Nathan Pierantoni, Thursday 4.7.11

NOAA Teacher at Sea: Nathan Pierantoni

University of Miami Ship R/V Walton Smith

South Florida Bimonthly Hydrographic Survey

Florida Bay, in transit from Dry Tortugas to Key West.

Thursday, April 7 2011

Weather Data from the Bridge

1400 hrs Local Time

Barometric pressure = 1017 Millibars

79 F

78% Humidity

Visibility = good

Wind SE 16 knots

Science and Technology Log

Dr. Neslon was very gracious and gave me free reign to learn as much as I could while aboard the R/V Walton Smith. Water sampling requires the most manpower and it is most common thing we are doing for this cruise, and therefore I have been involved in many vertical casts of the CTD. CTD stands for Conductivity, Temperature, and Depth, and when I refer to “the CTD” I am referring to the hefty apparatus that is pictured below, sitting on the fantail (the open deck at the stern of the ship). The procedure is as follows: as we get to our stations along our survey route, the boat stops and the we don our hardhats and life jackets and go out to the fantail,. We then lower the safety lines and prepare for a cast. Next, the captain goes to the stern of the upper deck where there is a winch cabin, from where he can pilot the ship and control the cast. The CTD is attached to a cable and is raised and lowered via an A-frame. The scientists give signals to the captain, and together, the device is lowered into the water where it does its work.

The CTD is actually a dual-purpose piece of equipment. It has sensors that measure conductivity (salinity), temperature, depth, chlorophyll, and dissolved oxygen. These sensors are built into a unit at the base of the apparatus and are protected by a metal cage.Above the sensor array is a rosette of tubes, which are able to collect water samples. Each tube holds 10 L of water, and our CDT has 12 tubes, called Nisken Bottles. The whole thing is electronically linked to the science deck through its cable, and in addition to the 2 scientists on deck who deploy the device, there is a CTD operator inside who monitors water parameter changes as the CTD goes from the surface to the bottom. This scientist is in communication with the captain in the winch cabin, and as the device returns to the surface the scientist is able to fire the Niskin bottles so that they fill with water. For example, we just finished a 340m CDT sample, and Nelson fired the CTD at three depths, 338 m, 70m, and 2 m. On the way down he was able to determine ‘where’ in the water column he wanted to collect his samples, because he was able to ‘watch’ the water parameters change on his computer monitor as the data from the CTD’s sensors streamed in. Interestingly, they fire two bottles at each depth in case one of them fails. It’s just another way to prevent against errors that would be too time consuming and thus too costly to fix. Once at the surface, the scientists and the winch operator guide the CTD back aboard the ship, and secure it to the deck.

While data from the sensors is logged and converted electronically to graphs, the chemical oceanographer begins her work. Cheryl Brown, aka ‘CB’ is an ocean scientist who I have had the pleasure of working with on the day shift. Cheryl works for the Cooperative Institute for Marine and Atmospheric Studies, a University of Miami institute that receives funding through NOAA. She participates in a variety of water quality projects, and spends about 25% of her time at sea. The other 75% of her work is in the lab, where she has multiple responsibilities that include filtration, data processing, and plotting of the samples from her fieldwork. This is common to most areas of field science, where for every hour of fieldwork yields at least double the time in the lab. CB has a degree in marine science, and specialized in marine invertebrates before finding her way to Miami.

The responsibilities on the chemistry deck are numerous. For each CDT deployment, there are a variety of samples that must be prepared from the water collected by the CTD. Each of this same series of samples is required for each depth of water that has been tested. On average, three depths are sampled per CTD deployment, but on this cruise some casts have collected water from four depths, and some have only collected water from the surface. The water from each depth is transferred to a bottle, which has been rinsed three times to avoid contamination, and brought into the wet lab. From there, a nutrient samples, chlorophyll samples, and dissolved CO2 samples are taken.

A nutrient sample is a general measure of ocean health, and includes many of the same samples that might be taken in a home aquarium, like ammonia, nitrates, and nitrites. To prepare the sample, we manually filter 50 ml of seawater into a sterile container, and preserve it with chloroform. It is then placed into the lab cooler. Finally, the time, location, depth, sample number, and collection number are logged.

