MJO?”

Data collected to date by the science groups suggests that we experienced an active MJO phase. Although It will take years to analyze and correlate the data collected from the various organizations involved in Project DYNAMO, the Revelle experienced high winds, colder surface water surface temperatures, and the intermittent storms separated by quiescent periods that are believed to accompany the active phase of the MJO. Based on initial data this active phase may have occurred between the approximate dates of Nov. 24 through Dec.2.

Wyrtki Jet Current

Before discussing the effects of the MJO on Indian Ocean circulation, it is useful to provide a brief background on the currents in the Indian Ocean which are more complicated than those in the Atlantic and Pacific Oceans in several ways:

  • Indian Ocean currents are poorly defined
  • They are influenced by the presence of the Eurasian continent
  • They are more variable than the Atlantic or Pacific Ocean currents. Some Indian Ocean currents vary with the seasons. For example, on the top diagram below, notice there are two unnamed gyres located in the northern hemisphere west and east of India.

Diagram of Indian Ocean Currents

The Revelle left station on December 2, and began north south transects across the equator to delineate the extent and the speed of the Wyrtki Jet Current. The Wyrtki Jet is a narrow jet-like surface current that flows eastward during the transition periods between the Northeast and Southwest Monsoon currents and is believed to accompany the active phase of the MJO.

A summary of the monsoon system in the Indian Ocean taken from the pdf version of Regional Oceanography: An Introduction by Tomczak and Godfrey. The Wyrtki Jet may be the Equatorial Jet identified on the below diagram.

Wyrtki jet speeds of 150 cm/s eastward at the surface were identified during the cruise.  In addition a current flowing westward was identified at a depth of 100 m. The purpose of the transects is to delineate the lateral and vertical extents of these currents.  The currents are measured using four Acoustic Doppler Current Profiler (ADCPs) located in the hull of the ship (these are Doppler sonars, analogous to Doppler radar and lidar measurements discussed in previous blogs).

Personal Log

I worked the winch for the last drop of Chameleon on Leg 3 of Project DYNAMO aboard the R/V Revelle.  I must say that I am proud of my work as a “Winch Winder”.  In the past 5 weeks, I experienced a range of emotions regarding the winch.  I initially felt fearful of working solo on such a valuable instrument. Once I began working solo, I was still intimidated because the winds and currents are so variable at the equator. Intimidation was finally replaced by competence after operating the instrument in 40 knot winds without slamming it into the ship! Aurelie Moulin was kind enough to shoot this video of me just before Chameleon was pulled out of the water on the last drop.

I would like to share my interview with Jude Irza, Ordinary Seaman aboard the R/V Revelle who provides extremely thoughtful advice and insight regarding career choices and preparation that may be helpful not only for students unsure of their future, but for those who may desire a career change at any stage in life.

Photograph of Jude Irza

Question: What made you decide on a career in this field?

 That question is straight forward enough but my answer is a little bit convoluted.  I never woke up one day and decided that I wanted to become a Merchant Marine and work on Oceanographic Ships.  In fact, I have been fortunate to have had two careers before this one:  Naval Officer and Finance Manager.  Here’s how I embarked on my first two careers.

 First, I attended college on a Naval Reserve Officers’ Training Corps Scholarship.  After college, I went to Flight School in Pensacola, Florida, and flew as a navigator in the United States Navy.  While in the Navy, I decided to expand my horizons and earn a Masters in Business Administration. While completing my MBA, I decided that a career in finance would be challenging and rewarding.  So I resigned my commission and I worked at a large telecom company in San Diego.  Later, I had the opportunity to join a telecom start-up and later a consulting company.   Although I enjoyed working in finance for fifteen years, I was ready to do something exciting and different.  I had always thought working as an Officer in the Merchant Marine would be fun. Expecting to be too old for this career, I was surprised and pleased when my research uncovered a new program where I could go to sea and work towards a Third Mate License through a two-year program offered by the Pacific Maritime Institute (PMI) in Seattle, Washington.  So, approximately two years ago, I joined the program and was partnered with the Scripps Institute of Oceanography.  I joined the R/V Revelle as an Ordinary Seaman.  Already, this is my fourth trip on the R/V Revelle and I am close to finishing PMI’s program.  I hope to take my Coast Guard License exams next summer and have my 1600 ton 3rd Mate License shortly thereafter.

 Question:  What are the positives and negatives of this line of work?

 The exact nature of the work depends on what billet or position one is filling and to an extent that determines the positives and negatives.  For example, an Ordinary Seaman like me spends most of the time cleaning, removing rust and painting.  Work is performed both inside and outside of the ship.  Mates, however, are Merchant Marine Officers, and spend most of their time standing watch, on the bridge of the ship.  Most, if not all, merchant mariners would agree that being able to travel and see the world are positives in this line of work.  The biggest negative is separation from family members for months at a time.  Typically, at Scripps, we are out to sea for eight months out of twelve.  Moreover, especially at the lower level positions, the work can be arduous and sometimes monotonous.

