Frank Hubacz: The Final Leg, May 10, 2013

NOAA Teacher at Sea
Frank Hubacz
Aboard NOAA ship Oscar Dyson
April 29 – May 11, 2013

 

Mission: Pacific Marine Environmental Laboratory Mooring Deployment and Recovery

Geographical Area of Cruise: Gulf of Alaska and the Bering Sea

Date: May 10, 2013

Weather Data from the Bridge (0200):

W wind 10 kt. Chance of light snow.

Air Temperature 2.6C

Relative Humidity 82%

Barometer 1025.5 mb

Surface Water Temperature 4.30 C

Surface Water Salinity 32.91 PSU

Seas up to 3 ft

Science and Technology Log

As we continue to complete CTD sampling on our last full day at sea, the major change from previous days is that the depth of the Bering Sea has increased dramatically. For the past couple of days we have been riding along the 70 m depth line.  We are now casting down to 1,500 m with the ocean bottom currently at 2,298 m.

My previous blogs have focused on the instrumentation and sampling methods used on the cruise.  I would now like to introduce you to the members of the science team on board the Oscar Dyson for this cruise.

William (Bill) Floering, Chief Scientist

William (Bill) Floering, Chief Scientist, NOAA-PMEL

William (Bill) Floering, Chief Scientist, NOAA-PMEL

Education:  BS Biology, University of Washington; BS Wildlife Biology, Oregon State University.

Position/Affiliation: Chief Scientist on Cruise, Field Operations Specialist/ NOAA/PMEL/OERD (30+yrs)

Duties on cruise: Oversee the entire cruise operations, objectives, staffing, and mooring deployment.  He is constantly “on duty” and serves as liaison between ship personnel and the science team.

Data:  Data collected will be used to better understand the physical and biological properties of the ocean water in the Gulf of Alaska and the Bering Sea.  PMEL makes this data readily accessible to scientist of many disciplines to use.

Alphabetically Listed

Carol DeWitt

Carol DeWitt, PMEL
Carol DeWitt, NOAA/PMEL/FOCI

Education:  BS Biological Oceanography, Florida Institute of Technology

Position/Affiliation: Field Operations Specialist/PMEL/FOCI (25+yrs)

Duties on cruise: Ensures that all of  FOCI’s instruments are prepped, shipped to the Oscar Dyson prior to departure, and in working order once the cruise begins.  Join in with all other team members in helping to complete onboard operations.

Data:  Data collected will be used to better understand the physical and biological properties of the ocean water in the Gulf of Alaska and the Bering Sea.  PMEL makes this data readily accessible to scientist of many disciplines to use.

Scott McKeever

Scott McKeever, NOAA-PMEL

Scott McKeever, NOAA-PMEL

Education:  BS Atmospheric Science, University of Washington

Position/Affiliation: Research Scientist, Physical Oceanography Technician (2+ yrs)/ NOAA/PMEL/OERD

Duties on cruise: Mooring deployment and recovery along with CTD water sampling.  Join in with all other team members in helping to complete onboard operations.

Data:  Data collected will be used to better understand and monitor the physical properties of the ocean water in the Gulf of Alaska and the Bering Sea.

Kathy Mier

Kathy Mier, NOAA-AFSC

Kathy Mier, NOAA-AFSC

Education:  MS Statistics, University of Louisiana, Lafayette

Position/Affiliation: Statistician (19+ yrs)/ NOAA/Alaska Fisheries Science Center (AFSC)

Duties on cruise: Complete CTD water sampling as well as oversee Bongo tows and preservation of tow samples.  Join in with all other team members in helping to complete onboard operations.

Data:  Some of the data collected by her group will be analyzed by scientist in Poland.  Kathy offers her statistical expertise to researchers reviewing collected data. Once data is analyzed it will be used to better understand and monitor the physical properties of the ocean water in the Gulf of Alaska and the Bering Sea.

Dan Naber

Dan Naber

Dan Naber

Education:  BS Geology, University of Alaska, Fairbanks

Position/Affiliation: Research, Mooring Technician (5+ yrs)/ UAF Institute of Marine Science

Duties on cruise:  Prepare various monitoring instruments for deployment on moorings.  Water sampling for nutrients, dissolved inorganic carbon, and dissolved oxygen.  Join in with all other team members in helping to complete onboard operations.

Data:  Data collected will be used to better understand and monitor the physical properties, including monitoring ocean acidification, of the ocean water in the Gulf of Alaska and the Bering Sea. 

Peter Proctor  

Peter Proctor, Ph.D., University of Washington

Peter Proctor, Ph.D., University of Washington

Education:  Ph.D., Case Western Reserve University

Position/Affiliation: Research Scientist/ Joint Institute for the Study of the Atmosphere and Ocean (JISAO), University of Washington (11+ yrs)

Duties on cruise: Oversee the operation and data collection of CTD casts.  Additionally, collect nutrient, salinity, DO samples from CTD drops. Join in with all other team members in helping to complete onboard operations.

Data:  Data collected will be used to better understand and monitor the physical properties of the ocean water in the Gulf of Alaska and the Bering Sea.  Data will also be used collaboratively in fisheries assessment within this geographical region.

Matthew Wilson

Matthew Wilson, NOAA-AFSC

Matthew Wilson, NOAA-AFSC

Education:  MS Fisheries, Oregon State University

Position/Affiliation: Fisheries Research Biologist (25+ yrs)/ NOAA/Alaska Fisheries Science Center (AFSC)

Duties on cruise:  Oversee Bongo tows and preservation of tow samples as well as ensure proper collection of chlorophyll samples.  Join in with all other team members in helping to complete onboard operations.

Data:  Chlorophyll samples will be used to standardize instrumentation used on board. Once data is analyzed it will be used to better understand and monitor the physical properties of the ocean water in the Gulf of Alaska and the Bering Sea. Matt’s research in helping to better understand Pollock fisheries will soon be published in the Journal of Marine Science.

If you are interested in pursuing a career in “marine science”, broadly defined, the collective advice from the science team is as follows: let your passion for studying the Ocean be your drive; experience this field firsthand through internships and volunteer opportunities aboard cruises; diversify your studies so that you have a broad background in several disciplines; through all of these experiences make certain that you truly do have a desire to pursue this field of science.

I would like to take this opportunity to thank Peter Proctor for his time, expertise, and willingness to share his knowledge of the ocean with me.  I also appreciated his patience in teaching me the techniques of CTD nutrient sampling, my “job” on the cruise. His humor and wit helped to make the downtime on our cruise enjoyable and always a learning experience.

Finally, I continue to be impressed with the leadership that Bill exhibits on board ship. His efforts ensured that valid “science” research was conducted during the cruise.  The data collected, once analyzed, will add to our knowledge base of the ocean waters of the Gulf of Alaska and the Bering Sea.  I would like to personally thank Bill for allowing me to have the opportunity to actively work alongside the science research team on this cruise.

Personal Log

In my “science and technology” log above I introduced you to the science crew.  In this section, I would like to introduce you to someone who works very hard to keep “everybody happy” on board ship.  Frank Ford is Chief Steward aboard the Oscar Dyson for this cruise. 

