Hydrographic survey – Page 6 – NOAA Teacher at Sea Blog

July 2, 2018July 3, 2018

Heather O’Connell: Surveying Tracy Arm, June 20, 2018

NOAA Teacher at Sea

Heather O’Connell

NOAA Ship Rainier

June 7 – 22, 2018

Mission: Hydrographic Survey

Geographic Area of Cruise: Seattle, Washington to Sitka, Alaska

Date: 6/20/18

Weather Data from the Bridge

Latitude and Longitude: 57°52.9’ N, 133 °38.7’ W, Sky Condition: Broken, Visibility: 10+ nautical miles, Wind Speed: Light Variable, Sea Level Pressure: 1013.5 millibars, Sea Water Temperature: 3.9°C, Air Temperature: Dry bulb: 17.8°C, Wet bulb: 14°C

Science and Technology Log

After the morning meeting of hearing everyone’s risk assessment before getting on the launches, I was part of the four person crew on launch RA-6. Our task for the day was to clean up the data, or collect data in places within the Tracy Arm polygon that weren’t already surveyed. We had to fill in the gaps in L and M polygons on the East point. The entire area of Tracy Arm needed to be surveyed because there are several cruise ships that are coming into this area now that Sawyer Glacier is receding and the area has not been surveyed since the late nineties. Navigation charts must be updated to ensure that the safety of the people that are visiting the area.

Once on the launch, the bright orange POS MV, or Positioning Orientation System Marine Vessel, must be powered to start the survey process. The new acquisition log was created as an excel spreadsheet to record the different casts along with the latitude and longitude, the maximum depth and the sound speed of the water at about approximately one meter. With all of the valuable data recorded, it is important to have a consistent system for managing all of the data so that it can be accessed and managed efficiently.

The EM-2040 Konsberg Sonar S.I.S., Seafloor Information System, program was powered on next. The EM processing unit, which is connected to the multi-beam sonar, has three lines of information when properly communicating with sonar. The right hand monitor in the launch displays the information from the sonar. Creating the file name is another crucial way of ensuring that the data can be managed properly. It is from this computer that you can manually adjust the angle of the beam swath with the sound pings.

Once the computers were started and communicating with each other, we completed a C.T.D. cast to obtain the sound speed profile of the water. There is also a device that measures this right on the multibeam sonar, but it is important that two devices have a similar sound speed profile to ensure data accuracy. If there is a large discrepancy between the two values, then another cast must be taken. Initially, the measuring sound speed profile at the interface was 1437.2 and the C.T.D. sound speed was 1437.8. The final algorithm that determines the depth of the water will take this information into account. Since we were somewhat close to a waterfall, the fresh water input most likely affected the sound profile of the water.

After viewing the data acquired in the sheet, or the assigned area of Tracy Arm to survey, Greg found areas where there were holes. He put a target on the map on the monitor on the left hand side computer. This HYSWEEP interface for multibeam and side scan sonar (which is a subset of HYPAC which is the multibeam software) screen shows a chart of the area with depths in fathoms and any rocks or shoals that would impede driving ability along with a red boat image of the vessel. This display is what the coxswain driving above also sees so that he or she is aware of what direction to travel. Once logging data, this screen also displays the beam so that you can ensure that all necessary data is being acquired. Previous surveys are depicted in a more subdued color so that you can see that the missing data is being collected. From the monitor, the survey technician must control the view of the map to be sure that it includes the targeted area, along with the path of the boat so that future obstructions can be avoided.

Since we were avoiding icebergs in the initial part of the clean up, we were going at about two knots. This slow pace allows for an increase in returns, nodes and soundings that increase the data density. Shallow waters take much longer to survey due to the smaller swath width. It is important to have accurate, high resolution data for shorelines since this is the area where many vessels will be traveling. When a sonar pings, every swath, or fan-shaped area of soundings, returns five hundred soundings. Five hundred soundings times a rate of seven pings per second means there are thirty five hundred soundings per second total. This data density enhances the resolution of the maps that will be generated once the data has been processed.

Since there are sometimes safety hazards when surveying there are several different approaches that can be used to ensure the entire area is surveyed in a safe manner. Half stepping included going back over previous coverage far enough away from the hazard. Scalloping is another method which involves turning right before the rock or obstruction. This sends the beam swath near the rock without putting the vessel in danger. Some areas that were too close to icebergs could not be surveyed since it was not safe. But, this hydrographic survey was able to acquire data closer to the Sawyer Glacier than ever before. Being a part of this data collection was gratifying on many levels!

