survey – NOAA Teacher at Sea Blog

June 29, 2026June 29, 2026

Jennifer Widdig: On the Front Lines of Charting, June 29, 2026

view from an upper deck of NOAA Ship Thomas Jefferson as a small launch vessel approaches for docking

NOAA Teacher at Sea

Jennifer Widdig

Aboard NOAA Ship Thomas Jefferson

June 17 – June 30, 2026

Mission: Hydrographic Survey
Geographic Area of Cruise: Lake Erie and Lake Ontario
Date: Monday, June 29, 2026

Weather Data from the Bridge

Latitude: 043^o15’N
Longitude: 077^o22’W
Sky Conditions: Sunny
Visibility: >10miles
Wind Speed: 1 knots
Dry Bulb: 19^oC
Wet Bulb: 18.5^oC

Science and Technology Log

Jen takes a selfie from the railing of a small launch vessel, angled so that we can see NOAA Ship Thomas Jefferson in the background at some distance. She wears a green hard hat and orange life vest. The sky is blue with only a few low white clouds, and the water is bright teal with some low waves. — Out on boat 2904 with NOAA Ship *Thomas Jefferson* in the background

One of the highlights of this leg was getting the opportunity to spend a day aboard survey launch 2904. Junior Officer Julian Santos served as our coxswain, while Senior Survey Technician Ali DiTommaso managed the survey equipment. It was a great opportunity to experience how NOAA conducts nearshore hydrographic surveys and to see firsthand the challenges of collecting data in shallow water.

Our mission for the day was to locate the 15-meter depth contour on our assigned survey sheet. Using the multibeam sonar, the display was configured so that anything shallower than 15 meters appeared black. As we “painted” the seafloor with the multibeam, we watched for that black boundary. Once we reached the 15-meter contour, we stopped collecting multibeam data in that area and moved on to find the next section of the contour. Eventually, we connected these sections to create a continuous 15-meter line across the sheet.

photo of a computer screen displaying multibeam data from the small launch vessel. the large portion of the screen shows the depth of the area, color coded; anything shallower than 15 m is shown in dark gray. — Multibeam data from boat 2904

After establishing the contour, we switched to side-scan sonar to survey the area shallower than 15 meters. Because side-scan sonar can cover a much wider swath of the seafloor than the multibeam, our survey lines were spaced farther apart, allowing us to efficiently search for underwater features and potential hazards. During our survey we operated the 75-meter side-scan system in water depths ranging from approximately 7 to 15 meters. We did not have the opportunity to switch to the 50-meter side-scan configuration, which is typically used in even shallower water, from about 4 to 8 meters.

phot of a computer screen displaying sidescan data. the center of the bathymetric map is a vertical black band, representing the track of the small vessel, which cannot collect data directly beneath it with the side-scan sonar. to the left and right of this band is detailed data showing the bumpy surface of the lake bottom. — Getting side-scan data from boat 2904

Working from a small survey launch requires constant multitasking. Since it was the weekend, recreational boat traffic was heavy, requiring extra vigilance while navigating and collecting data. Unlike aboard the ship, the launch crew must solve many equipment issues on their own or troubleshoot with assistance over the phone. At one point, our air conditioning stopped working. Although it certainly made for a warm day, it did not affect the safety of the operation, so we continued surveying.

view of the survey station on board a small vessel. inside the boat's cabin, facing ahead, a desk surface surrounds a single captain's chair. We can see three computer monitors. A survey tech in a purple t-shirt sits facing the computers (away from the camera.) — Ali DiTommaso manning the survey station on boat 2904

Although the surveying stops when the launch returns to the ship, the work is far from over. Every evening, the survey data is processed so it can be evaluated before the next day’s operations. During this process, the survey technicians apply the sound velocity information collected from the Sea-Bird CTD casts. Because sound travels at different speeds depending on the water’s temperature, salinity, and pressure, these measurements are essential for accurately calculating the depth of the seafloor.

