Scott Donnelly, April 20, 2008

NOAA Teacher at Sea
Scott Donnelly
Onboard NOAA Ship McArthur II
April 20-27, 2008

Mission: Assembly of Science Team and Movement of Science Gear/Equipment
Geographical Area: Coos Bay to Astoria, Oregon
Date: April 20, 2008

NOAA TAS Scott Donnelly (green helmet) and fellow science team member Bob Sleeth collecting zooplankton

NOAA TAS Scott Donnelly (green helmet) and fellow science team member Bob Sleeth collecting zooplankton

Science and Technology Log 

The start of the cruise has been delayed one day due to the rough, unpredictable, and potentially dangerous waters where the mighty eastward flowing Columbia River and its massive volume of freshwater collides head on with the cold, salty water of the vast Pacific Ocean. Where this water slugfest happens, sands bars shift repeatedly this way and that way as the pushing and shoving between the massive volumes of sea and freshwater continues without interruption. At low tide the sand bars are easily seen; they are numerous and of great area and irregular in shape.

On account of the delay, most of the day was spent making sure instruments worked properly and non-instrument equipment was organized to maximize efficiency. Perhaps though more importantly, the delay gave the eleven science team members— most of them complete strangers to one another—extra time to get to know one another. This is important because all of us will be shipboard for eight days confined to quaint sleeping quarters, working, eating, relaxing, playing, and interacting with each other. There’s no escaping once the ship moves away from the dock and goes out to sea. It also gave science team members time to get to know the ship’s crew, who themselves play a key role in the overall success of the mission.

Science team meeting in the dry lab aboard NOAA ship McARTHUR II

Science team meeting in the dry lab aboard NOAA ship McARTHUR II

Communication is a two-way street. From the science team perspective we have to communicate with each other and also with the crew in order to be productive and minimize mistakes. Ocean science truly is an interdisciplinary endeavor that relies on the talents and work ethic of the people involved. This brings me to my next topic. Science is a uniquely human pursuit; good science relies on people. Modern scientific inquiry is all about assembling the best minds and talent possible into a highly productive team. It’s not just about brains though. Personalities and people skills matter too. In fact, they matter a lot. They can make or break a scientific mission. All it takes is an individual with a 60-grit sandpaper personality to upset the ebb and flow of human group dynamics.

Ocean science is all about teamwork!  

In a few hours I’ll see how such dynamics work out on this cruise with this assemblage of people, the youngest being an undergraduate science major and the oldest a retired Silicon Valley engineer. Four of the eleven science team members (myself included) have never been at sea. We don’t know what to expect or, for that matter, think about with respect to what lies ahead this next full week.

After lunch we met as a group with the NOAA Corps officers and reviewed the ship’s rules and regulations. We then had a science team meeting whereby the cruise’s Chief Scientist, Dr. Steven Rumrill, gave a brief overview of the cruise’s scientific mission, discussed shipboard operations, the cruise’s plans and objectives, and the itinerary and the logistics associated with sample collection and data acquisition.

In summary, the science team will measure a number of salient water quality parameters (see my log April 19, 2008) and collect samples of marine invertebrates (boneless organisms) along the Oregon Continental Shelf (OCS) at varying depths and distances from the coast over the period of 20-27 April 2008. This time of year was chosen because it precedes the development of an upwelling/hypoxia event that is anticipated to develop later in the summer of 2008. (The oceanographic terms upwelling and hypoxia will be discussed later in this log.) Water and biological sampling will continue non-stop for 24hrs per day, every day of the cruise except the last day when preparations are made for eventual docking.

Each work shift is four hours in length and is followed by an eight hour rest & relaxation (R&R) period. My assigned shift mate is Bob Sleeth and the team leader Ali Helms, a research cruise veteran who works full-time under Chief Scientist Steve Rumrill at South Slough National Estuarine Research Reserve (SSNERR). Ali will work the CTD controls in the dry lab while Bob and I will collect water samples from the CTD Niskin bottles and also zooplankton and phytoplankton using specially designed nets deployed starboard (right side of ship) to various depths and eventually retrieved after a certain length of time. Our daily shift schedule is from 0100 to 0500 (1am to 5am) and 1300 to 1700 (1pm to 5pm) with an eight hour R&R period in between each shift. Once started operations will continue on a 24-hour basis without interruption unless for inclement weather or seas.

