Long-Term Ecological Research – Page 5 – NOAA Teacher at Sea Blog

September 15, 2018October 4, 2018

Mark Van Arsdale: What Makes Up an Ecosystem? Part III – Zooplankton, September 15, 2018

NOAA Teacher at Sea

Mark Van Arsdale

Aboard R/V Tiglax

September 11 – 26, 2018

Mission: Long Term Ecological Monitoring

Geographic Area of Cruise: North Gulf of Alaska

Date: September 15, 2018

Weather Data from the Bridge

Mostly cloudy, winds southerly 20 knots, waves to eight feet

57.56 N, 147.56 W (in transit from Gulf of Alaska Line to Kodiak Line)

Science Log

What Makes Up an Ecosystem? Part III Zooplankton

The North Gulf of Alaska Long-term Ecological Research Project collects zooplankton in several different ways. The CalVET Net is dropped vertically over the side of the boat to a depth of 100 meters and then retrieved. This net gives researchers a vertical profile of what is going on in the water column. The net has very fine mesh in order to collect very small plankton. Some of these samples are kept alive for later experiments. Others are preserved in ethanol for later genetic analysis. One of the scientists aboard is interested in the physiological details of what makes copepods thrive or not. Copepods are so important to the food webs of the Gulf of Alaska, that their success or failure can ultimately determines the success or failure of many other species in the ecosystem. When “the blob” hit the Gulf of Alaska in 2014-2016, thousands and thousands of sea birds died. During those same years, copepods were shown to be less successful in their growth and egg production.

Chief Scientist Russ Hopcroft prepping the Multi-net

The second net used to collect zooplankton is the Multi-net. We actually use two different Multi-nets. The first is set up to do a vertical profile. In the morning, it’s dropped vertically behind the boat. Four or five times a night, we tow the second Multi-net horizontally while the boat moves slowly forward at two knots. This allows us to collect a horizontal profile of plankton at specific depths. If the water depth is beyond 200 meters, we will lower the net to that depth and open the first net. The first net samples between 200 and 100 meters, above 100 meters we open the second net. As we go up each net is opened in decreasing depth increments, the last one being very close to the surface. Once the net is retrieved, we wash organisms down into the cod end, remove the cod end, and preserve the samples in glass jars with formalin. In a busy night, we may put away twenty-five pint-sized samples of preserved zooplankton. When those samples go back to Fairbanks they have to be hand-sorted by a technician to determine the numbers and relative mass of each species. We are talking hours and hours of time spend looking through a microscope. One night of work on the Tiglax may produce one month of work for technicians in the lab.

Underwater footage of a Multi-net triggering.

The last type of net we use is a Bongo net. Its steel frame looks like the frame of large bongo drums. Hanging down behind the frame is two fine mesh nets, approximately seven feet long terminating in a hard plastic sieve or cod end. Different lines use different nets based on the specific questions researchers have for that transect line or the technique used on previous years transects. To maintain a proper time series comparison from year to year, techniques and tools have to stay consistent.

I’ve spent a little bit of time under the microscope looking at some of the zooplankton samples we have brought in. They are amazingly diverse. The North Gulf of Alaska has two groups of zooplankton that can be found in the greatest abundance: copepods and euphausiids (krill.) These are food for most other animals in the North Gulf of Alaska. Fish, seabirds, and baleen whales all eat them. Beyond these two, I was able to observe the beating cilia of ctenophores and the graceful flight of pteropods or sea angels, the ghost-like arrow worms, giant-eyed amphipods, and dozens of others.

Deep sea squid, an example of a vertical migrator caught in our plankton trawls

By far my favorite zooplankton to watch under the microscope was the larvae of the goose neck barnacle. Most sessile marine organisms spend the early, larval stage of their lives swimming amongst the throngs of migrating zooplankton. Barnacles are arthropods, which are defined by their exoskeletons and segmented appendages. Most people would recognize barnacles encrusting the rocks of their favorite coastline, but when I show my students videos of barnacles feeding most are surprised to see the delicate feeding structures and graceful movements of this most durable intertidal creature. When submerged, barnacles open their shells and scratch at particles in the water with elongated combs that are really analogous to legs. The larva of the goose neck barnacle has profusely long feeding appendages and a particularly beautiful motion as it feeds.

