Staci DeSchryver: A Front Row Seat to the Bottom of the Ocean, August 12, 2011

NOAA Teacher at Sea
Staci DeSchryver

Onboard NOAA Ship Oscar Dyson
July 26 – August 12, 2011 

Mission: Pollock Survey
Geographical Area:  Gulf of Alaska

Location:  Kodiak, AK
Heading: back to the docks
Date: August 12, 2011

Weather Data From the Bridge: N/A

Science and Technology Log

My last night on the Oscar Dyson was a busy one!  Because our trip was cut so short, we had to “break protocol” so to speak.  Typically, nighttime operations consist of seafloor mapping (which I will get to in a minute), and do not consist of trawling for Pollock.  For science students, you probably have a good idea why – running operations only in the daytime means that the experiment is controlled.  Since Pollock behave differently in the night-time, it is important to only run operations when their behavior is consistent.  However, because we were so short on time, we had to make a “run” for the shelf break that got us to the area well after dark.  So we got to do one more trawl!  This one was the best kind, in my humble opinion.  We completed a bottom trawl, which means that the net went almost down to the bottom of the ocean – within a couple of meters.  The reason why bottom trawls are so neat is because there are plenty of ocean critters down there that the average Joe doesn’t get to see on a daily basis.  Of course, the scientists do their absolute best to catch only Pollock to minimize bycatch, but one or two fish of different species are difficult to avoid.  On this trawl, we had a few jellies, two Pacific Ocean Perch, and a Herring.  We finished late – right around one in the morning.  At that time, we began our night-time operations.

Night time operations are run by Dr. Jodi Pirtle.   Dr. Pirtle is a Post-Doctoral Research Associate at the University of New Hampshire  Center for Coastal and Ocean Mapping.  Her research is a collaborative effort between the UNH CCOM and the NOAA Alaska Fisheries Science Center.   Even though Jodi is traveling all the way from New Hampshire,  she is actually very close to home right now.  She is quite connected to the Alaska fisheries – she grew up in Alaska, and has both family and friends who are involved in the commercial fishing industry.  The fisheries hold a place very close to her heart, and her passion for her current line of work is well evident.

So, why, then, does Dr. Pirtle work in the cover of night?

acoustics lab
Here, the scientists are working in the acoustics lab on daytime operations. As you can see, most of the electronic equipment is used during the day. At night, Dr. Pirtle gets the opportunity to chart her own path and select an area to map without interfering with the ship's primary operations.

At first I suspected it was some sort of secret service operation, but the reality is much more strange and explainable.  Her line of work is a side project on the Oscar Dyson, which means that she can work when the ship is not working for its primary purposes.  Hence, she works from 6pm until 6am.   One focus of her research is to identify whether or not certain areas of the Gulf of Alaska are trawlable or untrawlable by the Alaska Fisheries Science Center bottom-trawl survey for groundfish.   How is an area determined to be untrawlable?  Let’s say, for example, there is a commercial fishing ship somewhere in the Gulf of Alaska.  This ship decides to do a similar trawl as the one that I did earlier this evening, but they use a net that makes contact with the seafloor because they are fishing for groundfish species – say, Rockfish, for example.  But, something happens.  When the net comes up, it is all torn up – as though it got caught on a series of rocks or ledges.  In order to warn other ships of the dangers of losing a very expensive net, the fisherman deems the area “untrawlable.”  It’s kind of like putting caution tape around the area.

Untrawlable areas are problematic for scientists because every area deemed untrawlable is an area where they can’t sample with the bottom-trawl gear.  For example, a large component of the groundfish fishery are several species of rockfish (Sebastes spp.) that associate with a rocky habitat.  Rockfish are delicious with garlic and butter, but they are sneaky little guys because they like hanging out around rocks (who knew?).  Many rockfish could be in areas that are untrawlable, but scientists would never know because it is inadvisable to tow a bottom-trawl net in the area to find out.  In a sense, untrawlable areas are a source of error, or uncertainty in the population estimate for species of groundfish in those areas.  This is where Dr. Pirtle’s research starts.

A few years ago, a group did research in an area called Snakehead Bank – a location previously deemed to be untrawlable.  They wanted to tighten the definition of “untrawlable.”  For example, there is a possibility that an untrawlable area is covered with steep cliffs, many sharp, large rocks, and impossibly tough relief.  However, there is also the possiblity that the area is relatively flat and trawlable, but the fisherman was just unlucky enough to drag his or her net over a rogue boulder that found its way onto the vast, flat, continental shelf.  So, the scientists decided to see what kind of “untrawlable” this particular area was.   The group took the time to make a bathymetric profile of the area and couple that research with camera drops – video cameras that would make the trek to the bottom of the ocean and provide a second set of data for scientists to confirm what the bathymetric profile showed them.  From the camera drops and the bathymetry, the scientists determined that Snakehead bank was not completely untrawlable – in fact, most areas could support trawl nets without the risk of tearing the nets.  Dr. Pirtle is continuing with this important work.

