Kristin Joivell, June 20, 2009

NOAA Teacher at Sea
Kristin Joivell
Onboard NOAA Ship Fairweather
June 15 – July 1, 2009 

Mission: Hydrographic Survey
Geographical area of cruise: Shumagin Islands, Alaska
Date: June 18-20, 2009

The boom lowers the launch into the foggy morning air.
The boom lowers the launch into the foggy air.

Weather Data from the Bridge 
Position: Koniuji Strait
Clouds: foggy
Visibility:  less than 0.5 mile
Wind: 11 knots
Waves: 2 feet
Temperature: 8.6 dry bulb
Temperature: 8.0 wet bulb
Barometer: 1005.9

Science and Technology Log 

Launches are used to acquire data in areas where it doesn’t make sense for larger ships to go.  They are more maneuverable and their hulls don’t extend as far into the ocean.  Small crews can travel in the launches and work together to cover specific areas, commonly called polygons. This week, we are using the launches to survey the ocean floor in the Koniuji Strait area. Getting ready for the launch requires some preparation. Dressing for the weather is a must; so layers and layers of clothing are necessary, especially on foggy, chilly days.  Additionally, a float coat or life jacket vest and a hard hat are necessary for safety reasons. There are a lot of lines and cables moving around when a launch is being deployed and the safety equipment helps protect everyone involved.

I’m watching the computer screens as multibeam data is collected.  The screen on the right shows the depth coloration of the line being swept.
I’m watching the computer screens as multibeam data is collected. The screen on the right shows the depth coloration of the line being swept.

Launches use a device called the Multibeam Echo Sounder (MBES, or commonly called the multibeam) to collect data about the ocean floor.  The mulitbeam is a device that sends out sound waves.  The sound waves bounce off the ocean floor and then back to the launch. The sound waves are commonly called “pings.” It is necessary to watch a computer screen to ensure that the pings are being collected to the fullest capacity. Sometimes adjustments must be made because pings are being lost or there is too much interference, or noise, in the data acquired. Another computer screen that must be watched shows the depth of the ocean floor being surveyed.  Depths are color coded throughout the spectrum with reds being shallow and violets being deep. Watching the depth coloration helps to predict when ocean floor features may be changing from deep to shallow and vice versa.  It is also possible to infer where ocean floor features like hills and valleys may be located.

Here, I prepare to cast the CTD in order to get a reading for conductivity, temperature, and density.
Here, I prepare to cast the CTD in order to get a reading for conductivity, temperature, and density.

Other computer screens show different views and aspects of the data being collected from the multibeam.  These screens help to troubleshoot problem areas and make decisions about data being gathered. In fact, there are four computer screens to watch while using the multibeam!  Multitasking is a necessity when you are the person in charge of the computer screens. Multibeams collect data from the ocean floor in wide sweeps so that no area is missed or skipped over. Overlaps are also built in to help prevent missed areas.  Sometimes an area is missed; these areas are called “holidays.”  It is sometimes necessary to resweep an area to fill in these holidays.  The driver of the boat helps to keep the boat on the line being swept.  Additionally, the driver helps to keep the boat traveling at approximately 6 knots so that data can be collected at the appropriate speed. This job is more difficult than it looks especially in a thick fog.

The use of the CTD device is necessary when collecting data from the launches.  CTD stands for conductivity, temperature, and density.  Since ocean water can vary in all of these depending on location, the CTD helps collect this information.  The information is then uploaded into the computer system on board the launch.  The sound velocity is determined using a formula containing these readings.  Then, the computer helps to correct for differences in the ocean water when using the multibeam.  A cast on the CTD is usually done every few hours.

Personal Log 

I attempt to work the line
I attempt to work the line

Launches are great for acquiring data, but they require the assistance of many people to be used effectively. Plans must be made to create polygons to survey.  People must use the radio to retain communications with the bridge of the main ship.  Different people are responsible for working the lines, or ropes, that attach the launch to the ship.  People must be able to use the multibeam computer software and information for the CTD appropriately so that significant data is collected. Someone must drive the launch so that it follows the lines for the sweeps.  People from the engineering crew must maintenance the launches so that the engines work properly.

Each of these jobs requires certain training and experience to be completed in an effective way.  I attempted to work the line to attach the launch back to the ship.  It was difficult to keep the line untangled and throw it to the receiver in the correct location.  I also attempted to steer the launch along the line for a sweep, but found myself overcorrecting and going in circles much of the time. It amazes me how the launches involve such a wide variety of skills and knowledge.  With each task being accomplished, there are different problems that present themselves.  Knowing how to deal with those problems involves a certain kind of personality. Being flexible, knowledgeable, and able to think on your feet while still remaining calm seem to be very important skills when working at sea!