The map to the right shows the major geographical regions where sampling will occur along the continental shelf of Oregon between Astoria (46O10’N, 123O50’W) and Cape Blanco (42O51’N, 124O41’W). At each sampling site biological (phytoplankton and zooplankton) samples will be collected at varying depths using special collection nets of varying mesh and design.

The operating area for this cruise is the nearshore region of the Oregon Continental Shelf (OCS), between Astoria (Cape Falcon 45o46’N, 124o40’W) and Cape Blanco (42o51’N, 124o41’W) at sites or stations ranging from 3 to 55 miles off the coast. Multiple sampling stations are scheduled along the Newport Hydrographic (NH) Line (maroon line), the Umpqua Estuary Line (green line), the Coos Bay Line (blue line), and the Coquille Estuary Line (orange line). The number of sampling stations is indicated by the number adjacent each colored line. Sampling also will take place at multiple sites (26 total) south of the Columbia River-Pacific Ocean interface and north of the NH Line as indicated by the purple circle on the map at right. Weather permitting, in total there are 59 sites where chemical and biological characterization of the water column will be carried out.

Previously I mentioned the oceanographic terms upwelling. So what is upwelling? A short definition is that upwelling is a vertical water circulation pattern in which deep, cold and typically nutrient- rich seawater moves upward to the ocean surface. Upwelling occurs in a number of places around the world on the western side of continents. It is caused either by strong, consistent winds blowing parallel to the shore as is the case on the Oregon coast in the summer months, or by deep, cold ocean currents smashing into the continental landmass and having no where to go but up as is the case in the southern hemisphere off southern Chile (South America) and Namibia (southwestern Africa). During summer in the northeastern Pacific, a clockwise rotating, high-pressure air system is positioned off the Washington-Oregon coast. Strong northerly winds blow south parallel to the Washington-Oregon coasts pushing the surface water towards the equator. At the southernmost region of the high pressure air system the water is pushed out to sea, away from the Oregon coast. As the surface water is pushed south toward the equator, deep, cold water from below upwells and thereby replaces the warmer, less dense surface water displaced to the south by winds of the high-pressure air system.

Hypoxia describes seawater that is low in dissolved oxygen gas (DO). Generally, the accepted concentration value for waters deemed hypoxic is less than (<) 1.5mg O2/L seawater. Marine organisms vary in their oxygen demand. The more active and larger swimming marine organisms such as tuna and mackerel typically require more oxygen per body weight in order to generate the metabolic activity necessary to supply their dense muscles with the requisite energy to slice through the water oftentimes counter to the current. So an active fish that moves into hypoxic waters decreases its chance of survival.

Oregon coast

Oregon coast

Personal Log 

As expected I didn’t sleep well last night, the first night on the ship. It wasn’t because of the ship’s movement either. It hardly moved as the Columbia River was calm with the wind blowing weakly. It’s a given that more often than not I sleep poorly in a new environment whether it’s a hotel, my in-laws home, or camping. Even if dead tired at best I’ll catnap for 1.5 hour intervals at the most, if lucky.

I was assigned to share living-sleeping quarters with three other science team members. The cabin contained two bunk bed units (top and bottom) separated by a wall, two small desks in the corners, ample storage space below each lower bunk bed and all along three of the four walls of the room, a (very) small lavatory with a hot/cold water shower and toilet, and a sink with hot/cold water to freshen up in the morning or before bed. In spite of the room’s relatively small size (~12ft x ~12ft), the storage capacity was more than enough to accommodate the personal gear of four people for simple, Spartan living. Every square inch of wall space was utilized for storage or some other useful, practical function. Basically, no space was wasted. Wall hooks were everywhere to hang jackets. Each bed had its own reading light, a full-length curtain for privacy (relatively speaking), and a side bumper so that when the ship rolled one didn’t roll out of bed onto the floor. Overall, it was a good example of efficient use of space for simple, practical, but productive living.