Personal Log

Seeing a white mountain goat amongst some of the most beautiful geological features that I have ever laid eyes on was another benefit of being out on the launch for the day. When a grizzly bear cub ran by a waterfall I continued to appreciate a day on the launch. Seals perched on icebergs were always a fun sight to see. And, the endless pieces of ice drifting by in the sea during our surveying never ceased to amaze me.

Seals on an Ice Berg — Seals on an Iceberg

After a day of surveying, kayaking to a waterfall in William’s Cove and exploring proved to be another fun adventure.

OLYMPUS DIGITAL CAMERA — Waterfall in William’s Cove

Growing Muscle like Growing Character

The other day as I ran on the treadmill, I had a realization. While looking at the lifting weights, I realized that in order to build muscle, one must tear old muscles and rebuild new strands of protein. When these new fibers build on top of each other, muscles grow. I realized that new officers go through a similar process of developing skills and character. Junior officers come in with a two year responsibility where they learn an incredible amount. They are constantly put into new and challenging learning experiences where they tear their muscles. As they acclimate to these experiences, they build character, or muscle. The cycle repeats with subsequent occurrences.

Junior Officer ENS Airlie Pickett has a small triangle tattooed on her inner left bicep. When I asked her the significance of it, she said that the only way that you can truly understand something is to observe how it changes. In math, integrals and derivatives explain this change.

As I appreciated her tattoo, I considered that she must learn quite a lot about herself as a junior officer constantly learning new things. I’ve appreciated the opportunity to experience and observe myself in an unfamiliar surrounding on Rainier. It’s humbling to not understand the nautical terms, endless acronyms of surveying and NOAA Corps structure of life. I appreciated that all hands on Rainier made me feel welcomed, and were patient with explaining new concepts to me. I am grateful for the opportunity to experience the Inside Passage while learning about hydrographic surveying. Living on a ship, learning about navigation and meeting all of the hard working people on Rainier has been an unique experience. Overall, this has been an incredible opportunity. Mahalo nui loa! (Thank you very much). A hui hou Rainier! (Until we meet again)!

Did You Know?

Barometers measure atmospheric pressure in millimeters of mercury or atmospheres. An atmosphere is the amount of air wrapped around the Earth and one atmosphere, atm, is the amount of pressure at sea level at fifteen degrees Celsius. As altitude increases, the amount of pressure decreases since the density of the air decreases and less pressure is exerted. A decrease in altitude increases the amount of pressure exerted and the density of the air increases.

Changes in pressure can signify weather patterns. A drop in barometric pressure means a low pressure system is coming in and there is not enough force to blow away the weather. Weather indicative of this includes windy, cloudy and/or rainy weather. An increase in barometric pressure means a high pressure system is coming in and cool, dry air pushes out the weather resulting in clear skies.

https://www.nationalgeographic.org/encyclopedia/barometer/

July 1, 2018

Victoria Obenchain: Surveying with Fairweather, June 30, 2018

Teacher at Sea Blog

Victoria Obenchain

Aboard NOAA Ship Fairweather

June 25^th-July 6^th, 2018

Mission: Arctic Access Hydrographic Survey

Geographic Area of Cruise: Northwest, Alaska

Date: June 30th, 2018

Weather Data from the Bridge

Lat.: 57^o57.7’ N
Long.: 145^o 45.7’ W
Sea wave height: 1 foot
Wind speed: 1 knot
Wind direction: West, southwest
Temperature: 10.8^oC
Visibility: 6.4 nautical miles
Sky Conditions: Cloudy

Science and Technology Log

The last two days have been surveying days. With the MVP (described in the last blog) deployed, the survey team got to work. This ship uses multibeam sonar which is affixed below the ship. Since surveying can be done at all times of day, 3 teams were created to do Survey Watch; each team worked two 4 hour blocks during the day to make sure the data was collected correctly. I was luckily placed on one of the teams, working the 3:30-7:30pm shift and the 3:30-7:30am shift. While these may not be the most normal of work day times, especially the latter, I was excited to be included and experience how work gets done on this ship.

This image, courtesy of NOAA, depicts a MBSS beam below the ship and the mapped results off the stern.