We have to “fish” for zooplankton at night for two reasons. The first is logistical. Some work needs to get done at night when the winch is not being used by the CTD team. The second is biological. Most of the zooplankton in this system are vertical migrators. They rise each night to feed on phytoplankton near the surface and then descend back down to depth to avoid being seen in the daylight by their predators. This vertical migration was first discovered by sonar operators in World War II. While looking for German U-boats, it was observed that the ocean floor itself seemed to “rise up” each night. After the war, better techniques were developed to sample zooplankton, and scientists realized that the largest animal migration on Earth takes place each night and each morning over the entirety of the ocean basins.

One of my favorite videos on plankton.

Personal Log

The color of water

This far offshore, the water we are traveling through is almost perfectly clear, yet the color of the ocean seems continuously in flux. Today the sky turned gray and so did the ocean. As the waves come up, the texture of the ocean thickens and the diversity of reflection and refraction increases. Look three times in three directions, and you will see three hundred different shades of grey or blue. If the sun or clouds change slightly, so does the ocean.

The sea is anything but consistent. Rips or streaks of current can periodically be seen separating the ocean into distinct bodies. So far in our trip, calm afternoons have turned into windy and choppy evenings. Still, the crew tells me that by Gulf of Alaska standards, we are having amazing weather.

Variations in water texture created by currents in the Gulf of Alaska.

Did You Know?

The bodies of puffins are much better adapted to diving than flying. A puffin with a full belly doesn’t fly to get out of the way of the boat so much as butterfly across the surface of the water. Michael Phelps has nothing on a puffin flapping its way across the surface of the water.

Animals Seen Today

Fin and sperm whales in the distance
Storm Petrels, tufted puffins, Laysan and black-footed and short-tailed albatross, flesh footed shearwaters

September 14, 2018October 4, 2018

Mark Van Arsdale: What Makes Up an Ecosystem? Part II – Phytoplankton, September 14, 2018

NOAA Teacher at Sea

Mark Van Arsdale

Aboard R/V Tiglax

September 11 – 26, 2018

Mission: Long Term Ecological Monitoring

Geographic Area of Cruise: North Gulf of Alaska

Date: September 14, 2018

Weather Data from the Bridge

Mostly cloudy, winds variable 10 knots, waves to four feet

58.27 N, 148.07 W (Gulf of Alaska Line)

Science Log

What Makes Up an Ecosystem? Part II Phytoplankton

Most of my students know that the sun provides the foundational energy for almost all of Earth’s food webs. Yet many students will get stumped when I ask them, where does the mass of a tree comes from? The answer of course is carbon dioxide from the air, but I bet you already knew that.

Scientists use the term “primary productivity” to explain how trees, plants, and algae take in carbon dioxide and “fix it” into carbohydrates during the process of photosynthesis. Out here in the Gulf of Alaska, the primary producers are phytoplankton (primarily diatoms and dinoflagellates). When examining diatoms under a microscope, they look like tiny golden pillboxes, or perhaps Oreos if you are feeling hungry.

Primary productivity experiments running on the back deck of the Tiglax.

One of the teams of scientists on board is trying to measure the rates of primary productivity using captive phytoplankton and a homemade incubation chamber. They collect phytoplankton samples, store them in sealed containers, and then place them into the incubator. Within their sample jars, they inject a C₁₃ isotope. After the experiment has run its course, they will use vacuum filtration to separate the phytoplankton cells from the seawater. Once the phytoplankton cells are captured on filter paper they can measure the ratios of C₁₂to C_13. Almost all of the carbon available in the environment is C₁₂and can be distinguished from C₁₃. The ratios of C₁₂ to C₁₃ in the cells gives them a measurement of how much dissolved carbon is being “fixed” into sugars by phytoplankton. Apparently using C₁₄ would actually work better but C₁₄ is radioactive and the Tiglax is not equipped with the facilities to hand using a radioactive substance.

During the September survey, phytoplankton numbers are much lower than they are in the spring. The nutrients that they need to grow have largely been used up. Winter storms will mix the water and bring large amounts of nutrients back to the surface. When sunlight returns in April, all of the conditions necessary for phytoplankton growth will be present, and the North Gulf of Alaska will experience a phytoplankton bloom. It’s these phytoplankton blooms that create the foundation for the entire Gulf of Alaska ecosystem.