The mission delay provided more time for me to talk to and get to know members of science team, particularly my assigned shift mate Bob Sleeth, a retired Silicon Valley electronics engineer. After a hearty breakfast we spent Sunday morning exploring the quiet Astoria waterfront. Bob and a friend sailed in a 35 foot yacht from San Diego to French Polynesia in the South Pacific, spending a year sailing to and from the small islands that constitute the vast archipelago of beautiful islands including Bora Bora and Tahiti.

Cargo ship arriving at Astoria port

Cargo ship arriving at Astoria port

After lunch I spent a considerable amount of time studying the wrestling match between the ebb and flow of the high and low tides of the Columbia River. Salt water vs. fresh water. Bob gave me a few pointers on how wave structure gives a clue about the subtle changes in wind direction and speed at the water’s surface. This led to a lengthy conversation about how the nameless but intrepid mariners of ancient times, the Vikings, and those of the Age of Maritime Discovery of the European Renaissance (Ferdinand Magellan, Christopher Columbus, James Cook and many more) used their observational powers to chart the vast oceans without the aid of longitudinal coordinates. For example, the appearance of a certain bird over water, marine organism, or the change in surface water color or texture possibly meant that land or an island, yet unseen over the curvature of the earth’s surface, lay just below the horizon.

Throughout the day a number of cargo ships loaded with goods made their way slowly into port. That led to a discussion about how a seemingly small decrease in water volume translates into cargo ships having to shed weight else they run aground. Early tomorrow morning we start the mission and head out to the intimidating, deep waters of the Pacific Ocean. 

Scott Donnelly, April 19, 2008

NOAA Teacher at Sea
Scott Donnelly
Onboard NOAA Ship McArthur II
April 20-27, 2008

Mission: Assembly of Science Team and Movement of Science Gear/Equipment
Geographical Area: Coos Bay to Astoria, Oregon
Date: April 19, 2008

Loading gear onto the McARTHUR II in the snow and rain

Loading gear onto the McARTHUR II in the snow and rain

Science and Technology Log 

The long, winding drive along US Highway 101 from Oregon Institute of Marine Biology in Charleston to Astoria was well worth it. For the most part every turn opened to a panoramic view of the Pacific Ocean to the west. To the east, lush, verdant open meadows, some inundated with small ponds and bordered by thick coniferous forests, pleased our eyes. We stopped in Newport, OR to pick up a science team member and had lunch at a local restaurant with a microbrewery. I feasted on Kobe Chili.

NOAA Teacher at Sea, Scott Donnelly, next to a CTD with Niskin bottles in port at Astoria, OR

NOAA Teacher at Sea, Scott Donnelly, next to a CTD with Niskin bottles in port at Astoria, OR

After arriving at the Astoria dock (45O12’N, 124O50’W) late afternoon and loading all the gear, equipment, and supplies aboard the McARTHUR II, we spent the evening moving personal gear into our assigned shipboard cabins, setting up and troubleshooting the computer and data collection systems, organizing the ship’s wet lab, installing dissolved oxygen (DO) and chlorophyll fluorometer sensors onto the shipboard Conductivity-Temperature-Depth (CTD) platform, and calibrating the instruments in preparation for the cruise.  The scientific instrumentation that will be used on the cruise is impressive and worth mentioning since in science data are only as good and believable as the tools used to collect it. The cruise’s instrument workhorse will be the CTD as it will be used at every sample site. The following physical-chemical water quality parameters will be measured continuously as the CTD descends and then ascends through the water column: conductivity, temperature, depth, dissolved oxygen (DO), and chlorophyll a fluorescence. Attached to the CTD are twelve cylindrical Niskin bottles, each with a volume capacity of 2.5 liters (0.66gal). Water collected in the Niskin bottles at various depths will be collected and taken to the ship’s wet lab where the following water quality parameters will be measured using a multi-sensor sonde or probe: salinity, pH, and turbidity. The photo below shows the CTD with Niskin bottles.

