Mission: Long Line Shark/ Red Snapper survey Leg 1
Geographic Area: 30 19’ 54’’ N, 81 39’ 20’’ W, 10 nautical miles NE of Jacksonville, Florida
Date: August 9, 2018
Weather Data from Bridge: Wind speed 11 knots, Air Temp: 30c, Visibility 10 nautical miles, Wave height 3 ft.
Science and Technology Log
Sharks have senses similar to humans that help them interact with their environment. They use them in a specific order and rely on each one to get them closer for navigational reasons, and to find any food sources in the area around them. The largest part of the shark’s brain is devoted to their strong sense of smell, so we’ll start there.
snout of Tiger shark
snout of sharpnose shark
Smell– Sharks first rely on their strong sense of smell to detect potential food sources and other movement around them from a great distance. Odor travels into the nostrils on either side of the underside of the snout. As the water passes through the olfactory tissue inside the nostrils, the shark can sense or taste what the odor is, and depending which nostril it goes into, which direction it’s coming from. It is said that sharks can smell one drop of blood in a billion parts of water from up to several hundred meters away.
Ampullae of Lorenzini and nostrils of a sharpnose shark
Sharks can also sense electrical currents in animals from long distances in several ways. Sharks have many electro sensitive holes along the snout and jaw called the Ampullae of Lorenzini. These holes detect weak electrical fields generated by the muscles in all living things. They work to help sharks feel the slightest movement in the water and sand and direct them to it from hundreds of meters away. This system can also help them detect the magnetic field of the earth and sharks use it to navigate as well.
Ampullae of Lorenzini and nostrils of a sharpnose shark
Hearing– Sharks also heavily use their sense of smell to initially locate objects in the water. There are small interior holes behind their eyes that can sense vibrations up to 200 yards away. Sound waves travel much further in water than in the air allowing them to hear a great distance away in all directions. They also use their lateral lines, which are a fluid filled canal that runs down both sides of the body. It contains tiny pores with microscopic hairs inside that can detect changes in water pressure and the movement and direction of objects around them.
Sight– Once sharks get close enough to see an object, their eyes take over. Their eyes are placed on either side of their head to provide an excellent range of vision. They are adapted to low light environments, and are roughly ten times more sensitive to light than human eyes. Most sharks see in color and can dilate their pupils to adapt to hunting at different times of day. Some sharks have upper and lower eyelids that do not move. Some sharks have a third eyelid called a nictitating membrane, which is an eyelid that comes up from the bottom of the eye to protect it when the shark is feeding or in other dangerous situations. Other sharks without the membrane can roll their eyes back into their head to protect them from injury.
dilated pupil of sharpnose shark
Touch– After using the previous senses, sometimes a shark will swim up and bump into an object to obtain some tactile information. They will then decide whether it is food to eat and attack, or possibly another shark of the opposite gender, so they can mate.
Taste– Sharks are most famous for their impressive teeth. Most people are not aware that sharks do not have bones, only cartilage (like our nose and ears) that make up their skeletal system, including their jaw that holds the teeth. The jaw is only connected to the skull by muscles and ligaments and it can project forward when opening to create a stronger bite force. Surface feeding sharks have sharp teeth to seize and hold prey, while bottom feeding sharks teeth are flatter to crush shellfish and other crustaceans. The teeth are embedded in the gums, not the jaw, and there are many rows of teeth behind the front teeth. It a tooth is damaged or lost, a new one comes from behind to replace it soon after. Some sharks can produce up to 30,000 teeth in their lifetime.
Sandbar Shark teeth
Great Hammerhead Shark teeth
Personal Log
While I had a general knowledge of shark biology before coming on this trip, I’ve learned a great deal about sharks during my Teacher at Sea experience aboard the Oregon II. Seeing, observing, and holding sharks every day has given me first hand knowledge that has aided my understanding of these great creatures. The pictures you see of the sharks in this post were taken by me during our research at sea. I could now see evidence of all their features up close and I could ask questions to the fishermen and scientists onboard to add to the things I read from books. As an artist, I can now draw and paint these beautiful creatures more accurately based on my reference photos and first hand observations for the deck. It was amazing to see that sharks are many different colors and not just different shades of grey and white you see in most print photographs. I highly encourage everyone that has an interest in animals or specific areas of nature to get out there and observe the animals and places firsthand. I guarantee the experience will inspire you, and everyone you tell of the many great things to be found in the outdoors.
TAS Stephen Kade with a sharpnose shark
TAS Stephen Kade removes the hook from a sharpnose shark
Animals Seen Today: Sandbar shark, Great Hammerhead shark, Sharp nose shark
Geographic Area: Northwest Hawaiian Island Chain, Just past Mokumanamana (Necker Island)
Date: July 20, 2017
Weather Data from the Bridge:
Science and Technology Log:
As promised in Blog Post #3, I mentioned that “Thing number four we deliberately throw overboard” would have a dedicated blog post because it was so involved. Well, grab some popcorn, because the time has arrived!
Thing number 4 we deliberately throw over the side of a ship does not get thrown overboard very often, but when it does, it causes much hubbub and hullaballoo on the ship. I had the unique opportunity to witness one of only ten ocean noise sensors that are deployed in US waters come aboard the ship and get redeployed. These sensors are found all over US waters – from Alaska to the Atlantic. One is located in the Catalina Marine Sanctuary, and still others are hanging out in the Gulf of Mexico, and we are going to be sailing right past one! To see more about the Ocean Noise Sensors, visit the HICEAS website “other projects” tab, or just click here. To see where the Ocean Noise Recorders are, click here.
The Ocean Noise Sensor system is a group of 10 microphones placed in the “SOFAR” channel all over US waters. Once deployed, they collect data for two years in order to track the level of ocean noise over time. It’s no secret that our oceans are getting louder. Shipping routes, oil and gas exploration, and even natural sources of noise like earthquakes all contribute to the underwater noise that our cetacean friends must chatter through. Imagine sitting at far ends of the table at a dinner party with a friend you have not caught up with in a while. While other guests chat away, you and the friend must raise your voices slightly to remain in contact. As the night progresses on, plates start clanging, glasses are clinking, servers are asking questions, and music is playing in the background. The frustration of trying to communicate over the din is tolerable, but not insurmountable. Now imagine the host turning on the Super Bowl at full volume for entertainment. Now the noise in the room is incorrigible, and you and your friend have lost all hope of even hearing a simple greeting, let alone have a conversation. In fact, you can hardly get anyone’s attention to get them to pass you the potatoes. This is similar to the noise levels in our world’s ocean. As time goes on, more noise is being added to the system. This could potentially interfere with multiple species and their communications abilities. Calling out to find a mate, forage for food, or simply find a group to associate with must now be done in the equivalent din of a ticker-tape parade, complete with bands, floats, and fire engines blaring their horns. This is what the Ocean Noise Sensor is hoping to get a handle on. By placing sensors in the ocean to passively collect ambient noise, we can answer two important questions: How have the noise levels changed over time? To what extent are these changes in noise levels impacting marine life?
Many smaller isolated studies have been done on ocean noise levels in the past, but a few years ago, scientists from Cornell partnered with NOAA and the Pacific Islands Fisheries Science Center (PIFSC) and the Pacific Marine Environmental Lab to streamline this study in order to get a unified, global data source of ocean noise levels. The Pacific Marine Environmental Lab built a unified sound recording system for all groups involved in the study, and undertook the deployments of the hydrophones. They also took on the task of processing the data once it is recovered. The HICEAS team is in a timely and geographical position to assist in recovery of the data box and redeploying the hydrophone. This was how we spent the day.
The recovery and re-deployment of the buoy started just before dawn, and ended just before dinner.
Our standard effort of marine mammal observation was put on hold so that we could recover and re-deploy the hydrophone. It was an exciting day for a few reasons – one, it was definitely a novel way to spend the day. There was much to do on the part of the crew, and much to watch on the part of those who didn’t have the know-how to assist. (This was the category I fell in to.)