Personal Log

Interesting things to see

The night shift is not getting any easier. The cumulative effects of too little sleep are starting to catch up to me, and last night I found myself dosing off between plankton tows. The tows were more interesting though. Once we got past the edge of the continental shelf, the diversity of zooplankton species increased and we started to see lantern fish in each of the tows. Lantern fish spend their days below one thousand feet in the darkness of the mesopelagic and then migrate up each night to feed on zooplankton. The have a line of photophores (light producing cells) on their ventral sides. When they light them up, their bodies blend in to the faint light above, hiding their silhouette, making them functionally invisible.

A lantern fish with its bioluminescent photophores visible along its belly.

Once I am up in the morning, the most fun place to hang out on the Tiglax is the flying bridge. Almost fifty feet up and sitting on top of the wheelhouse, it has a cushioned bench, a wind block, and a killer view. This is where our bird and marine mammal observers work. Normally there is one U.S. Fish and Wildlife observer who works while the boat is transiting from one station to the next. On this trip, there is a second observer in training. The observers’ job is to use a very specific protocol to count and identify any sea bird or marine mammal seen along the transect lines.

Today we saw lots of albatross; mostly black-footed, but a few Laysan, and one short-tailed albatross that landed next to the boat while were casting the CTD. The short-tailed albatross was nearly extinct a few years ago, and today is still considered endangered. That bird was one of only 4000 of its species remaining. Albatross have an unfortunate tendency to follow long-line fishing boats. They try to grab the bait off of hooks and often are drowned as the hooks drag them to the bottom. Albatross are a wonder to watch as they glide effortlessly a few inches above the waves. They have narrow tapered wings that are comically long. When they land on the water, they fold their gangly wings back in a way that reminds me of a kid whose growth spurts hit long before their body knows what to do with all of that height. While flying, however, they are a picture of grace and efficiency. They glide effortlessly just a few inches above the water, scanning for an unsuspecting fish or squid. When some species of albatross fledge from their nesting grounds, they may not set foot on land again for seven years, when their own reproductive instincts drive them to land to look for a mate.

Our birders seem to appreciate anyone who shares their enthusiasm for birds and are very patient with all of my “What species is that?” questions. They have been seeing whales as well. Fin and sperm whales are common in this part of the gulf and they have seen both.

A Laysan Albatross, photo credit Dan Cushing

Did You Know?

Albatross, along with many other sea birds, have life spans comparable to humans. It’s not uncommon for them to live sixty or seventy years, and they don’t reach reproductive maturity until well into their teens.

Animals Seen Today

Fin and sperm whales
Storm Petrels, tufted puffins, Laysan and black-footed and short-tailed albatross, flesh footed shearwater

September 13, 2018October 4, 2018

Mark Van Arsdale: What Makes Up an Ecosystem? Part I – Chemistry, September 13, 2018

NOAA Teacher at Sea

Mark Van Arsdale

Aboard R/V Tiglax

September 11 – 26, 2018

Mission: Long Term Ecological Monitoring

Geographic Area of Cruise: North Gulf of Alaska

Date: September 13, 2018

Weather Data from the Bridge

Clear skies, variable winds, swell 4-6 ft

59.58 N, 148.38 W (Gulf of Alaska Line)

Science Log

What Makes Up an Ecosystem? Part I Chemistry

CTD (water chemistry) data visualized along the Gulf of Alaska Line.

The scientists aboard this ship are trying to understand the working parts of the North Gulf of Alaska ecosystem. Since Descartes, the western approach to science has required that the understanding of complex systems begin with the reduction of a system it to its simpler working parts. For example, to understand the clock, you must take it apart and try to understand the mechanism of each piece separately. The Gulf of Alaska is huge, and its ecosystem is both highly complex and highly variable. Changes take place because of weather, season, and climactic regime. Nonetheless, the first step to understanding it is to understand its chemistry.

The CTD gets dropped or “cast” at each station. On this boat, that means four people shoving it out the back door while trying not to fall out themselves. There is more than $100,000 worth of equipment attached to the CTD Rosette and there is a moment in each cast where the CTD swings precariously before the winch lowers it down into the water. When the CTD comes back up, all of that data is run through a computer and it paints a picture of what conditions are like at depth.