Let’s begin by talking about a CTD, which measures seawater’s conductivity (more or less the amount of dissolved ions in a given mass or volume of seawater), its temperature, and depth of the surrounding water column at the time a measurement is made. The latter two parameters are self-explanatory so let’s focus on conductivity. Seawater conducts electrical current because seawater contains dissolved ions, i.e. charged particles, either positive or negative. The major ions in seawater contributing to its conductivity are predominately sodium (Na+) and chloride (Cl) but other ions in varying amounts, depending on location and depth, are present as well. Examples include magnesium (Mg+2), calcium (Ca+2), carbonate (CO3-2), bicarbonate (HCO3), and sulfate (SO4-2). Other important elements found in trace or very small amounts in seawater are lithium (Li+), iodine (I), zinc (Zn+2), iron (Fe+2 and Fe+3), and aluminum (Al+3). This list is not exhaustive by any means.

Conductivity is related to salinity. In general, the greater seawater’s conductivity, the greater its salinity. Salinity of seawater though is not constant; it depends on a number of factors, two of the more important being depth and temperature.  Atmospheric gases, namely molecular nitrogen (N2), oxygen (O2), and carbon dioxide (CO2), readily dissolve in seawater, particularly so at the ocean’s surface where wave action facilitates this process. A dissolved oxygen (DO) probe (or sensor, typically the two words mean the same thing) measures the mass (or weight) of O2 dissolved in a given mass or volume of water. The units associated with a measured value then would be either mg O2(g)/kg seawater or mg O2(g)/L seawater. The symbol mg means milligrams, kg means kilograms (1kg = 1,000g = 2.2 pounds), and L means liter. Why is the denominator in the ratio either kg or L? The unit kg is a unit for mass, which does not depend on temperature. The mass (or weight) of a substance does not change simply because it gets warmer or cooler because mass measures the quantity of matter of the substance. The mass of any substance then is independent of temperature. If a book weighs one pound, it weighs one pound regardless if it’s placed in the sun or in the freezer. The unit L (liter) is a unit for volume, the value of which does depend on temperature. An object of some mass occupies a greater volume when warm than when cool.

Also attached to the CTD platform is a chlorophyll a fluorescence sensor, which measures the mass of chlorophyll (typically in micrograms, mcg or μg) per volume (typically one liter, L) seawater (overall units mcg/L). Small biological organisms called phytoplankton contain chlorophyll and hence carry out photosynthesis. Like the photosynthesis carried out by terrestrial vegetation, phytoplankton utilize the red and blue light-absorbing molecule called chlorophyll and the carbon dioxide (CO2) dissolved in seawater to produce biomass and molecular oxygen gas (O2). The famous equation for photosynthesis is:

CO2 + red and/blue light + H2O Ö biomass + O2 Photosynthesis though doesn’t work unless sufficient red and/or blue light from the sun is available at the depths phytoplankton are found. The zone in the ocean near the surface where marine photosynthesis takes place is called the photic zone.

The amount of chlorophyll measured by the sensor is in direct proportion to the amount of photosynthesizing phytoplankton found in seawater. Chlorophyll then can be counted so to speak by making the chlorophyll molecule in phytoplankton fluoresce, i.e. emit light. A chlorophyll fluorescence sensor (CFS) shoots a pulse of blue light into the surrounding seawater. A chlorophyll molecule absorbs the blue light which causes it to emit (give off) red light. The CFS sensor measures the red light emitted. Basically, the more red light that’s emitted means the more chlorophyll-containing phytoplankton present in the surrounding seawater at the depth where the measurement occurs.

Pelagic snail collected off the southern Oregon coast near Coos Bay

Pelagic snail collected off the southern Oregon coast

A CO2 probe interfaced with a computer for continuous real-time data collection measures the amount of gaseous CO2 (in milligrams, mg) dissolved in a given volume of water (typically one liter). Measuring CO2 in seawater is done to gauge the extent of CO2 gas the ocean “cleans” or “scrubs” (not the television show) from the atmosphere. The world’s oceans are huge CO2 sinks because they absorb enormous amounts of gaseous CO2 from the atmosphere annually, a good amount of which is converted into biomass by the photosynthetic activity of phytoplankton.