The data is also corrected using the vessel’s position, motion, and orientation throughout the survey. Every pitch, roll, heave, and heading change of the launch is accounted for so the seafloor is mapped in its true position rather than being distorted by the boat’s movement. Water level corrections are also applied to account for changes in lake level during the survey.

a zoomed-in view of a nautical chart showing a portion of the southern coastline of Lake Ontario in beige and the water of the lake in blue. There are contour lines at 3 m, 5 m, 7 m drawn extending away from shore. Elsewhere, floating numbers represent depths as deep as 69 m. In a boxed off section of the chart, color coded shading indicates the depths of an entire swath surveyed by NOAA Ship Thomas Jefferson, with lime green indicating about 15 m deep and darker blue indicating about 23 m deep. — Processed data for the sheet that Boat 2904 has been working on

Once these corrections have been made, the software combines the overlapping survey lines and “smooths” the edges between them to create a continuous, high-quality map of the seafloor. Processing also helps identify any holidays, small gaps where little or no data was collected. If holidays or other data quality issues are found, the area will need to be resurveyed before the sheet can be considered complete.

survey data (shading, color coded by depth) overlaid on a section of a nautical chart of a portion of Lake Ontario. some areas are shaded in rectangles; some are wide diagonal lines showing the survey data collected as the ship transited from one place to another — Total amount of processed data for this leg of NOAA *Thomas Jefferson*

Personal Log

Jen poses for a photo with a man in a navy sweatshirt and a woman wearing a large headset over years. They are inside the cabin of the small launch vessel. — Coxswain Junior Officer Julian Santos, Senior Survey Technician Ali DiTommaso, and myself aboard boat 2904

Going out on a survey launch was one of the highlights of my time aboard NOAA Ship Thomas Jefferson. I already love being out on the water, so I knew my biggest challenge wouldn’t be seasickness but trying not to be rocked to sleep! The water was calm, with waves less than a foot high, something the crew was very thankful for, even if I secretly wouldn’t have minded a little more excitement.

After boarding 2904, we were lowered over the side of the ship. I followed Senior Survey Technician Ali DiTommaso onto the bow, where she released the locking clamps that connected us to the davit. It was fascinating to watch how smoothly the process worked and to finally experience a launch from the small boat perspective.

Jen sits at the helm of the small launch vessel, her left hand on the wheel, and turns her head to smile for a photo — Taking a turn at the wheel on boat 2904

We spent the day on the water from about 6:30 a.m. until 3:30 p.m. The launch may be much smaller than the ship, but it is surprisingly well equipped. We brought water, hot water for tea, breakfast, and snacks, and there was even a small refrigerator stocked with sandwich supplies and a microwave for lunch. It felt like a tiny floating office.

With Junior Officer Julian Santos serving as coxswain and Ali running the survey operations, I jokingly felt like the “passenger princess” for the day. While they handled the work, I had the opportunity to observe every aspect of the survey. Seeing hydrography on a smaller scale helped me better understand the process.

view from a distance of a small launch vessel approaching NOAA Ship Thomas Jefferson — Boat 2903 getting ready for recovery by NOAA Ship *Thomas Jefferson*

One of the most impressive moments came at the end of the day during recovery. Watching the coxswain carefully maneuver alongside the TJ looked effortless, but I quickly realized how much coordination is required. The engineers stand by in case there are any issues with the davit or the launch, the Bosun operates the davit, crew handle the lines, and the entire evolution is supervised by the Commanding Officer and Executive Officer. Meanwhile, the bridge monitors everything from the bridge wing to ensure the recovery is completed safely and efficiently.

view from an upper deck of NOAA Ship Thomas Jefferson of the recovery of a small launch vessel. The small vessel has pulled up alongside the large ship, and two davit arms with cables are lowering toward the boat. seven crewmembers with hard hats stand distributed around the two davits, read to help bring the small boat aboard. we can see other crewmembers watching the operation from higher decks. — Boat 2904 being recovered by the crew of NOAA Ship *Thomas Jefferson*

Before I had the chance to ride on one of the launches, I had watched them return to the ship from the deck. Seeing the boats racing across the water toward the TJ with spray flying behind them reminded me of something straight out of an old James Bond movie. They looked fast, powerful, and just a little dramatic. It felt like they were in slow motion!