At dawn, an underwater acoustic command was sent to the depths to release a buoy held underwater attached to the hydrophone. While the hydrophone is only 1000m below the surface seated nice and squarely in the SOFAR channel, the entire system is anchored to the ocean floor at a depth of 4000m. Once the buoy was released, crew members stationed themselves around the ship on the Big Eyes and with binoculars to watch for the buoy to surface. It took approximately 45 minutes before the buoy was spotted just off our port side. The sighting award goes to CDR Stephanie Koes, our fearless CO. A crewmember pointed out the advancement in our technologies in the following way: “We can use GPS to find a buried hydrophone in the middle of the ocean…and then send a signal…down 4000m…to a buoy anchored to the ocean floor…cut the buoy loose remotely, and then actually have the buoy come up to the surface near enough to the ship where we can find it.” Pretty impressive if you think about it.
The buoy was tied to the line that is attached to the hydrophone, so once the buoy surfaced, “all” we had to do was send a fast rescue boat out to retrieve it, bring the buoy and line back to the ship, bring the crew safely back aboard the ship, hook the line up through a pulley overhead and back to a deck wench, pull the line through, take off the hydrophone, pull the rest of the line up, unspool the line on the wench to re-set the line, re-spool the winch, and then reverse the whole process.
Watching the crew work on this process was impressive at least, and a fully orchestrated symphony at best. There were many tyings of knots and transfers of lines, and all crew members worked like the well-seasoned deck crew that they are. Chief Bos’n Chris Kaanaana is no stranger to hauling in and maintaining buoys, so his deck crew were well prepared to take on this monumental task.
Much of the day went exactly according to plan. The buoy was safely retrieved, the hydrophone brought on board, the lines pulled in, re-spooled, and all sent back out again. But I am here to tell you that 4000m of line to haul in and pay back out takes. A Long. Time. We worked through a rainstorm spooling the line off the winch to reset it, through the glare of the tropical sun and the gentle and steadfast breeze of the trade winds. By dinner time, all was back in place, the buoy safely submerged deep in the ocean waters, waiting to be released again in another two years to repeat the process all over again. With any luck, the noise levels in the ocean will have improved. Many commercial vessels have committed to adopting “quiet ship” technology to assist in the reduction of noise levels. If this continues to improve, our cetacean friends just might be able to hear one another again at dinner.
Personal Log
So, I guess it’s pretty fair to say that once you’re a teacher, you’re always a teacher. I could not fully escape my August to May duties onboard, despite my best efforts. This week, I found myself on the bridge, doing a science experiment with the Wardroom (These are what all of the officers onboard as a group are called). How is this even happening, you ask? (Trust me, I asked myself the same thing when I was in the middle of it, running around to different “lab groups” just like in class.) Our CO, CDR Koes, is committed to ensuring that her crew is always learning on the ship.
If her staff do not know the answer to a question, she will guide them through the process of seeking out the correct answer so that all officers learn as much as they can when it comes to being underway – steering the ship, preparing for emergencies, and working with engineers, scientists, and crew. For example, I found out that while I was off “small-boating” near Pilot Whales, the Wardroom was busy working on maneuvering the ship in practice of man overboard scenarios. She is committed to ensuring that all of her staff knows all parts of this moving city, or at a minimum know how to find the answers to any questions they may have. It’s become clear just how much the crew and the entire ship have a deep respect and admiration for CDR Koes. I knew she was going to be great when we were at training and word got out that she would be the CO of this Leg on Sette and everyone had a range of positive emotions from elated to relieved to ecstatic.
As part of this training, she gives regular “quizzes” to her staff each day – many of them in good fun with questions for scientists, crew, engineers, and I. Some questions are nautical “things” that the Wardroom should know or are nice to know (for example, knowing the locations of Material Safety Data Sheets or calculating dew point temperatures), some questions are about the scientific work done onboard, while others are questions about personal lives of onboard members.
The Chief Medical Officer, “Doc” gives a lesson on water quality testing.
It has been a lot of fun watching the Wardroom and Crew seek out others and ask them where they live while showing them their “whale dance” to encourage sightings. It has exponentially increased the interactions between everyone onboard in a positive and productive way.
The other teaching element that CDR Koes has implemented is a daily lesson each day from Monday to Friday just after lunch. All NOAA Officers meet on the bridge, while one officer takes the lead to teach a quick, fifteen minute lesson on any topic of their choosing. It could be to refresh scientific knowledge, general ship operations, nautical concepts, or anything else that would be considered “good to know.”
The Chief Engineer gives a rundown on the various ship emergency alarms.
This sharing of knowledge builds trust among the Wardroom because it honors each officer’s strong suits and reminds us that we all have something to contribute while onboard.
I started attending these lunchtime sessions and volunteered to take on a lesson. So, this past Tuesday, I rounded up some supplies and did what I know best – we all participated in the Cloud in a Bottle Lesson!
Here I am learning to use a sextant for navigation.
The Wardroom had fun (I think?) making bottle clouds, talking about the three conditions for cloud formation, and refreshing their memories on adiabatic heating and cooling. It was a little nerve wracking for me as a teacher because two of the officers are meteorologists by trade, but I think I passed the bar. (I hope I did!)
Teaching about adiabatic cooling with the the Cloud in a Bottle Demo with the Wardroom!
It was fun to slide back into the role of teacher, if only for a brief while, and served as a reminder that I’m on my way back to work in a few weeks! Thanks to the Wardroom for calling on me to dust up my teacher skills for the upcoming first weeks of school!
ENS Holland and ENS Frederick working hard making clouds.
Facebook Asks, DeSchryver Answers
I polled all of my Facebook friends, fishing (ha ha, see what I did there?) for questions about the ship, and here are some of the questions and my answers!
Q: LC asks, “What has been your most exciting moment on the ship?”
It’s hard to pick just one, so I’ll tell you the times I was held at a little tear: a) Any sighting of a new species is a solid winner, especially the rare ones b) The first time I heard Sperm Whales on the acoustic detector c) The first time we took the small boat out for UAS operations….annnndddd d) The first time I was on Independent Observation and we had a sighting!
A group of Melon-Headed Whales, or PEPs, cruise along with the ship.
Q: JK asks, “What are your thoughts on the breakoff of Larsen C? And have there been any effects from the Alaskan quake and tsunami?”
We’re actually pretty isolated on board! Limited internet makes it hard to hear of all the current events. I had only briefly heard about Larsen C, and just that it broke, not anything else. I had no clue there was a quake and tsunami! But! I will tell a cool sort of related story. On Ford Island, right where Sette is docked, the parking lot is holding three pretty banged up boats. If you look closely, they all have Japanese markings on them. Turns out they washed up on Oahu after the Japan Tsunami. They tracked down the owners, and they came out to confirm those boats were theirs, but left them with NOAA as a donation. So? There’s tsunami debris on Oahu and I saw it.
Q: NG asks, “Any aha moments when it comes to being on the ocean? And anything to bring back to Earth Science class?”
So many aha moments, but one in particular that comes to mind is just how difficult it is to spot cetaceans and how talented the marine mammal observers are! They can quite literally spot animals from miles away! There are a lot of measures put in place to help the marine mammal observers, but at the end of the day, there are some species that are just tougher than nails to spot, or to spot and keep an eye on since their behaviors are all so different. And as far as anything to bring back to our class? Tons. I got a cool trick to make a range finder using a pencil. I think we should use it!
Q: MJB asks, “Have you had some peaceful moments to process and just take it all in?”
Yes. At night between the sonobuoy launches, I get two miles of transit time out on the back deck to just absorb the day and be thankful for the opportunities. The area of Hawai’i we are in right now is considered sacred ground, so it’s very powerful to just be here and be here.
These sunsets will give Colorado sunsets a run for their money. No green flash in Colorado = point awarded to Hawai’i.
Q: SC asks, “What souvenir are you bringing me?”
Well, we saw a glass fishing float, and we tried to catch it for you, but it got away.
Q: LC asks, “What’s the most disgusting ocean creature?”