The “unused” dissolved CO2 forms carbonic acid, H2CO3, which in turn drops the seawater pH, thereby eventually making seawater more acidic. This added acidity (drop in pH) is countered or buffered by the ocean’s natural basic pH, resulting in essentially no net change in pH. But this buffering capacity has limits. If the buffering capacity is exceeded by the addition of too much CO2 in a given time period or the reduction in phytoplankton photosynthesis, then the net result is a drop in pH, making the seawater more acidic. This change in seawater chemistry, in turn, can have deleterious effects on the biology of marine organisms, especially those organisms that live and reproduce in a limited pH range.

One marine organism that is expected to succumb to the predicted net acidification of the oceans over the next decade or so, if not sooner, is the pelagic snail (see photo below). The term pelagic means open so a pelagic snail is found in the open ocean away from the coast.

Why is the pelagic snail threatened? Acidification of the ocean increases the solubility of calcium carbonate (CaCO3), the major constituent of the shells of marine organisms. Solubility is a chemistry term that relates the amount of substance (CaCO3) dissolved in a liquid, in this instance seawater. Essentially a drop in pH (acidification) increases the amount of calcium carbonate in the exoskeleton or shells of marine organisms dissolved, thereby producing thinner shells. Ultimately the shell becomes too thin and any major wave action will break the shell and the organism dies. To show this process, place an egg in a glass of vinegar overnight. The egg shell’s chemical composition is CaCO3. Vinegar is acidic. Over time the shell becomes progressively thinner. Eventually the egg shell dissolves away completely if the egg remains in the vinegar long enough. The yolk inside the egg then is no longer protected by the shell.

Personal Log 

NOAA vessel McARTHUR II in port in Astoria, OR

NOAA vessel McARTHUR II in port in Astoria, OR

I awoke Saturday morning to the music of song birds and a slight drizzle. I couldn’t identify which type of song bird but it didn’t matter; it was a good start to what would be a great day. Early Saturday morning we packed the scientific gear and sensitive equipment/instruments for the seven-hour vehicular transport along US Highway 101 to Astoria, Oregon (45O12’N, 124O50’W), where the NOAA research ship and crew of the McARTHUR II (see photo left) were docked and awaiting our arrival. The south-north drive along US Highway 101 is long and winding but is replete with breathtaking scenery at every turn. It’s highly recommended when visiting Oregon.

The seven-hour drive in the minivan from Coos Bay to Astoria was a good chance to interact with and talk to some of the other science team members, all of whom I had never met nor talked to previous to today. We all would be shipboard with each other for nine straight days. I had better get to know them and get an idea what makes them tick. I’m sure they thought the same.

In addition, over the past year or so I have developed a keen interest in how ships work and as I came to find out during the seven-hour drive so too did a fellow science team member, Bob Sleeth, who sat adjacent to me during the drive to Astoria. The NOAA crew was most welcoming and eager to talk about their ship. Bob and I were treated to an immensely educational tour of the McARTHUR’s navigational systems capabilities from Ensign Andrew Colegrove, a NOAA junior officer who obviously is passionate about both his job and maritime history; he also has a wealth and breadth of knowledge about the practical, engineering ins-andouts of modern ship technology and operational systems. I lost track of time but I’m sure the personal tour lasted more than two hours.

Elizabeth Eubanks, August 3, 2007

NOAA Teacher at Sea
Elizabeth Eubanks
Onboard NOAA Ship David Starr Jordan
July 22 – August 3, 2007

Mission: Relative Shark Abundance Survey and J vs. Circle Hook Comparison
Geographical Area: Pacific Ocean, West of San Diego
Date: August 3, 2007

Weather Data from the Bridge taken at 1300 (5am)  
Visibility: 10+ miles
Air temperature: 18.7 degrees C
Sea Temperature at surface: 21.9 degrees C
Wind Direction: 010N
Wind Speed: 5 kts
Cloud cover: partially cloudy– stratus
Sea Level Pressure: 1014.2 MB
Sea Wave Height: 1-2 ft
Swell Wave Height: <1 ft

Science and Technology Log 

Cleaning – Cleaning – Cleaning. We fuel for 4+ hours – Amazing! We will be in port by 2pm today.