Santos and Ali really made the day great, and I was lucky enough to get to tag along with them!

Did You Know?

The Great Lakes span 4,530 miles of coast and account for 21% of the world’s freshwater, with more that 30 million people relying on them for drinking water.
The nautical term “holiday” comes from the 17th century when missing a spot while painting a ship. “Were you on a holiday?” or “Do you need a holiday?”

August 13, 2018August 16, 2018

Tom Savage: Surveying the Coastline of Point Hope, Alaska, August 12, 2018

NOAA Teacher at Sea

Tom Savage

Aboard NOAA Ship Fairweather

August 6 – 23, 2018

Mission: Arctic Access Hydrographic Survey

Geographic Area of Cruise: Point Hope, northwest Alaska

Date: August 12, 2018

Weather data from the Bridge

Wind speed 8 knots
Visibility: 10 nautical miles
Barometer: 1010.5 mB
Temp: 8.5 C 47 F
Dry bulb 8 Wet bulb 6.5
Cloud Height: 5,000 ft
Type: Alto Stratus
Sea Height 2 feet

Science and Technology

Why is NOAA taking on this challenging task of mapping the ocean floor? As mentioned in an earlier blog, the ocean temperatures worldwide are warming and thus the ice in the polar regions are melting. As the ice melts, it provides mariners with an option to sail north of Canada, avoiding the Panama Canal. The following sequence of maps illustrates a historical perspective of receding ice sheet off the coast of Alaska since August 1857. The red reference point on the map indicates the Point Hope region of Alaska we are mapping.

This data was compiled by NOAA using 10 different sources. For further information as how this data was compiled visit https://oceanservice.noaa.gov/news/mar14/alaska-sea-ice.html.

The light grey indicates 0-30% Open Water – Very Open Drift. The medium grey indicates 30 – 90 % Open drift – Close Pack. The black indicates 90 – 100% very close compact.

Ships that sail this region today rely on their own ships sonar for navigating around nautical hazards and this may not be as reliable especially if the ships sonar is not properly working (it’s also problematic because it only tells you how deep it is at the ship’s current location – a sonar won’t tell you if an uncharted hazard is just in front of the ship). Prior to mapping the ocean floor in any coastal region, it requires a year of planning in identifying the exact corridors to be mapped. Hydrographers plot areas to be mapped using reference polygons overlaid on existing nautical charts. Nautical charts present a wealth of existing information such as ocean depth, measured in fathoms(one fathom is equal to six feet) and other known navigation hazards.

As mariners sail closer to the shorelines, the depth of the ocean becomes increasingly important. Because of this uncertainty in the depth, the Fairweather herself cannot safely navigate safely (or survey) close to shore. In order to capture this data, small boats called “launches” are used. There are a total of four launch boats that are housed on the boat deck of the Fairweather. Each boat can collect data for up to twelve hours with a crew of 2-5. Depending on the complexity of the area, each daily assignment will be adjusted to reasonably reflect what can be accomplished in one day by a single launch. Weather is a huge factor in the team’s ability to safely collect data. Prior to deployment, a mission and safety briefing is presented on the stern of the ship by the Operations Officer. During this time, each boat coxswain generates and reports back to the operations officer their GAR score (safety rating) based on weather, crew skills and mission complexity (GAR stands for Green-Amber-Red … green means low risk, so go ahead, amber means medium risk, proceed with caution; red means high risk, stop what you’re doing). In addition, a mission briefing is discussed outlining the exact area in which data will be collected and identified goals.