Frank Ford, Chief Steward

Frank Ford, Chief Steward

Frank is an experienced chef providing us with nutritional, well balanced, food 24 hours per day.  On a ship, meals are served at specific times but everyone works different shifts and therefore is not always able to be at a serving.  Therefore, Frank needs to ensure that all of our dietary needs are met regardless of our personal work schedule. As I have indicated in previous blogs, I never went hungry. There is always a wide range of fruit, yogurt, snacks, leftovers, etc. available.  Frank also closely monitors the temperament of the crew as we eat our meals in the galley, via his open kitchen, and is always there to chat with us.  Thanks Frank for your multiple and varied menu offerings! I know that my students would be very pleased to have Frank Ford as our head chef on campus.

Prepping the Prime Rib!

Prepping the Prime Rib!

Seasoning with a "special blend"

Seasoning with a “special blend”.  Notice the open kitchen!

My favorite meal aboard ship

My favorite meal aboard ship!

On this cruise I have had the opportunity to not only work with the science team but to also meet and work with members of the NOAA Officers Corp as well as the NOAA deck crew.  I have discovered that they come from a variety of backgrounds as well as from all over the United States. However, they all have in common a love for being on the open sea.  I am impressed with their candor, openness, and their professionalism.  I have made many new friends! Thank you for the opportunity to sail on your ship!

Since leaving Seward, Alaska on April 29th, we have steamed over 2,000 nautical miles (2,300 miles) and traversed from the Gulf of Alaska (North Pacific) into the Bering Sea.   This journey has truly been a rewarding and phenomenal educational opportunity for me.  I am truly honored to have had the opportunity to be a NOAA Teacher at Sea “student” and truly hope that other teachers, from across the United States, will continue to have this opportunity.  Recognizing and understanding the role that the “Ocean” plays in the overall health of our Planet is critical.  It is imperative that we provide our students with a robust education along with an understanding and appreciation for the discipline of Ocean science research. 

Did You Know?

Seniors, not to worry , I will be back on campus to attend your graduation!

Bill cleaning recovered mooring instruments

Bill still working!

Farewell Alaska!

Farewell Alaska!

 

Frank Hubacz: Introduction, Sailing Aboard the Oscar Dyson, April 29 – May 11, 2013

NOAA Teacher at Sea
Frank Hubacz
Aboard NOAA ship Oscar Dyson
April 29 – May 10, 2013

Mission: Pacific Marine Environmental Laboratory Mooring Deployment and Recovery
Geographical Area of Cruise:  Gulf of Alaska and the Bering Sea
Date:  April 17, 2013

Teacher at Sea Frank Hubacz

Teacher at Sea Frank Hubacz

Greetings!  My name is Frank Hubacz, and I teach General Chemistry and Environmental Chemistry at Franklin Pierce University where we are celebrating our 50th Anniversary.  Our main campus is located in Rindge, New Hampshire near the base of Mount Monadnock; this 3,165-ft. mountain summit is the most frequently climbed mountain in North America.  At Franklin Pierce, we encourage our student body of approximately 1400 students to embrace their education and to achieve academic success through the integration of liberal arts and our various professional programs.

I first started teaching biology in 1976; however my interests soon migrated into the study and teaching of chemistry.  I have been teaching  general chemistry at Franklin Pierce University since 1992.  While attending the 2006 National Science Teachers Association (NSTA) Annual Convention in Anaheim, CA I had the good fortune to attend the headline presentation given by Jean-Michele Cousteau.  His presentation, entitled “Responsible Living…Because Everything is Connected”, considered the vital relationship between the health of our planet, as monitored by way of the health of the Ocean, and our actions as residents of the Earth.  Cousteau offered that, “When we think about our actions as teachers, students, tourists, parents, builders, farmers or name a profession, we must recognize all of our actions have environmental consequences…Because our health depends on the health of the planet, being aware of these connections can help us live responsibly” (NSTA Convention Program Itinerary, 2006).  During his appearance, Cousteau impressed upon his audience the importance of understanding how the Ocean can help us to monitor the health of our Earth.  Please note that I purposely use the term “Ocean” as opposed to “oceans” to emphasize the interconnectedness of this large body of water that covers over 70% of the Earth’s surface.  I then began to reflect upon the fact that I did very little relative to incorporating ocean systems in our study of general chemistry.  At this same conference, I was also introduced to the NOAA Teacher at Sea Program (TAS) and decided to apply during my next sabbatical leave in order to experience ongoing Ocean research with the hope of bringing this experience back into the classroom.

My goal as a TAS participant is to use this experience to help me explicitly incorporate Ocean related phenomena into the study of general chemistry topics such as density, conductivity, gas behavior, acid/base chemistry, solubility equilibrium, and kinetics.  Additionally, I hope to develop new laboratory exercises that are Ocean related as well as to help students to realize the wealth of live NOAA data available to help them better understand the complexity of the Ocean.  As a result I hope that students will gain a better understanding of “ocean chemistry” as well as to develop an appreciation of the interconnectedness among their actions, the health of our planet, and the health of the Ocean.  Additionally, by actively participating in an ongoing ocean research project, I will develop a deeper understanding of the various career and research opportunities available for my students to pursue.  I hope to convey to them the excitement of discovery as it relates to the Ocean thereby causing them to give serious consideration to following this line of study upon graduation.

A little bit about me…

I live with my wife of 38 years, Joan, in a rural community in central Massachusetts.  Our daughter Jessica lives in Vermont and has provided us with three beautiful grandchildren.  She currently leads their family’s home-school program and is expecting a new baby in June.

Jess, Josh, and family sledding with Grampie

Jess, Josh, and family sledding with Grampie

Our son Daniel is currently pursuing his Ph.D. program in Geology at the University of Delaware having completed his Master’s degree at this same institution.  His studies focus on fluvial geomorphology.

Maggie, Dan, and Joan

Maggie, Dan, and Joan

Kayaking at Race Point in Provincetown

Kayaking at Race Point in Provincetown

Whenever possible my wife and I “escape to the Cape” to enjoy all that Outer Cape Cod has to offer.  Our favorite activities include kayaking, freshwater, as well as saltwater fishing, dune riding, shell fishing, collecting mushrooms, collecting sea glass on long walks, and the peaceful views of the ocean beaches.

Frank and Joan enjoying the beach!

Joan and I enjoying the beach!

We also have a marine reef aquarium in our home, maintained steadfastly by my wife.  The aquarium currently contains many varieties of soft corals that we are learning to propagate along with several types of reef “critters”.

During the winter months I enjoy downhill skiing and am a night-league NASTAR (NAtional STAndard Race) racer on a team known as the Sled Dogs.  Our team’s motto, “strive for mediocrity” ensures that we focus on having fun and enjoying a winter’s evening of skiing at our local mountain.

In summary, I am eagerly looking forward to participating in the Teacher at Sea Program aboard the Oscar Dyson and all that this adventure has to offer!  I will use this experience to help my students to better understand “ocean chemistry” as well as to develop an appreciation of the interconnectedness among their actions, the health of our planet, and the health of the Ocean.

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.

Staci DeSchryver: Don’t Hate, Just Calibrate! August 9, 2011

NOAA Teacher at Sea
Staci DeSchryver

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

Mission: Pollock Survey
Geographical Area of Cruise: Gulf of Alaska
Location: Barnabas Strait  57 deg 22.630 N, 152 deg 24.910W 
Heading: 67.8 deg
Date: August 9, 2011

Weather Data From the Bridge
Partly Cloudy Skies
Temp: 13.5 deg
Dewpoint:  6 deg
Barometric Pressure: 1020 mb, falling, then steady
Wind:  240 deg at 12kts
Seas:  Calm
stn model 08.11

Science and Technology Log

The start of my first official shift onboard the Oscar Dyson was an interesting one!  We had lost some time (11 days) to some complications, so our cruise goals shifted a bit from the original plan.  We had to focus on the most important aspects of the mission, and sacrifice carefully, as it wasn’t plausible to complete the entire mission in the time allotted.  One of the major steps for completing the season was to do what is known as a calibration.  In order to save time, we did the calibration on my first night out on the job!