Screen shot 2013-04-18 at 7.23.31 AM

Personal Log 

Thank you, thank you, thank you. I have been honored to be selected to participate in NOAA’s Teacher at Sea program. This has been a life-changing adventure. I am wiser and have so much to share with my students and community.

A huge thanks to all of the scientist for being so nice and so helpful. I feel honored to have worked with Dr. Suzi Kohin, Dr. Russ Vetter and Dr. Jeff Graham as well as grad students Lyndsay Field, Heather Marshall, Dovi Kavec (thanks for being my on board conscience!), Noah Ben Aderet, Alfonsia “Keena” Romo-Curiel, South West Fisheries staff (including Suzi and Russ), Anne Allen (thanks for taking me to the bow chamber), Eric Lynn, Monterey Bay Aquarium staff, Ann Coleman (thanks for teaching me how to set and haul and collect data), and my roommate Leanne Laughlin from California Department of Fish and Game.  The crew has been awesome. I give you many, many thanks and wish you the best at sea. Chico – I am happy and I know it – so my face surely shows it! Jose – “any minute now” and you will catch a fish.

Peter good luck at the Maritime Academy and with the guitar.

LCDR Keith Roberts, thanks for your command. XO Kelley Stroud, thanks for your help with kids’ supplies. I am going to stop here, in case I forget someone, but please know I appreciate all of the folks on the deck, bridge, engine room (Great tour John!) and the galley (the food was amazing) so much. Thanks for your interviews – you will be famous. This trip has been amazing!

Screen shot 2013-04-18 at 7.23.46 AM

Questions of the Day 

What sounds most interesting about the adventure at sea? Would you like to go to see to study sharks? 

Question of the trip: Which hook, the J or Circle, will catch more sharks? 

Please make a hypothesis. Utilize resources to justify your hypothesis. ———Yes, you get extra credit for this. 

Elizabeth Eubanks, August 1, 2007

NOAA Teacher at Sea
Elizabeth Eubanks
Onboard NOAA Ship David Starr Jordan
July 22 – August 3, 2007

Mission: Relative Shark Abundance Survey and J vs. Circle Hook Comparison
Geographical Area: Pacific Ocean, West of San Diego
Date: August 1, 2007

Weather Data from the Bridge  
Visibility: 10 miles
Air temperature: 17.4.0 degrees C
Sea Temperature at 500 m: 4 degrees C
Sea Temperature at surface: 15.2 degrees C
Wind Direction: 300 W
Wind Speed:  13 kts
Cloud cover: cloudy–stratus
Sea Level Pressure: 1014.7 MB
Sea Wave Height: 1-2 ft
Swell Wave Height: 3-4 ft

Science and Technology Log 

Make use of all or your resources! Yes, this ship is charted to study sharks, but as mentioned previously there are many other research projects going on. Dr. Russ Vetter and Eric Lynn are administering a CTD apparatus twice daily in the proximity of where the long lines are set: every night at 2000 (8pm) and every morning at 0500 (5am). CTD stands for Conductivity, Temperature and Depth. This machine costs approximately $15,000 and helps give scientist data to evaluate. The apparatus is dropped from a J Frame, a crane-like structure, from the ship into the ocean, while being guided by E. Lynn and R. Vetter who are strapped to the ship. See photos above and below. The apparatus contains two bottles, similar to a large thermos. Both bottles are open all the way down, depending at what depth the CTD drops to. On this trip it has ranged between 250m and 1,000m down. Once it gets to its destination the scientist pushes a button on their computer that is connected to the bottles and tells them to fire. This action shuts the bottles trapping water samples inside. One bottle is used for maximum depth water collection and the other is used for water sample collections at 10m. They have boxes filled with water samples that will be taken back to San Diego for testing by other scientists.

NOAA scientists, Eric Lynn and Dr. Russ Vetter prepare to lower the CTD. Notice the green cylinders on the left side of the CTD – they are bottles for water samples.