Safety Briefing by LT Manda – photo by Tom Savage

Deploying a launch boat – photo by Tom Savage

The sonar equipment that transmits from the launch boats is called EM2040 multi beam sonar. A multi beam sonar is a device that transmits sound waves to determine the depth of the ocean. It is bolted to the hull that runs parallel to the boat, yet emits sound perpendicular to the orientation of the sonar. In the beginning of the season, hydrographers perform a patch test where they measure the offsets from the sonar to the boat’s GPS antenna, as well as calculating any angular misalignments in pitch, roll or yaw. These measurements are then entered in to software that automatically corrects for these offsets.

deploying CTD — TAS Tom Savage deploying the conductivity, temperature and density probe ~ photo by Megan Shapiro

The first measurement to collect is the ocean’s conductivity, temperature and depth. From this information, the scientists can determine the depths in which the density of the water changes. This data is used to calculate and correct for the change in speed of sound in a given water column and thus provide clean data. The boats travel in pre-defined set lines within a defined polygon showing the identified corridor to be collected. Just like mowing a lawn, the boat will travel back and forth traveling along these lines. The pilot of the boat called the Coxswain, uses a computer aided mapping in which they can see these set lines in real time while the boat moves. This is an extremely valuable piece of information while driving the boat especially when the seas are rough.

The coxswain will navigate the boat to the position where data collection will begin inside a defined polygon. Since the multibeam echosounder transmits sound waves to travel through a deep column of water, the area covered by the beam is wide and takes longer to collect. In such stretches of water, the boat is crawling forward to get the desired amount of pings from the bottom needed to produce quality hydrographic data. The reverse is true when the boat is traveling in shallow water. The beam is very narrow, and the boat is able to move at a relatively fast pace. The boat is constantly rolling and pitching as it travels along the area.

As the boat is moving and collecting data, the hydrographer checks the course and quality of the data in real time. The depth and soundings comes back in different colors indicating depth. There is at least four different software programs all talking to one another at the same time. If at any point one component stops working, the boat is stopped and the problem is corrected. The technology driving this collection effort is truly state of the art and it all has to operate correctly, not an easy feat. Every day is different and provides different challenges making this line of work interesting. Troubleshooting problems and the ability to work as a team is crucial for mission success!

Personal Log

I have found the work on the Fairweather to be extremely interesting. The crew onboard has been exceptional in offering their insights and knowledge regarding everything from ship operations to their responsibilities. Today’s blog marks my first week aboard and everyday something new and different is occurring. I look forward in developing new lesson plans and activities for my elementary outreach program. Prior to arriving, I was expecting the weather to be mostly overcast and rainy most of the time. However, this has not been the case. Clear blue skies has prevailed most days; in fact I have seen more sun while on the Fairweather than back home in Hendersonville in the entire month of July! For my earth science students, can you make a hypothesis as to why clear skies has prevailed here? Hint, what are the five lifting mechanisms that generate instability in the atmosphere and which one(s) are dominant in this region of Alaska?

Question of the day. Can you calculate the relative humidity based on the dry and wet bulb readings above? Data table below…… Answer in the next blog

Until next time, happy sailing !

Tom

May 2, 2018May 3, 2018

Cindy Byers: Above the Queen Charlotte Fault, May 2, 2018

NOAA Teacher at Sea
Cindy Byers
Aboard NOAA Ship Fairweather
April 29 – May 13, 2018

Mission: Southeast Alaska Hydrographic Survey

Geographic Area of Cruise: Southeast Alaska

Date: May 2, 2018

Weather From the Bridge

Latitude: 54°41.2 N
Longitude: 134°15.3 W
Sea Wave Height: 5 feet
Wind Speed: 7 knots
Wind Direction: 330°
Visibility: 2 nautical miles
Air Temperature: 9.9°C
Sky: Complete Cloud Cover

Science and Technology Log

NOAA Ship Fairweather is now 46 miles off the southeast coast of Alaska, mapping the ocean floor over a fault. This a transform boundary, so it is a strike slip fault. It is the boundary between the North American and Pacific plates. The United States Geologic Survey (USGS) has hired NOAA to survey the ocean floor in this area called the Queen Charlotte fault. The entire section of the fault is called the Queen Charlotte – Fairweather fault (named for Mount Fairweather, just like the ship’s name.) It runs for over 1,200 kilometers from Yakatat, Alaska to the north and British Columbia to the south. This is a part of a long fault along this plate boundary that is called the San Andreas fault when it is on land in California

The last time this particular area was surveyed was for the creation of navigational charts, between 1900 and 1938, but without accuracy or data density that the multibeam sonar being used today has. Once this portion is surveyed, the entire fault will have been mapped. The mapping has been done by the USGS, the Canadian Geologic Survey, and NOAA.