Boy that’s a loaded question because I guarantee if I name a creature, someone out there studies it for a living. But! I will tell you the most delicious ocean creature. That would be Ono. In sashimi form. Also, there is a bird called a Great Frigate bird – it feeds via something called Klepto-parasitism, which is exactly how it sounds. It basically finds other birds, harasses them until they give up whatever they just caught or in some cases until it pukes, and then it steals their food. So, yeah. I’d say that’s pretty gross. But everyone’s gotta eat, right?
Q: KI asks, “Have you eaten all that ginger?”
I’m about two weeks in and I’m pretty sure I’ve eaten about a pound. I’m still working on it!
Q: HC asks, ”Have you seen or heard any species outside of their normal ocean territory?”
Sort of. Yesterday we saw Orca! They are tropical Orca, so they are found in this area, but they aren’t very common. The scientific team was thinking we’d maybe see one or two out of the entire seven legs of the trip, and we saw some yesterday! (I can’t say how many, and you’ll find out why in an upcoming post.) We have also seen a little bird that wasn’t really technically out of his territory, but the poor fella sure was a little far from home.
Q: JPK asks, “What kinds of data have you accumulated to use in a cross-curricular experience for math?”
We can do abundance estimates with a reasonably simplified equation. It’s pretty neat how we can take everything that we see from this study, and use those numbers to extrapolate how many of each species is estimated to be “out there.”
Q: AP asks, “What has surprised you about this trip?”
Many, many things, but I’ll mention a couple fun ones. The ship has an enormous movie collection – even of movies that aren’t out on DVD yet because they get them ahead of time! Also? The food on the ship is amazing. We’re halfway through the trip and the lettuce is still green. I have to find out the chef’s secret! And the desserts are to die for. It’s a wonder I haven’t put on twenty pounds. The crew does a lot of little things to celebrate and keep morale up, like birthday parties, and music at dinner, and shave ice once a week. Lots of people take turns barbecuing and cooking traditional foods and desserts special to them from home and they share with everyone. They are always in really high spirits and don’t let morale drop to begin with, so it’s always fun.
Celebrating Engineer Jerry’s Birthday.
Q: TS asks, “What’s the most exciting thing you’ve done?”
I’ve done lots of exciting things, but the one thing that comes to mind is launching on the small boat to go take photos of the pilot whales. Such a cool experience, and I hope we get good enough weather to do it again while we’re out here! Everything about ship life is brand new to me, so I like to help out as much as I can. Any time someone says, “Will you help with this?” I get excited, because I know I’m about to learn something new and also lend a hand.
At home in New England, where you can enjoy the mountains and the sea all in a day.
Greetings from New Hampshire! Our variable spring weather is getting me ready for the coolness at sea compared to hot Galveston, Texas, where I will ship off in a few days.
It is currently 50 F and raining with a light wind, the perfect weather to reflect on this upcoming adventure.
Science and Technology Log
I am excited to soon be a part of the 2017 SEAMAP Reef Survey. The National Oceanic and Atmospheric Administration (NOAA) writes the objective of these surveys is, “ to provide an index of the relative abundances of fish species associated with topographic features (banks, ledges) located on the continental shelf of the Gulf of Mexico in the area from Brownsville, Texas to Dry Tortugas, Florida.” The health of the Gulf is important from an ecological and economic perspective. Good science demands good research.
We will be working 12 hour shifts aboard the NOAA Ship Pisces. I expect to work hard and learn a lot about the science using cameras, fish traps, and vertical long lines. I also look forward to learning more about life aboard a fisheries research vessel and the career opportunities available to my students as they think about their own futures.
Personal Log
I’ve been teaching science in Maine and New Hampshire for eight years and always strive to stay connected to science research. I aim to keep my students directly connected through citizen science opportunities and my own continuing professional development. Living in coastal states, it is easier to remember the ocean plays a large role in our lives. The culture of lobster, fried clams, and beach days requires a healthy ocean.
I love adventure and have always wanted to “go out to sea.” This was the perfect opportunity! I was fortunate to take a Fisheries Science & Techniques class with Dave Potter while attending Unity College and look forward to revisiting some of that work, like measuring otoliths (ear bones, used to age fish). I have also benefited from professional development with The Bigelow Laboratory for Ocean Sciences and other ocean science experiences. One of the best parts of science teaching is you are always learning!
Science teachers benefit from quality professional development to stay informed in their content areas.
There was a lot of preparation involved since I am missing two weeks of school. I work at The Founders Academy, a public charter school in Manchester, New Hampshire. We serve students from 30 towns, but about a third come from Manchester. The school’s Vision is to: prepare wise, principled leaders by offering a classical education and providing a wide array of opportunities to lead:
Preparing students to be productive citizens.
Teaching students how to apply the American experience and adapt to become leaders in today’s and tomorrow’s global economy.
Emphasis on building ethical and responsible leaders in society.
I look forward to bringing my experiences with NOAA Teacher at Sea Program back to school! It is difficult to leave my students for two weeks, but so worth it. It is exciting to connect with middle and high school students all of the lessons we can learn from the work NOAA does. My school community has been very supportive, especially another science teacher who generously volunteered to teach my middle school classes while I am at sea.
I am grateful for the support at home for helping me participate in the NOAA Teacher at Sea Program.
My boyfriend too is holding down the fort at home and with Stone & Fire Pizza as I go off on another adventure. Our old guinea pigs, Montana & Macaroni, prefer staying at home, but put up with us taking them on vacation to Rangeley, Maine. I am grateful for the support and understanding of everyone and for the opportunity NOAA has offered me.
Did You Know?
NOAA Corps is one of the seven uniformed services of the United States.
NOAA is the scientific agency of the Department of Commerce. The agency was founded in 1970 by consolidating different organizations that existed since the 1800’s, making NOAA’s scientific legacy the oldest in the U.S. government.
As a science teacher, it is funny that I really do have guinea pigs. Here is our rescue pig Montana, who is 7-8 years old.
Day 3 weather was Hazardous with gusts up to 20 knots. Travel in the small C.E Stillwell not advisable.
Day 4 was beautiful and started out with light to variable winds with 0-1 ft seas and ended with 5-10 knots winds with 2-3 ft seas.
Science and Technology Log
Day 3 we attempted our usual 6:00 a.m. departure but after entering the bay it was obvious the working conditions attempting to tag sharks in our small boat would be almost impossible. We monitored the weather for a possible late morning departure but the weather only increased. We set ourselves to remarking the intervals on the mainlines as the markings were very faint and difficult at times to see where to set the gangion.
Ben Church and Matt Pezzullo remarking the thousands of feet of line.
Day 4 We were on the water and had our first line (set) in the water before 7:00 a.m. The conditions were great and we started right outside of Lewes, DE. In the morning we did 3-50 hook sets and 1-25 hook set in what is called deep hole which is on the Delaware side of the main shipping channel that runs through Delaware Bay.
One of the numerous large ships heading up Delaware Bay
As you can see by the picture numerous large ships enter the mouth of the bay and head up.
While we were pulling the line on the deep hole set this large Sand Tiger came to the surface after a lot of hard work by Matt.
Same shark we pulled out of deep hole.
At the end of the day we were able to complete a total of 8 sets. After finishing deep hole we spent the afternoon on the New Jersey side of the bay just off Cape May. As can be seen by the July 2015 stations Day 4 was spent at the mouth of the bay. On the Delaware side we did JY10, JY27, JY28 and Deep Hole. All JY sets are 50 hook sets while all others are the larger hooks with 25 per main line.
July 2015 Stations. Delaware Bay
During the afternoon we did JY26, JY18, EX06 followed by JY19. The order may seem odd looking at the map but sets are planned to ensure that they are retrieved in the correct time frame. JY18 was just off Sunset Beach in Cape May New Jersey.