One focus of the research is determining seafloor trawlability in the Gulf of Alaska using the same acoustic transducers that we use to catch fish in our daytime operations.  The fishery that the  survey is concerned about  is groundfish –   a general term that encompasses many species such as flatfish, cod, and rockfish.  These sneaky guys enjoy habitats that are associated with rocky areas, so we are not getting the best estimate of populations in those areas.  Dr. Pirtle is looking in to alternative methods to determine whether an areas of the seafloor is untrawlable or trawlable using the mulibeam sonar.  Not only is she looking for areas that can now be considered trawlable, she’s also using the data she collects to determine certain seafloor characteristics.  Hardness, roughness, and grain size are all data that can be collected using the acoustic transducers.  This information will help her to determine the relative trawlability of an area, as well.  Therefore, the groundfish survey benefits because she is either finding areas to be trawlable (thus, they can now sample there) or somewhat trawlable, which can tell them ahead of time that alternative sampling methods might be needed in a particular area.

Her research is also concerned with developing alternative sampling methods for untrawlable locations.  These methods could involve a combination of acoustic seafloor mapping to characterize seafloor habitats for groundfish, acoustic midwater data (to observe the fish that like to hang out on tall pinnacles and rocky banks) and, the most fun method – dropping a camera to the ground to identify species and biomass assessment (which is a fancy term for seeing how many fish are in a particular area).  Improved understanding of groundfish habitats can lead to better management models, and the work Dr. Pirtle is doing can also contribute to conservation of areas that are sensitive to fishing gear that touches the seafloor.

The area that Dr. Pirtle decided to survey this evening was an area that was deemed to be untrawlable surrounded by many trawlable areas.  These areas are often good candidates for mapping and camera surveys because both untrawlable and trawlable seafloor types are likely to be encountered, so the area can more easily be compared against existing data.  We began our transects – driving transects with the ship over the area while sending sound waves to the bottom of the ocean to figure out differing ocean depths and seafloor type.  Transect lines are close together and driven in a pattern similar to mowing a lawn, which gives Dr. Pirtle 100% coverage of her targeted area.  Dr. Pirtle selects a location to drop a CTD – Conductivity, Temperature, and Depth meter – usually in the middle of the mapped area.  The CTD is used to estimate sound speed in the location she is mapping.  This is important because ocean depth is measured by the amount of time it takes for a sound wave to leave the ship, bounce off the ocean floor, and return back to the ship.

This is a photograph of a halibut on the uncharted pinnacle discovered by Dr. Pirtle, similar to what I saw real-time on the camera late at night.

She then selects three to five areas to conduct camera drops.  The camera travels to the bottom of the ocean where she can see if the area is untrawlable or trawlable based on what the camera shows her.  I, on the other hand, get to see deep ocean critters in their habitats, which is also very cool.   There are two types of camera drops – ones that record the information and then get played back later, and real-time camera drops where we can literally watch the camera make the trek to the bottom of the ocean in real-time.  Dr. Pirtle uses the camera data to “groundtruth” or check the seafloor type against her acoustic map, to identify fish and other animals in the area, and to observe how species use the seafloor habitat.

As my shift was coming to a close, I could barely keep my eyes open, but I didn’t want to miss this.  Tonight, we dropped the live camera into the depths.  I stayed awake for the first drop so I could see what these operations looked like.  Dr. Pirtle expertly maneuvered the camera into the deep using something that looked much like an old-school Atari controller.

slide o' fun
This photograph shows Dr. Pirtle's work in combination - the area she surveyed is in the bottom right corner. The other three photos are snapshots of the surveyed area.

As the camera dropped, we saw a few pollock and some other unidentified neritic creatures, but the real fun started when we got to the bottom.  It was intense as Dr. Pirtle relayed information back to the bridge about the direction in which to travel, holding the ship still in the waves and currents when she wanted to examine an area more closely, and communicate with the technicians on the hero deck to relay the height that she wanted the camera held at.  We saw all sorts of interesting creatures on the ocean floor – some arrowtooth flounder, a halibut, and Pacific Ocean Perch.  We also observed beautiful cold-water corals and sponges that form a living component of seafloor habitat for many marine animals, including our target – rockfish.   We even saw a shark!  It was completely worth getting to bed a little bit later to see this incredible work in real-time.

unmapped pinnacle
This is the unmapped pinnacle discovered by Dr. Pirtle and her colleague! Now, seafloor maps have been updated to include this potentially dangerous sea hazard.