The next step is to prepare a chlorophyll sample, and this is done with another process. In order to increase accuracy, two-200 ml samples are filtered through a small pad that is connected to a vacuum system. The water passes through the filter and is discarded, but the dissolved chlorophyll stays behind. Both small filters are placed into one vial, and the vial is stored in a liquid nitrogen container on deck. Then the samples are logged.

At some of our stations we have collected dissolved CO2 samples. This measure is also an important measure of ocean health, because CO2 is important to the photosynthetic processes that many reef organisms require. To collect a CO2 sample, a sterile flask is filled to the top with seawater, and 2 microliters of Mercury Chloride (HgCl2) are added. These samples are also logged.

This entire process gets repeated for each depth of water that was brought up in the tubes on the CTD. In the end, a whole lot of lab methods are practiced in a very short amount of time. You can imagine that as the week has gone on, these tasks have become easier and easier. At first, we were running stations about every half an hour, and the seas were quite rough. The amount of work to do in short intervals was a little bit overwhelming, but Cheryl let us all know that is would get easier as the week went on, and we she was right! As I finish up this log and we steam from the Tortugas back to the Keys I am looking forward to perfecting my CTD technique before we finish off the week!

Personal Log

It’s been really inspiring to get to know more about the people I am working with. Everyone here is very passionate about the work they are doing, and it is clear that if it weren’t for the love of the job they wouldn’t be out here bobbing around in the ocean! It is also interesting to hear about the different routes that people have taken to get here. This morning during breakfast I had the chance to talk at length with Cheryl about her recent Peace Corps experience. She was sent to the South Pacific island nation of Vanuatu for 27 months to do environmental work and to help facilitate a bank that was going to make micro-loans to women in business. When she got there, plans changed, and she ended up living on a small island called Paama. The island was 2 miles x 7 miles and has 21 villages spread around the coast. What had been an environmental mission turned into an educational one, and she ultimately spent her time on Paama rebuilding a primary school that had been destroyed by a cyclone. She had a canoe specially built for her so she could move about roadless island, and while on Paama she had to adapt to the lifestyle that sounds a lot like backcountry camping to me! Ultimately she had to jump islands on small planes, bargain with shipping captains and work with the entire community to get the school completed.

As I listened to Cheryl tell her story, enthralled by the adventure and romance of her experience, I was reminded of how lucky we are in America to have the education system that we have. It is my hope for my students and colleagues that you all really take advantage of the resources, facilities, and especially the technology what we probably take for granted at times. As I learn more about the future of oceanography I have been especially interested in the direction it is moving, toward space. As more and more remote sensing capabilities are developed, the need for ground proofing will also increase. What is clear to me is that oceanography, like all fields of science, will require dedicated researchers who are passionate about their work and skilled in technology, math, and engineering. There is only one place to get these skills, and its at school, and it requires practice, time, and patience. Thanks to Cheryl’s work, students in that small village on the coast of Paama are able to work toward their education. I challenge everyone at Heights Middle School, myself included, to do their personal best to taking advantage of all of the resources we have in order that our students will become the problem solvers of tomorrow!

I’ll keep posting pictures when I can, and I’m excited to come back to school on Monday!

Here is a shot from the CTD monitor inside the ship. The operator can see what is going on on deck, and follow the ater parameters at the same time.

CTD Monitor inside the ship
CTD Monitor inside the ship

In this shot Cheryl and I are preparing to Launch the CTD. I am signaling the winch operator.

Launching the CTD
Launching the CTD

Another shot of the fantail, and you can see the CTD controlled by a cable via the A-frame.

Fantail
Fantail

Here is the CTD collecting a surface sample.

Collecting a Surface Sample
Collecting a Surface Sample

Here I am in the process of collecting water out of a Niskin bottle, so that I can take it inside for preparation. Notice the instrumentation on the bottom of the CTD.

Collecting Water
Collecting Water out of a Niskin bottle

Here is a shot of Cheryl getting started in the lab on the sample preparation.

Sample Preparation
Sample Preparation

I like this shot, it shows a clean filter pad and a ‘dirty’ one. The pad attached to the vacuum has just finished filtering 200 ml of seawater. The materials on the pad will be analyzed back in Cheryl’s lab on land.

