Philip Hertzog, July 29, 2005

NOAA Teacher at Sea
Philip Hertzog
Onboard NOAA Ship Rainier
July 25 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: Aleutian Islands, AK
Date: July 29, 2005

Tide gauge equipment
Tide gauge equipment

Weather Data from Bridge

Latitude: 58˚ 53.36’ N
Longitude: 158˚ 50.4’ W
Visibility:  10 nm
Wind Direction: light
Wind Speed: airs
Sea Wave Height:  0 feet
Sea Water Temperature:  12.2˚ C
Sea Level Pressure: 1013.5 mb
Cloud Cover: 8, cumulus, stratocumulus, altocumulus

Science and Technology Log 

Today I worked on what the hydrographic map makers call “vertical control” and “horizontal control.” When NOAA makes maps showing how deep the water is, they have a problem in that the depth changes when the tides come in and go out. If a rock exists in the water, there may be no problem at high tide, but ships can run into the same rock at low tide.

hertzog_log5To overcome this problem, NOAA measures bottom depths on their charts starting at a constant elevation called mean lower low water.  Low tide occurs twice a day, but one low tide is always lower than the other.  By keeping track of all the lowest, low tides of the day and averaging their elevations over many years, scientists can come up with an elevation for mean lower low water (MLLW).  You want to start measuring from your lowest tide level to ensure that ship captains can trust the chart to protect them from danger even during low tide. All of the ocean bottom charts are based on depth below MLLW.  However, when you collect sonar data, your height above MLLW constantly changes with the tide in a vertical position (up and down). Hence the term “vertical control” because the chart maker needs to know how to correct the sonar data so the maps are based on MLLW, not the current tide height. In remote areas like Alaska, limited tide data exists so the RAINIER crew installed a device called a tide gauge to measure and record the rise and fall of the tide in the mapping area.  The information from the tide gauge will help us to correct the sonar data so we can make the charts based on MLLW.

Working with the equipment
Working with the equipment

The RAINIER crew installed a tide gauge on Mitrofania Island 1.5 weeks ago before I got on board. Today I rode in an open boat to help the crew check the tide gauge.  Ensign Andrew Halbach led our mission with assistance from Survey Technician Matt Foss and Ensign Laurel Jennings. Mike Laird, the other Teacher at Sea also joined our group. Carl Verplank, Ordinary Seaman, drove the skiff and stayed off shore after dropping us off to ensure the boat won’t get stuck when the tide goes out.  Carl had the best job because he fished for salmon until we needed a pick up. I hope he shares some fish with us tonight!

Upon reaching shore, Matt Foss and I walked over to the tide gauge station to check it out. Matt carried “bear repellant” with him which is pressurized pepper put into a spray can. If a grizzly bear should approach and attack us, the pepper spray might keep the bear from eating us.  On the other hand, maybe bears like to have a little pepper on their steaks. In any event, we need to stay alert in bear country.

GPS work
GPS work

We found the tide gauge in good working order.  Matt told me that Scuba Divers helped to put the gauge in and that it sends tide information via satellite back to Washington, DC for further analysis.  Now that our vertical control (up and down movement) has been taken care of, Matt and I hiked over to join Ensign Halbach and Ensign Jennings who are working on “horizontal control” or side-to-side motion.

Normally, the crew of the RAINIER knows its horizontal position through the use of global positioning satellite (GPS). As discussed in previous log entries, GPS works by using signals from several satellites to locate your horizontal position on the Earth in terms of latitude and longitude.  The chart makers combine sonar data with GPS data to create accurate maps of ocean bottom depth.  Atmospheric conditions can affect the satellite signals so scientists calculate correction factors. Special radio stations transmit these factors which allow the launch crews to correct the GPS data. These corrections are called “horizontal control.”

Unfortunately, the remoteness and steep mountains of the Mitrofania Island area prevent the RAINIER from receiving good radio signals.  We need to set up our own radio transmission and GPS base station to get good control.  This task took up the rest of our day.