In this picture, you can see the NOAA ship traveling while using the multibeam.  The glowing material coming out of the ship represents the actual pings. The green area is the portion of the ocean floor that is being surveyed.  Picture provided courtesy of NOAA training materials.
In this picture, you can see the NOAA ship traveling while using the multibeam. The glowing material coming out of the ship represents the actual pings. The green area is the portion of the ocean floor that is being surveyed. Picture provided courtesy of NOAA training materials.

Create Your Own NOAA Experiment at Home 
You can simulate the way that the NOAA multibeam devices acquire data to help you get a better picture of how this complicated system works.  Using a paint roller, some paint, and a piece of cardboard, you can better envision the sweeps of the multibeam system.  First, draw a sketch of your cardboard on a piece of paper.  You can even add islands and land features to the cardboard to make it more complex.  Determine shapes of polygons that you will be sweeping; squares and rectangles work well in large spaces, but you may need to create some different shapes around your islands and land masses.  Lay out the cardboard on a flat surface.  Then, use the paint and roller to make wide sweeps on the cardboard.  You can even use different colors of paint for each line you sweep to keep your information more organized.  Since the paint and roller are simulating the path of the launch, try to keep your paint and roller going at the same speed (remember in a launch this would be around 6 knots).  Try not to create any holidays during your sweeps because you will need to go over those again.  The picture below may also help you to visualize how multibeam works.

 

Kristin Joivell, June 17, 2009

NOAA Teacher at Sea
Kristin Joivell
Onboard NOAA Ship Fairweather
June 15 – July 1, 2009 

Mission: Hydrographic Survey
Geographical area of cruise: Shumagin Islands, Alaska
Date: June 17, 2009

A launch is deployed in preparation for the day’s tasks.
A launch is deployed in preparation for the day’s tasks.

Weather Data from the Bridge  
Position: Big Koniuji Island
Clouds: Light Drizzle
Visibility: 5 miles
Wind: 17 knots
Waves: 2 to 3 feet
Temperature: 8.0 dry bulb
Temperature: 7.1 wet bulb
Barometer: 993.4

Science and Technology Log 

Today I had the opportunity to travel to Herendeen Island in one of the launches.  The two main tasks that I worked on were placing a new benchmark and taking measurements from a tidal gauge.  Benchmarks and tidal gauges are used to help the surveying team vertically reference their survey data to the tidal datum.

The first task to accomplish after landing on the island was placing the new benchmark.  Benchmarks can be found in many places.  You might even walk near a benchmark everyday and not even be aware of it! The national geocaching website describes a benchmark as “a point whose position is known to a high degree of accuracy and is normally marked in some way.” On this website, you can also search for benchmarks in an area by typing in the zip code where you would like to search. I’ve seen benchmarks in my travels hiking and biking; one was even near an old fire tower.  Benchmarks can be very old, but today I helped to place one that was brand new! I think the most exciting part about placing the benchmark was the knowledge that it is a permanent fixture.  Years from now, I will be gone, but the benchmark I helped place on Herendeen Island will still be there!

Here I am drilling the hole to insert the Here I am pounding the benchmark into benchmark’s post.  Later this hole will be place.  Later, this benchmark will be filled with cement to preserve the integrity of surveyed and its exact location recorded the benchmark’s location. and added to the database.
Here I am drilling the hole to insert the Here I am pounding the benchmark into benchmark’s post. Later this hole will be place. Later, this benchmark will be filled with cement to preserve the integrity of surveyed and its exact location recorded the benchmark’s location. and added to the database.

The second task that I worked on today involved some very basic process skills of science:  observing, recording, and calculating data.  My task was to record the level of the ocean’s water using a tide staff. I watched the water for one minute over six minute intervals for three hours.  During that one minute, I recorded the high and low water levels displayed on the tide staff. Then, I calculated the average of those water levels to be used by the surveying team.  This important information helps the surveying team reference the measurements from the automatic tide gauge to the benchmarks we installed.

I reached an understanding of the importance of this type of data collection by thinking about a ship traveling through the ocean during high tide and then during low tide. The ship traveling at high tide might read 30 feet deep on their depth gauge, but the same ship traveling at low tide might read 20 feet deep on their depth gauge. If the ship’s hull is close to those depths, it may be in danger of scraping the bottom. Knowing the depth of the water at the lowest of the low tides is important for the safety of the ship traveling through the water.