Day 1 sets: JY24, JY20, JY22, BG02, SB01, SB02
Day 2 sets: JY07, JY01, JY11, JY13, EX04, ST05, EX07
Day 4 sets: JY10, JY28, JY27, Deep Hole, JY26, Jy19, JY18, EX06
Map of Delaware Bay
The following video is from day 1 but gives an idea of how hard it can be to tail rope the sharks.
Once a shark is tail roped and the gangion is cleated to the front of the boat we can collect the biological data and tag the shark.
The following video is long but if you watch to the end you will see what happens when a hook comes out while a shark is still tail roped.
We also had the opportunity to encounter a few rays. The following video is of a large Spiny Butterfly Ray we caught
Personal Log:
The shark tagging experience was extremely physically taxing but very rewarding. I had the opportunity to gain hands on experience in an exciting research project that will allow me to bring knowledge and excitement back to my classroom. My time working on this survey brought me a memorable experience that I will never forget.
I would personally like to thank the other scientists on the survey Nathan Keith, Ben Church and the Chief Scientist on the cruise Matt Pezzulo for sharing their expertise and knowledge on shark morphology and identification. These individuals were always willing to explain any part of the process or answer any questions I had. They took the time to teach me every part of the process early on so that I could become a contributing member from the start. This type of analysis on sharks takes grit and hard work and I appreciate the opportunity I was given through the Teacher at Sea Program.
NOAA Teacher at Sea Emily Whalen Aboard NOAA Ship Henry B. Bigelow April 27 – May 10, 2015
Mission: Spring Bottom Trawl Survey, Leg IV
Geographical Area of Cruise: Gulf of Maine Date: May 5, 2015
Weather Data: Air Temperature: 8.4°C
Water Temperature: 5.1ºC
Wind: 15 knots NW
Seas: 1-2 feet
Science and Technology Log:
Lobsters!
This is a large female lobster. The claw on the right is called the crusher and the claw on the left is called the pincer. For scale, consider that this lobster is inside a standard 5-gallon bucket!
Not everything that comes up in the net is a fish. One of the things that we have caught many of on this trip is Homarus americanus, commonly known as the lobster. Lobsters are invertebrates, which means they don’t have a backbone or an internal skeleton. Instead, they have a hard outer shell called an exoskeleton to give their body structure and protect their inner organs. Because their exoskeleton cannot expand as the lobster grows, a lobster must molt, or shed its shell periodically as it gets bigger. In the first few years of their lives, lobsters need to molt frequently because they are growing quickly. More mature lobsters only molt yearly or even every few years.
Another interesting fact about lobsters can regenerate lost body parts. After a claw or leg is lost, the cells near the damaged area will start to divide to form a new appendage. The developing structure is delicate and essentially useless while it is growing, but after a few molts, it will be fully functional.
This lobster lost a claw and is in the early stages of regenerating it. What challenges do you think a single-clawed lobster might face?This is a lobster that has almost completed regenerating a lost claw.This is a lobster with two fully functional claws. Why do you think each claw has a different shape?
When we catch lobsters, we measure and record the distance from their eye cavity to the posterior end of the carapace. Many of the lobsters we have caught are similar in size to those you would find at the grocery store, which typically weigh about a little more than pound. Commercial fishermen can only keep male lobsters that are over 101 millimeters. Can you guess why? We have seen some smaller lobsters that measure about 50 millimeters, and also some much larger lobsters that measure as much as 150 millimeters!
These are the calipers used to measure the carapace of each lobster.This is one of the larger lobsters that we have seen. Some lobsters can live to be over a hundred, although everyone’s best estimate for this one was about 20 years. I put my hand next to the claw so that you could see how big it is! I wasn’t brave enough to put my hand any closer!
One of the members of my watch is Dr. Joe Kunkel, who is doing something called ‘landmark analysis’ on some of the lobsters that we have caught. This process involves recording the exact location of 12 specific points on the carapace or shell of each lobster. Then he compares the relative geometry different lobsters to look for trends and patterns. In order to do this, he uses a machine called a digitizer. The machine has a small stylus and a button. When you push the button, it records the x, y and z position of the stylus. Once the x,y and z position of all 12 points has been recorded, they are imported into a graphing program that creates an individual profile for each lobster.
Here I am using a digitizer to pinpoint 12 different landmarks on this lobsters carapace, or shell. So far, the offshore lobsters seem to have different geometry than the onshore lobsters, even though they are the same species.
So far, it appears that lobsters that are caught inshore have different geometry than lobsters that are caught further offshore. Typically, an organism’s shape is determined by its genes. Physical variations between organisms can be the result of different genes, environmental factors or physiological factors like diet or activity. Dr. Kunkel doesn’t have a certain explanation for the differences between these two groups of lobsters, but it may suggest that lobsters have different activity levels or diet depending on whether they live near the shore our out in deeper waters. In recent years, a shell disease has decimated lobster populations south of Cape Cod. This study may give us clues about the cause of this disease, which could someday affect the lobster fishery.
This is a grid that represents the digitization of a lobster. The single point on the right hand side represents the rostrum, which is analogous to the nose, and the two points furthest to the left represent the place where the carapace or shell meets the tail.
Moving Forward
In order to move from station to station as we complete our survey, the Bigelow has a powerful propulsion system different from most other types of ships. Typically, a ship has an engine that burns diesel fuel in order to turn a shaft. To make the ship move forward (ahead) or backward (astern), the clutch is engaged, which causes the shaft to spin the propeller. The throttle can then be used to make the shaft spin faster or slower, which speeds up or slows down the boat. Throttling up and down like this affects the amount of fuel burned. For those of you who are new drivers, this is similar to how your car gets better or worse gas mileage depending on what type of driving you are doing.
Like this class of ship, the Bigelow has a giant propeller at the stern which is 14 feet across and has 5 blades. However, the unlike most ships, the propeller on the Bigelow is powered by electricity instead of a combustion engine. There are four electricity-producing generators on the ship, two large and two small. The generators burn diesel fuel and convert the stored energy into electricity. The electricity powers two electric motors, which turn the propeller. While the electricity produced powers the propeller, it is also used for lights, computers, pumps, freezers, radar and everything else on the ship. There are several benefits to this type of system. One is that the generators can run independently of each other. Running two or three generators at a time means the ship makes only as much electricity as it needs based on what is happening at the time, so fuel isn’t wasted. Since the ship can speed up or slow down without revving the engine up or down, the generators can always run at their maximum efficiency.
Also, there is much finer control of the ship’s speed with this system. In fact, the ship’s speed can be controlled to one tenth of a knot, which would be similar to being able to drive your car at exactly 30.6 or 30.7 mph. Finally, an added benefit is that the whole system runs quietly, which is an advantage when you are scouting for marine mammals or other living things that are sensitive to sound.
Personal Log
I have seen a lot of fish on this trip, but it would be a lie to say that I don’t have some favorites. Here are a few of them. Which one do you think is the coolest?
This is a sea raven. Most of the ones we have seen are brown and green, but this one was a brilliant yellowWindowpane flounder. We have seen many types of flounder, but I think these are the coolest.Last night we caught 1,700 kilograms of mackerel like these on the Scotian Shelf!I find the pattern on this cod particularly striking.How can you not love this little spoonarm octopus?This immature cusk eel will lose these colors and eventually grow to be a dull grey color.These squid have chromatophores, which are cells that can change color. You can see them in this picture as the reddish purple dots.This Atlantic hagfish has circular rasping teeth that it uses to burrow into its prey. Even as they ride along the conveyor belt, they are trying to bite into an unsuspecting fish!You can see the gills of this goosefish by looking deep into its mouth. This fish has a giant mouth that allows it to each huge meals. Some of the goosefish we catch have stomachs that are larger than their whole bodies!We have only seen one of these little blue lumpfish. While most fish feel slippery and slimy, this one has a rough skin.