Matt and I found the others busily setting up the GPS station and taking measurements to ensure good location information.  Ensign Halbach carefully leveled the GPS antenna and oriented it towards north. After setting up the GPS station, Carl picked us up and drove the open boat to another location about a mile away where we repeated the process and set up a second GPS station. However, constructing the radio transmitter tower proved to be our big challenge. Nobody in our group ever set up a tower before so we worked as a team to figure it out. We returned to the RAINIER and hit the machine shop where we measured out metal, drilled boltholes and scavenged any thing to help us build the tower.

We carefully load the skiff and quickly motored back the mile across the water to the transmitter site located on a sand bar that sticks out into Mitrofania Bay.  Ensign Halbach led us in constructing the tower and it went up faster than planned.  Two people hold the tower straight up and balance it while the other three string guy ropes to metal stakes pounded in the ground. The tower made us proud of our team work, but no one dares to climb it.  Maybe some of you students reading this log entry would like to come to Alaska and try to climb it.  We returned to the RAINIER and could see our tower on the horizon where it will transmit horizontal control data to all the launches conducting sonar work over the next two weeks.

Personal Log 

This was the most physical day yet on the research vessel.  I actively participated in setting up the tower instead of just observing.  I really enjoyed working in a team today and helping to solve problems.  I also had a good physical workout by carrying heavy equipment to the GPS and radio transmitter sites.  The work out really helped because the food on board the RAINIER is delicious and plentiful with three large cooked meals a day.  I need to watch my weight on this trip.

The tower project showed me you need both technical training and practical construction skills when out in a remote area like Alaska.  My students tend to be either hands-on or all academic, but you need a balance of both these skills to be successful upon graduation. Many of the crew on the RAINIER learned their jobs while on the boat and had to solve difficult problems without any outside help. Hopefully my students can use the RAINIER’s crew as an example on the importance of seeking balance in their lives. Speaking of balance, it’s time for me to catch a salmon.  Here I am ready to go. See you tomorrow.

Question of the Day 

What causes the tide to rise and fall and how does it change over the course of an entire month?

Philip Hertzog, July 28, 2005

NOAA Teacher at Sea
Philip Hertzog
Onboard NOAA Ship Rainier
July 25 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: Aleutian Islands, AK
Date: July 28, 2005

Launch lowering into the water
Launch lowering into the water

Weather Data from Bridge

Latitude: 55˚ 53.36’N
Longitude: 158˚ 58.4’ W
Visibility:  10 nm
Wind Direction: light
Wind Speed: airs
Sea Wave Height: 0 feet
Sea Water Temperature:  12.8˚ C
Sea Level Pressure: 1013.2 mb
Cloud Cover: 5, cumulus, altocumulus

Science and Technology Log 

I awoke to a beautiful sunrise and partly cloudy skies.  The waters of Cushman Bay calmly rock the RAINIER gently back and forth.  I could see pink salmon jump near the ship and seabirds feeding in the water. Mike Laird (the other Teacher at Sea) and I stayed on board the RAINIER today to catch up on our log entries and to see what the rest of the crew does.  We had a quiet day of writing, talking to the crew, and taking photographs.

At 8:00 am I watched the deck crew lower the launches for the mapping teams.  Lowering the launches can be dangerous work and the deck crew does it carefully while wearing hard hats. Two winches move each launch out over the water as shown here (left and right) and then survey crew board the vessel and load gear.  After the survey crew loads the launch, they work with the deck crew to disconnect the cables and hooks from the launch. The launch then speeds off to start a busy day of mapping the waters of Mitrofania Bay.

Launch in the water
Launch in the water

Once the launches left, the deck crew worked on other tasks.  I saw crew washing decks and maintaining machinery.  Other crew members used a crane to move one of the smaller boats (called skiffs) into the water: Other crew members went about the ship conducting other tasks such as preparing meals, keeping the engines running, contacting the launches to help solve problems, and conducting bridge watch. In later log entries, I will try to describe the different departments on board the RAINIER.