Even though the tide staff had been placed some time ago, it was still embedded firmly in the rock.  However, the seaweed growing on the rocks near the base of the tide staff seemed to be getting in the way of the observations initially.  This required some cutting and trimming of the material to improve data accuracy.  I think this is a good real world example of reducing the number of variables in an experiment that can’t be overlooked.

Here I am collecting data from the tide staff on Herendeen Island. You can see the excess seaweed throughout the water and near the shore.  This factor proved to be a troublesome variable in the initial stages of data collection.
Here I am collecting data from the tide staff on Herendeen Island. You can see the excess seaweed throughout the water and near the shore. This factor proved to be a troublesome variable in the initial stages of data collection.

Personal Log 

Yesterday, I was part of a shore party in the small port town of Sand Point.  The ship needed to stop there for a personnel change and to pick up some mail from the post office. In my past travels, I saw some small fishing villages in Costa Rica, Venezuela, and Mexico, but here is a town in the United States whose existence revolves around fishing. The docks seemed to take up much of the area of the town. There were many boats docked there and the majority of which were fishing boats. I even got to see some boats coming back from the day’s fishing trip and begin to unload their catches. There were also people working on boats, nets, and general items associated with the fishing trade. Some boats looked like they were abandoned, but most looked as if they were used daily.  Living and working near the ocean must be an interesting life, especially in such an isolated place as Sand Point, Alaska.

Create Your Own NOAA Experiment at Home 
You can collect and record data using the same technique that NOAA scientists use for their tide staff data experiment.  Select an area in your backyard on which to make observations.  Perhaps a simple selection such as the growth rate of the grass would be appropriate for your first attempt at this experiment.  Next, decide on your observation times.  It’s a good idea to make your observations at the same time each day so that you can compare results and reduce variables.  Finally, you’ll need something to record your data, usually a pen and paper, but you could also take a photograph for data collection.  Record your data and try to make inferences and draw conclusions based on the data collected in your experiment.

Here I am posing near a boat on dry land in Sand Point.  It is interesting to note how much square area of the boat will be under water when launched; this helps illustrate the point of the importance of hydrography.
Here I am posing near a boat on dry land in Sand Point. It is interesting to note how much square area of the boat will be under water when launched; this helps illustrate the point of the importance of hydrography.

Leyf Peirce, July 9, 2004

NOAA Teacher at Sea
Leyf Peirce
Onboard NOAA Ship Rainier

July 6 – 15, 2004

Mission: Hydrographic Survey
Geographical Area:
Eastern Aleutian Islands, Alaska
Date:
July 9, 2004

Time: 16:00
Latitude: N 55°26.60
Longitude: W 159°33.97
Visibility: < 1 foot
Wind direction: 221
Wind speed: 13 knots
Sea wave height: 0 – 1 foot
Swell wave height: 1 –2 feet
Sea water temperature: 10.6 °C
Sea level pressure: 1016.0 mb
Air temperature: 11.7 °C
Cloud cover: fog

Science and Technology Log

Most of my day was spent exploring the pages within Nathaniel Bowditch’s The American Practical Navigator: An Epitome of Navigation. I took notes mostly from a chapter titled “The Oceans”. It primarily discussed oceanography and the branches that are studied as a part of oceanography: geography, geology, chemistry, physics, and biology, “with their many subdivisions, such as sedimentation, ecology, bacteriology, biochemistry, hydrodynamics, acoustics, and optics” (427). With the main focus on the physical characteristics of the ocean, this chapter further detailed the importance of understanding salinity, density, temperature, and pressure—the main factors that affect most of the oceans’ behavior. There are several concepts within this chapter that can be watered down for my sixth, seventh, and eighth graders, however the one most applicable to hydrographic research is the study of the speed of sound waves within salt water. Because echo sounding is used to chart the ocean floor, the speed of sound within saltwater is essential to ultimately creating nautical charts. According to Bowditch, the speed of sound within a given fluid can be calculated using the following equation:

U = 1449 + 4.6T – 0.055T2 + 0.0003T3 + 1.39(S – 35) + 0.017D

In this equation:

U = sound of speed (m/s)
T = temperature (°C)
S = salinity (psu)
D = depth (m)

Using this information, one can calculate the speed of sound given different parameters. These measurements are determined using a CTD test (conductivity—which correlates with salinity, temperature, depth test) and a depth probe about every 4 hours that we are conducting hydrographic research. This information is then accounted for when employing the echo sounding devices. This equation can also easily be used by 7th and 8th graders. I plan on gathering real data and using these concepts in my classes along with graphing the data and outcomes.