Calibrations are typically done during the daytime because the fish are curious little beasts.  During the day, they move lower in the water column, and therefore do not interfere with the calibration of the system, mainly because they are so far away they are oblivious to it.  At night, however, they party at a shallower depth, and sometimes their acoustic signatures can mar the data collected during a calibration.  It is critical to the scientists that they calibrate the acoustic system accurately, and if there is a school of fish swarming the calibration tools, well, it’s a big ‘ole mess.  Given that we are on a shortened time schedule, it made practical sense to conduct the calibration overnight.

krill

Marshmallow has been very helpful on the trip. Here he is counting krill. I don't have the heart to inform him that these krill have already been counted.

Why do we calibrate the acoustic transducer?  Think of it like this.  Have you ever baked cookies before and followed the directions to the letter, only to have them come out of the oven like crispy critters or balls of goo?  Or, let’s say, you have a favorite recipe you use all the time, and you gave the recipe to a friend who makes the same cookies the same way, yet complains that they are overcooked?  Well, one of the reasons that the recipe may have not turned out was because either your oven, or your friend’s oven was not properly calibrated.  Let’s say, for example, the recipe calls to bake the cookies at 350 degrees for 15 minutes.

If you turn the dial to 350 degrees, it is reasonable to expect that the oven is, in fact, 350 degrees.  But there is an equal possibility that the oven is actually only 325, or maybe even 400 degrees.  How would you double check to see if your instrument is off its mark?  One solution is to heat the oven to 350, and use a meat or candy thermometer that you know has an accurate readout and then put the thermometer in the oven.  If the candy thermometer reads out at 350, you can be certain that your oven really is 350 when you turn it on.  If the candy thermometer reads out at 375, then you can be certain there’s an error in the readout of your instrument.  Calibration corrects for those errors.

downrigger

Here you see Cat and I showing off the downrigger - the piece of equipment that holds the calibration spheres under the ship.

Calibration on this survey is important because scientists use information from the acoustic transducer to determine the types and abundance of organisms in the water column.  If the instrument they use to make these predictions is off in any way, then all of the data they collect could be determined to be insufficient or unreliable.  Calibration also ensures that acoustic measurements (and survey results) are comparable between different cruises, locations, and times.

Calibration is done much in the same way as an oven is calibrated.     We take an object that has a known and reliable return rate on the acoustic transducer, and hang it below the ship.  Then, the scientists will “ping” acoustic soundings off of the object and see how well the return matches up with the known return rate.  If it’s off, then they can “tune” the transducers, much like a guitar is tuned.

downriggers ii

Here, the chief scientist, Chris Wilson, double checks our superior downrigging work!

It is only necessary to calibrate the transducers twice per survey – once at the beginning of the survey (one was done in June) and one at the end of the survey (which was now).  When the transducer is calibrating, the ship must be as close to stationary as possible.  This is why the lead scientist chose to do the calibration at night – we can’t calibrate and conduct assessment surveys at the same time.  Therefore, it’s a one-pony show when the transducer is calibrating.  Almost all other scientific field work ceases while the calibration is completed.

There are two materials used for calibration for this particular transducer on the Oscar Dyson.  The first is Tungsten Carbide, and the second is pure Copper.  These small, spherical objects are quite cleverly hung below the ship off of three downriggers attached to the port and starboard rails.  In order to hang the spheres, the strings on either side of the ship must connect.  In a sense, we ask the Dyson to “jump rope” to get the calibration sphere underneath the ship in the correct position.

Calibration takes about six to eight hours to complete.  I got to help with setting the downriggers up, changing out the calibration spheres, and breaking down the equipment.  As it turns out, the transducer only needed minor adjustments this time, which is pretty typical for the ship.  However, it’s important to double check so that if there is a problem, it can be detected early and corrected.

Personal Log

Today, the chief engineer of the ship, Jeff, gave us a tour of the engine room.  Holy cow, was that impressive!  I don’t know what I was thinking when I  thought that the guts of this beast were contained in one small room.  They most decidedly are not.  There are two whole decks below the lowest level I know of – and they are filled with all kinds of interesting equipment.  We got to see all of the engines (there are 4 diesel generators), where the water is purified for consumption, and all of the internal components of the winch system that lowers and raises our fishing nets.  As if that weren’t enough, we popped open a floor hatch, climbed down the ladder two flights, and got to stand right on the “skin” of the boat.  Translation:  The only thing separating my feet and the big blue sea was a thin little piece of metal.  It was so cool.  The ship is designed to be “acoustically silent” – like a stealth fighter, except they don’t call it stealth and we aren’t fighting enemies – we are hunting fish.  Because of this, many of the larger pieces of equipment are hoisted up on platforms that silence their working parts.  The ship has diesel-electric propulsion.

engine rm

Here is just ONE of the four massive engines on the ship!

This means that there are four diesel generators that make electricity,  which then gets split into two different forms  – one type is for propulsion, and the other is for our lights and other conveniences.  It sounds really complicated, and much of what the engineers do on board is quite complicated, but everything onboard is smartly labeled to help the engineers  get the job done.  I also learned today what the funny numbers on all of the passage doors mean.  See the caption for a description.

door signs

Here is one of the door signs on the ship, which act like a "you are here" sign on a map. The first number tells us what floor we are on. The second number tells us what area of the ship we are in. The third number tells us whether we are port, starboard, or in the center of the ship.

One thing that Cat and I were discussing this morning while searching through binoculars in Alitak Bay for interesting woodland creatures was that we can go pretty much wherever we want to go on this ship.  Everyone who works and lives here is so friendly and welcoming.  They answer any of our questions (even the silly ones) and they all have such cool life stories.  What’s better is that everyone is willing to share what they’ve learned, experiences they’ve had, and accomplishments they’ve achieved to make it here.  I am aboard a utopian city bursting with genuine people who love what they do.  Now, please understand that it’s not that I ever expected the opposite for even a single second.  The science and technology is definitely neat, but the people who live and work here are what is making this trip a once-in-a-lifetime experience.

Do you know….

Your Ship Superstitions?

1.  Bananas on a boat are considered bad luck.

2.  Black luggage for sailors is considered bad luck.

3.  One should never whistle – especially on the bridge or in the wheelhouse – you may whistle up a storm.

4.  To see a black cat before boarding is good luck.

5.  Dolphins swimming along the ship are good luck.

6.  Never sail on Friday – it’s unlucky.

7.  Never sail on the first Monday in April – also unlucky.

8.  Never say the word “Drown” on a ship, as it encourages the act.

9.  Sailors should avoid flat-footed people – they are bad luck.

10.  Never step onboard a ship with your left foot first.

Staci DeSchryver: Fossilotimus Abundicus! August 6th, 2011

NOAA Teacher at Sea
Staci DeSchryver

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

Mission: Pollock Survey
Geographical Area of Cruise: Gulf of Alaska, Kalsin Bay
Heading: 213.0 (Stationary)
Date: August 6, 2011,  11:24 pm

Weather Data From the Bridge: click to view station model
Dry Bulb Temp:  10.8C
Wet Bulb temp:  9.9C
Skies: Partly Cloudy, Stratocumulus
Pressure:  1013.3mb, falling then steady
Dewpoint:  10C

Science and Technology Log

As part of our stay on shore, we took some time to travel out to a place called Fossil Beach.  Fossil Beach is located on the south-eastern side of Kodiak Island, on Chiniak Bay.  It is a popular attraction on Kodiak because it is near the Kodiak launch complex (a defense missile base !) and it is a popular surf beach.  I, however, find it incredible for a completely separate reason:  an utter abundance of fossils!