Ali Johnson monitoring 5 screens to make sure the sonar mapping is done correctly.

I was teamed up with two amazing female scientists and surveyors on Survey Watch, Megan Shapiro and Ali Johnson.

Megan is from Maryland and got her undergraduate degree from UNC Wilmington in Marine Biology Conservation. She has a love for whales and that is what brought her to Alaska, as she used to work in Seward, Alaska as a deck hand and naturalist on whale watching excursions. To NOAA’s luck, this is where Megan learned about NOAA Ship Fairweather and its hydrographic mission. Megan joined the ship about three month ago and has gotten tons of on the job training to help her learn how to map the sea floor.

Ali Johnson is from Iowa, and got her undergraduate degree in Environmental Studies, with a dual minor in Biology and Coastal Management from Eckerd College. She learned about NOAA and its work with sonar while she was volunteering at Gray’s Reef National Marine Sanctuary in Georgia. NOAA was actually using sonar in the preserve to help learn about diurnal fish migrations and predator prey relationships in the area.

While on Survey Watch, Megan and Ali monitor the ships sonar readings along the sea floor, deploy the MVP continuously throughout the trek to gather up to date data, and make sure the information is being recorded correctly. They work along side the officers to monitor the ship’s course to make a full coverage map of the area, which means having the ship go back and forth, like a lawn mower might do in your yard, until all pieces of an area are mapped. And then once all the sonar soundings are in, weeks of processing that data starts. They use correctors for the data, such as: tides, roll and pitch of the boat, sound speed, and position, to then help create the most accurate representation of the sea floor.

I wanted to know more about these amazing scientists. NOAA Ship Fairweather is a fairly large ship which can hold approximately 50 people, Megan and Ali are two of the only five women who work onboard.

What is the most rewarding part of this job?

Megan: Probably knowing that the work I am doing is going to be making the nautical charts used by mariners all over the world, it’s cool to know I am taking part in that.

Ali: I like the high quality and accuracy of data we provide, it allows for others to use the data in other applications, such as tsunami and hurricane planning, hazard mitigation and in other facets of NOAA.

What are some of the perks working for NOAA and on NOAA Ship Fairweather?

Megan: Getting to travel to new places and getting to meet a lot of new people, many of which are like minded.

Ali: We get to travel and gain access to remote areas of the world which are stunning. I like being out on the water as well. Additionally, we get access to new release movies before they hit stores, so that’s pretty nice, too!

What are some of the challenges to this type of work?

Megan: It’s hard staying in touch with friends and family since the ship is normally out of cell service range and the wifi can be slow. Additionally, I miss cooking! While the ship offers us great cooked meals, I sometimes miss cooking for myself.

Ali: One of the biggest challenges is just being away from cities. If we wanted to go to the east coast, or home for a long weekend, its kind of hard. It is a 17 hour trip, from Juneau, with all the connections.

What have been some of the coolest or most memorable moments on the job?

Megan: While processing the data for an area known as Tracy Arm, my coworker and I discovered a previously unknown underwater trench! When we were looking at the area during processing, the area looked like it had a cut or dip in the surface. Once it was 3-d imaged you could see the trench. It was pretty cool.

20180629_081130

Ali: Last year, a fishing/crabbing vessel, F/V Destination, went down in February with six on board. NOAA Ship Fairweather was passing through the area in June, and it had yet to be found. Since we were in the last known area of the vessel the Coast Guard asked us if we could spend a day or two in the area and use our sonar to see if we could help find it. We had only planned on spending one day looking since we were on our way to the Arctic, but when that day was done we decided to do one last pass and on the 26^th hour the sonar ended up finding it. It was nice to be able to provide the families with closure.

What did you want to be when you were growing up?

Megan: I wanted to be a zoo keeper! Or really anything with animals, I thought about being a teacher, too.

Ali: I knew I wanted to do something with the oceans. Originally I wanted to work with ocean animals, possibly mammals or cephalopods.

Where do you see yourself in 20 years?

Megan: Hopefully, having a farm by the ocean where I can have lots of dogs. I would love to have an Irish Wolf Hound, Collie and a Borzio in particular. Maybe get my masters in Marine Biology and continue studying whales.

Ali: Maybe I’ll be retire from NOAA by then and look into starting a nonprofit for the ocean. I’ll probably live somewhere warm and tropical; maybe lead a dive school to get others interested in the ocean, as well. And I’ll have some dogs, too!