 Question:  What advice would you give students who are unsure of their career goals?

 I would give students five pieces of advice:

1. Get Information and Prerequisites – Get on the internet and research the careers in which you might be interested.  Learn about what qualifications and prerequisites are necessary for each career.  Try to find a person who is in that career and ask them good questions.  Be realistic, but also look for unconventional pathways.

 2. Inventory your Skills and Abilities – Try to determine what you enjoy doing and what you are good at.  Try and see what careers other people chose that have your talents and abilities.

 3. Get Real-World Experience – Try and experience careers directly without investing too much time and energy by taking a part-time, internship or volunteer position.  You’ll learn an enormous amount by working alongside other people.

 4.  Change your Career if you find that it is not Right for You – Some people, including myself, are not suited to only one career.  Don’t be afraid to try something new if you no longer find enjoyment in your current line of work.  But be financially responsible and try to not incur too much debt especially in your younger years.  You want to keep your options open and debt can limit options.

 5.  You are Never Too Old to Start Again – I am forty-five years old, but feel energized doing something new.  I don’t know if I will be in this career ten years from now, but I am certainly enjoying it now.

Elizabeth Bullock: Day 3, December 13, 2011

NOAA Teacher at Sea
Elizabeth Bullock
Aboard R/V Walton Smith
December 11-15, 2011

Mission: South Florida Bimonthly Regional Survey
Geographical Area: South Florida Coast and Gulf of Mexico
Date: December 13, 2011

Weather Data from the Bridge
Time: 4:45pm
Air Temperature: 23.5 degrees C
Wind Speed: 15 kt
Relative Humidity: 68%

Science and Technology Log

Liz deploys a drifter
I'm deploying a drifter!

Last night, we deployed our first drifter.  There will be three deployed over the course of this cruise.  The frame of this drifter is built by the scientists at AOML (Atlantic Oceanographic and Meteorological Laboratory).  Afterwards, they attach a satellite transmitter so they can track where the drifter goes.  This helps them measure the surface currents.

What are some other types of research being conducted onboard?  I’m glad you asked!  Two NOAA researchers, Lindsey and Rachel, are studying water chemistry and chlorophyll.  They take samples of surface water from the CTD to study CO2 and the full carbonate profile.  They also use water collected at many different depths to study the chlorophyll content.  Chlorophyll is an indicator of the amount of phytoplankton in the water.

Collecting water from the CTD
Collecting water from the CTD.

Sharein, a PhD student at the University of Miami Rosenstiel School of Marine and Atmospheric Science, is studying a specific type of plankton called copepods.

The particular copepod that she is studying is food for the larval stages of some commercially important species of fish such as bill fish (which include blue marlin, sail fish, white tuna, and yellowfin tuna) and different species of reef fish.  If a species is commercially important, it means that many people depend on this particular fish for their livelihoods.

Female Copepod
Here is one of the species of copepods that Sharein is studying.

Do you think you would be interested in working at sea?  You would be a good candidate if you:

1)      Like meeting new people and working as part of a team

2)      Are interested in the ocean, weather, and/or atmosphere

3)      Don’t mind getting your feet wet

Personal Log

When we were on our way to the Tortugas, we didn’t have cell service and the TV in the galley had no signal.  It was nice to be disconnected for a while.  Although there are still 29 computers onboard which all have the internet, so we’re hardly off the grid!

It was hard at first to adjust to the night shift, but everyone onboard was really supportive.  Working the night shift means that you work from 7pm to 7am.

Species seen last night in the Neuston net:

Flying fish

Needle fish

Different kinds of sea grasses and sargassum

Moon jellies

Elizabeth Bullock: We Are Underway! December 11, 2011

NOAA Teacher at Sea
Elizabeth Bullock
Aboard R/V Walton Smith
December 11-15, 2011

Mission: South Florida Bimonthly Regional Survey
Geographical Area: South Florida Coast and Gulf of Mexico
Date: December 11, 2011

Weather Data from the Bridge
Time: 2:30pm
Air Temperature: 24.5 degrees C (76 degrees F)
Wind Direction: 65.9 degrees east northeast
Wind Speed: 15.8 knots
Relative Humidity: 78%

Science and Technology Log

Today is the first day of the research cruise.  The R/V Walton Smith left its home port in Miami, FL this morning at about 7:30am.  After a delicious breakfast, the crew and scientific party received a safety briefing from Dave, the Marine Tech.  We learned about the importance of shipboard drills and we were shown the location of all the safety gear we might need in case of an emergency.  This ship works like a self-contained community.  The crew of the ship must also be the policemen and firemen (or policewomen and firewomen).