The photo above shows the features of the sea floor. It is set on top of a navigational chart. You can see the numbers on the old chart that represent depth reading. The data collected today shows depth for the entire area mapped and the features on the sea floor.

Looking at what NOAA Ship Fairweather has already mapped, the fault is very distinct as are the channels that have been offset by past seismic activity. These channels were created from runoff as the glaciers receded from this area 17,000 years ago. Using the offset measurements and the time since the canals where formed, scientists have given a slip rate of 5.5 centimeters per year to this area of the fault. This makes it one of the fastest moving continental – ocean transform boundaries.

Mapping

NOAA ship Fairweather has sonar that was built for detecting hazards for surface navigation, but it is capable of surveying to several kilometers in depth. The survey team has figured out how map at these great depths up to 2,100 meters. It involves going slowly over the area, and gathering richer data by going over part of the previous survey lines. This is much like painting a wall, where the painter overlaps their brushstrokes so there are not gaps in the coverage. The multibeam solar is also directed in a narrow band, at this depth, for more accurate data.

Bridge Computer — The blue squiggly lines show where mapping is happening. The other colors are where we have been.

Why do you think this information is wanted by geologists?

The fault has produced at least seven earthquakes with a magnitude greater than 7. An 8.1 magnitude earthquake was generated from this fault near British Columbia in 1949. To date, it is the largest Canadian earthquake recorded. In 1958, a magnitude 7.8 earthquake above Lituya, Alaska created a massive underwater landslide which produced a tsunami sending water 525 meters (1700 feet feet) up a mountainside. More recently in 2012, a 7.5 magnitude earthquake was measured from this fault, and in 2013, Craig, Alaska was hit with a magnitude 7.5 earthquake.

Surveyors computer These five screens are used by the survey team when the multibeam sonar is in use. — These five screens are used by the survey team when the multibeam sonar is in use.

Scientists want to know more about this fault, which could cause further damage to areas of southeast, Alaska. From the seabed mapping, geologists hope to better understand the slip rate and the intervals between earthquakes.

Personal Log

I have been so impressed with the people on NOAA Ship Fairweather. Everyone has been so welcoming and kind. This small group of people living in small quarters could be difficult for many people, but everyone here is so enthusiastic about the mission and their jobs. They are very open to sharing what they know with me, including explaining the science and technology of the equipment and how the ship functions.

It has been really fun learning about this fault and the surrounding underwater topography. Being able to see the sea bottom as we continue over it is amazing!

I am so happy I will get a chance to share this science with my students. I hope they noticed, as they read this post, the highlighted terms and concepts that we learned this year about faults and earthquakes.

Did you know?

I found a term that was new to me, tectonic geomorphology. It is the study of the interaction between active plates and land process, and how these shape landscapes.

Information used in this post can partly from:

“A Closer Look at an Undersea Source of Alaskan Earthquakes.” Earth and Space Science, vol. 99, no. 2, 2018, pp. 1–6.

April 27, 2018April 27, 2018

Victoria Cavanaugh: West of Prince of Wales Island, April 26, 2018

NOAA Teacher at Sea
Victoria Cavanaugh
Aboard NOAA Ship Fairweather
April 16-27, 2018

Mission: Southeast Alaska Hydrographic Survey

Geographic Area of Cruise: Southeast Alaska

Date: April 26, 2018

Weather Data from the Bridge

Latitude: 54° 40.914′ N
Longitude: 134° 05.229′ W
Sea Wave Height: 8-9feet
Wind Speed: 15 knots
Wind Direction: NNW
Visibility: 10 km
Air Temperature: 9.5^oC
Sky: Partly Sunny in the AM, Cloudy in the PM

Science and Technology Log

Over the past two days, the crew of NOAA Ship Fairweather has been hard at work on the first major project of the season, charting the ocean floor along the Queen Charlotte-Fairweather Fault System. The project itself will take seven days, though with two days at sea before heading to port in Ketchikan, the survey techs have been focusing on the first sheet, D00245, roughly 900 kilometers offshore in an area known as West of Prince of Wales Island.