On a side note, in a previous leg of the survey, Dr. Pirtle and her colleague from UNH CCOM, Glen Rice,  found an underwater pinnacle that was later determined to be a navigational hazard!  This pinnacle came so close to the surface of the water that in a “perfect storm” of low tide and a large enough ship with a deep enough hull, it could have unknowingly collided with this unmapped pinnacle – which could have potentially been disastrous.  Glen, a NOAA hydrographer, was able to update the navigational charts in the area, alerting ships to the pinnacle’s presence.  It just further supports the idea that the our oceans are so vastly unexplored – there is so much we don’t know about the feature that takes up the biggest portion of our Earth!   I asked her if she named it because she discovered it – I quickly learned that just because you find something in the Ocean, it doesn’t mean you get to keep it.  Apparently, you can’t name it, either.  But I still called it Pirtle’s Pinnacle.  I think it has a nice ring.

Personal Log

It was a sad day today watching the scientists pack up and box and tag the lab equipment and computers.  As everyone bustled about, I spent some time hanging out for the last time on the bridge, in the galley, and in the fish lab thinking about my journey coming to its close.  Although we spent the majority of it tied to the dock, I am so grateful for the opportunities we experienced that we otherwise would not have – it was a blessing in disguise, because we really got to experience all of Kodiak, and much of the bays and inlets around the island from the ship.  The pictures will bring no justice to the beauty I’ve experienced in the last three weeks, whether it was walking along a beach with wild horses or staring in all directions to find nothing but water for as far as the eye could see.  I spent an hour one night on the bridge watching the Leonids streak across the sky – a front row and first class seat, in my opinion.  I never though that dodging whales would be an area of concern in my small life until we sailed through pods of them every day.  If you would have told me three years ago I’d be petting an octopus three weeks ago, I would have called you a fool.  If you would have told me three hours ago that this experience would be coming to a close three minutes from now, I would believe you even less.  In the last three weeks, I have never laughed harder, worked more eagerly, or learned more with and from these incredible individuals who call this ship Home.  As I quietly stood on the bridge watching the fast rescue boat dart off to the docks, I remembered the last time it was in the water watching carefully over us as we swam around the ship in our gumby suits.  As we drove silently through the still waters to the city docks, we bade farewell to the animals that accompanied us on our trips – otters, eagles, puffins, and even sea lions gathered around to see us off to our homes and families.  Or, they just so happened to be there looking for food and doing other instinctual things, but I do really think I saw an otter wave me goodbye.

whale!
Here is a whale "waving goodbye" with his fluke in the Gulf of Alaska - I will never forget the journey I had here!

Thank you so much to the crew and scientists of the Oscar Dyson – you fed my soul this summer and rejuvenated me in a way I never could have imagined.  I am more revived today than I was on the first day of my second year of teaching (because, let’s face it, the first day of your first year you spend most of your time trying not to vomit) and I owe it completely to the Teacher at Sea Program and to all of the fine people I got to work with.  To my partner in crime, Cat Fox – I’ll see you when we’re landlocked again!  It was a total blast working with you.  Thanks for always being there for a good laugh and for finding me so many salmon berries!  If you are wondering whether or not you should apply for this program in the 2012 season – this is the advice I will give to you:  JUST APPLY!  It will change your life – promise.

Until our next adventure,

Staci DeSchryver

Did you know…

While I was working my night shift, I got the opportunity to help Dr. Pirtle “log the turns” of the ship as it was “mowing the lawn” in the zigzag pattern.  This meant that I got to communicate with the bridge via radio every time they ended a transect and began turning in the opposite direction.  I’m sure you may have predicted that this was most certainly a highlight of my work.  It took great restraint on my part to behave myself with the radio, as everyone knows that radios can be a lot of fun.  I did, however, let a few nautical words fly on the airwaves up to the bridge, one of them being “Roger, Willco.”

I had no clue where the origin of the word “Roger” came from.  But now I do…

Roger, which starts with the letter R, means “Received”, which means, “I received your last transmission.”  A long time ago, the radio alphabet (you know, Alpha, Bravo, Charlie, Foxtrot, Whiskey, etc.) used Roger to represent the letter R.  It has since been changed to “Romeo.”  Adding Willco to the end, means “I received your transmission, and I WILL COmply.”   So saying that I received a message from the bridge and I was going to comply with it really made me look like a navigational moron – because they weren’t asking me to comply with anything.  But I still had fun.