Filter Pads
Filter Pads

Here is a shot of Nelson Melo. He has been operating the CTD during the day, and he is holding a graph that charted Chlorophyll, temperature, O2, and salinity. This CTD was launched to a depth of 340 m.

Nelson Melo
Nelson Melo

Nelson’s work (which I described in my Tuesday log) and the data Cheryl pulls out of the samples we’ve collected will help to refine scientist’s capabilities for remote sensing in oceanography. I think its pretty significant that the latest issue of the scientific journal

Oceanography Journal
Oceanography Journal

Oceanography has a satellite on it. This is the direction that ocean science has headed!

Nice Sunset! Almost as good as our New Mexico sunsets!

Sunset
Sunset

Caroline Singler, August 31, 2010

NOAA Teacher at Sea: Caroline Singler
Ship: USCGC Healy
Mission: Extended Continental Shelf Survey
Geographical area of cruise: Arctic Ocean
Date of Post: 31 August 2010

Back to School – Tuesday 31 August 2010

Midnight in the Arctic Ocean
Midnight in the Arctic Ocean
Location and Weather Data from the Bridge
Date: 31 August 2010 Time of Day: 00:00 (12:00 a.m. local time); 07: UTC
Latitude: 76 º 37.6 ‘ N Longitude: 138 º 31.2 ‘ W
Ship Speed: 8.7 knots Heading: 197 º (SSW)
Air Temperature: 0.19 ºC/ 32.3 ºF
Barometric Pressure: 1009.0 mb
Humidity: 98.8 %
Winds: 6.3 knots W Wind Chill: -5.3 ºC/ 22.4 ºF
Sea Temperature: -0.3 ºC Salinity: 25.32 PSU
Water Depth: 3666.9 m
This is a special message for my new Earth Science students, members of the class of 2014 who are participating in 9th Grade Orientation at Lincoln-Sudbury Regional High School today. I am sorry that I cannot be there with you. I am excited to be your teacher this year – you are important to me, and I look forward to getting to know you when I return. You are in the caring and capable hands of Mrs. Iskandar during my absence. Please be respectful of her and thank her for agreeing to cover my classes for the next week in addition to her normal responsibilities in the Science Department.
As you can see, I am a bit too far north to get there on time. I am currently in the Arctic Ocean on board the U.S. Coast Guard Cutter Healy. The ship icon on the map below shows where I was at midnight on 31 August, which was 3 a.m. in Massachusetts. The red lines on the map show different places that we have been during the last month.
Map of Locations
Map of Locations

We left Dutch Harbor, Alaska (pictured on the right) on Monday 2 August, cruised North through the Bering Sea, and have been in the region of the Arctic known as the Beaufort Sea and the Canada Basin for the last four weeks. I am here participating in an oceanography research expedition as a representative of the NOAA Teacher at Sea program. The research mission is called the Extended Continental Shelf Project. It is an international, multiyear effort between the United States and Canada to map the seafloor and the subsurface in the Arctic Ocean off the coasts of the two countries. Healy (pictured on right) and the Canadian Coast Guard Ship Louis S. St. Laurentare both icebreaker ships designed specifically for scientific expeditions in the polar regions. We made it as far north as 82.5º North and are now moving south again. There is still ice around us now, but not as much as we saw just a few days ago. I have been taking a lot of pictures, and I can’t wait to share them with you. Here are just a few from the last couple of days.

USCGS Cutter Healy
USCGS Cutter Healy
Arctic ocean at night
Arctic ocean at night
Louis at Sunset
Louis at Sunset

A week from now, on Monday, 6 September, we will leave the Healy by helicopter at Barrow, Alaska, the northernmost town in the United States. I expect to be back at school on Friday, 10 September.

Ice
Ice
Breaking Ice
Breaking Ice

Before then, I hope you will take some time to look through my blog and read about some of the things I have seen and done. Then, I would appreciate it if you would send me a short email at this address: caroline.singler@healy.polarscience.net Introduce yourself to me and then either make a comment or ask a question about the Arctic, either based on something you read in my blog or just something you wonder about and would like to know. I will do my best to answer all your questions, and I will give you an extra credit homework grade for your effort.