Chart of survey area — The Survey Starts Here: Note Sheet D00245 to the Left in Blue

Fairweather is completing the survey in collaboration with the United States Geological Survey (USGS) which has spent the last three years researching and mapping the seafloor along the fault. Geologists are particularly interested in this fault as little is known about the region and the seafloor here is largely unexplored. Geologists believe that by studying the fault line and the geology of the ocean floor, they may be able to unlock secrets about the history of our oceans as well as develop new understanding of seismic activity that can keep communities safer when future earthquakes strike.

Plot room — The Plot Room: Survey Techs aboard Fairweather Can View the Data Being Collected in Real-Time

One of the reasons the USGS turned to NOAA to complete its charting efforts is because of the tremendous ocean depths. The survey techs are using Fairweather‘s multibeam echosounders for the project which will take a total of seven days to complete. Sonar pings from the ship’s transducer hit the ocean floor and bounce back to the ship, creating 2D and 3D charts of the ocean floor. Additionally, survey techs can learn more information about the type of surface on the ocean floor (sandy, rocky, etc.) based on the strength of the return of the sonar pings. Despite the seafloor in the area being some 15,000 years old, it has never been explored! Thus, for the survey techs and geologists working on this project, there is a sense of pure excitement in being able to explore and discover a new frontier and help others sea what humans have never seen before.

Depth reading — 1520 Meters Down: The Number at the Top Left of the Screen Shows We’re in Water Nearly a Mile Deep!

One of the geologists remarked that he was surprised to see that despite how old the ocean floor in the area is, little appears to have changed, geologically speaking in thousands of years. Another surprise for geologists is how the fault appears to be one large, long crack. Many other fault areas appear to be made up of lots of small, jagged, and complicated “cracks.” Another question to explore!

Shallower depth reading — A Much More Shallow Area: Notice the Sonar Here Shows We’re Just 247 Meters Deep

Notice the colors which help survey techs see the changing depths quickly. The green, mostly vertical lines, show the ship’s course. To collect data, Fairweather runs about 6 hours in one direction, before turning around to run 6 hours in the opposite direction. This allows survey techs to gather more data about ocean depths with each turn. In total, survey techs collected nearly 48 hours of data. This meant survey techs working all night long to monitor and process all of the new information collected.

Bekah and CTD — Survey Tech Bekah Gossett Prepares to Launch a CTD off the Ship’s Stern

Just like on the launches during patch tests, survey techs deploy CTD’s to measure the water’s conductivity (salinity), temperature, and pressure. This information is key in order to understand the speed of sound in a given area of water and ensure that the sonar readings are accurate.

Survey techs ready CTD — The Survey Techs Work in Rough Seas to Ready the CTD

Personal Log

View off bow — Nothing But Blue Skies in Every Direction!

In striking contrast to the beautiful coastlines that framed the Inside Passage, the last two days have provided endless blue skies mixing with infinite blue seas. No land in sight!

Nautical chart — Finding the Survey Area West of Prince of Wales Island on a Chart

The Ship’s Radar Shows Just One Vessel Nine Miles Due East

The open ocean is challenging (huge waves make the entire ship sway constantly and gives new meaning to earning one’s “sea legs”), but far more inspiring. I’m grateful for the glimpse into life at sea that NOAA has provided me. There is deep sense of trust among the crew, in their collective hard work that keeps us all safe in the middle of the ocean. There is also a wonderful sense of adventure, at being part of discovering something new. Just as explorers have sought after new frontiers for hundreds of years, Fairweather today is charting areas still unknown to humankind. There is something truly invigorating about watching the sonar reflect the ocean floor in a rainbow of colors, in watching as peaks and valleys slowly are painted across the monitors in the plot room and bit by bit, another sliver of science is added to the charts. There is something particularly refreshing and exciting about seeing whales spray and play in the waves while standing on the ship’s bridge. I’m truly grateful to all onboard Fairweather and NOAA’s Teacher at Sea Program for this remarkable opportunity, and I look forward to sharing what I’ve learned with students back at Devotion.