Personal Log 

I had a very quiet day and spent it catching up on paper work and cleaning up my digital photos. After looking at my photos and talking with XO Julia Neander, we decided that our whales from the other day are not fin, but Sei (pronounced “say”) whales.  We saw white spots on the whales back and a prominent ridge on the whale’s forehead which are give away signs for Sei. I spent the evening fishing for salmon off the fan deck (located at the rear of the ship).  Several other crew members also fished of the stern, but only Raul, one of our cooks, caught salmon. He pulled in four cohos weighing around 7-8 pounds each. Will he share and surprise us for supper tomorrow night? I can’t wait to find out.

Securing the lines
Securing the lines

Question of the Day 

The RAINIER is like a small community made up of 50 people.  What kinds of jobs does this community need in order to sustain it for 3 weeks at sea without any outside help?

The launch in action
The launch in action

Philip Hertzog, July 27, 2005

NOAA Teacher at Sea
Philip Hertzog
Onboard NOAA Ship Rainier
July 25 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: Aleutian Islands, AK
Date: July 27, 2005

Securing the launch
Securing the launch

Weather Data from Bridge

Latitude: 55˚ 53.3’ N
Longitude: 158˚ 58.4’ W
Visibility:  10 nm
Wind Direction: light
Wind Speed: airs
Sea Wave Height: 0 feet
Sea Water Temperature:  12.2˚ C
Sea Level Pressure: 1012 mb
Cloud Cover: 2, cumulus

Science and Technology Log 

The RAINIER is now anchored for the next several days in Cushman Bay on the north side of Mitrofania Island. Today the ship’s crew began their first full day of mapping the bottom of the waters surrounding the island.  The Captain assigned me to observe operations on board one of the RAINIER’s six survey launches.  The launches are small craft equipped with sonar and computer equipment to collect bottom data as seen in the following photographs:

Each launch has a crew of three and four launches go out at a time.  On my launch, Ensign Brianna Welton serves as the hydrographer in charge with Matt Boles as the Assistant Survey Technician. Able Body Seaman Corey Mussey drives the launch and makes sure it stays on course using a computer screen directs him where to go.

A winch lowered our launch into the water. We jumped about two feet from the side of the ship to get into the launch. We carried no equipment in our hands or on our backs and wore life jackets to ensure we safely crossed the deep water.

Screen shot 2013-04-09 at 9.42.37 AM

Once underway, Ensign Welton turned on the Differential Global Positioning System (DGPS). The DGPS uses satellite signals to determine our location and even can tell our direction and speed. Unfortunately, our DGPS did not work correctly and Ensign Welton and Matt Boles struggled over the next 2 hours to trouble shoot the problem.  When out at sea and hundreds of miles from the nearest repair shop, the crew of the RAINIER has to become creative to solve problems in order to achieve their mapping mission.  The DGPS problem finally got fixed after the antenna was taken apart and the connecting cables cleaned. Matt told me that whenever one starts a new field survey, you commonly find problems that must be fixed due to the difficulties of working in the harsh environments found at sea and in Alaska.

Screen shot 2013-04-12 at 9.05.01 PMWith the DGPS fixed, the crew sent a SEACAT probe through the water column to the bottom to collect temperature, salinity and pressure data.  Sonar mapping works by bouncing sound waves off the bottom and measuring how fast the waves return to the ship. Sound travels through salt water at 1435 meters per second, but its speed can be changed by temperature, salinity or pressure.  The computer takes the data from the SEACAT and makes corrections to the sonar data so we have a better measurement of the bottom depth.

Sunset over the bow
Sunset over the bow

We spent the rest of the day running transects to map the bottom. Transects are long, parallel lines that are spaced to ensure we cover the entire bottom of the area being mapped with some overlap. To better understand what “running a transect” means, think about mowing your lawn.  When you mow the lawn, you run the mower in parallel lines, but you always go over part of the path you mowed before in the previous line. Just like mowing, the sonar is able to map the entire bottom of the map area by using a transect pattern.