There isn’t much background information to be found on Fossil Beach.  The greatest extent one might find on the internet is “Drive southeast on the only road out of Kodiak.  Find fossils.”  To the layperson going out fossil hunting, that should be enough information.  But for me, however…I wanted to know much more about the conditions of formation, the types of fossils found there, and the age of the rocks in which I was digging.  As it turns out, if I wanted to dig up information on Fossil Beach, I would have to be as clever as I was the day I discovered so many of our extinct marine critter shells.   This experience turned into a bit of a scientific research project for me, as I formed hypotheses, tested my predictions, and revised my original ideas based on new findings.  This, kids, is science.

Walking around the outcrop gave some insights into the environment in which this rock strata formed.  The fossils were definitely nested in dark, muddy shale.  I noticed lots of mollusks, particularly clamshells, at first glance.  Shells were deposited in big, thick, chunks and layers.  What I noticed initially is that they weren’t really fossils.  A fossil, by definition, has been mineralized to a certain extent.   These weren’t.  However, some scientists conclude that the actual fossilization process is not necessary to call a particular dead animal a fossil – the only requirement is an extended period of time locked up in a rock.

fossil beach

Here is just one example of the plethora of fossils found at fossil beach! it's hard to walk away and not try to find the story of these guys.

What are the criteria for fossil formation?  A dead critter needs rapid burial and possession of hard parts.  An anoxic environment helps, as well.  Most soft-bodied critters do not survive the fossilization process, as their flesh will decay so rapidly that there isn’t enough time to fossilize.  It is not unheard of, however, to find soft parts fossilized.  For example, a fly or mosquito trapped in amber is considered to be a fossil – its entire body intact in the clear, honey-colored stone.

My first question, of course, was “what was the environment of formation for this particular set of fossils?”  Meaning, what type of environment did these critters live in before they croaked?  We can narrow it down to two distinct, but broadly categorized areas:  land? Or sea?   Well, let’s think for a moment about the standard conditions for fossil formation and use that to define the environment of formation.  Criteria 1:  Rapid burial.  Criteria 2:  Possession of hard parts.  Criteria 3:  Anoxic environment.  Consider for a moment rapid burial.  In what places may we find rapid burial?  Volcanic eruptions?  Maybe.   Land or mudslide?  Also a viable solution.  The next step is to rule out (or in) these two options.  In a volcanic eruption, the fossils would most certainly be nested in a layer of ash.  In a mudslide or a landslide, these critters would be nested in coarse-grained rock like sandstone. In our mystery case, we have fossils buried in a shale – which is a fine-grained, silty rock associated with slow-moving or stagnant water.  Neither of these options work.

Let’s try criteria 2 – possession of hard parts.  These shells are mainly mollusk – in particular clam shells.  Where do clams live?  The water.  It wouldn’t make sense for a clam to be fossilized in the middle of the desert, now would it?  In addition, the presence of shale does not necessarily indicate rapid burial, but it does indicate that if it were at the bottom of the ocean, it would be undisturbed for many years as it was buried.

Criteria 3 – an anoxic environment.  In this case, if a clam dies at the bottom of the ocean, it may be considered an anoxic environment, but not for certain.

Hypothesis:  confirmed.  These critters once roamed our seas, based on Criteria 2.

concretions

Here is an example of calcareous concretions - something I saw at fossil beach, and later used the article to confirm that this formation was indeed the Narrow Cape Formation. The Narrow Cape Formation is characterized partly by this conspicuous row of calcareous concretions. Two points for cross-referencing evidence to a published document! Woot! Minus two point for not putting something next to it for scaling purposes - the concretion is about the size of a soccer ball. Par for the course.

The next question to ask was “how long ago did the fossilization party take place?”  This one is a little more difficult to answer, but with some stealthy sleuthing and some assistance from my fellow Teacher at Sea, Cat, we came to a reasonable conclusion regarding the time frame.

At first glance on a large geologic map of Alaska, Fossil Beach is described as a Paleozoic Era beach.  However, this map was so broad and basic that if we were to “zoom” in on it right down to fossil beach, our perceptions would change about the age and conditions of formation.

I thought I saw large ammonite fossils at the beach, which would have confirmed my suspicions about a Paleozoic beach.  What didn’t fit, however, was that the mollusk fossils were not “fossilized” – and a Paleozoic/Mesozoic fossil like an ammonite would make the rock layers any age between 542 and 206 million years old.  Now, it’s not completely unheard of to find fossil in your midst that has retained all of its qualities and still be extremely old – there are a few fossils out there that are considered fossils, but haven’t “fossilized” in the traditional sense.  But 206 million years?  One would suspect that is plenty of time for a fossil to fossilize.  It didn’t jive.  This was my first clue that maybe this beach was much younger than the broad geologic map suggested.

The broad geologic map is a bit like a mosaic.  When viewed from far away, all a person may see is the color “blue”.  Up close, however, the intricate pieces that make up the mosaic are individually selected for their different shades and textures.  With the broad geologic map of Alaska, I discovered it wasn’t detailed enough to give me the information I needed.  At a distance, there is one big picture – the colors on the map key indicate that the rock formations that make up Kodiak are predominantly Paleozoic Sedimentary rocks.  This is a bit like calling a brand new pair of Louis Vuitton peep toe black patent leather heels “shoes.”  It just doesn’t do it justice.

After looking further, Cat found a great article published online that discusses the nature of the formation of the beach. (I will cite it at the end of the post).  Most of the information following comes from that particular document.

microfossils

The article also cites an abundance of microfossils. These could be an example of microfossils. They could also be nothing, but given the location, I'm pretty sure we have something, here.

The paper focuses on Sitkinak Island, an island just to the south of Kodiak, but it also mentions that the formation of rocks is one and the same.  The Kodiak formation is just a bit younger.  As it turns out, the rocks are deposited as part of the Narrow Cape Formation, a late Oligocene/early Miocene formation.  This translates into somewhere on the order of 10 million years old or so.  In particular, the paper cites the Juanian stage, which is the time frame that encompasses the last portion of the Oligocene and the first portion of the Miocene.

Even more interesting is that this paper reveals the type of ocean these particular fossils came from.  They originated from the outer edge of the neritic zone to the continental shelf.  If you recall, the neritic zone is the point at which the lowest of the low tide is all the way out to a depth of 200 meters.  Furthermore, the study reveals that the water was a cool-temperate marine climate, which means that the warmest water at the surface was about 10oC for approximately 3-4 months out of the year.