Caroline Singler, August 7-9, 2010

NOAA Teacher at Sea: Caroline Singler
Ship: USCGC Healy

Mission: Extended Continental Shelf Survey
Geographical area of cruise: Arctic Ocean 41 miles north of Alaska
Date: 9 August 2010

Seeing the Bottom — 7 August 2010

It’s taken me several days to write and post this entry. I wanted to learn more about the sonar technology that we are using for the bathymetric mapping, then we lost internet early on the morning of 8 August 2010 while heading north in the Beaufort Sea. This happened at about the same time as we started encountering heavy ice, but I do not believe that the two events were related. I am including location and weather data for several days to give you a sense of where we were and where we are heading as well as the physical changes in our environment.Thankfully, email works even when internet does not – it took my non-IT oriented mind a while to wrap itself around that concept. While I am out of range, my dear sister Rosemary has agreed to post for me as long as I can get emails to her. (Thanks, Ro!) You already have her to thank for the polar bear post. Please keep emailing and/or posting comments. I look forward to reading comments when I come home.
Location and Weather Data from the Bridge
Date: 7 August 2010 Time of Day: 1400 (2:00 p.m.) local time; 22:00 UTC
Latitude: 70º47.6’N Longitude: 142º42.3’W
Ship Speed: 15.1 knots Heading: 111º (southeast)
Air Temperature: 5.1ºC /41.6ºF
Barometric Pressure: 1005.3 millibars
Humidity: 87 .9%
Winds: 27.7 Knots NE
Sea Temperature: 2.3ºC
Salinity: 20.22 PSU (practical salinity units)
Water Depth:1270 .8 mDate: 8 August 2010
Time of Day: 1245 (12:45 local time); 20:45 UTC
Latitude: 72º12.72’N
Longitude: 138º28.7’W
Ship Speed: 7.7 knots
Heading: 36.2º (NE)
Air Temperature: 0.5ºC /32.9ºF
Barometric Pressure: 1012.7 millibars Humidity: 86.3%
Winds: 19.3 Knots NE
Wind Chill: -7.48ºC/18.53ºF
Sea Temperature: -1.2ºC Salinity: 25.5 PSU
Water Depth:2547.8 mDate: 9 August 2010
Time of Day: 1530 (3:30 local time); 22:30 UTC
Latitude: 72º 29.8’N
Longitude: 139º 40.9’W
Ship Speed: 6.3 knots
Heading: 183.5º (SSW)
Air Temperature: -0.03ºC /31.94ºF
Barometric Pressure: 1009.7 millibars Humidity: 92.2%
Winds: 17.7 Knots NE
Wind Chill: -6.02ºC /21.17ºF
Sea Temperature: -1.2ºC Salinity: 25.08 PSU
Water Depth:2969.0 mScience and Technology Log
The primary objectives of the science mission are to map the seafloor and image the underlying sediments. Bathymetry is the measurement of depth of water bodies, derived from the Greek bathos meaning deep and metria meaning measure. Early bathymetric surveys used the “lead-lining” method, in which depths are manually recorded using a weighted line. This method is slow and labor intensive, and it is not practical for depths greater than about 100 feet. (Ironically, I spent the summer of 2009 doing just such a survey of a small lake on Long Island, NY working with two other teachers as DOE-ACTSinterns at Brookhaven National Laboratory.) Modern bathymetric surveys use echo sounding, or SONAR (Sound Navigation and Ranging) to determine depth and shape of the seafloor. These systems make it possible to map large areas in extreme detail, leading NOAA to name the 20th Century advancements in hydrographic surveying techniques to its list of Top Ten Breakthroughs during the agency’s first 200 years.SONAR uses sound signals to locate objects beneath the sea surface. Passive systems use receivers such as hydrophones to detect signals transmitted by other sources, such as animals or submarines. Active systems transmit and receive signals. A transmitter mounted on the ship’s hull emits a signal. The signal travels through the water column and bounces off an object in its path. It returns as an echo to a transmitter on the ship that measures the strength of the return signal. The time between transmission and reception is used to determine range, where range equals (speed of sound in seawater) times (travel time divided by 2). When the object that reflects the signal is the seafloor, the range is the water depth.

There are single beam and multibeam sonar systems. Single beam systems measure along a single line beneath the ship and produce a line of depths. Multibeam systems send signals out along a line perpendicular to the ship and generate a “swath” of data for the area beneath the ship. The advantage of this system is that it creates a map that shows depth and shape of the seafloor. The diagram below shows a schematic comparison of three bottom survey methods.

Chart of three survey methods
Chart of three survey methods
Me on watch
Me on watch
Healy is equipped with a hull-mounted multibeam sonar system. It runs continuously whenever Healy is at sea, collecting bathymetric data to add to our knowledge of the seafloor at high latitudes. I serve as one of the watch standers in the geophysics lab each night from 8 p.m. to 12 a.m. We keep an eye on several computer monitors that display the data from the different geophysics tools and others that display water quality and geographic position data. The photo on the right shows me with my watch partner, USGS scientist Peter Triezenberg sitting at the watch station.
There are many variables that can influence the quality of the multibeam data. The speed of sound in water is influenced by many different variables, including temperature and salinity. Therefore, seawater samples are collected from the ship’s seawater intake system to generate a thermosalinograph (TSG) profile to keep the speed of sound accurately calibrated. Additionally, expendable probes (XBTs) are launched twice a day to update the sound speed profiles. Other instruments monitor the attitude (pitch, roll and heave) of the ship and feed that data to the multibeam system. Finally, the ship keeps extremely precise track of time of day and geographical position so that the data can be used for accurate bathymetric mapping of the seafloor. My job as a watch stander is basically to be sure that everything is running properly, and to notify one of the specialists if something is not right.
Multibeam monitors:
Multibeam Monitors
Multibeam Monitors
TSG display:

The end result is a detailed map of the seafloor in which different colors represent different depths. The picture below shows an image of the raw multibeam data superimposed on a seafloor map which we can see on the ship’s Map Server display. The red line shows the ship’s track, and the new multibeam data extends perpendicular to that line. Other data on the map are from transects mapped on earlier Healy cruises and other sources.