Personal Log

I keep finding myself outside the ship to view the Alaskan coastline or to scope for animals. It is truly beautiful here. So far I have been lucky enough to see quite a few whales, sea lions, porpoises and sea birds including albatross. It is a bit cold, so I can only be outside for a little bit, but I find the time completely worth it. Soon my time will be up and I want to be able to remember this experience and the Alaskan beauty I am in.

July 1, 2018

Eric Koser: Hydrography 101 – and the Tools to Make it Happen, June 28, 2018

NOAA Teacher at Sea

Eric Koser

Aboard NOAA Ship Rainier

June 22 – July 9, 2018

Mission: Lisianski Strait Survey

Geographic Area: Southeast Alaska

Date: June 28, 2018: 0900 HRS

Weather Data From the Bridge
Lat: 57°52.59′ Long: 133°38.7′
Skies: Broken
Wind 1 kt at variable
Visibility 10+ miles
Seas: calm
Water temp: 5.6°C

Science and Technology Log

Long Line Boat — A typical longline fishing boat. The fishing lines get spread out behind the boat from the large booms on either side.

The ultimate focus of Rainier is to assure accurate navigational charts are available to all mariners. This task is critical to the safety of many industries. About 80% of all the overseas trade in the US (by weight) is moved over water. Here in SE Alaska, it appears the largest industry is commercial fishing. Many boats fish both with nets and long lines to catch halibut, rockfish, cod, and several varieties of salmon.

Another major industry here is certainly tourism. As we conduct our work, we often see very large cruise ships. It’s an interesting juxtaposition to be in a narrow inlet surrounded by mountains, ice, and wildlife and then come across a large ship. We passed the brand new ship Norwegian Bliss around 11 PM on our transit to Tracy Arm. This ship is 1,082 feet long, carries a crew of 2,100 people and has a guest capacity of 4,004 people! The safe navigation of all of these vessels depends upon the accuracy of charts produced by NOAA.

The cruise ship Norwegian Bliss as we passed her port to port in the evening.

The freely available charts offered by NOAA are created with three essential steps. First, the bulk of the depth data in this area is measured with MBES (Multi-Beam Echo Sounder). This creates a three-dimensional digital image of the bottom.

Secondly, important features to navigation that are shallow are best identified by our launches which travel along the shorelines and inspect for rocks, ledges, and other potential dangers. The locations of features are identified by GPS location and charted digitally by hydrographers on each launch.

Thirdly, bottom samples are collected by launch crews to confirm the type of material present on the bottom.

The MBES systems aboard Rainier and the launches come from Kongsberg Maritime. Two transducers (devices that transmit and receive) work in tandem. The transducer that is oriented front to back sends out an array of sound signals in a wide beam. The width of the beam on the sea floor depends directly on the depth – deeper water allows the beam to spread farther before reflecting. The transducer that is oriented side to side in the water receives a narrow swath of the ‘pings’ of sound that were transmitted. The time it takes any ping to get to the bottom and reflect back to the ship is recorded. The greater the time, the larger the depth.

MBES on a launch — This shows the position of the MBES on the bottom of one of several launches.

This is the pair of MBES transducers on a launch, looking from the bow towards the stern.

Hydro Sonar — This image, courtesy of NOAA, depicts an MBSS beam below the ship and the mapped results off the stern.

A couple of issues provide challenges to this technique. One, the speed of sound in water depends on several factors. The salinity (concentration of salt in the water), the conductivity (how easily electricity passes through the water), and the temperature each fluctuate as the depth changes and affect the speed of the sound waves. As hydrographers receive data, the system has to account for these changes in speed to produce an accurate depth measurement. One way to do this is with a static CTD sensor. This device is lowered from the launches all the way to the bottom as it measures the speed of sound in the water. It provides a set of three charts as the depth changes which are used to adjust the time data from the MBES accordingly. There is also a version of the CTD, called a MVP (Moving Vehicle Profiler or ‘fish’), that can be pulled behind Rainier as we are moving and take dynamic data.

Here is a NOAA article on hydrographic surveying. Here is further explanation of MBSS.

Deploying Depth Profiler — Here the crew lowers the profiler “fish” into the water.

Speed Profiler Data — These three plots represent the speed of sound, temperature, and salinity (from left to right) vs. depth (on the vertical axis).