Around 4:30 pm we returned to the RAINIER and the deck crew winched the launch back on board. I handled the stern line and threw it to a deck hand on the ship. I also attached the hook from the winch onto the launch, but I didn’t do it correctly on my first try. You have to be careful because the launch weighs 14,000 pounds and the seas can bounce it around. I got too close to the block and tackle on the winch, but Ensign Welton pulled me back and showed me how to properly connect the cables.  To the right here is a picture of Ensign Welton correctly hooking up the launch.

Once the launch returned to the RAINIER, the mapping crew’s duties were not f inished. After supper, the crew down loaded the launch’s computers onto the ship’s main frame and “cleaned up” the data.  Clean up consisted of looking at the data and matching it with maps on the main frame computer.  The survey technician also had to correct the data with tidal information and look for false sonar signals to remove from the data set. Upon finishing clean up, an officer checked the work for quality.  Here is a picture of Dan Boles, Matt’s older brother, cleaning up some data.

Personal Log 

I had a great time today going out on the launch and learning what the survey crews do.  The landscape overwhelms one with large open areas of water surrounded by mountains covered in green, low lying vegetation.  Mount Veniaminof dominates the background with its glacier covered dome that rises 7,075 feet above sea level.

As we traveled in the launch, I could see whales blowing spray out their blow holes in the distance and pink salmon jumping out of the water.  At the end of work, we took 10 minutes to fish off the launch and Matt caught a ling cod while I had one on the hook that got away.

I enjoyed talking to Matt Boles and learning about how he ended up on the RAINIER with his brother Dan. Matt has a two year college degree in computers and Dan has a Bachelors degree in geology and French. I see a lot of potential for my own students to get jobs aboard ships like the RAINIER and to have a great time exploring wild places like Matt and Dan.

Question of the Day 

Why do temperature, salinity and pressure change the speed of sound in water?

Kathy Virdin, July 25, 2004

NOAA Teacher at Sea
Kathy Virdin
Onboard NOAA Ship Rainier

July 20 – 28, 2004

Mission: Hydrographic Survey
Geographical Area:
Eastern Aleutian Islands, Alaska
Date:
July 25, 2004

Latitude:55degrees 17.215 N.
Longitude: 160 degrees 32.231 W.
Visibility:1 nautical mile
Wind direction:140 degrees
Wind speed: 10 kts.
Sea wave height: 0-1 ft.
Swell wave height: 2-3 ft.
Sea water temperature:10 degrees C.
Sea level pressure: 997.4 mb.
Cloud cover:Cloudy, light rain

Science and Technology Log

Today we had a visitor from Tenix Lads, Inc. named Mark Sinclair who does LiDAR depth readings for NOAA. LiDAR means light detection and ranging. It is done from a small aircraft, flying at an altitude of 1800-2200 ft. They over fly an area with two laser beams that measure the surface of the water and the depth of the water. They get the difference in these heights, with geometric corrections for tides and other factors, to give them the ocean floor depths. They are able to take an incredible 324 million soundings in an hour! Their information is used for nautical charting, coastal zone management, coastal engineering, oil and gas development, military applications and research and development. They will identify depths, buoys, beacons, lighthouses, kelp areas on digital display (via computers) and on spreadsheets. The benefits of the LiDAR technology is that it is very cost effective, has amazing speed, and greater safety. They do 200% coverage of an area by measuring lines and then taking new lines in between the first lines. They run a swath beam that is 192 meters, which is larger than the ones that the RAINIER does. Each beam of pulsar light is 15 meters with 4 meters in between.

They are finding changes that need to be made on maps that date back to the 1940s. NOAA contracts with this company to do soundings for them and NOAA picks small segments of these areas to do spot checks with the ship to compare accuracy. So far, they have been extremely accurate. At this point in time, they are not comfortable with the greater depth measurements that the RAINIER does, but expect that to change in the future. Various crew members that I’ve spoken with foresee this becoming the depth measurement instrument of the future. Eventually, all depth readings may be done from satellites, which could become very accurate, as well as safe. Right now, NOAA will continue to use both methods.