Inside the "van" where water samples are processed for trace medals — Inside the “van” where water samples are processed for trace medals

CTD stands for conductivity, temperature, depth. In reality, it tests for those things plus salinity, dissolved oxygen, nitrates, pressure, and florescence (which is a measurement of the chlorophyll in phytoplankton). The CTD also has a camera onboard that takes gray-scale images of particles and plankton in the water column as it goes down. Most of our CTD “casts” are showing a water column that is highly stratified, with a surface layer that is relative warm (34^o Celsius), lower salinity, and a chlorophyll maximum around twenty meters. The CTD shows a thermocline (rapid change in temperature) around fifty meters. Below that, the water is colder and has a higher salinity, both of which results in water with a higher density. The density differences between these two layers make it so that they don’t easily mix. The stratification effect had been intensified by the recent stretch of sunny weather and light winds. Stratification by density “traps” phytoplankton at the surface in waters ideal for photosynthesis except that in September, the availability of nutrients needed for growth is quite low. Nitrates, nitrites, and silica have been used up by growing phytoplankton earlier in the summer and their absence now limits growth.

Catch from a Multi-net, mostly small euphausiids (krill)

We have scientists on board measuring the surface waters for trace metals – iron in particular. It’s a common joke on board that the smaller the subject you study, the greater the equipment needs. Whale watchers just need binoculars but the chemists have their own lab set up inside a twenty-foot shipping container or “van” strapped to the top deck. The metals team drags a missile shaped device along the side of the boat known as an “iron fish.” The iron fish, is connected to a long plastic tube and pump that provides them a constant stream of surface water. Samples are continuously collected and frozen for later analysis back in Fairbanks. Months of work will be required to process all of the samples collected on this trip.

Our plankton catches were much less variable last night. The Multi-net caught almost exclusively small euphausiids (krill.) The Methot net caught four kinds of jellies, including one moon jelly that the jelly expert was very excited about – perhaps a species not described in Alaska before. The Methot net also caught a lot of small fishes swimming at the surface. One of which was the three-spine stickleback. This was exciting for me because the three-spine stickleback is a species we use in my AP Biology class as an easy to understand and highly local example of natural selection. The three-spine stickleback is a small fish, around 1 inch in size, found in both fresh and saltwater. In saltwater, they have three large spines that discourage predators from eating them. Out here in the ocean, the spines give the fish a selective advantage. During the last ice age, some sticklebacks were trapped in fresh water ponds and lakes in South Central Alaska. There, they underwent a change. The spines which were such a great defense in the ocean were a disadvantage to them in freshwater. Aggressive dragonfly larva use the spines like handles to grab the small fish and eat them. Over time there was a selective advantage to have smaller spines, and today freshwater sticklebacks have greatly reduced pelvic spines as compared to their saltwater cousins. Natural selection did not design a better fish, it simply picked which variants were more likely to survive and reproduce in its environment.

Personal Log

Cetacean acoustic recording buoy recovered by the Tiglax.

My second night shift was not any easier, but it was more pleasant. Just before sunset, we took a slight detour from our transect line to recovery a buoy for a scientist from Scripps Institution of Oceanography. An acoustic recorder, designed to count whales by their unique calls, it had been deployed a year earlier in 900 meters of water. The crew had onboard a device that would talk to the buoy and signal it to release from its mooring. It took about a half an hour, but eventually there we saw it bobbing at the surface. Luckily the seas were pretty calm, and we were able to pull it through the side door.

The seas and weather continue to be excellent. Last night we were treated to a display of the aurora around 3:30 AM. It was so calm and so quiet that at one point, we could hear whales breathing around us. Both served as distractions to the routine of net deployment, net retrieval, sample containment, repeat.

As we traveled the ten nautical miles between stations, the flood lights on the front deck were turned off and I would sit down to watch the stars. To ancient mariners, the clear night sky was a map that could direct you across an ocean. It made me think of the Polynesian navigators tracking their small canoes across the Pacific. It also made me think about Ptolemy, who thought the Earth was encased in a perfect glass sphere with stars painted along its interior. I could see how you would think of such a sky as art.

Did You Know?

Did you know the Earth is round? It seems silly to have to say, but as a science teacher, the battle against the fantasies and fallacies of the Internet are never ending. Last year was the first year in twenty-one years of teaching that I was challenged by a student to prove to him that the Earth is round, and it happened twice. So here goes. On a boat in the Gulf of Alaska on a clear day, you know the Earth is round because as you move slowly away from the mountains, they disappear from the bottom up. By the end of the day we had traveled far enough from shore that we saw just the snow-covered tips of mountain peaks.