Map Server Display
Map Server Display
Personal Log

Breaking ice
Breaking ice
We experienced a range of sea and ice conditions over the last several days as we traveled east of Barrow Alaska and headed north into the Beaufort Sea. Our earliest ice encounters were a gentle preview of what was to come – mostly bumps and scrapes with small pieces as we headed eastward parallel to the Alaska coastline. By midday on Saturday, we began to cross larger floes, and at times the ship was really rocking. One science team member said it feels like riding the subway, that’s a pretty good analogy. Sitting in the Mess on the main deck of the ship – which is about one floor above water line – I hear the grinding of ice on steel and it feels like I’m sitting in a big tin can that’s being crushed in a trash compactor. Fortunately, the ship is tougher than the ice. At times we move so much that everything in the room shakes. Because we are on a ship, everything is bolted down, but I still look up to be sure there is no danger of anything falling on my head. Some team members from California say the sensation reminds them of an earthquake.

Late Saturday morning, we crossed out of ice and back into open water. As we approached the last pieces of ice before open water, I saw waves hitting the distant edges of the ice; it looked like waves breaking on the shore. At first, I did not grasp the significance of this observation – I thought it was pretty and snapped some pictures and marveled at how we could be in thick ice and then suddenly in open water.

Waves on ice
Waves on ice

In the next hour, I realized that these were the largest waves we had encountered so far on the trip, and while they looked pretty, they also made the ship roll considerably more than it had before. Over the next few hours, I began to sense the movement more than I had in a few days. By dinner time, I had difficulty walking straight across the mess deck, and I was becoming a little apprehensive. I took a motion sickness pill as a preventative measure, and I took a nap because it was far more pleasant to lie in my rack and be rocked by the ship’s motion than to try to remain vertical. We eventually moved into calmer waters, and soon after that, we were back in heavy ice, which I somehow do not find as unpleasant as the waves. Since then, our movement has been slow and steady along our transects through the ice, with an emphasis on slow.

We don’t get much darkness up here in the Arctic, but we do occasionally get treated to some great sunrises and sunsets, if one is awake to catch them. Here are some photos of the sunset on Saturday 7 August 2010. The first was taken about an hour before sunset from the port side of the ship. I was as captivated by the horsetail clouds as I was by the color of the sky. The second was taken just at sunset, right before my camera battery died!

Sunset
Sunset
Sunset from the port side
Sunset from the port side

Anne Marie Wotkyns, July 8, 2010

NOAA Teacher at Sea
Anne Marie Wotkyns
Onboard NOAA Ship Pisces
July 7-13, 2010

NOAA Teacher at Sea: Anne Marie Wotkyns
NOAA Ship Pisces
Mission: Reef Fish Survey
Geographic Area: Gulf of Mexico
Date: Thursday, July 8, 2010

Weather Data from the Bridge

Wind: 7-9 mph
Other Weather Features:
Sunny, scattered light clouds
Waves 1’; Swells 3-4’
Location: 28.37.2 N
089.33 W

Science and Technology Log

Hello, my name is Anne Marie Wotkyns and I am participating in the NOAA Teacher at Sea program. I teach 4th grade at J.B. Monlux Magnet School in North Hollywood, California. I joined the NOAA ship Pisces on the evening of July 6 to begin a 6 day cruise in the Gulf of Mexico. I will be posting logs to share the information I learn and the experience of working aboard a scientific research vessel. We will be working on the SEAMAP Reef Fish Survey of Offshore Banks, a project which provides information about the relative abundance of fish species associated with geographic features such as banks and ledges on the continental shelf of the Gulf of Mexico. I’ll be explaining this project more in my next log entry.

Me in front of the Pisces
Me in front of the Pisces

After meeting the other Teacher at Sea, Liz Warren and bird expert Scott Mills, at the Gulfport Mississippi Airport, we were driven to the NOAA docks in Pascagoula, Mississippi. It was quite late when we boarded the Pisces, so we found the cabin Liz and I would share, explored the ship a bit, and turned in for the night.