While I read a lot today, I also got to tour the engine room. I have seen many engines and know the basics of how they work, thanks to my Mechanical Engineering degree, but I have never seen one so powerful! The twin 1200 horsepower engines can have up to 210 RPM. There are also two generators aboard the ship. What amazed me most on my tour was the control room where the control board looked like ones I have seen in museums—I thought that they would have moved to computers by now! One of the engineers assured me that this switch would be made in the near future.

Personal Log

I woke up this morning to what seemed like even thicker fog—this is the third foggy day in a row! Feeling a new energy from sleeping so well, I decided to try to work out on the treadmill in the ships workout room. I was told about there being a TV and VCR, and knowing that the workout room is on the same level as the engine room, I decided to take a movie with me and play it very loud. While the movie and TV worked great, the treadmill was a whole new experience. In all my years of exercising and training, I have never been on a treadmill that pitches and rolls with a boat! I felt as if my running counted as twice the exercise since I was not only running forward on the treadmill, but I was also adjusting every step with the motion of the ship—a very odd experience! After 45 minutes of exercise, I decided I had enough. The rest of the day was spent reading Nathaniel Bowditch’s The American Practical Navigator: An Epitome of Navigation, thinking of ideas for incorporating the concepts into next year’s curriculum, and playing cribbage, a card game the other Teacher at Sea, Sena Norton, taught me. Lt. Slover also informed me that I will be going on one of the launches tomorrow to help conduct research! While he was reviewing the small boat safety, the fog lifted to reveal beautiful snow covered mountains and islands—we had stopped the hydro research with the Rainier and were headed to our anchor point near Egg Island. We are expected to anchor around 21:00, with a possible stop for fishing along the way. Just finished dinner, I am now sitting in the chart room, looking out the window at dramatic cliffs plummeting into the sea—a reminder that these islands are, in fact, formed from a volcanic chain. I can’t believe how green these islands are—I must be sure to take plenty of pictures. As I day dream at these islands that are reminiscent of the islands in the BVI’s, the fog horn goes off again—the first time in a few hours. I guess this is the changing weather of the Alaska coast line; I just hope that tomorrow there is no fog when we are out on the launches.

Question of the Day:

My sister, Dr. Shayn Peirce at the University of Virginia, emailed me some interesting questions. P.S. Shyla Allen was a great source for these answers:

Dr. Peirce’s questions:

“My questions for you…can the echo scanner detect a whale on the bottom of the ocean? If so, how do they know it’s a whale and not a rock bump in the ocean floor or something else.

2nd question: what is the difference in echo scanning that you’re doing on the boat and ultrasound that they use in biomedical diagnostics…(to image babies in the womb or ovarian cysts?) Both involve acoustic imaging…is the frequency or wavelength of the sound emitted and detected different? Obviously the biomedical application requires a much smaller resolution with less depth penetration while the ocean application requires large penetration depth and not as much resolution…by the way what is the resolution of the echo signal…a few square feet of the ocean floor? Could you pick up the signal of that 1 foot long wench you dropped in the BVIs at 150 ft ocean depth?”

Answers:

1) Yes, the equipment here can detect a whale at the bottom of the ocean. In fact, it can even detect a wreck very well! I saw an image yesterday of a wreck and you could see the mast and bowsprit and everything—very detailed! I am trying to get a copy of that picture. Usually the whale will be moving, so that motion will also be picked up and cause more “static” in the data that needs to be cleaned. This rarely happens though.

2a) The echo sounding aboard the Rainier and ultrasound that they use for biomedical diagnostics are actually the same process, just with different frequencies!

2b) The resolution of what is done aboard this ship depends on water depth and the size of the footprint left by the scanner; the deeper the water, the larger the footprint, and the less resolution. However, they are required to have a resolution of 3 pings per 2 square meters in a depth of 40 meters or less (given the equipment used, there are up to 240 pings in a 160 degree swath). 40 meters is chosen because that is the maximum draft of a tanker vessel. P.S. Allen told me that, unfortunately, the 1 foot wench I lost somewhere in the BVI’s is probably long gone and undetectable by the equipment used aboard this ship. However, in shallow water, she has been able to see not only lobster pots, but their mooring lines as well. Their mooring lines have about the same diameter as the mooring line we descended in the Caymans on our dive trip. I also asked if the equipment could pick up a diver. P.S. Allen said yes, but that it is VERY bad for your body—so much power!