Sunset, it must be time to go to work. — Sunset with the mountains receding in the background, it must be time to go to work.

Animals Seen Today

Dall porpoise
Lots of seabirds including black-footed and Laysan albatross, sooty shearwater, puffins and fulmars.

September 13, 2018October 4, 2018

Mark Van Arsdale: Night Work, September 12, 2018

NOAA Teacher at Sea

Mark Van Arsdale

Aboard R/V Tiglax

September 11 – 26, 2018

Mission: Long Term Ecological Monitoring

Geographic Area of Cruise: North Gulf of Alaska

Date: September 12, 2018

Weather Data from the Bridge

Partially Cloudy, Variable Winds, Seas to 3ft

59.43 N, 149.21 W (Gulf of Alaska Line)

Science Log

Night Work

Most of day one was spent loading, sorting, unpacking, and storing gear. Scientists do not travel light. There were more action packers on board than I have ever seen in once place. At midday, we had a safety training, which consisted of learning how to put on a survival suit and how to use the coffee machine without flooding the galley. For night work, I was assigned a mustang float coat, a water activated flash light, and satellite locator, so that they could find my body if I went overboard.

After dinner, work shifted to putting together various nets and the CTD which I will describe in more detail later. We got underway at about 8:00 PM, just as the sun was setting. I slept for an hour and was woken at 10:30 to begin my shift doing zooplankton tows.

The first tow uses a Methot net, which is a large square steel frame attached by d-rings to a heavy mesh net, ten meters long. The net ends in a plastic sieve tube called a “cod end” that keeps any jellies from escaping. The net is quite heavy, and it takes four of us to guide it as a crane raises it off of the deck and then lowers it over the side. The net is dragged at the surface for twenty minutes. In the darkness of night, it glows slightly green as ctenophores and other bioluminescent jellies smash into it.

Dave demonstrating the proper technique for putting on a survival suit

After the Methot net is retrieved and secured on deck, we leave the collected jellies for a few minutes to go deploy the next net, called a Multi-net. The Multi-net is a steel box about the size of a dishwasher with a funnel entrance and five separate fine-mesh nets hanging off of the back. The net also has a heavy “fish fin” that acts to drag it down and keep it moving straight. The four of us work the net to the edge of the boat, open the back gate, and use two winches to lower it overboard. Once in the water and if the bottom depth allows it, the Multi-net gets dropped to a depth of two hundred meters and the first net is opened. The Multi-net allows you to “carve up the water column.” Each net can be triggered remotely to open and collect a horizontal sample of zooplankton at a specific depth. The electronics also allow you to measure how much water volume flows through the net. Each net is about two meters long, made of a fine mesh that funnels plankton into a soft sieve or “cod end”. While the Multi-net is “fishing,” we sort, classify, and measure the jellies collected in the Methot net tow.

The Seward Line Transect is made up of fifteen stops or stations. Each one designated as GAK1, GAK2, etc. Once we finish sampling a station, the boat speeds up and drives us ten nautical miles to the next station. Last night we managed to sample four stations, finishing the last one just as the sun rose around 7:00 AM. When daylight comes, the Tiglax makes its way back to the place the night shift began. All of the day-time sampling has to be done at each of the stations we sampled the night before. The day-time sampling uses different tools, the main tool being the CTD Rosette Sampler. The Rosette is a steel cage with water collecting “Niskin Bottles” and lots of other instrumentation strapped into the cage. There are fifteen bottles and each is triggered by computer to close at a specific depth. This allows the scientists on board to measure a variety of physical and chemical properties of the water at depth.

Personal Log

The night shift was surprisingly dark. That may sound obvious, but after a long Alaskan summer, with campfires and hikes that often went past midnight in perfect daylight, dark is an adjustment. The night was beautiful and warm, but the work of deploying and retrieving nets was tedious and physical. By morning I was exhausted, but I was reminded repeatedly that there are no cutting corners. No matter how tired you get, each sample needs to be meticulously cared for.

After the sun came up, I forced myself to eat some breakfast and then I fell in bed for a hard sleep. I could only stay there for a couple hours before my well-trained, morning-self wanted to greet the day. The day was flawless, picture-perfect, sunny and calm, the kind of days you don’t often seen in the stormy Gulf of Alaska.

Animals Seen Today

Dall Porpoise
Lots of seabirds, including black-legged kittiwakes, pelagic cormorants, and sooty and flesh-footed shearwaters.