NOAA Teacher at Sea Emily Whalen Aboard NOAA Ship Henry B. Bigelow April 27 – May 10, 2015
Mission: Spring Bottom Trawl Survey, Leg IV
Geographical Area of Cruise: Gulf of Maine Date: May 1, 2015
Weather Data from the Bridge: Winds: Light and variable
Seas: 1-2ft
Air Temperature: 6.2○ C
Water Temperature: 5.8○ C
Science and Technology Log:
Earlier today I had planned to write about all of the safety features on board the Bigelowand explain how safe they make me feel while I am on board. However, that was before our first sampling station turned out to be a monster haul! For most stations I have done so far, it takes about an hour from the time that the net comes back on board to the time that we are cleaning up the wetlab. At station 381, it took us one minute shy of three hours! So explaining the EEBD and the EPIRB will have to wait so that I can describe the awesome sampling we did at station 381, Cashes Ledge.
This is a screen that shows the boats track around the Gulf of Maine. The colored lines represent the sea floor as determined by the Olex multibeam. This information will be stored year after year until we have a complete picture of the sea floor in this area!
Before I get to describing the actual catch, I want to give you an idea of all of the work that has to be done in the acoustics lab and on the bridge long before the net even gets into the water.
The bridge is the highest enclosed deck on the boat, and it is where the officers work to navigate the ship. To this end, it is full of nautical charts, screens that give information about the ship’s location and speed, the engine, generators, other ships, radios for communication, weather data and other technical equipment. After arriving at the latitude and longitude of each sampling station, the officer’s attention turns to the screen that displays information from the Olex Realtime Bathymetry Program, which collects data using a ME70 multibeam sonar device attached to bottom of the hull of the ship .
Traditionally, one of the biggest challenges in trawling has been getting the net caught on the bottom of the ocean. This is often called getting ‘hung’ and it can happen when the net snags on a big rock, sunken debris, or anything else resting on the sea floor. The consequences can range from losing a few minutes time working the net free, to tearing or even losing the net. The Olex data is extremely useful because it can essentially paint a picture of the sea floor to ensure that the net doesn’t encounter any obstacles. Upon arrival at a site, the boat will cruise looking for a clear path that is about a mile long and 300 yards wide. Only after finding a suitable spot will the net go into the water.
Check out this view of the seafloor. On the upper half of the screen, there is a dark blue channel that goes between two brightly colored ridges. We trawled right between the ridges and caught a lot of really big fish!
The ME70 Multibeam uses sound waves to determine the depth of the ocean at specific points. It is similar to a simpler, single stream sonar in that it shoots a wave of sound down to the seafloor, waits for it to bounce back up to the ship and then calculates the distance the wave traveled based on the time and the speed of sound through the water, which depends on temperature. The advantage to using the multibeam is that it shoots out 200 beams of sound at once instead of just one. This means that with each ‘ping’, or burst of sound energy, we know the depth at many points under the ship instead of just one. Considering that the multibeam pings at a rate of 2 Hertz to 0.5 Herts, which is once every 0.5 seconds to 2 seconds, that’s a lot of information about the sea floor contour!
This is what the nautical chart for Cashes Ledge looks like. The numbers represent depth in fathoms. The light blue lines are contour lines. The places where they are close together represent steep cliffs. The red line represents the Bigelow’s track. You can see where we trawled as a short jag between the L and the E in the word Ledge
The stations that we sample are randomly selected by a computer program that was written by one of the scientists in the Northeast Fisheries Science Center, who happens to be on board this trip. Just by chance, station number 381 was on Cashes Ledge, which is an underwater geographical feature that includes jagged cliffs and underwater mountains. The area has been fished very little because all of the bottom features present many hazards for trawl nets. In fact, it is currently a protected area, which means the commercial fishing isn’t allowed there. As a research vessel, we have permission to sample there because we are working to collect data that will provide useful information for stock assessments.
My watch came on duty at noon, at which time the Bigelowwas scouting out the bottom and looking for a spot to sample within 1 nautical mile of the latitude and longitude of station 381. Shortly before 1pm, the CTD dropped and then the net went in the water. By 1:30, the net was coming back on board the ship, and there was a buzz going around about how big the catch was predicted to be. As it turns out, the catch was huge! Once on board, the net empties into the checker, which is usually plenty big enough to hold everything. This time though, it was overflowing with big, beautiful cod, pollock and haddock. You can see that one of the deck crew is using a shovel to fill the orange baskets with fish so that they can be taken into the lab and sorted!
You can see the crew working to handling all of the fish we caught at Cashes Ledge. How many different kinds of fish can you see? Photo by fellow volunteer Joe Warren
At this point, I was standing at the conveyor belt, grabbing slippery fish as quickly as I could and sorting them into baskets. Big haddock, little haddock, big cod, little cod, pollock, pollock, pollock. As fast as I could sort, the fish kept coming! Every basket in the lab was full and everyone was working at top speed to process fish so that we could empty the baskets and fill them up with more fish! One of the things that was interesting to notice was the variation within each species. When you see pictures of fish, or just a few fish at a time, they don’t look that different. But looking at so many all at once, I really saw how some have brighter colors, or fatter bodies or bigger spots. But only for a moment, because the fish just kept coming and coming and coming!
Finally, the fish were sorted and I headed to my station, where TK, the cutter that I have been working with, had already started processing some of the huge pollock that we had caught. I helped him maneuver them up onto the lengthing board so that he could measure them and take samples, and we fell into a fish-measuring groove that lasted for two hours. Grab a fish, take the length, print a label and put it on an envelope, slip the otolith into the envelope, examine the stomach contents, repeat.
Cod, pollock and haddock in baskets waiting to get counted and measured. Photo by Watch Chief Adam Poquette.
Some of you have asked about the fish that we have seen and so here is a list of the species that we saw at just this one site:
Pollock
Haddock
Atlantic wolffish
Cod
Goosefish
Herring
Mackerel
Alewife
Acadian redfish
Alligator fish
White hake
Red hake
American plaice
Little skate
American lobster
Sea raven
Thorny skate
Red deepsea crab
Atlantic Herring
Goosefish. Does this remind you of anyone you know?
Mackerel. Possibly the best looking fish in the sea.
I think it’s human nature to try to draw conclusions about what we see and do. If all we knew about the state of our fish populations was based on the data from this one catch, then we might conclude that there are tons of healthy fish stocks in the sea. However, I know that this is just one small data point in a literal sea of data points and it cannot be considered independently of the others. Just because this is data that I was able to see, touch and smell doesn’t give it any more validity than other data that I can only see as a point on a map or numbers on a screen. Eventually, every measurement and sample will be compiled into reports, and it’s that big picture over a long period of time that will really allow give us a better understanding of the state of affairs in the ocean.
Sunset from the deck of the Henry B. Bigelow
Personal Log
Lunges are a bit more challenging on the rocking deck of a ship!
It seems like time is passing faster and faster on board the Bigelow. I have been getting up each morning and doing a Hero’s Journey workout up on the flying bridge. One of my shipmates let me borrow a book that is about all of the people who have died trying to climb Mount Washington. Today I did laundry, and to quote Olaf, putting on my warm and clean sweatshirt fresh out of the dryer was like a warm hug! I am getting to know the crew and learning how they all ended up here, working on a NOAA ship. It’s tough to believe but a week from today, I will be wrapping up and getting ready to go back to school!
NOAA Teacher at Sea
Theresa Paulsen
Aboard NOAA Ship Okeanos Explorer
March 16-April 3rd
Mission: Caribbean Exploration (mapping) Geographical Area of Cruise: Puerto Rico Trench Date: April 2, 2015
Weather Data from the Bridge: Partly Cloudy, 26 C, Wind speed 12 knots, Wave height 1-2ft, Swells 2-4ft.
Science and Technology Log:
What are the mappers up to?
After we completed our two priority areas of the cruise, the mappers have been using Knudson subbottom sonar to profile the bottom of the trench. Meme Lobecker, the expedition coordinator sends that data directly to the United States Geological Survey (USGS) for processing. They returned some interesting findings.
The subbottom sonar sends a loud “chirp” to the bottom. It penetrates the ocean floor. Different sediment layers reflect the sound differently so the variation and thickness of the layers can be observed. The chirp penetration depth varies with the sediments. Soft sediments can be penetrated more easily. In the picture below, provided by USGS, you can see hard intrusions with layers of sediments filling in spaces between.