Wednesday, July 7 found us eager to get started on our TAS adventure. We started the day at the NOAA office and lab building, adjacent to the ship docks. There we met Kevin Rademacher, Chief Scientist for the SEAMAP (Southeast Area Monitoring and Assessment Program) offshore reef fish survey which we will be participating in on our cruise. He showed us around the NOAA facilities, which house the Southeast Marine Fisheries Offices, Seafood Inspection, and Documentation Approval and Supply Services. The fisheries division deals with resources surveys, harvesting, and engineering related to commercial fishing. The seafood inspection division deals with issues related to seafood safety and chemical and microbiological analysis of seafood. These labs can help determine if the “red snapper” your favorite restaurant serves is really red snapper or a different type of fish! This division will also be testing some of the fish we collect on our cruise for baseline data on fish from areas outside the oil spill for possible later comparison to fish collected within the spill zone.

Me in Front of the Southwest Fisheries Building
Me in Front of the Southwest Fisheries Building

Now a little more about the Pisces, my home away from home for the next 6 days. The Pisces was commissioned in 2009 and is one of NOAA’s newest ships. She is 63.8 meters (209 feet) long, 15 meters (49.2 feet) wide, and has a draft of 6 meters (19.4 feet.) Her cruising speed is 14.5 knots and she can stay out to sea for 40 days if necessary. On this cruise there are 22 crew comprised of a commanding officer, deck officers, engineering officers, deck hands, engineers, stewards, and survey and electronic technicians. There are 6 on our science team and 2 bird observers conducting surveys of pelagic seabirds possibly affected by the oil spill.

NOAA Ship Pisces
NOAA Ship Pisces

After we set sail on Tuesday afternoon, we spent much of the late afternoon up on the flying bridge, the highest deck on the ship. We observed a wide variety of boats and ships in the channels around Pascagoula Bay. Scott and Ron, the bird observers, helped us identify the bird species we saw, including Brown Pelicans, Laughing Gulls, and Sandwich Terns. We also saw several Atlantic Bottlenose Dolphin swimming near the ship. Soon the seas grew rougher and after dinner and a short welcome meeting, we retired to our cabins for the night.

Wednesday morning brought calmer seas, and the start of “science “ on board the Pisces. Before we reached the areas selected for the SEAMAP fish surveys, Chief Scientist Kevin Rademacher wanted to conduct bathymetric mapping of an area called Sackett Bank, off the coast of Lousiana. This involves sailing the ship in a series of overlapping transects 1.6 miles long, .05 miles apart, similar to “mowing your lawn” at home. The ME70 multibeam acoustic system covers a swath of 120 degrees using 27 beams which can detect and map features on the sea floor down to .5 meters in size. This will allow NOAA to produce highly accurate nautical charts of the region. The charts will eventually be available to commercial and sport fishermen, sailors, shipping companies, and anyone else who is interested.

Mapping Sackett Bank
Mapping Sackett Bank

When a ship is conducting activities like this bathymetric mapping or other “Restricted Mobility and Manuevers” work, they hoist a nylon “Ball-Diamond-Ball” to notify other ships in the area that it is restricted in its movement so the other ships can change their course. This message is also sent electronically by VHF radio signal. I happened to be on the bridge while they prepared to start the first transect, so Commanding Officer (CO) Jeremy Adams let me hoist the ball-diamond-ball.

Hoisting the ball-diamond-ball
Ball-diamond-ball

    Hoisting the ball-diamond-ball
Hoisting the ball-diamond-ball

Transect Lines
Transect Lines

In this photo, the green boat indicates the position of the Pisces as we conduct the mapping transects.

Tomorrow the plans are to begin the SEAMAP reef fish surveys, “one hour after sunrise” – looks like we’ll be working from about 7 am to 7 pm with the fish! Bring it on!!

Personal Log

After submitting Teacher at Sea applications for 3 years (the first 2 years I was not selected) I am thrilled to be here! The opportunity to participate in a cruise like this on such an amazing ship is truly a once in a lifetime experience!

Here are a few more pictures of life aboard the Pisces.

Stateroom
Stateroom

Desk
Desk

Galley
Galley

Our cabin is a little small, but very clean and functional. Liz volunteered to take the top bunk, so I have the bottom. I love the little curtains that can enclose the bunk – makes a dark little “cave” for me! And the reading lamp lets me read late at night! We have a flatscreen TV, but so far we have only been able to watch the USA network – one channel only. But we don’t spend much time in the cabin anyway. The bathroom is very similar to a cruise ship bathroom, and the shower has great water pressure – however the ship is under water conservation so showers need to be quick. Notice we’re eating on paper plates with plastic utensils. No dishwashing either! After the ship moves farther from the oil spill they will able to use their salt water to fresh water conversion process and we’ll be able to use water more freely.

Pascy chooses his dinner in the “mess” – sorry – no fish!

In Pascagoula I purchased a small stuffed penguin and named him “Pascy” (for Pasacagoula.) Pascy has been exploring the Pisces so here are some shots of him around the ship!