After our safety briefing, the science party went outside to our first station of the day.  The first piece of equipment we put into the water was a CTD.  The CTD is named after the three factors the equipment measures: conductivity, temperature, and depth.  The CTD will be deployed at precise locations along our route.  Since they conduct this research cruise twice a month, they can see if conditions are changing or staying the same over time.

Liz at computer
Here I am, reading the data that came up from the CTD.
CTD
This is the CTD, which measures conductivity, temperature, and depth.

Question for students: What is the relationship between salt and electrical conductivity?  If the salt content in the water increases, will it conduct electricity better or worse?

The next piece of equipment we deployed was the Neuston Net.  This net sits at the water line and skims organisms off the surface of the ocean.  The net is in the water for 30 minutes at a time.  After bringing the net onto the deck, the fun part starts – examining the contents!  Our Neuston Net had two main species: moon jelly (Aurelia) and sargassum.  The term sargassum actually describes many species, so the scientists on board will study it carefully in order to classify which kinds they caught in the net.  Sargassum is an amazing thing!  It is planktonic (which means that it floats with the current) and it serves as a habitat for bacteria and small organisms.  Since it is such a thriving habitat, it is also a great feeding ground for many different species of fish.

Once we emptied the contents of the Neuston Net, Lindsey and Rachel, two of the scientists on board, began to measure the quantity of each species they caught.  In order to measure the weight of the moon jellies, they used the displacement method.  This is because we can’t use regular scales onboard.  Here are the steps we took to measure the moon jellies:

1)      We poured water into a graduated cylinder and recorded the water level.  For example, let’s say that we poured in 100ml of water.

2)      We put a moon jelly into the graduated cylinder and recorded the new water level.  For example, let’s say that the new water level read 700ml.

3)      We subtracted the old water level from the new, and we could tell the volume of the moon jelly we had caught.  For example, based on the numbers above, we would have caught a 600ml moon jelly!

Neutson Net
Lindsey examines what we caught in the Neuston Net.

Both the CTD and the Neuston Net will be deployed many times over the course of the cruise.

 

Personal Log

Despite a bit of seasickness, I am having a wonderful time!  Everyone on board is very welcoming and happy to answer my questions.  Everyone is so busy!  It seems like they have all been working nonstop since we arrived on board yesterday.

Answers to your questions

First, let me just say that these are great questions!  Good job, Green Acres.  Here are some answers, below.

1)      How do the currents make a difference in the water temp?  The currents play a major role in water temperature.  In the Northern Hemisphere, currents on the east coast of a continent bring water up from the equator.  For example, the Gulf Stream (which is a very important current down here in Florida) brings warm water from the tropics up the east coast of the United States.  This not only keeps the water temperature warm, but it also affects the air temperature as well.

2)      How does the current affect the different algae populations?  Currents regulate the flow of nutrients (which phytoplankton needs to survive).  Strong currents can also create turbidity, which means that it stirs up the water and makes it harder for light to penetrate the water column.  As you know, phytoplankton rely on sunlight to grow, so if less light is available, the phytoplankton will suffer.  I’m told by Sharein (one of the phytoplankton researchers) that algae are hearty creatures.  This means that as long as the turbid conditions are temporary, algae should be able to thrive.

Elizabeth Bullock: Introduction, December 8, 2011

NOAA Teacher at Sea
Elizabeth Bullock
Aboard R/V Walton Smith
December 11-15, 2011

Introduction

Hello! My name is Elizabeth (Liz) Bullock and I work for the NOAA Teacher at Sea Program (TAS).  Before I worked at NOAA (the National Oceanic and Atmospheric Administration)  I was in graduate school at Clark University in Worcester, MA studying Environmental Science and Policy.  As my final project, I created an environmental curriculum for the Global Youth Leadership Institute (GYLI).  Through this experience, I realized how much I love both science and educating others about the importance of the natural world.

I have been invited to take part in a research cruise on the R/V Walton Smith.  I will be participating in the Bimonthly Regional Survey / South Florida Program Cruise.  The researchers on this survey are  from NOAA’s Atlantic Oceanography and Meteorological Laboratory (AOML) which is located in Miami, FL.

What will we be studying?  The scientists on this survey are very interested in knowing about the strength and health of the ecosystem.  They can judge how strong it is by looking at various indicators such as water clarity, salinity, and temperature.  They can also record information about the phytoplankton and zooplankton that live in the water.

Question for students: Why do you think it is important to learn about the phytoplankton and zooplankton?  What can they tell us about the ecosystem?  Please leave a reply with your answers below by clicking on “Comments.”

Here is a map of the route the R/V Walton Smith will be taking.

Research Map
The R/V Walton Smith will be leaving Miami, FL and traveling around the Florida Keys into the Gulf of Mexico.

I am so excited and I hope you will follow along with me on this journey of a lifetime!