Wave heights — The View out a Port Window Shows Some of the More Extreme Wave Heights as Fairweather Rocks and Rolls

Did You Know?

Prince of Wales Island is one of the southernmost parts of Alaska. Home to some 4,000 inhabitants, Prince of Wales Island is the 4th largest island in the US and the 97th largest island in the world. Originally home to the indigenous Kaigani Haida people, Spanish, British, and French explorers all passed by the island in the 1700 and 1800’s. In the late 1800’s, miners came to the island looking for gold, copper, and other metals. Today, most of the land is protected as the Tongass National Forest covers a great portion of the island.

Challenge Question #5: Devotion 7th Graders – Can you find the depths of the Charles River, the Boston Harbor, and 900 kilometers offshore the Massachusetts coast? What sort of aquatic life exists in each area? What does the river/seafloor look like in these areas? Create a comic strip or cartoon showing your findings.

June 24, 2016April 22, 2021

Donna Knutson: Last Leg of Leg III Atlantic Sea Scallop Survey 2016, June 24, 2016

NOAA Teacher at Sea Donna Knutson
Aboard the Research Vessel Sharp
June 8 – June 24, 2016

2016 Mission: Atlantic Scallop/Benthic Habitat Survey
Geographical Area of Cruise: Northeastern U.S. Atlantic Coast
Date: June 24, 2016

Last Leg of Leg III Atlantic Sea Scallop Survey 2016

Mission and Geographical Area:

The University of Delaware’s ship, R/V Sharp, is on a NOAA mission to assess the abundance and age distribution of the Atlantic Sea Scallop along the Eastern U.S. coast from Mid Atlantic Bight to Georges Bank. NOAA does this survey in accordance with Magnuson Stevens Act requirements.

Science and Technology:

Latitude: 41 29.84 N

Longitude: 070 38.54 W

Clouds: partly cloudy

Visibility: 5-6 nautical miles

Wind: 3.58 knots

Wave Height: 6 in.

Water Temperature: 53 F

Air Temperature: 67 F

Sea Level Pressure: 30.0 in of Hg

Water Depth: 26 m

It has been an action packed two weeks. The men and women who dedicate themselves to the scallop survey are extremely hard working scientists. It is not an easy job. The sorting of the dredged material is fast and furious, and it needs to be in order to document everything within the catch before the next one comes in. The baskets are heavy and it takes a strong person to move them around so quickly.

DSCN8159 (2) dredge team — Han, Jill, Mike, Vic, Me and Ango

In small catches every scallop is measured. In dredges with many baskets of scallops, a percentage is measured. It is a random sampling system, taking some scallops from each of the baskets to get a general random sample of the whole. Mike led an efficient team, he told us what to look for and oversaw the measuring.

DSCN7780 (2)mike and nicki — Mike and Nikki

He often set samples aside to show me later, when we were not as busy. A few examples were how to tell the difference between the red and silver hake or the difference between the Icelandic and Atlantic sea scallop. He showed me how the little longhorn sculpin fish, “buzz bombs” known to fisherman, vibrate when you told it in your hand.

Mike even took the time to dissect some hake and to show me the differences in gonads, what they were feeding on by opening their stomach, and the otolith within the upper skull. The otolith is a small bone in the inner ear that can be used to identify and age the fish when in a lab looking through a microscope. Mike answered my many questions and was always eager to teach me more.