Pascy helps check off each transect in the acoustics lab.
A little coffee is always good in the morning.
The cookies here are great!

Another big event today was the fire drill and abandon ship drill. We were assigned “muster stations”, places we would go to in event of an emergency. Part of the drill was to practice donning our “survival suits” – one piece insulated buoyant suits that would keep us afloat and warm if we ever had to abandon ship. The hardest part of the drill was getting the awkward suit on and off – they seem to be one-size-fits all and I seem to be smaller than most sailors!

Even Pascy got to participate in the drill! I don’t think he need to worry about staying afloat or warm in the water! Good thing, because that lifejacket looks a little big!

Immersion suit
Immersion suit

Me in my Gumby Suit
Me in my Gumby Suit

Christine Hedge, September 5, 2009

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

Mission: U.S.-Canada 2009 Arctic Seafloor Continental Shelf Survey
Location: Beaufort Sea, north of the arctic circle
Date: September 5, 2009

Weather Data from the Bridge  
Latitude: 770 13’N
Longitude: 1370 41’W
Temperature: 290F

Science and Technology Log 

The two icebreakers are tying up side-by-side so that we can visit each other.
The two icebreakers are tying up side-by-side so that we can visit each other.

More Ways to Use Sound to See Beneath the Sea Floor 

Today we “rafted” with the Louis (the ships tied together side by side). I have been eager to see the science instruments that the Canadian ship is carrying. Once the ships were securely tied together we could just walk back and forth between them and tour the Canadian vessel.

The Healy has been breaking ice so that the Louis can have an easier time collecting data using seismic reflection profiling.  The goal is for the Canadian scientists to determine how deep the sediments are in this part of the Arctic Basin.  The sound waves their instrument sends out can penetrate about 1500 meters below the seafloor. Using sound they can “see” inside the earth – amazing!

FOR MY STUDENTS:  Remember your Latin/Greek word parts?  Look up “seism”. 

Seismic sled being hauled out of the water on the Louis. (Photo courtesy of Ethan Roth)
Seismic sled being hauled out of the water on the Louis. (Photo courtesy of Ethan Roth)

Here is how it works. The Louis steams forward at a low speed following in the path that the Healy has created through the ice. The Louis tows behind a weighted sled with 3 airguns suspended from the bottom.  This sinks about 10 meters below the water. Attached to the sled is a long tube filled with hydrophones (underwater microphones) called a streamer.  This streamer is about 400 meters long and stretches out behind the ship. It is best for the ship to move continuously so that the streamer will not sink or float to the surface.

FOR MY STUDENTS: Try to picture a 400-meter long “tail” on a ship. That is longer than 4 football fields. 

The airguns create a huge air bubble in the water.  When it collapses, it creates a sound pulse.  Two of the guns use a low frequency, which will penetrate deep into the sea floor but will create a low-resolution image.  The other gun uses a high frequency, which does not penetrate as deep but gives a high-resolution image.  The 16 sound recorders in the streamer record the echo created by these sounds reflecting from the sediment layers below the sea floor. The final product this instrument creates is an image of a cross section through the Earth. Scientists can look at these by observing this geologic history, the scientists are looking back in time. You can imagine that ice can cause lots of problems when a ship is towing a 400-meter long streamer behind it.  This is why we are working on collecting this data together.  One ship breaks, the other collects the seismic reflection data.

Steamer on deck of Louis. The blue steamer is out of the water and lying on deck when we visit the Louis.
Steamer on deck of Louis. The blue steamer is out of the water and lying on deck when we visit the Louis.

Personal Log 

The crew has been looking forward to the two ships tying up together for the entire cruise.  Everyone is curious about the other ship. What are the staterooms like?  What is the food like? How is their bridge different from our bridge? And of course there is shopping!! Both of the ship stores had their best Louis and Healy gear ready for the eager shoppers.

After learning about the science instruments aboard the Louis, it was nice to finally see the seismic sled, streamers, and the computer nerve center where the seismic images are received. The ships are pretty different in their appearance.  The Louis is an older vessel and has wooden handrails, panels cover the wires in the ceiling, and there are some larger windows with actual curtains.  The Healy was built to be a science research icebreaker and so has many large spaces for science and looks generally more industrial. The Louis was an icebreaker first and some of their science spaces have been added later and are less spacious.

The bubble created by the airguns on the Louis. (Photo Courtesy Pat Kelley USCG)
The bubble created by the airguns on the Louis. (Photo Courtesy
Pat Kelley USCG)

Shopping and tours were fun but the most anticipated events of the day were the evening meal, contests and games.  The ship’s officers exchanged gifts in a formal presentation and then we had an amazing buffet together.  Personnel from both ships enjoyed scallops, halibut, salmon, shrimp, lobster, pork, beef, cheese, salads, and desserts. This was an exceptional meal and a great social event.  The idea of having Teachers at Sea (TAS) was a new one for most Canadians I spoke with and as we talked they seemed to think this TAS would be a great idea to stimulate interest in young Canadians about maritime careers.  The evening concluded with some friendly competitions between the crews and the science parties.  This entire event was a lot of work for the Coast Guard crews.  The science party really appreciates all the hours they put into planning this event!