It was great to uncover the mysteries of fossil beach.  The only mystery remains is, what about the Ammonite I thought I found?  At this time, I absolutely cannot reconcile what happened there.  There are a couple of strong leads in terms of solutions to this question:  first, it may not be an ammonite at all.  Second, the broad geologic map does indicate Paleozoic sedimentary rock, which would be a perfect candidate for a critter like an ammonite.  Maybe the ammonites were from a completely different rock formation?

ammonite?

This is the mysterious ammonite (?) fossil. I'm not sure anymore if this is what this large critter is. I hope someone out there can help shed some light on this mysterious former beast.

Until I get back to land and get my hands on a copy of the Roadside Geology of Alaska (I looked everywhere in Kodiak to no avail!) this will have to suffice for my level of satisfaction with respect to fossil beach.  Check back to this blog often to see if my predictions were right!

Personal Log

Well, wouldn’t ya know it?  A tsunami line is painted right on base here at the Coast Guard!  There is no reason to travel or hike a ridiculous  amount when you can just stay right here and visit.  (However, for more information on ridiculous Alaskan hikes, please visit my other blog at www.mrsdisonaboat.blogspot.com – you’ll love it.)  We did see the line on the first day, I just haven’t had time to blog about it again, plus it took a considerable amount of time for me to finally get up the nerve to ask someone to stop a car so I could snag a picture!

It didn’t look that imposing at first.   At first glance, it looked like it was only about 3 or 4 feet from the ground.  I thought to myself, “Gee, this doesn’t look so bad…” until I walked up to the line.  It was bigger than I was!  Holy cow!  Even if I reached my arms all the way above my head, I couldn’t touch the lower portion of the line.  The picture is extremely deceptive, that’s for sure!  I thought about what it would be like to be a person who hears the siren warning of the impending emergency, and what it would be like to make for higher ground, hoping that however high you climbed would be enough to save you from the wicked influx of water.

Eesh…  I am thankful that so few lost their lives, but the sight of that line is a bit imposing.  Also (and not at the expense of the destruction, of course) wickedly, beastly cool.

Wow! The water level for this particular tsunami is enormous!

In other news, we have successfully thrown off the bow lines and set sail!  We were supposed to head out yesterday, but then something went wrong with the water system, causing a delay, and then one of the officers got sick and had to go home.  Luckily, we had a replacement officer standing by to take over.  We are so sorry that she came down ill, but so grateful that we had someone to take over!  As we left Women’s Bay this morning, I saw many otters playing about in the bull kelp.  Those little critters are too dang cute for words!  They poked their heads up for a few moments before doing a graceful backflip back in to the water.  But the most impressive sight of all took place about thirty minutes after we set sail.  Up on the flying bridge, we saw the telltale blow of a whale.  This was followed by two or three playful fluke slaps on the surface of the water.

breaching whale

Here, you can see the breaching whale....wait...Marshmallow! Get out of the way! Just kidding, I didn't get a picture of the whale breach - that happens so quickly! I have a lot of respect for people who can get a snapshot of such a cool experience!

And then, because he (or she) was as excited as we were to be sailing, the whale performed for us the most impressive breach!  You, go, sister!  We like the ocean, too!  In my fumbling wonder, I of course, took 9 or so pictures of the breaching whale using stop-motion photography for you to see below.  Too bad Marshmallow is in the way.

I am so happy and thankful to be out on the sea.  Now I see why people love it so much.  It has an interesting dichotomy.  On one hand, I feel so small – a large, blue, fog-covered expanse stretches out before me, nothing in sight for miles and miles.  On the other hand, I feel enormous.  As we left the bay, we traveled past the peninsula we had walked on so many times before.  Along the shoreline was an oil spill containment kit stored in a freight-train style container.  It looked so tiny from where we stood on the flying bridge.  It was as if we swapped positions – now we were the behemoths, and the spill kit was nothing more than a busted up shoreside lego.

I’m fascinated by the scales of this magnificent place – more so about how I fit in to them.  Everywhere I turn, the sizes of things – animals, projects, decks, horizons, anti-seasick meds, stories, waves, meals, ocean expanses, rock outcrops – everything, everything is large, even that which is the tiniest and seemingly insignificant.  Here is the place where small things commit powerful acts  – a tiny three-foot swell makes its presence known in more ways than one, and a small anti-seasick pill can keep me from worshipping at the feet of its effects.  A big ocean can throw around an enormous ship, and a humpback whale can effortlessly cut through it with its imposing  fins.  A project seemingly small (at least in this context of one ship, one crew, one survey leg, and one set of scientists) can spread awareness about the health of our fisheries to a something the size of a nation.  To top it off, we are completing it along the coast of our largest state – one that blends quietly in with our neighbors to the north, but not forgotten as a beautiful and expansive supplier of natural resources.  Everything small is large out here, and everything large is large.  For those who have spent too long at the dock, today they are home.  For those who have never left a dock before, today we feel your freedom.  And we love it, too.

*Information on Sitinak Island/Fossil Beach was summarized from the following:

Allison, Richard C.  A late Oligocene or Earliest Miocene molluscan fauna from Sitinak Island, Alaska.  United States Department of the Interior, Washington; 1981.

Staci DeSchryver: A Major Ursus, August 3, 2011

NOAA Teacher at Sea
Staci DeSchryver

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

Mission: Pollock Survey
Geographical Area of Cruise: Gulf of Alaska
Location:  57.43287 N, 152.28867 W
Heading:  
241.2 (Stationary)
Date: August 3, 2011

Weather Data From the Bridge
Overall Weather:  Clouds and fog

Science and Technology Log

One of the most serious emergencies that can take place onboard a ship is a fire.  The NOAA Ship Oscar Dyson has many security measures in place in the event of a fire while underway.  During our time in port, the crew of the Dyson planned a ‘’Safety Stand Down” Day to review safety protocol for all types of emergencies, particularly what the crew should do in the event of such a serious issue.

Before we began discussing some of the features of fire-fighting and emergency equipment, we participated in a survival activity that will certainly be used for the first days of school in my AVID class.    The activity consisted of a list of 15 items that we had in a mock abandon-ship emergency situation.  We were supposed to rank order the items of greatest to least importance for survival.  Some items were quite obviously important (water, food, and shelter, for example) and some were quite important but at first glance appeared to be about as useful as chewing gum.  There was a third group of items that appeared to be important, but in reality, ended up being about as valuable as a lawn ornament.  We rank ordered the items first on our own, and then formed groups of four or five to discuss our lists and come up with a group consensus of what is valuable.  As I predicted, repurposing items was the name of the game and those seemingly useless chewing gum items realized their full potential for being used for some other function.  Overall, I won!  I will be accepting applications for spaces in my life raft in the event of an emergency.  Preference will be given to those who can demonstrate strong paddling capabilities and have a deep aptitude for celebrity impersonations for entertainment purposes while on the raft.  Although all candidates will be judged carefully, those who write detailed, yet succinct and poignant essays will be given highest consideration due to limited on-raft seating.