The intrusions are basement relief, likely uplifting deformation ridges created by the subduction of the North American Plate. The subduction is now oblique, with the North American and Caribbean plates mostly sliding past each other now – sort of like the San Andreas Fault – but there is still some subduction happening. Subbottom Image and caption courtesy of USGS.
How does the bathymetry look?
In the last two days, I have been really enjoying the incredible details in the bathymetry data the multibeam sonar has gathered. We mapped over 15,000 square miles on our voyage! Using computer software we can now look at the ocean floor beneath us. I tried my hand at using Fledermaus software to make fly-over movies of the area we surveyed (or should I say swim-over movies). Check them out:
I also examined some of the backscatter data. In backscatter images soft surfaces are darker, meaning the signal return is weaker, and the hard surfaces are whiter due to stronger returns. One of the interns, Chelsea Wegner, studied the bathymetry and backscatter data for possible habitats for corals. She looked for steep slopes in the bathymetry and hard surfaces with the backscatter, since corals prefer those conditions.
On the next leg, the robotic vehicle on the ship will be used to examine some of the areas we were with high-definition cameras. You can watch the live stream here. You can also see some of the images and footage from past explorations here.
This is a short video from the 2012 expedition to the Gulf of Mexico to tempt you into tuning in for more.
Personal Log:
The people on this vessel have been blessed with adventurous spirits and exciting careers. Throughout the cruise, I heard about and then came to fully understand the difficulty of being away from family when they need us.
I would like to dedicate this last blog to my father, Tom Wichman. He passed away this morning at 80 years of age after battling more than his share of medical issues. As I rode the ship in today I felt him beside me. Together we watched the pelicans and the boobies fly by. I am very glad I was able to take him on a “virtual” adventure to the Caribbean. He loved the pictures and the blog. I thank the NOAA Teacher at Sea program for helping me make him proud one last time.
My Parents, Tom and Kate Wichman
“To know how to wonder is the first step of the mind toward discovery” – L. Pasteur. These words decorate my classroom wall but are epitomized by the work that the NOAA Okeanos Explorer and the Office of Exploration and Research (OER) do each day.
Thank you to the Meme, the CO, XO, the science team, and the entire crew aboard the Okeanos for teaching me as much as you did and for helping me get home when I needed to be with family. I wish you all the best as you continue to explore our vast oceans! My students and I will be watching and learning from you!
I would also like to thank all of the people who followed this blog. Your support and interest proves that you too are curious by nature. Life is much more interesting if you hold on to that sense of wonder, isn’t it?
Answers to My Previous Questions of the Day Polls:
1. Bathymetry is the study of ocean depths and submarine topography.
2. The deepest zone in the ocean is called the hadal zone, after Hades the Greek God of the underworld.
3. It takes the vessel 19 hours and 10 minutes to make enough water for 46 people each using 50 gallons per day if each of the two distillers makes 1 gallon per minute.
NOAA Teacher at Sea Theresa Paulsen Aboard NOAA Ship Okeanos Explorer March 16-April 3rd
Mission: Caribbean Exploration (Mapping) Geographical Area of Cruise: Puerto Rico Trench Date: April 1, 2015
Weather Data from the Bridge: Partly Cloudy, 26˚C, waves 1-3ft, swells 3-6ft.
Science and Technology Log:
Dr. Wilford (Bill) Schmidt has demonstrated the saying, “Where there is a will, there is a way,” throughout this entire cruise. He knew this voyage would put his new free vehicle design to the test and he came prepared to modify this, tweak that, collaborate with the crew, confer with his university team, test, and repeat. He is an engineer and that is the name of the game.
1. The first deployment looked great. The vehicle reached 1000m. The magnetometer and 3-axis accelerometer worked great. All systems were a go. A water sampling device was used as a dummy payload.
The free vehicle with a water sampling device as a dummy payload.
Data from the Test Deployment
Crossing fingers for more success.
2. The next step was to attach a CTD (a probe that measures Conductivity, Temperature, Depth). The deployment and retrieval process again went smoothly, this time to 2126m, but there was a problem retrieving the log file from the bottom sphere and one of the anchor burn wires did not burn.
The free vehicle with CTD attached.
Collaboration required with folks on shore and the electronics technicians on this ship. Tweak this, fix that.
Dave Blessing, Electronics Tech, and Bill Schmidt troubleshooting.
Bill opened the spheres to change the batteries for the satellite transponder.
One of the opened spheresZamara Fuentes keeping a log of all of the adjustments and parametersRolf Vieten pressurizing the sphere
All systems were a go again.
3. The crew deployed the free vehicle with the CTD to 4679 m. It took a little longer to find and retrieve the vehicle.
Retrieval of the free vehicle
The data files indicated that the galvanic releases released the anchor prematurely, at about 100 meters from the bottom. Both spheres worked during the mission. Data files were retrieved from each. During inspection water was found in the bottom sphere. Spalling of the glass (flaking) was seen on the inside. The leak is assumed to have taken place as the surface under low pressure conditions, otherwise the damage would have been worse. The electronics were in good shape but the bottom sphere had to be retired.
Oh no! Is that the end? Not when you have great minds on board!
This is where engineering in the ocean environment gets tricky. Bill can’t just head back to the university and make the necessary repairs. Instead he needs to make use of the very valuable ship time by pinch-hitting. Bill recalculated the buoyant force on the vehicle with only one sphere. It might just work!
Tweak this, lighten that, new attachments there. Ready for a float test!
The single sphere float test was a success!
Will the single sphere allow it to ascend from the bottom fast enough for us to deploy and retrieve it during our mission? That question required further testing. So the crew planned to lower it into the water a short distance with the winch and allow it to float back up. The weather would not allow it. The seas were too rough to allow the ship to stay in one place during the vehicle test without dragging the free vehicle thereby negating the results of the test.
Operations team meeting
Plan B? The operations team hatched a plan to tie the free vehicle to buoys on a long rope. That allowed the vehicle to sink and be recovered easily if it rose too slowly. First a buoyancy test had to be done to make sure the buoys wouldn’t sink with the vehicle.
Buoy float test
The vehicle rose in less than 10 minutes so the team was back on track! With a few extras like flags for better visibility, the vehicle was ready to dive!
Preparing for the big dive to 8000+ meters!
4. The deployment into the trench went smoothly. The crew had that routine down pat. After 10 hours it was time for the retrieval. Everyone gathered at the bridge to try to spot it.
On the lookout for the free vehicle.Port side lookoutsThe free vehicle returns from the deep!
It successfully collected data down to the bottom at 8379m, a possible record for a free vehicle!
Bill content with a successful dive
The CTD data was processed and looked great during the descent.
Free vehicle CTD data from the Puerto Rico Trench
Inspection of the data log showed that while the vehicle was ascending from the bottom, something was triggering a mission cancel order – 28 times! This bug required more testing and mission simulating before another deployment in the trench. Just after 8pm, Bill announced his equipment was ready to go for a 6 am deployment the next day.
5. The next day, the retrieval took a bit longer due to choppier sea conditions.
The crew bringing the free vehicle aboard.
Again the vehicle logs showed “cancel mission” messages during the ascent. It is confounding Bill and his team back home, because during mission simulations the mission goes to completion without a problem.
In all the voyage has been very constructive for Bill’s engineering team. They successfully deployed the vehicle to the bottom of the Puerto Rico Trench known to be the deepest part of the Atlantic Ocean. That is something to celebrate! They have learned a great deal about what types of modifications they should make to improve the retrieval process.
This was a great first test of the free vehicle design. The next time out at sea will come soon enough and Bill’s team will be ready!
Personal Log
As the voyage comes to an end and we travel nearer to shore, I am filled with mixed emotions. I will miss the ocean, the feeling of being a part of an exploration expedition, and these people. I am also very happy to be going home to my family and my students. I am looking forward to sharing what I have learned. I will be looking for partnerships to help get students involved in reseach on our inland sea, Lake Superior. If you have any suggestions, please leave a comment below!