Another helpful team member was Vic. Vic taught me how to run the HabCam. He has been involved in the HabCam setup since it started being used four years ago. There is a lot of work to do to set up the multiple monitors and computers with servers to store all the images collected by the HabCam. Vic overlooks it all from the initial set-up to the take down. I admire Vic’s work-ethic, he is always going 100% until the job is completed. Sometimes I just needed to get out of his way, because I knew he was on a mission, and I didn’t want to slow him down.

DSCN8132 (2) monitors — Control center for Habcam and Dredging

When we weren’t dredging, but rather using the HabCam, there was a pilot and copilot watching the monitors. The HabCam, when towed behind the ship, needs to be approximately 1.7 m off the ocean floor for good resolution of the pictures, and keeping it at that elevation can be a challenge with the sloping bottom or debris. There is also sand waves to watch out for, which are like sand bars in a river, but not exposed to the surface.

When not driving HabCam there are millions of pictures taken by the HabCam to oversee. When you view a picture of a scallop you annotate it by using a measuring bar. Fish, skates and crabs are also annotated, but not measured. It takes a person a while to adjust to the rolling seas and be able to look at monitors for a long period of time. It is actually harder than anticipated.

DSCN7768 (2)skate — HabCam Picture of a skate.

Han was making sure the data was collected from the correct sites. She works for the Population Dynamics branch of NOAA and was often checking the routes for the right dredges or the right time to use the HabCam. Between the chief scientist Tasha and Han, they made sure the survey covered the entire area of the study as efficiently as possible.

DSCN7839 (2)tash han mike — Tasha, Han and Mike discussing the next move.

Dr. Scott Gallager was with us for the first week and taught me so much about his research which I mentioned in the previous blogs. Kat was with us initially, but she left after the first week. She was a bubbly, happy student who volunteered to be on the ship, just to learn more in hopes of joining the crew someday. Both vacancies were replaced by “Ango” whose real name in Tien Chen, a grad student from Maine who is working on his doctoral thesis, and Jill who works in Age and Growth, part of the Population Biology branch of NOAA. Both were fun to have around because of their interesting personalities. They were always smiling and happy, with a quick laugh and easy conversation.

DSCN8131 (2)the three — Jill, Ango and Han after dredging.

The Chief Scientist, Tasha, was extremely helpful to me. Not only does she need to take care of her crew and manage all the logistics of the trip, plus make the last minute decisions, because of weather or dredges etc, but she made me feel welcome and encouraged me to chat with those she felt would be a good resource for me. On top of it all, she helped me make sure all my blogs were factual. She was very professional and dedicated to her work, as expected from a lead scientist leading a scientific survey.

DSCN8146 (2)tash and jim — Evan, Tasha and Jimmy discussing route.

I spent as much time as possible getting to know the rest of the crew as well. The Master, Captain James Warrington “Jimmy” always welcomed me on the bridge. I enjoyed sitting up there with him and his mates. He is quick witted and we passed the time with stories and many laughs. He tolerated me using his binoculars and searching for whales and dolphins. There were a few times we saw both.

He showed me how he can be leader, responsible for a ship, which is no small feat, but do so with a great sense of humor, which he credits he inherited from his grandmother. The other captains, Chris and Evan, were just as friendly. I am sure all who have been lucky enough to travel with them would agree that the RV Sharp is a good ship to on because of the friendly, helpful crew and staff.

DSCN7785 (2)KG — KG, oceanic specialist, helped with dredges.

Because this was my second experience on a survey, the first was a mammal survey, I have really come to appreciate the science behind the study. It is called a survey, but in order to do a survey correctly, it takes months of planning and preparation before anyone actually gets on a ship.

There is always the studying of previous surveys to rely on to set the parameters for the new survey. Looking for what is expected and finding, just that, or surprising results not predicted but no less valued, is all in a scientist’s daily job. I admire the work of the scientist. It is not an easy one, and maybe that is why it is so much fun. You never know exactly what will happen, and therein lies the mystery or maybe a discovery to acquire more information.

DSCN8127 (2)big goose — I had to hold the largest goose fish we caught!

It was a challenging two weeks, but a time I’m so glad I had the opportunity to have with the members of Leg III of the 2016 Atlantic Sea Scallop Survey.