After we finished the safety exercise, we were given the opportunity to take a look at the fire-fighting gear.  Think about this:  what happens when there is a fire at home?  It is usually detected by a smoke alarm, then, if there is time, the type of fire is determined.  Did it start with grease in the kitchen?  Or is it coming from an unknown source, maybe like an electrical fire?  The type of fire will determine what can and cannot be used to put it out.   If the fire can’t be put out quickly, the next step is to…call…the…fire…department.  Now, think about this:  What would happen on a ship in the event of a fire?  Well, many people are typically on watch to ensure that fires don’t start to begin with.  But fires can start on board in all of the same ways they can start at home.  So, in preparation for this, the ship must be equipped not just for fire, but for all kinds of fire.  If the fire can’t be put out quickly, the next step is to…call…the…fire…department…but wait!  That really can’t be done.  Who, then, do we call?  (Not the Ghostbusters, but good try.)  The crew doubles as the fire department.   In fact, any person who is on the ship is a member of the fire-fighting team to a certain extent.  My job is to be accounted for and stay the heck out of the way so the pros can do their job.

All of the crewmen are trained in firefighting procedures.  There are two fire lockers, one fore and one aft of the ship.  Inside the fire locker is a treasure trove of nozzles, hoses, and fire axes.  They are ready for anything on the ship because they have equipped themselves with a variety of means with which to fight different kinds of fires.

fire gear

Here, two members of the Oscar Dyson practice changing out air supply tanks.

What I found both interesting and important is that all of the hose lengths must be able to reach any connection on the ship so that all parts of the ship are covered in the event of a fire.  This can easily be explained if you think about a poorly designed sprinkler system.  If your sprinklers don’t cover all areas of the yard, you end up with conspicuous brown patches in the grass where the water doesn’t reach.  However, if the sprinkler system is set up correctly, no brown patches exist.  The Oscar Dyson requires that all of the hoses are long enough so that there are no “brown areas” on the ship.  If appropriate and necessary, the hoses will pull seawater out directly from the ocean to fight a fire in favor of the purified water onboard.  Usually, they prefer to use carbon dioxide to fight the fire.  It’s relatively benign in terms of dangerous reactions that could potentially take place.  For example, if there was a grease fire onboard, it wouldn’t make much sense to put water on it, but Carbon Dioxide would be a great option.

Next, we were given a demonstration of all of the nifty features of the firefighting gear. Ensign David Rodziewicz, the head safety officer, gave pointers on how to effectively put fire-fighting gear on.  The goal is to be able to get in and out of fire gear in less than two minutes, with the ideal time being less than a minute.  ENS Rodziewicz indicated that the most important way to be successful with suiting up is to have the gear properly set up – if boots are tipped over and gloves are strewn all over the place, not much will be accomplished in the time frame allotted – and being able to fight a fire quickly, while critical in all areas, is imperative on a boat.  Where land-based fires are a tragic and sobering experience, there is often an escape.  One can leave and go to a wide parking lot or out to the street away from the flames.  On the ship, the only place to go if things really take a turn for the worse is the ocean.  This is why timing is so important.There are some neat features on the fire-fighting equipment.  The air supply tanks are equipped with a 45-minute supply of air.  Most fire fighters are not expected to stay in an active fire area for that long, but the supply is large enough just in case there is a problem.   There is no need to keep time while fighting fires.  A “heads-up” display is clearly visible in the fire mask, with green, yellow, and red indicator lights representing the percentage of air left in the tanks.  The batteries for the light displays are changed quarterly – an important thing to check off on a to-do list!  Of all of the things to remember to do on a ship, it seems to me like that would be an easy task to forget.  But, they never do.  Another interesting feature is the communications system.  Each fire-fighting mask has a built-in communications system, so there is no need to take a radio in to an area with flames.  It’s almost like having a fire-fighting Bluetooth.  Each coat is also equipped with a flashlight and an emergency nylon strap in case of an emergency.  The neatest feature to me was the emergency bypass for the oxygen tanks.  If a crew member runs out of air, he or she can “latch” on to another person’s tank by ENS Rodziewicz utilizing a connector hose from the back of the rescuing party’s tank.  This will give approximately a ten minute air supply, although  points out that if one finds    himself or herself in that kind of a situation, he or she should not be in a fire zone for an additional ten minutes.  The emergency air supply is to safely remove a crew member only – not for fighting fires.One of the most useful ways to fight fire on a ship is to simply cordon off the area and then let the fire run its course in the offending room.  On the ship, there are many fire-retardant walls built into the bulkhead.  At that point, the fire fighters will utilize a tactic known as “boundary cooling.”  When you shut off a single room in the ship, the above and below decks can still conduct heat.  Therefore, the crew will spray a layer of ocean water in the rooms directly above and below the target area to ensure that the fire does not spread above or below floors.  Water has a high specific heat, so it acts as an excellent energy absorber.   This tactic is called boundary cooling, and is used often used in fire-fighting on a ship.Afterward, we watched the crew practice putting on, activating, and utilizing their fire-fighting equipment.  Each person who is responsible for fire-fighting has a partner who assists him or her in getting suited up, changing out air supply tanks, and assisting in other duties as necessary.Here, Cat and I are pret-a-porte in our stylish life-saving devices. Will we go into the water? Check out my other blog to find out…

From there, the day got really exciting, but if you want to read about it, you’ll have to visit my other blog at www.mrsdisonaboat.blogspot.com– a quick hint:  it involves a gumby suit and a big splash!  It’s not for the faint of heart.  Here’s a preview in the picture to the left.  Also, be sure to check out Cat’s blog:  www.blueworldadventures.blogspot.com to see what she’s been up to!  Cat does some incredible cartoons that are really funny and informative, so she is capturing this adventure in a completely different light.  We make a great team!

Personal Log

Will Cat and I make a big "splash?" Check out my other blog to find out!

Will Cat and I make a big "splash?" Check out my other blog to find out!

Yesterday, Cat and I went out to Fort Abercrombie.  Fort Abercrombie was an established World War II outpost that was designed to defend American soil in the event of an attack from the Axis Powers.  We found this really interesting interpretive trail called the Wildflower Trail.  Along the trail, there were informative signs about various wild flowers, their scientific name, their Inuit name, and uses for the roots, blossoms, stems, and leaves.  After encountering a sign, it was a sure bet that we would see the celebrity flower just a few clicks up the trail.  The trail carried us to a decrepit lookout post over the inlet that we could enter into and see what the defenders of our nation saw when they looked out on the glass blue waters of the bay.

The lookout

Here at Ft. Abercrombie, Marshmallow busied himself by taking post in the military lookout. He claims he was scanning the air for potential threats to our borders. Since there are not imminent threats to Alaska at this juncture, I maintain that he stole Cat's binoculars to look for Salmon.

Old buildings stood steadfast, fighting reclamation by the forest while many had a legacy left only by a sign pounded in to a rotting foundation.  Again, I found myself trying to tell the story of those who used to call this enchanted forest home.

We also (sound trumpets!) saw a Kodiak Brown Bear!  There is a difference between a Brown Bear, a Kodiak Bear, and Grizzly Bear – mainly demographic.  A Brown Bear (Ursus arctos) is called a brown bear because it is found in coastal areas.  Kodiak Bears are the largest of the Brown bears and are found only on Kodiak Island.  Inland bears (like the ones you find in Yellowstone) are called Grizzlies (Ursus arctos horriblis).  Bears on boats are called Marshmallows.  All bears (excepting Marshmallow himself) are in the genus Ursus.   Brown bears, Grizzly Bears, and Kodiak Bears are Ursus arctos, while Marshmallow’s distant cousins to the north are Ursus maritimus.  After discovering this as his namesake, Marshmallow was quite revolted.  He has decided to write a strongly worded letter to the Linnaeus Society as the term maritimus paints a less menacing and voracious picture of polar bears than does the Grizzly’s namesake.