Enjoy your first week of high school. Don’t get too overwhelmed by the size of the building or the crazy way the class schedule works. You will get used to it in no time. Have fun.

I’m looking forward to hearing from you. I will see you soon.
Miss Singler

Richard Jones & Art Bangert, January 7, 2010

NOAA Teacher at Sea
Richard Jones
Onboard NOAA Ship KA‘IMIMOANA
January 4 – 22, 2010

Mission: Oceanographic Survey
Geographical Area: Hawaiian Islands
Date: January 7, 2010

Cups heading to the depths
Cups heading to the depths

Science Log

Today was a day of transit. We did a lot of work on the buoys, preparing them for deployment and Rick, with the help of Tonya our Chief Survey Technician, got about half of the cups that his students decorated for ‘shrinking’ into the mesh bags to attach to the deep CTD when we do one . The CTD is a rosette of bottles that are sent to depth, in this case 3000 meters (how many feet is that and how many atmospheres of pressure?) where water samples and a record of the Conductivity (salinity), Temperature, and Depth are taken. These CTD’s will help provide a double check for the electronic data that our buoys collect and add to the data used to model El Nino/La Nina. One of the side activities of the CTD is to send down the cups to be squeezed by the pressure. We also have a cup of similar size that will be used as a control so that students will be able to see the changes that the cups undergo. Rick also has brought along a Styrofoam wig head from his daughter Teri to see the effect on a larger scale.

In addition to our work on the buoys we had our first at sea drills including an abandon ship drill.But since we had a similar drill in port we only were required to muster to our stations with our exposure suits, long sleeve shirt, head cover, and long pants and wear our personal flotation device.

Ship safety drill
Ship safety drill

A wee bit rocky today.We have a swell that seems to be coming from the starboard (right) aft quarter, which gives the ship a strange movement that has made some of the folks a little queasy.Ships tend to roll (movement around an imaginary line running bow to stern) pitch (movement up and down around an imaginary line running 90 degrees to the direction of roll) and yaw (movement left or right of the imaginary line running bow to stern).Today the KA is doing all three at the same time which is why we are encouraged to take Meclizine HCL (Dramamine) for a few days prior to the trip and for the first few days at sea. Taking this makes it easier for the crew to function in an environment that has un-natural motion without getting ‘seasick’. Even with the weird motion of the ship, we still have work to do and for us “newbies” things to learn before we are allowed to do them, like learn how to set the ‘painter line’ for the RHIB so that we will stay attached to the ship in the advent that the engine of the RIHB doesn’t start or other various bad things that can happen to a little boat in a big ocean. We didn’t actually ride in the RHIB today, we simply learned how to enter the boat, where to sit , where the emergency items are located, and how to start and steer the boat.

Out on the deck
Out on the deck

One of the tasks that needs to be done prior to the deployment of our first Buoy at 8N:155W is to determine (as close as possible) the ideal position for the buoy’s anchor. To do this it is essential to know the true depth of the ocean and the topography (collectively called bathymetry) of the area within a few miles of the target latitude and longitude for the buoy.Brian, our Chief Scientist, will determine the depth and location for the anchor by using both satellite sea surface heights and actual sonar depth data from ships that have been in the area. In reality, there really isn’t much hard data, physical sonar tracks, for much of the ocean and much of the depth is determined by the actually height of the sea surface as measured by satellite. These measurements take into account variables, such as orbit of the satellite, atmospheric effects on radar, and tides and compare the computer result to a mathematical ellipsoid model of the Earth’s shape. Sounds pretty complicated, and it is, but we can use this calculated sea surface to help determine the depth of the ocean since the surface mirrors the actual topography of the ocean floor. For Academy students, you will have the opportunity to do two activities from the American Meteorological Society (AMS) that will help you understand what it is that we are attempting to do.

Bathymetric map
Bathymetric map
Catch of the day!
Catch of the day!