Exciting moments? Seeing these creatures!
Small whale swimming next to the vessel.A dolphin playing in our wake. Photo credit: Jossue Millan
Other great moments include driving the ship and making video fly-bys of the ocean floor with the bathymetry and backscatter data. Very awesome! The videos will be coming soon so stay tuned!
Did you know?
Do you remember the flying fish I wondered about a few blogs ago? I have never seen them before. At first I thought I was seeing things. I thought I saw a very large dragonfly dive into the water. Then I saw more. – schools of them jumping away from the boat all at once. In a blink of an eye they were gone.
A flying fish. Image courtesy of “Bermuda: Search for Deep Water Caves 2009 Exploration,” NOAA Ocean Explorer
According to Wikipedia, there are 64 species of flying fish! They fly out of the water to evade predators. That’s a pretty cool adaptation! You can learn more here.
NOAA Teacher at Sea Theresa Paulsen Aboard NOAA Ship Okeanos Explorer March 16-April 3rd
Mission: Caribbean Exploration (Mapping) Geographical Area of Cruise: Puerto Rico Trench Date: March 29, 2015
Weather Data from the Bridge: Partly Cloudy, 26.7˚C, waves 1-3ft, swells 2-4ft.
Science and Technology Log:
We launched and recovered a CTD earlier this week.
A CTD (Conductivity, Temperature and Depth probe) is used to study the characteristics of ocean water masses, as well as to insure data quality and accuracy from XBTs (Expendible Bathythermograph). In a previous blog, I discussed how the XBT is used to measure the temperature of the water to a depth of about 760 meters. That coupled with the conductivity sensors on the vessel are used to calculate salinity and pressure to derive a measure of the velocity of sound through water, an important factor when collecting sonar data.
An XBT can be launched while the vessel is underway without pausing the sonar, but it doesn’t collect data all the way to the bottom of the water column.
Trying my hand at launching an XBT
A CTD can go all the way to the bottom, depending on the depth of the ocean, the length of the tether cable, and the pressure rating of the frame and equipment making up the CTD. The titanium frame and equipment making up the CTD currently aboard the Okeanos can be lowered to 6500 meters. It is very large and requires the vessel to stay put during the entire process since it is tethered to the ship.
Since a CTD collects all three factors involved in the computation of speed of sound in water (salinity, temperature, and depth) and is therefore more accurate than an XBT which only collects temperature, it is used at least annually to provide comparison data for the XBT measurements. This is the reason our scientists used it on this cruise. Additionally, scientists on board a vessel may want to deploy a CTD more often if water masses are expected to change, or if they are interested in studying other features of the water column such as particulates, gaseous seeps, dissolved oxygen or oxygen reduction potential, or if they want to collect water samples at different depths.
Survey Tech, Scott Allen and the CTD.
In the above photo the small red arrow is pointing to the water sample tubes, the large blue arrow to the CTD, and the large red arrow to the altimeter which senses when the probe is within 200 meters from the bottom allowing winch operators to slow the descent to avoid damaging equipment. Scott Allen is the Survey Tech on board. His job is to maintain and calibrate the CTD. He helps launch and recover the CTD and then operates the software to collect and process the data.
Our first CTD launch data.
The CTD software plots the temperature (green), sound velocity (pink), conductivity (yellow), and the salinity (blue) on the x-axes against depth on the y-axis. You can see locations on the graph where the values for temperature and salinity shift in a significant way with changes in depth. These shifts can indicate a boundary between different water masses. The upward spikes in the data are likely caused by some error in the equipment connections.
Let’s conduct an experiment!
Have you ever wondered what would happen to a styrofoam cup if you lowered into the water 2100 meters? The folks here tell me you get some pretty interesting results, so we had to give it a try.
Problem: Determine the effect of extreme pressure on a styrofoam cups.
Background: Styrofoam, properly called expanded polystyrene foam, is made by infusing air into polystyrene (a synthetic polymer) using blowing agents. Learn more here.
Hypothesis: What is your hypothesis? What do you think will happen to the air pockets if we send the cups to the depths of the ocean?
Procedure:
1. Decorate your cups, leaving one as a control for comparison after submersion.
Decorating 12 oz styrofoam cupsMore cup designs
2. Place the cups in a mesh dive bag and attach to a CTD.
Our cups are ready to dive!
3. Lower the CTD to 2100 meters
Launching the CTD
4. Raise the CTD and examine the cups.
Raising the cups and CTD
Analysis:
So how much pressure was exerted on the cups at 2100 meters? We can use this formula to calculate it:
P = pgh
Pressure in a fluid = (density of water) x (acceleration due to gravity) x (height of the fluid above the object).
If the density of seawater is 1027 kg/cubic meter, the acceleration due to gravity is 9.8 m/s/s and the depth is 2100 meters, what is the pressure?
You should get 21 million Pascals (Newtons/square meters) or 21,000 kPa. If 1 kPa = 0.145 psi, how many pounds of pressure per square inch are exerted on each cup? About 3000 pounds per square inch. That’s about the weight of a compact car over each square inch! For comparison, at sea level the atmospheric pressure is 14.7 psi.
So what happened to our cups under all that pressure? Check it out!
Our cups after a dive to 2100m. They are tiny!More shrunken cups.Showing off my shrunken cups.
Conclusion:
Was your hypothesis supported or refuted? What happened to the air trapped in the styrofoam?
Air extraction is the reason that Dr. Wilford Schmidt uses iron rebar rather than cement to provide the anchor for his free vehicles. The cement crumbles as the air pockets give way and air is squeezed out. Cement is not as flexible as the polystyrene.
The free vehicle with rebar anchor
What other materials might change under pressure? If you don’t have access to the deep ocean or a CTD, you could always try a pressure cooker – but be safe!
Personal Log:
I am inspired by all the people working on this vessel. They are so adventurous and have seen so much. I wondered what inspired them to do what they do. Here are some of their answers:
Mapping Intern, Kristin Mello: Took a class in scuba diving and realized she loved it and wanted to learn more. Her dive instructor encouraged her to do an internship as a research diver and she has been studying the ocean ever since.
Free Vehicle Tech, Zamara Fuentes: Built a model of a volcano in school became very interested in geology. Now she studies tsunami impacts on the Caribbean islands.
NOAA Corps Officer, Nick Pawlenko: Had never really spent much time on boats as a kid, but was inspired by Clive Cussler novels to explore the ocean.
Expedition Coordinator, Meme Lobecker: Her love of the oceans made her want to put her geography skills and interest in data collection to work in the ocean environment.
Engineer, Chris Taylor: Wanted to put his love of engineering to work for good pay. “There is never a dull moment,” he says.
Mapping Watch Lead, Melody Ovard: Just likes being near the ocean. “It’s a proximity thing. I am curious about what goes on in it,” she says.
Free Vehicle Scientist, Bill Schmidt: Loved surfing and was interested to learn what caused the changes in the surfing conditions day-to-day. Then he read Willard Bascom’s book, Waves and Beaches, and was hooked.
NOAA Corps Officer, Bryan Pestone: Swimming competitively and lifeguarding on the beach led him to a degree in marine biology.
Mapping Intern, Jossue Millan: An astrobiology poster caught his eye in his physics class, which peaked his interest in life in extreme environments. He enjoys the interdisciplinary sciences.
Teacher at Sea, Theresa Paulsen: I am inspired by the wonder in a kid’s eye or on a proud parent’s face and by the beauty that surrounds us from the depths of the oceans to the expanses of space. Life is amazing – and far too short to waste, so we have to make the most of it while we can.
Thanks for the inspiring conversation everyone!
What inspires you? Post a comment and let me know!
Did You Know?
For every 10 meters you go below the surface, pressure increases by one atmosphere (14.7 psi). Scuba instructors typically don’t recommend diving deeper than 40m to decrease the risk of decompression sickness, known as “the bends,” or equipment failures that could lead to drowning.