Mbear in the flowers

Marshmallow has been quite incorrigible since his discovery of his species name. I suggested that he attach this photo to his strongly worded letter, which paints him in a most frightening manner.

He has suggested instead to be called Ursus kickyerbuttus.    I maintain that Marshmallow should be renamed Ursus domesticus stuffedus wimpus, because the closest he has ever been to a salmon run is from the comfort of his 60 inch HDTV.  He has a stateroom for crying out loud.

As we drive along the road, we slow down to a crawl at all of the river crossings hoping to see Kodiak Bears.  Our luck was good that day, because we saw three in a matter of about 4 hours.  Here he is now.

Brown Bear

This bear is not a Marshmallow. Nor is he a Pooh or a Yogi. Let me break this down into a simple equation: No stuffing + large + curious and furtive glances at surrounding humans + large teeth and claws = I should probably be further away than I am right now.

A fisherman nearby hypothesized he was a juvenile male, about 2 or 3 seasons away from his mamma and on his own as a hunter.  He was pretty indifferent to the existence of people, but not menacing in any way.  He ambled along, chasing after magpies and hopping in and out of the water.  It was neat to see him up so close, but still have the safety of the bridge to keep us at a safe distance.  This was of course, until he decided to climb up onto the road.  He was quicker than I would have liked him to be!

After dinner, we were driving back to the ship along Women’s Bay and one ran out in front of the car!  His shoulder blade was at the same level as the roof of the Impreza we were driving – no fish tale.  He glanced casually at us and loped off into the trees toward the salt marsh.  The next creek up the bay hosted a third bear, but we only got a glimpse of him as he was gone by the time we turned the car around.  It was really a blessing to get to see (more than once!) such neat little critters.  And by little critters I mean large toothed, long clawed beasts that have the capability to chew your head off in one fell swoop.  Thankfully, they are more interested in salmon at this time of year, and really don’t have much of a taste for people.  (In defense of Mr. Kodiak, there are more casualties from dogs in a given year than there are fatal maulings in ten years from Kodiak Browns.  We would have much more to worry about if we tasted like Salmon or Salmonberries, as this is what comprises the majority of their diet.  However, they should be treated with a healthy respect – especially a momma bear with her cubs.)

It has been an action packed week so far.  We are hoping to learn as much as we can about the island while we are here, and we are making the best of being in port while we wait to set sail.  It’s been wonderful to walk out on the peninsula every morning and have some time to myself to show gratitude for all that has been done for me to get me out here and experience this first hand.  The standing joke when we witness something truly spectacular is to say “I think in my evaluation of the Teacher At Sea program I am going to suggest that they actually find places for us to go that aren’t so ugly.  This place is such an eyesore…”  I hope you sense the sarcasm dripping in my voice.

Trivia Question:

True or False?  Sea Stars are Echinoderms that can regenerate lost body parts.

Answer:  True.  “Sea stars are remarkable, as they are able to regenerate lost or damaged parts of their bodies. An arm that is broken off can be regrown. Some species can actually regrow a complete new body from a single severed arm, if it is attached to part of the central disc.”

**http://www.marineparks.wa.gov.au/fun-facts/95-sea-stars.html

Anne Mortimer: Swell Sleeping, July 12, 2011

NOAA Teacher at Sea
Anne Mortimer
Onboard NOAA Ship Oscar Dyson
July 4 — 22, 2011 

Mission: Pollock Survey
Geographical area of cruise: Gulf of Alaska
Date: July 12, 2011

Weather Data from the Bridge
Conditions: Foggy and windy, changing to partly sunny and windy
Air Temperature: 10.1 ⁰C
Sea Temperature: 7.6 ⁰C
Wind direction: 237 ⁰C
Wind speed: 20 knots
Wave height: 2-3 ft.
Swell height: 5-6 ft.

Science and Technology Log

Last night we had a “splitter” catch. The scientists found an area that they couldn’t pass up fishing, so at about 9pm the trawl was put in the water. The 540 ft. long Aleutian wing trawl brought in lots of pollock and Pacific ocean perch, a type of red-colored rockfish.  A catch is called a splitter when it is so big it won’t all fit on the table. To get a weight of the whole catch, the deck crew use a crane to weigh the net, then empty it out.  Then the catch is dumped into a bin that is split in two parts. Only one part of the bin is then raised, putting a sub-sample on the table to be worked-up. It took a long time to process all of the catch. We separated the species on a conveyor belt system, then the messy stuff happens. I mentioned that otoliths and stomachs are collected, but I don’t think I emphasized just how gross this can be. To sex the fish, we use a scalpel to slice the fish down the side, then look for larger pink-colored ovaries or a stringy, twisted looking testes. To collect otoliths, the fish skull is cut just behind the eyes and cracked open. The otoliths are then picked put with tweezers. If you are really good at pulling otoliths, you can pull both at once, which can be very challenging. My double-take record is only 2 in a row, but I’ve pulled both at once at least 5 times now!  The last messy thing is stomach collection. You can imagine what this entails, I’m sure. I’m happy to say that I’ve only had to hold the baggie for the stomach, not cut any out! Processing this catch took several hours– we didn’t end until after 1am.

red rockfish

This red-colored fish is a pacific ocean perch, or P.O.P. to a fish biologist.

Pacific ocean perch

When I am not processing a trawl or on the bridge observing, I have been working to annotate some videos from the cam-trawl. The cam-trawl is a stereo-camera system that takes snapshots of whatever comes through the net. This cam-trawl was designed by several of the scientists on the pollock survey. They are hoping it will help lead to less actual fish samples needed if the images can accurately provide evidence of species, numbers, and sizes. Some trawls would still have to be taken aboard for sexing, weights, and otolith and stomach samples.  Annotating the images basically means that I click through the images, counting each species of fish or invertebrate (usually jellies) that I see. This can very tedious, but the whole idea of the project is very exciting. I’ll talk more about the cam-trawl and this technology in my next blog.

Personal Log

Yesterday was my first real encounter with rocking and rolling on the Oscar Dyson. The winds were blowing at about 30 knots (that’s about 35 mph), and there was a lot of swell. Swell waves are long-wavelength surface waves that could have originated from a storm hundreds or thousands of miles away. The combination of these two made for a very rocky ride until we hid behind an island until sunrise. Since I go to bed at 4:30am, it wasn’t long before the boat was headed back out to unprotected waters, and I was rudely awakened by the swell. To say I didn’t have a swell sleep is an understatement. I had to take a nap this evening to compensate for my lost hours!

Pre-trip Pondering

 NOAA TEACHER AT SEA
CATHRINE PRENOT FOX
ONBOARD NOAA SHIP OSCAR DYSON
JULY 24 – AUGUST 14, 2011
 
Personal Log
I will be traveling in a few short weeks to join the crew of the NOAA ship the Oscar Dyson in the Gulf of Alaska.  During the voyage, I will be keeping this log up to date and documenting my “adventures” with a cartoon series as well.  
I hope that you will follow along, ask lots of questions, and travel with me digitally.  
Until our next adventure, Cat 

Richard Chewning, June 6-7, 2010

NOAA Teacher at Sea
Richard Chewning
Onboard NOAA Ship Oscar Dyson
June 4 – 24, 2010

NOAA Ship Oscar Dyson
Mission: Pollock Survey Geographical area of cruise: Gulf of Alaska (Kodiak) to eastern Bering Sea (Dutch Harbor)
Dates: June 6-7, 2010

Weather Data from the Bridge

Position: Snakehead Bank, Gulf of Alaska
Time: 1700 hrs
Latitude: N 56 00.390
Longitude: W 153 46.380
Cloud Cover: Overcast
Wind: 12 knots from the SE
Temperature: 7.1C
Barometric Pressure: 1016.9 mbar

Science and Technology Log

I have been impressed by the wide array of oceanographic research the Oscar Dyson is able to conduct. A few examples include biological studies of organisms ranging from microscopic plankton to massive marine mammals, collecting a variety of weather data, describing both physical and chemical characteristics of seawater (such as temperature, salinity, chlorophyll, and dissolved oxygen), conducting acoustic surveys of marine life and the sea floor, and much more.