NOAA scientists, Eric Lynn and Dr. Russ Vetter prepare to lower the CTD. Notice the green cylinders on the left side of the CTD – they are bottles for water samples.

There are many other structures on the CTD that measure, salinity, temperature, depth, oxygen levels and fluorescence. Fluorescence measures how much chlorophyll is in the ocean and can be compared to the oxygen levels. Chemical Scientists who work for NOAA have put CO2 detection equipment on board many of the NOAA ships including the NOAA ship DAVID STARR JORDAN. The scientists do not travel with the ship, but come and check the data quite often. Global warming and CO2 levels in the atmosphere have been a hot topic. Many, many years ago when scientists were determining what to do with all the extra CO2, they had thought about pumping into the ocean. Thinking has changed a lot since then. Now scientists realize that the extra CO2 in the ocean is just as detrimental to the ocean as it is to the atmosphere. We’re all connected, we’re all affected. 

A very simple way to think about this is to think of the age-old science experiment of when you put a tooth in a bottle of soda and after a short time the tooth dissolves.  When CO2 is added to ocean water it creates a carbonic acid. Our bones are made of the mineral calcium (Ca) which keeps them hard and allows them to support our bodies.  Sea creatures that have bones or a shell count on Ca as well. Can you imagine what would happen to a clam that didn’t have enough Ca to make a shell? Or could you imagine a clam that had a shell and the acidic ocean water ate it up? These are things we need to imagine. Because of the increase in CO2, our average ocean Ph has dropped from ~ 8.1 down to 7.8, thus making the ocean more acidic. What I write here is only a first stepping stone to so many various things that are occurring with an increase of CO 2 levels on our planet.

The CTD being lowered from the J Frame on the NOAA ship DAVID STARR JORDAN

The CTD being lowered from the J Frame on the NOAA ship DAVID STARR JORDAN

Personal Log 

I can recall sitting in my classroom sometime in March or April. Maggie, a student, was in the room and it was well over an hour after school. I checked my email as I do routinely and there it was, the long awaited message from NOAA. I was a little nervous opening it, but did rather quickly. I was so excited to find out that I had been chosen to participate and immediately shared the news with Maggie, Rob and Dr. Finely the principal of my school. Anticipation filled my life until I got my assignment which was to board the NOAA Ship ALBATROSS IV in July, out of Woodshole, Mass to do a sea scallop survey. Of course I started reading all of the logs teachers had written. I prepared myself for working 12-hour shifts and measuring scallops. In May, when the staff at NOAA realized I would be in San Diego and that there was an opening on the NOAA Ship DAVID STARR JORDAN, they called and asked if I wanted to work with sharks.

It only took me 24 hours to accept that position and then I had new logs to read and new things to anticipate. I was extremely excited and equally as nervous. Would I get sick? Would people be nice? Would I feel safe and comfortable? Would I like the jobs I needed to do? Was I capable of doing the jobs? Oh no – I am not so great with the metric system, will people think I am stupid if I have to think and research before making a conversion? How much will I miss Rob? Will I like boat life? Then my questions even got more specific. Will have enough food? Which snacks should I bring? What does closed-toed shoes mean– can I wear Keens? Do I bring a towel? How many hobby supplies or books should I bring? How many girls will be there? Do we have to share a room with a guy (really I didn’t know)? You can imagine all of the questions I had and they didn’t stop until I had spent 24 hours on the ship and then I understood.

Here I am 11 days into this amazing adventure that has far surpassed anything I imagined. I have 2 more nights to get a giant “rock” (from the ocean waves) to sleep and 3 days to live on the Pacific Ocean. We only have 2.5 sets left to do.  Amazing. – I am going to enjoy every bit – starting right now – I am going to enjoy some of the great folks on board.  

Question of the Day 

What are some things YOU can do to further prevent the ocean from becoming more acidic?

What is a terapod?

What are some things that you anticipate about the upcoming school year?

Question of the trip: Which hook, the J or Circle, will catch more sharks? 

Please make a hypothesis. Utilize resources to justify your hypothesis. ———Yes, you get extra credit for this.