A second issue is GPS signal drift. Over time, the location information can shift slightly. To account for this potential problem, the scientists place a HORCON (Horizontal Control) station onshore in the area where they are mapping. I described this tool in my previous post.

Another interesting technology that is currently being developed is called “backscatter” mapping. Here scientists look not only at the time it takes the sound waves to bounce back to the transducer, but also at the quality of the return signal. Different materials on the seafloor reflect the sound differently – hard surfaces like rocks have a sound signature that is much different than soft surfaces like silt or plants. NOAA is continually improving the tools they use to learn!

Here is an example of the chart that we are updating in Tracy Arm.

Personal Log

I had a chance to take the helm yesterday! It’s interesting how sensitive the steering on this large vessel really is. The rudders are able to turn from “amidships” or their center position, up to about 35° to either side. But while traveling at about 8 knots, we tend to use a maximum of about 5° of rudder to alter the ship’s direction. While at the helm, we keep close track of the heading (compass bearing) of the ship as indicated by the gyro compass and magnetic compass on board. Then we provide steering input to hold the ship to the course ordered by the CONN. I had the chance to help steer around several icebergs as we transited into Tracy Arm. Careful attention to detail – and willingness to promptly follow commands make for success!

I also took an opportunity to head out in a kayak from the ship where we are anchored! Two of my new colleagues and I paddled across this bay and had a great chance to look very closely at pieces of ice. The ice is really beautiful and forms many interesting shapes. The quiet of the bay – hearing only the distant waterfalls, birds, and our paddling was beautiful!

Iceberg — This piece of ice drifted through Tracy Arm from the glacier. It was temporarily ‘grounded’ on the bottom by the receding tide.

It’s crazy to consider the ice we were seeing may have been formed thousands of years ago in the glacier – and it just now melting as it floats away.

Did You Know?

President Thomas Jefferson signed a mandate in 1807 ordering a survey of the nation’s coasts. This fundamental task is always ongoing, with 95,000 miles of US Coastline.

About 90% of any floating piece of ice will be submerged below the salt water. Because the density of frozen fresh water just slightly less than salt water, the ice floats very low in the water! Read more here!

Who is Onboard?

I’d like you to meet HST (Hydrographic Survey Technician), Amanda Finn! Ms. Finn has been with NOAA since last September – and started working aboard NOAA Ship Rainier in October of 2017. As an HST, Amanda works with the team of hydrographers to collect MBES data from either the ship or any of the launches. Amanda graduated from the University of Connecticut in 2016 with a bachelor of science degree in GeoSciences and a minor in Oceanography. At the end of her college experience, she knew that seafloor mapping was her passion but wasn’t sure how to make that into a job. But it all came together when she found NOAA through a friend of a friend!

HST Amanda Finn with recently acquired depth data for Lisinaski Inlet!

Amanda was performing at her first harp concert (another skill!) when she met a relation of a hydrographer who works on a NOAA ship! Based on her experience, her advice to students is: “When things don’t seem to be going the way you want, take time to focus on something else you like instead. In good time, things will work out!”

One positive challenge Amanda shares working here on a hydro ship is developing an understanding of systems integration. Many different pieces must come together to create the finished charts. The people aboard Rainier make the experience very positive! The passion for seeking the unknown is the drive to continue!

June 29, 2018June 29, 2018

Brandy Hill: Chat with Chief Engineer and My First Tuna Catch, June 28, 2018

NOAA Teacher at Sea

Brandy Hill

Aboard NOAA ship Thomas Jefferson

June 25, 2018 – July 6, 2018

Mission: Hydrographic Survey- Approaches to Houston

Geographic Area of Cruise: Gulf of Mexico

Date: June 28, 2018

Weather Data from the Bridge

Latitude: 28° 50.7’ N

Longitude: 093° 34.4’ W

Visibility: 10+ nm

Sky Condition: 4/8

Wind: 12 kts

Temperature:

Sea Water: 29.6° C

Air: 29.3° C

Science and Technology Log

This afternoon I spent an hour with Chief Marine Engineer, Thom Cleary. As promised, he gave me a tour of the Engine Room. Thom arrived on the Thomas Jefferson in 2011 and has worked not only on maintaining operations, but greatly improving them. When asked about his favorite ship mechanism, he responded with one that is not his favorite but of which he is most proud. The Thomas Jefferson, along with most other ships, typically used to rid greywater and sewage by offloading into the ocean. The EPA states that ships must be at least one nautical mile from land or people in the water and three nautical miles from aquaculture (2018). With hydrographic survey operations taking place in “no discharge” areas (close to shore), this could complicate and/or slow down the Thomas Jefferson’s progress.