 

Richard Jones & Art Bangert, January 6, 2010

NOAA Teacher at Sea
Richard Jones
Onboard NOAA Ship KA‘IMIMOANA
January 4 – 22, 2010

Mission: Survey
Geographical Area: Hawaiian Islands
Date: January 6, 2010

Science Log

The KA is under her own steam, well actually diesel and electric, and we are making 10 knots (you should figure out how fast that is in miles per hour) at a heading of 173 degrees. The KA uses diesel generators to create the current to drive here electric propulsion motors. She is a vey quit ship because of this configuration which was part of her original deign…to be quite. The KA is a former Navy antisubmarine warfare ship and needed to be quiet to play her role listening for submarines that might have been lurking around the oceans. Now that quiet nature makes it nice for those of us about to have our first night at sea.

Our current position was 157degrees 51 minutes and 7 seconds west longitude (157:51:07 W) and 22 degrees 55 minutes and 8 seconds north latitude (22:55:09N) at 19:30 lcl on the 5th of January. At that time we had been at sea for about five hours and have many more to go on our way to work the 155 W Buoy line. Sunset was fantastic, but very short. It seems to take almost no time to go from day to night here in the tropics. You can see how it looks behind some of the “birds” (anemometers) that will measure windspeed and direction on the buoys. We are now (09:10 lcl) about 40 nautical miles south of the Big Island and can just see it in the distance. It will be some time before we see land again.

Since we are running a little slow on the internet I will simply post a few images from our first day rather than a video. I will attempt to post a video or two later on but currently we are limited on our bandwidth to about 128K.

For two days I have been overwhelmed as I observed all of the aspects of the crew’s preparation for the TAO mission to Samoa. I am fascinated with everything about this operation – watching the crew load the ship, observing the ship being fueled, viewing the massive nuclear submarines located in Pearl Harbor, and assembling the sensors that collect climate data from each of the buoys we will deploy. Yesterday, in preparation for our voyage, we continued to calibrate instruments and assemble sensors.Last night was our first night at sea, I slept like a baby -the gentle rocking of the boat was like being in a giant cradle.

Robert Oddo, August 10, 2009

NOAA Teacher at Sea
Robert Oddo
Onboard NOAA Ship Ronald H. Brown 
July 11 – August 10, 2009 

Mission: PIRATA (Prediction and Research Moored Array in the Atlantic)
Geographical area of cruise: Tropical Atlantic
Date: August 10, 2009

Weather Data from the Bridge 
Outside Temperature 28.21oC
Relative Humidity 78.32%
Sea Surface Temperature 27.62oC
Barometric Pressure 1019.42 inches
Latitude 23 41.483 N Longitude 80 40.363 W

My last sunset from the Ronald Brown
My last sunset from the Ronald Brown

Personal Log 

I just finished watching my last sunset on the Ronald Brown and it is time that I reflect a little on this entire NOAA Teacher at Sea experience.  The cruise gave me a first-hand look at some of the important work that atmospheric scientists and physical oceanographers examine.  I discovered that the ocean system is huge and scientists around the world are compiling information about the ocean so we can better understand it.  This work is like putting one of those big 1000 piece jigsaw puzzles together. The more pieces that you are able to put together, the better you understand how the pieces fit into the entire picture.  Also because the system is so large, it takes the collaborative effort of many different scientists to really get some sort of understanding about what is happening. This cruise would never have been possible without the crew, the scientist and the NOAA Corp officers working as a team. There was science happening 24 hours and everyone did his or her part.

Sitting at my desk in the computer lab
Sitting at my desk in the computer lab

I feel particularly lucky to be selected as the Teacher at Sea on this cruise and I would like to thank everyone that made it possible.  The crew, the scientists, the NOAA Corp officers were friendly, helpful and always willing to explain things about the ships operation and the science that was happening on the ship. Thank you to the Teacher at Sea support staff that helped with logistics and information pertaining to the cruise.  Special thanks go to than Dr. Rick Lumpkin, the chief scientist, for coordinating the cruise, explaining the science, and reviewing sea logs and Field Operations Officer, Nicole Manning for reviewing sea logs and coordinating things.

Finally thank you to all the people that followed along with this adventure. It was always nice to see how many people were viewing the journal and photos. The questions were great and thanks for all the emails. The impacts that these experiences have on teachers and their students have implications that are far reaching. This has really been a special summer for me and thank you to everyone that made it possible.

Research cruise plan
Research cruise plan