Behind the wheel on the bridge of the Louis S. St. Laurent.
Behind the wheel on the bridge of the Louis S. St. Laurent.

Christine Hedge, September 4, 2009

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

Mission: U.S.-Canada 2009 Arctic Seafloor Continental Shelf Survey
Location: Beaufort Sea, north of the arctic circle
Date: September 4, 2009

Sometimes kittiwakes follow the ship.  I caught this one as it passed by the Healy.
Sometimes kittiwakes follow the ship. I caught this one as it passed by the Healy.

Weather Data from the Bridge  
Latitude: 780 12’N
Longitude: 1360 33’W
Temperature: 290F

Science and Technology Log 

Part of NOAA’s mission is to conserve and manage marine resources. To this end, the Healy has a Marine Mammal Observer (MMO) on board. Our MMO is Justin Pudenz. He collects data on any interactions we might have with marine mammals during our voyage.  Both the Louis and the Healy have observers on board.

Using a field guide to identify the Yellow Wagtail
Using a field guide to identify the Yellow Wagtail

Justin spends his time on the bridge of the Healy, binoculars in hand, notebook near by, always on the lookout for life on the ice or in the air. He lives in southern Minnesota when he is not on a ship. Justin tries to spend 6 months at sea and 6 months at home. He has been a fisheries or marine mammal observer since 2001. The company he works for is MRAG Americas.  NOAA hires observers from this company when they are needed. While on board the Healy, Justin spends hours each day watching for marine mammals and recording his observations.  The data he collects goes back to NOAA.

Justin has traveled to many bodies of water as an observer including the Pacific near Hawaii and the Bering Sea for fisheries observation.  His next mission will be on a crabbing vessel in mid-October. If you can picture the television show “DEADLIEST CATCH” – that is the type of vessel he will sail on. On a fisheries trip Justin will collect data on the species of fish caught, their sex, weight, length and other information NOAA needs, to understand the health of ocean ecosystems.  Justin grew up enjoying the outdoors and always knew a desk job was not for him.  He has a degree in Wildlife and Fisheries Science and has been lucky enough to find a job that gets him outdoors and is ever changing. 

A yellow wagtail has been seen from the ship in the past few days.  I wonder what this bird is doing so far out to sea - ideas?
A yellow wagtail has been seen from the ship in the past few days. I wonder what this bird is doing so far out to sea – ideas?

FOR MY STUDENTS: How are your observation skills?  Would a job at sea be a good match for you? 

I asked Justin what he has seen from the Healy. Our “trip list” follows. The farther away from land we get, the fewer species of birds we see. Most of these bird species were spotted before we hit the heavy ice.

The Marine Mammal Observer has seen these birds since we departed Barrow, AK: Pacific loon, Northern fulmar, red phalarope, long-tailed jaeger, Ross’ gull, Arctic tern, spectacled eider, pelagic cormorant, parasitic jaeger, glaucous gull, black-legged kittiwake, yellow wagtail.

The Marine Mammal Observer has seen these mammals since we departed Barrow, AK: bearded seal, ringed seal, Arctic fox, polar bear.

Personal Log

Many people have asked about the living spaces inside this ship.  It is an amazing vessel when you think about all that happens here.  The Healy is truly a floating city with 120 people on board.  Any function that your town does – this ship needs to do.  A city needs to clean water, sewage treatment, trash pick up, recycling, electrical power, food, shelter, and recreation.  All of these are provided for on the Healy. I have attached a few pictures of life on the Healy below.

Our bunk beds have curtains to keep out the 24-We each have our own desk and filing cabinet and hour sun. Note the stuffed polar bear. This was most important a porthole window! Notice the color a gift from Mrs. Campbell and Mrs. Taylor. outside – we are getting a few hours of twilight in the early morning hours.
Our bunk beds have curtains to keep out the 24-We each have our own desk and filing cabinet and hour sun. Note the stuffed polar bear. This was most important a porthole window! Notice the color a gift from Mrs. Campbell and Mrs. Taylor. outside – we are getting a few hours of twilight in the early morning hours.
This is the place where the science party relaxes,  plays cards, and watches movies.
This is the place where the science party relaxes, plays cards, and watches movies.
We each have our own desk and filing cabinet and most important a porthole window! Notice the color outside – we are getting a few hours of twilight in the early morning hours.
We each have our own desk and filing cabinet and most important a porthole window! Notice the color outside – we are getting a few hours of twilight in the early morning hours.
 The main library has computers for the crew to email friends and family and plenty of reading material.
The main library has computers for the crew to email friends and family and plenty of reading material.