Realizing the inefficiency and in an effort to improve, Thom investigated other options. It was decided that a fuel storage tank would be converted to hold more wastewater. After a long wait period, the new method was installed. Within the first season 38,000 gallons of sewage was stored and discharged to a shore treatment facility. Today, the tanks have gone almost two months without release into the Gulf of Mexico. This improvement has allowed hydrographic operations to continue without interruption, conserves fuel, and increases efficiency.

Renovations to the Thomas Jefferson did not stop there. Originally constructed in 1991, the ship has room for many other improvements. Thom and team advocated for all natural lubricants (rather than petroleum), switched all light fixtures to LEDs, and adjusted the ballast system. In 2016 the roughly 122,000 gallon ballast system changed from using sea to municipal water. This now allows the ship to move from multiple coastal waters without concern for carrying invasive species in the ballast tanks. In addition, the new waste water tank was strategically placed in the center of the ship to help with stability.

Ballast diagram showing invasive species risk. (CC)

Thom is an innovator and self-described incorrigible tinkerer. Many of these changes would not have been made without his (and team’s) desire and advocacy to make things better. When I asked if these upgrades were standard on ships, he mentioned that the Thomas Jefferson is a trailblazer.

Chief Engineer Thom Cleary and the desalination/ reverse osmosis system. The RO typically operates at 650 psi (with 900psi maximum potential) and pushes sea water through a membrane creating potable water for the ship.

Personal Log

CO (Commanding Officer) authorized a launch on one of the boats. After some mishaps with a fuse, the crew performed multiple safety checks and we were cleared to go. Mission: collect survey data near a stationary platform. CO’s comfort level to obstructions with the main ship is a half-mile, so having the smaller launch boats is helpful when surveying areas like this.

Launch Boat Approach — The launch boat crew from left to right: Lt. Klemm, Kevin Brown, Pat Osborn, and Brandy Hill (below deck).

SurveyNearPlatform — Survey area near the stationary platform. The ship to the left is a supply vessel.

While cruising out to the survey area, I spoke with Pat Osborn, part of the Thomas Jefferson’s deck crew and our survey line driver for the day. Pat has two years of training and was explaining that he is still learning parts of his job. (Everyone on the ship wears multiple hats.) He spoke highly of his job and appreciated the multi-dimensional relationship between CO and the crew. Pat explained that CO is not expected to be an expert in all areas of the ship- there are safety checks (such as preparing for the launch) where the CO asks lead crew members to evaluate and sign-off prior to action. Every mission I’ve observed and attended has proceeded in this manner. It is a highly respectful and safe environment.

AllisonLaunchApproach — Chief Survey Technician, Allison Stone, awaiting launch boat arrival.

Launch Return to Ship — Patrick Osborn approaching ship Thomas Jefferson with the launch boat.

KevinDeployingCTD — Kevin Brown lowers the CTD while the boat is stationary. A CTD captures the salinity, temperature, depth, and concentration of particles in the water column. This information is used for analyzing the survey data. On the ship, this information is collected using an MVP which allows the ship to stay in motion.

As soon as we had the survey equipment set up and running, survey technician Kevin Brown brought out a fishing pole. I hadn’t realized that we could fish while out on the boat! We proceeded to catch and release about 10 tuna (likely False Albacore and Bonito). Kevin reeled in two, then passed the pole to me. I couldn’t believe how hard it was to real in a fish. I was reading that they can stay on the line and swim up to 40 mph!

Brandy reeling — Brandy Hill’s active line power stance.

Brandy Hill and her first fishing boat catch, False Albacore.

Peaks

+ Witnessed hard work and precision paying off- the launch boat survey data had an error of 0.0006 meters. The data is highly accurate!

+ Drove “the survey line” on the launch boat. (More of an explanation coming soon.)

+ Reeled in a beautiful, tough fish.

Note: After the seasickness subsided, I’ve decided to leave out the “Valleys” category. I’m having a great time.