Shearwater taking off, photo credit Callie Gesmundo

September 7, 2018September 7, 2018

Mark Van Arsdale: Flexibility, September 5, 2018

NOAA Teacher at Sea

Mark Van Arsdale

Aboard R/V Tiglax

September 11 – 27, 2018

Mission: Long-Term Ecological Research in the North Gulf of Alaska, aka The Seward Line Transects

Geographic Area of Cruise: North Gulf of Alaska

Date: September 5, 2018

Latitude: 61.3293° N
Longitude: 149.5680° W
Air Temperature: 60° F
Sky: Clear

Logistics Log

When I read the instructions for my application to NOAA Teacher at Sea, they emphasized the necessity for flexibility. Alaskans, in my mind, epitomize flexibility. The climate demands it. When the weather changes, you have to adjust to it. Not doing so can put you or others at risk.

My original cruise should have departed this weekend into the Bering Sea, but NOAA Ship Oscar Dyson developed problems with its propulsion system. Rather than sailing this research cruise, she will be in Kodiak under repair. I was pretty bummed when I got the news, but I really feel for all of those PhD students whose thesis projects needed the data from that trip.

The wonderful folks at NOAA told me that they were working on a new assignment, most likely in Southeastern US. I tried to wait patiently, but I was thinking about how much I wanted to teach Alaskan kids about the ocean just a few miles from them. Meanwhile, I had to cancel my substitute teacher. My sub has done some biological fieldwork, and when I talked to him he was very understanding. The funny thing was I got an email from his wife the next day, saying that she might have a berth for me. It turns out she works for the North Pacific Research Board and was familiar with most of the fisheries and ecological research going on in coastal Alaska. The berth was on the R/V Tiglax (TEKH-lah – Aleut for eagle). The Tiglax is not a NOAA vessel. It is owned by U.S. Fish and Wildlife Service and operated jointly by the National Science Foundation. NOAA Teacher at Sea does occasionally partner with other organizations. After a few days of waiting, I was told that this cruise met the NOAA Teacher at Sea criteria.

Bringing an end to my long logistical story, I leave Monday on a trip into the Gulf of Alaska for seventeen days aboard the Tiglax.

Science Log

The science behind my new project is pretty exciting. The Seward Line Transects have been run every summer since 1997 – every May and every September. Weather permitting, we will repeat the Seward Line Transect (seen below in black) along with four other transects. Each transect begins at a near shore location and makes it past the edge of the continental shelf into the deep waters of the Pacific. At each transect station, water is collected using a CTD to test the physical and chemical properties of the water at that location. A variety of plankton collection nets will be also be deployed. One of these sampling stations (GAK-1) has been sampled continuously for plankton and water chemistry for forty-eight years, representing an incredible wealth of long term ecological data.

Here is Caitlin Smoot (who will be on board with me) talking about how Zooplankton is collected aboard the R/V Sikuliaq, another vessel that operates in the Gulf of Alaska.

Personal Log

The transect lines that make the North Gulf of Alaska Long Term Ecological Research Project

My job will be working the night shift, helping to collect plankton. I go out of my way in all of my classes to look at plankton. I even wrote a lab using diatoms to investigate a suspicious drowning death for my forensic science class. I’ve been collecting and examining freshwater plankton around my home in Eagle River, Alaska with my science classes for years, but rarely have I gotten to look at marine plankton. I’m excited to learning how plankton is collected at sea and how those collections are used to calculate relative abundance of plankton in the Gulf of Alaska from these samples.

In my classroom, I am always on the look out for how to better connect students to the science I am teaching. I’ve taught Oceanography for fifteen years but never been on an oceanographic cruise. I am hopeful this trip gives me a depth of experience that my students will benefit from.

As I get closer, I am not without some anxieties. I’m the very definition of a morning person, so working the night shift is going to be an adjustment. Just being aboard the Tiglax is going to be an adjustment. At a length of 120 feet, the Tiglax is a small research vessel with pretty limited facilities and no Internet connection. I’ve been in a lot of boats, but I don’t recall ever being beyond the sight of land. Those transect lines go way out into the ocean, and I wonder what it will feel like to be 150 miles from shore.

Did You Know?

The average depth of the ocean approaches 3,700 meters (12,000 feet.) The Seward Line transect begins in water only 100 meters deep and moves into water greater than 4000 meters in depth.