Three Saints Bay nautical chart

One of the Dyson’s ‘bread and butter’ surveys is our survey studying the distribution, biomass, and biological composition (male/female ratios and age) of walleye pollock in the Bering Sea. Walleye pollock is a very important fishery for Alaska. You have almost certainly been a part of this fishery as most fish sandwiches in fast food restaurants and fish sticks in the frozen food section of your local grocery store are Alaskan-caught pollock.

One of the Oscar Dyson’s many tools for this research is her impressive array of acoustic sensors located on the ship’s hull and centerboard. The centerboard is an extension of the hull that can be raised and lowered in the water in order to position most of the Dyson’s sensitive acoustic sensors below the bubbles often found near the water’s surface. These air bubbles interfere with sound traveling through the water and degrade the quality of the data being collected. The Dyson has six downward looking centerboard-mounted transducers, each transmitting a different frequency. Why so many frequencies? Since different types of marine organisms interact with sound waves differently producing varying acoustic signatures, the Dyson must be equipped with a variety of sensors to best characterize the variety of marine life encountered during a survey.

For example, lower frequencies are better suited for fish such as pollock and the higher frequencies are better suited for smaller organisms such as plankton. Think of transducers as a downward shining flashlight illuminating the depths of the ocean with sound rather than light.

The Dyson also has other acoustic sensors such as the ME-70 multibeam echosounder that has the unique ability to look over a much wider angle through the water. Acoustic research works on the same echo location principle that bats and marine mammals employ to find food and navigate. By sending out sound waves and measuring the time the sound takes to travel back after encountering an object, one can learn a great deal about that object’s properties such as distance, size, and movement.

Before traveling to the Bering Sea to start our pollock survey, the Dyson’s scientists must take great care to ensure that their echo-sounding equipment is calibrated correctly. Calibrating the transducers is similar in concept to tuning a piano string or zeroing a sight on a rifle. To this end, the Dyson anchored in Three Saints Bay, a sheltered bay protected from the wind, waves, and currents of the open ocean, at least theoretically. While a troublesome storm passed almost directly overhead, scientists from the Midwater Assessment and Conservation Engineering (MACE) Program (part of the Alaska Fisheries Science Center (AFSC) located in Seattle, WA), the US Fish and Wildlife Service (FWS located in Anchorage, AK), and the Pacific Institute of Fisheries and Oceanography (located in Vladivostok, Russia) worked diligently to fine tune their acoustic sensors.

Copper sphere used to calibrate the acoustic sensors

Bill and Patrick positioning spheres under the Dyson

Paul Walline, Patrick Ressler, Darin Jones, Bill Floering, and Mikhail ‘Misha’ Stepanenko worked day and night calibrating their equipment using metal spheres positioned directly under the ship.

Spheres of different sizes and materials with known acoustic signatures (such as tungsten carbide and copper) are used to calibrate the transducers.

The crew of the Dyson works around the clock as ship time is precious. The scientists work 12 hour shifts, either from 4am to 4pm (the shift to which I am assigned) or from 4pm to 4am. The acoustics lab where the data is collected and analyzed is affectionately called ‘The Cave’ as there are no portholes (windows) to tell the time of day outside.

The acoustic lab, a.k.a. “the cave”

Personal Log

I wasn’t sure when the Dyson arrived at Three Saints Bay as I had retreated to my stateroom early in the evening of the 4th as I was feeling the effects of the rolling seas. I am being berthed with the ship’s 2nd Cook, Floyd Pounds, who is also from Georgia but now calls the Dyson home.
Floyd works with the Chief Steward, Rick Hargis, who has been with NOAA for 20 years and is originally from Washington State. So far the meals have been very filling and satisfying (there is even an ice cream bar!).

My stateroom is located on the crew deck, one level below the main deck near the bow (the pointy end of the ship) on the starboard side (the right side when facing the bow). Utilizing every nook and cranny and with no wasted space, my berth is quite cozy and is surprisingly comfortable. Fortunately with the help of some seasickness medication, I soon found my sea legs and awoke feeling refreshed and hungry (always a good sign!). Seasickness comes from conflicting messages received from the inner ear and the eyes by the brain (the inner ear feels the motion of the boat rolling and pitching in the water but the eyes report a stable environment confusing the brain).

Snug as a bud in a rug

Richard, ready for a swim

A person soon observes that safety is paramount onboard the Dyson as with any NOAA vessel. For example, within 24 hours of leaving Kodiak, the entire crew conducted fire and abandon ship drills. These drills are conducted once a week and are essential for maintaining readiness in the event of an emergency. During the abandon ship drill, I was able to practice donning my survival suit just like our visiting Coast Guard kids did in Kodiak! Although the suit is designed to be quite snug to keep cold water out and to keep the body warm, I was thankful I didn’t have to put the suit to the test by going over the side. To my surprise, Chief Marine Engineer Jerome ‘Jerry’ Sheehan and ENS Russell Pate did just that, going for a dip in the frigid 7.3 degrees Celcius or ~45 degrees Fahrenheit waters! Jerry and Russell used dry suits to scuba dive under the Dyson to check the hull, the prop, and the transducers for anything out of place such as barnacles on the transducers or tangled fishing gear. The only discovery was of a piece of bull kelp snagged on one of the blades of the prop which may explain a noise that was heard on the hydrophones (microphones located under the Dyson’s hull) during our departure from Kodiak.

CO Hoshlyk overseeing recovery divers Jerry Sheehan and ENS Russell Pate

After completing our calibrations and safety operations, the Dyson sailed for a site called Snakehead Bank located 60 nautical miles southeast of Kodiak. The name comes from the bathometric profile of the seafloor of this area which resembles the head of a snake. We soon began conducting camera operations for ground-truthing sea floor composition that I will discuss in my next log!

Remnants of Nunamiut, earliest Russian settlement 1792 in three saints bay, Kodiak

Departing Three Saints Bay

 

Where did the NOAA ship Oscar Dyson’s name originate?

 

The Oscar Dyson is named for an Alaskan fisherman who was very influential in fisheries development and management in Alaska. From his days as a commercial fisherman, Oscar Dyson was a pioneer and advocate for Alaska fisherman and was very influential in the growth of this important industry. Alaska’s commercial fishing industry spans the state and includes salmon, herring, pollock, various shellfish, and various ground fish like halibut. While traveling through the Ted Stevens International Airport in Anchorage, I learned that Alaska is a land defined by water with more than three million lakes and more coastline than the rest of the United Sates combined! Alaska is also the only state in the US to have coastlines with three different oceans/seas: the Pacific Ocean, the Arctic Ocean, and the Bering Sea.