June 29, 2018

Vickie Obenchain: Starting a Hydrographic Survey, June 28, 2018

NOAA Teacher at Sea

Victoria Obenchain

Aboard NOAA Ship Fairweather

June 26 – July 6, 2018

Mission: Arctic Access Hydrographic Survey

Geographic Area of Cruise: Northwest Alaska

Date: June 28th, 2018

Weather from the Bridge

Latitude: 54^o 25.5’ N
Longitude: 134^o13.7’ W
Wind Speed: 13 Knots
Wind Direction: South, Southwest
Temperature: 12.2^oC
Visibility: 10 nautical miles
Wave Height: 1 foot
Current Sky Conditions: Overcast

Science and Technology Log

This morning I spent some time on the bridge with the officers. NOAA Ship Fairweather is manned day and night with men and women making sure we are safely on course. While the ship is equipped with GPS, the ship is also full of experienced mariners who plot our position on paper nautical charts to help guarantee the technology is working correctly and helps the officers orient themselves with the area. Every 15 minutes, an officer plots our position either by using GPS coordinates, radar returns, or fixed land triangulation using an alidade. This last mode of determining our coordinates, at least to me, is the most difficult. You must use 3 fixed land points on either side of the ship, determine their direction using the compass on the alidade and then using sliding protractors plot our triangulated position on the chart. Both Executive Officer (XO) Michael Gonsalves and ENS Cabot Zucker have been incredibly helpful in teaching me these different plotting techniques.

XO Gonsalves in the foreground and ENS Zucker in the back plotting our course.

Today we are headed to the Queen Charlotte-Fairweather Fault System. This is a strike slip fault line extending 746 miles off shore of Vancouver Island to the Fairweather range in southeast Alaska. USGS has partnered with NOAA Ship Fairweather to help to create part of a comprehensive map of one of the fastest moving underwater tectonic plates in the world, moving of a slip rate of 2 inches a year. Over the next 24 hours they will survey the area using multibeam sonar to help complete the mapping which as taken almost 4 years to complete.

To start this, the survey team had to deploy a Moving Vessel Profiler (MVP) into the water. The MVP follows behind the ship and by detecting water temperature and salinity of the water, the MVP can then determine the speed of sound in water needed to accurately detect the sea floor. With this knowledge the survey team can correctly calibrate their sonar to map the sea floor. Below you will see Sam Candio and Simon Swart of the survey team deploying the MVP.

MVP, Moving Vessel Profiler

Sam and Simon deploying the MVP

Survey technicians Sam Candio and Simon Swart view the MVP controls

Next blog will cover the amazing people working with the sonar, all times of day and night to make the sea floor maps! (Stay tuned!!)

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Another short term visitor on this ship is a college student from Loyola University Chicago, Paul Campion, who is on board doing an internship with NOAA. Each year NOAA accepts approximately 130 college sophomores into their two-year-long Hollings internship program to give students an opportunity to take part in research, gain job experience and see what NOAA does. While on board, Paul has been working with the survey team to learn how they do their work, as well as create his own project. Paul has been looking at the electronic navigational charts (ENC) used today by most mariners which show the depth of the sea floor. As NOAA Ship Fairweather surveys an area, these ENC’s can then be updated with more accurate and up to date data. While some areas may remain the same, some areas may show changes or even characteristics which may not have been mapped prior and need to be highlighted. Paul has been working to help create an efficient way to show where the ENCs are different to the new NOAA Ship Fairweather data and may need to be altered or updated.

Personal Log

Since we are out in the sea, and do not have neighboring island chains around us, the boat has been tossed around a bit more and is definitely rolling around in the waves. Luckily, I have not been sick… yet. I have been taking sea sickness pills, and making sure I get plenty of fresh air, but the boat is definitely more difficult to work in. You find yourself moving both with the boat’s inertia and then having to fight against it to move. Walking uses walls and railings, sitting requires holding on to the closest counter top or nailed down object and to get into rooms you need to shove doors away from you to open them, yet hold on so they don’t swing completely away from you and slam the opposite wall. It is kind of challenging and yet amusing.

After lunch today, I went to take a shower. I was given some good advice since I had not done this when the boat was in open water. These words of advice included: Use the walls, kind of squat down to lower your center of gravity, don’t take a razor with you (nothing good will come of that), and if the soap drops be especially careful! All things I took to heart and I am glad to report I am clean, unscratched and ready for another day.