Personal Log

I spent the day working on the computer, listening to the LiDAR presentation and reading the information about this new system. It’s very interesting to predict how useful this will become in the next 10-20 years. I’d love to see some of my students flying the airplanes that will send back this newer technology. Right now, the RAINIER is anchored while launches go out to do shallow survey each day. It’s fascinating to watch them lower the launches and bring them back onto the boat. They use hydraulic winches that raise and lower the boats. Everyone has to be very careful at this point, wearing hard hats, because it’s a time when equipment failure could bring a dangerous situation. Generally three or four people go out on each day’s launch. They have several more days of launches scheduled, then they must go to the Kodiak Coast Guard base to refuel.

Virdin 7-25-04 screenshot

Kathy Virdin, July 24, 2004

NOAA Teacher at Sea
Kathy Virdin
Onboard NOAA Ship Rainier

July 20 – 28, 2004

Mission: Hydrographic Survey
Geographical Area:
Eastern Aleutian Islands, Alaska
Date:
July 24, 2004

Latitude: 55 degrees 17.194 N.
Longitude: 160 degrees 32.23 W.
Visibility: 3 nautical miles
Wind direction: 100 degrees
Wind speed: 10 kts.
Sea wave height: 1-2 ft.
Swell wave height: 2-3 ft.
Sea water temperature: 10 degrees C.
Sea level pressure: 1002.0
Cloud cover: Cloudy with rain

Science and Technology Log

Today we went out on a launch (my first in the Shumagin Islands). We traveled near the area of Simeon Bight to run lines to check depth measurement. An example of why this is so important is that in one of their launches, they found after an earthquake, a 30 meter drop-off near a fault line. This wasn’t on any charts because it had been caused by the earthquake itself. Before they begin the depth measurements, it’s vital that they take a cast with the salinity, pressure and temperature instrument. This information is then hooked directly into the computer to be calculated into the depth findings, so that the depth can be corrected by these factors. We ran cross lines (lines that cris-crossed each other) as a quality check to be sure that no area had been missed. The transducer (which sends out a multi-beam swath of sound) is lowered into the water by a mechanical arm. This is high-tech stuff! The computers are also recording the GPS (global position system) location of our boat at all times. When we learn the depths of the waters we pass over, we have to know exactly where we are in order to record this on nautical charts. Out of 24 satellites, we need at least 5-7 within range plotting our location to ensure accuracy. The computers divide the screen into sections which show our depth reading, a picture of the ocean floor by sonar calculations and the range our instruments will accurately reflect. We have traveled a range of 88 meters in depth to 6.7 meters in depth. Interestingly, one possible technology that is being tested and may be the best method of the future is called Lidar, which means sonar transmitted from an airplane, which flies over coastal areas and can give a depth reading on land and in the ocean. The RAINIER is testing one area that has been measured by Lidar to compare our measurements with theirs to check their accuracy. This would be a safer method, since lowering the launch boats and retrieving them has a certain amount of risk.

We’ve just seen some lazy puffins that are swimming on top of the water, which makes them look like sitting ducks. As we return to the RAINIER in the late afternoon, we bring back a lot of data that the survey technicians will assess and correct to be submitted to the cartographers.

Personal Log

We had a rainy, foggy afternoon on the water while we were surveying, with clouds that hovered over the green, craggy cliffs. It makes a beautiful sight. We felt we got a lot accomplished and returned with some good data. In talking with various members of the crew, I’ve gotten some good ideas to use in my lesson plans as they help me think of ways to explain their operations that will simplify it, such as flashlights taped together to represent a multi-beam sonar swath. I’m going to catch up tonight on correspondence, and refine my lesson plan ideas tomorrow. I can’t wait to take all these ideas back to the classroom!