Question of the Day:
The deepest successful dive in the Guiness Book of World Records is currently 332.35 meters (1090ft)! Yikes! Read about it here.
NOAA Teacher at Sea Theresa Paulsen Aboard NOAA Ship Okeanos Explorer March 16 – April 3, 2015
Mission: Caribbean Exploration (Mapping) Geographical Area of Cruise: Puerto Rico Trench Date: March 28, 2015
Weather Data from the Bridge: Scattered Clouds, 26˚C, Wind speed 13-18 knots, Wave height 5-7ft
Science and Technology Log
Mapping of our first priority area is now compete and we have moved to the priority two area on the north side of the Puerto Rico Trench. We are more than 100 miles from shore at this point. Land is nowhere in sight. Able-Bodied Seaman Ryan Loftus tells me that even from the bridge the horizon is only 6.4 nautical miles away due to the curvature of the earth. At this point with no frame of reference other than celestial bodies, navigation equipment becomes essential.
The ship uses Global Positioning Systems, GPS units:
GPS Units aboard the vessel
Radar:
The radar display.
On the radar display, we are in the center of the circle. Our heading is the blue line. Since this photo was taken near shore, the yellow patches on the bottom indicate the land mass, Puerto Rico. The two triangles with what look like vector lines to the left of us are approaching vessels. On the right, the Automated Identification System displays information about those vessels, including their name, type, heading and speed. The radar uses two radio beams, an S-Band at 3050 MHz and an X-band at 9410 MHz, to determine the location of the vessel relative to other vessels and landmarks within a 1% margin of error.
Gyrocompasses:
A gyrocompass
A standard compass points to the magnetic north pole rather than true north, therefore mariners prefer to use gyrocompasses for navigation. Before departing, a gyrocompass is pointed to true north. Using an electric current, the gyroscope in the device is spun very fast so that it will continually maintain that direction during the voyage. Slight errors build up over time and must be corrected. The watch standers post the necessary correction on the bridge. Since the device is electronic, it can feed data into the system allowing for automated navigation and dynamic positioning systems to work well.
The Electronic Chart Display Information System (ECDIIS) Screen
On the Electronic Chart Display Information System (ECDIS) screen, watchstanders can view the course planned by the Expedition Coordinator in charge of the science conducted on the voyage (in red), see the bearing they have set (thin black line), and see the actual course we are on (the black, dashed, arrowhead line).
The Dynamic Positioning System
The dynamic positioning system allows the vessel to remain in one spot in very delicate situations, such as when they lower a tethered device like the robotic vehicle they will be using on the next cruise or a CTD (Conductivity, Temperature and Depth probe). It is also helpful for docking.
The electronics are able to control the ship due to the ingenious way the engine system is designed. The diesel engine powers generators that convert the mechanical energy into electrical energy. This way electrical energy can be used to control main hydraulic propellers at the stern as well as electric bow and side thrusting propellers.
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What happens if the power goes out and the electronic navigation devices fail? There are back ups – no worries, students and family!!
The vessel can sail onward. It is equipped with a magnetic compass and the watchstanders are well versed in reading charts, using a sextant, and plotting courses by hand – they often do that just to check the radar and GPS for accuracy.
The superimposed red arrow is directing your attention to the magnetic compass above the bridge.Operations Officer, Lt. Emily Rose cross checking the radar and GPS with nautical charts.Seaman Ryan Loftus teaching me how to use a sextant.
They also have a well-used copy of the “bible of navigation,” The American Practical Navigator written in 1802 by Nathaniel Bowditch.
The American Practical Navigator, The “Bible” of navigation for over 200 years.
They even let me take it for a spin – okay it was about a 90˚ turn – but hey, it feels pretty cool to be at the helm of a 224ft vessel!
Steady as she goes! Mrs. Paulsen’s at the helm!
So where are we right now?
As I said we have begun mapping in our second priority zone, more than 100 miles north of Puerto Rico. We are near the boundary of the Sargasso Sea. It is not bordered by land, like other seas. Instead it is bordered by ocean currents that keep the surface water in one area.
The Sargasso Sea. Image Credit: US Fish and Wildlife Service
Remember the seaweed I wondered about in an earlier post? It is called Sargassum. It grows in rafts in the Sargasso Sea. This is actually where the Sargasso sea got its name. According to NOAA’s National Ocean Service, these rafts provide habitat for certain fish and marine life. Turtles use them as nurseries for their hatchlings. In recent years large blooms of Sargassum have been washing up on nearby coastlines causing problem along the shore. (Oct 1, 2014, USA Today) More research needed! There are always more questions. Is this caused by warming oceans, by oil spills, or by a combination? Nothing lives in isolation. All life forms are connected to each other and to our environment. Changes in the ocean impact us all, everywhere on the globe.
A Sargassum Mat. Photo courtesy of NOAA.
Want to explore yourself? Check out NOAA Corps to become ship officer!
Acting Executive Officer (XO) Lieutenant Fionna Matheson is augmenting on this leg of the trip, meaning she is filling in for the XO currently on leave. Otherwise, in her current “land job” she works at NOAA headquarters for the NOAA Administrator, Dr. Kathryn Sullivan. Dr. Sullivan, a former astronaut and the first American woman to walk in space, reports to the Secretary of Commerce, Penny Pritzker. Working on the headquarters team, LT Matheson learns a great deal about the breadth and importance of NOAA’s mission.
Lt. Fionna Matheson
To become a member of the NOAA Corps you must have a Bachelor’s degree in Science or Math. It is a competitive process, so some sort of experience with boating is advantageous, but not required. NOAA Corps officers are trained not only to drive and manage ships, but also to handle emergencies including fire-fighting, and follow maritime law. They act as the glue between the scientists and the crew (wage mariners), making sure the scientific mission is accomplished and the safety of the crew and the vessel are secure. Fionna has been part of the corps for 11 years. She explains that NOAA Corps officers are stationed for about 2 years at sea (with some shore leave) followed by 3 years on land throughout their careers. During her NOAA career, Fionna has sailed in the tropical Pacific maintaining deep-ocean buoys, fished in the North Atlantic, collected oceanographic samples in the Gulf of Mexico, and now mapped part of the Caribbean. She has also worked as part of an aerial survey team in San Diego, studying whales and dolphins.
Fionna’s advice to high school students is this, “The difference between who you are and who you want to be is action. Take the initial risk.”
Personal Log
What do we do for fun in our free time?
We read.
Jason Meyer, Mapping Watch Lead, reading on the Okeanos during his off hours.
We play games like chess, although I am not very good. I try, and that is what is important, right?
Chief Steward Dave Fare and CO Mark Wetzler playing a warm up game before the chess tournament.
We watch movies – even watched Star Trek on the fantail one evening. Very fitting since we are boldly going where no one has gone before with our high-resolution sonar.
Movie night on the fantail.
And we watch the sun go down on the ocean.
A view from the fantail of the ship.
Mostly, I like watching the water when I have time. I would have made a great lookout – I should look into it after I retire from teaching. I have been trying to use my Aquaman powers to summon the whales and dolphins, but so far – no luck. Maybe on the way back in to shore we’ll catch another glimpse.
What do I miss?
My family and friends. Hi Bryan, Ben, Laura, Dad, Mom, and the rest of the gang.
My family
And my students and coworkers. Go Ashland Oredockers!
Ashland Public Schools, Ashland, Wi
I am fortunate to have such supportive people behind me! Thanks, guys!
I do not miss snow and cold weather, so if you all could warm it up outside in northern Wisconsin over the next week, I’d appreciate it. I’ll see what kind of strings I can pull with these NOAA folks! ¡No me gusta la nieve o el frío en la primavera!
Did you know?
Sky conditions on the bridge are determined by oktas. An okta is 1/8th of the sky. If all oktas are free of clouds the sky is clear. If 1-2 oktas contain clouds, the bridge reports few clouds, 3-4 filled oktas equal scattered clouds, 5-7 equal broken clouds, and 8 filled oktas means the sky is overcast.
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