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.

Kathy Virdin, July 26, 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 26, 2004

Latitude:55 degrees 17.192 minutes N.
Longitude: 160degrees 32.214 minutes W.
Visibility: 6 nautical miles
Wind direction: Light
Wind speed: Airs
Sea wave height: 0-1 ft.
Swell wave height: 0-1 ft.
Sea water temperature:10.6 C.
Sea level pressure:998.9 mb.
Cloud cover: Cloudy

Science and Technology Log

Today I interviewed Nicola Samuelson, who is an ensign. Her job on the RAINIER is multi-faceted. She is responsible for the ship’s safety, must represent the Captain when he is not here, drive the ship from point A to B as assistant navigation officer, preparing the ship’s sail plan, and is also a morale officer, who plans activities for the crew when they are in port. She has an undergraduate degree and a master’s degree in ocean engineering. She works in four hour shifts and as an officer, may be on 24-hr. duty when the ship is in port. She chose this job because she enjoys the beautiful scenery, likes the important survey work they do, and enjoys working in a setting where you must bring a camera. She also has an interesting background that steered her in the direction of working for NOAA. She grew up on a sailing vessel as her parents sailed around the world. She was home schooled on the boat and sailed around the South Pacific from the time she was three years old until she was twelve years old. They would stop in various ports, such as New Caledonia, Fiji Islands, Samoa, New Zealand, Singapore, Malaysia, New Guinea, and Thailand when they needed to pick up supplies or work for a while. She only lived on land for the first time when she was 17 years old. She grew up speaking English and French as her parents spoke both languages. Because of her upbringing, she knew she wanted a job where she would be on the ocean. After graduate school, she received three months of NOAA officer training, where she learned firefighting skills, first aid, navigation, and how to drive a ship. She feels that her job is extremely significant, since some of the waters in Alaska have never been surveyed.

Virdin 7-26-04 map

An area that the RAINIER just surveyed, that covered 30 miles by 50 miles only had about 5 depth soundings. Ships would have to go around that area, because it’s just too dangerous to navigate through without the true depth measurements on the charts. A ship needs 40 feet of water clearance below deck level in order to successfully navigate the waters. Lack of accurate charts means that cruise and cargo ships are limited in where they can sail in the Alaskan waters. Opening up new areas, because of their surveys, means NOAA is contributing toward improvement of safety, commerce and tourism.

Personal Log

We have learned today, that because of an oil leak, the RAINIER will go into port early. We’ll have an all hands on deck meeting this afternoon to find out the exact plans. It will be interesting to find our how a ship this size will handle repairs. The weather has turned off pretty this afternoon, so those of the crew who are not working have gone on deck to fish. They will pack their catches in ice to mail back to their families. Fishing in Alaska is some of the best in the world!

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!

Leyf Peirce, July 14, 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 14, 2004

Time: 10:00
Latitude: N 55°17.24
Longitude: W 160°32.17
Visibility: 6 nm

Wind direction: 060
Wind speed: 1 knots
Sea wave height: 0 – 1 foot
Swell wave height: —
Sea water temperature: 10.0 °C
Sea level pressure: 1009.3 mb
Air temperature: 11.7 °C
Cloud cover: 7/8

Science and Technology Log

This morning I went out on launch boat 1 to conduct shoreline hydrography. Shoreline research differs very much from the other research I have seen so far, for it does not require “mowing the lawn” lines. Instead, it is a technique that is used to check the data collected from the LIDAR (airplane) labs. As I learned earlier this week, the data collected using a laser from the airplane primarily focuses on the shoreline and depths up to 30 meters. Today, we went along the shoreline checking questionable data points such as rocks and shoals that may have been confused with kelp or other variances in data collection. In order to do this checking, the survey technicians and officers conducting the research look at the LIDAR chart the day before launching and determine where rocks might be misplaced or not including at all. During surveying, which is what we did today, the researchers take a boat with a single beam echo sounding system and go to the places of concern. With some one on the bow to look out for uncharted rocks, the captain then drives over the areas where there might or might not be a rock. Because all of this is done very close to shore, it is very important to drive slowly. There is also a lot of kelp that can get in the way. Once the boat has past over the area a few times, the true depth is recorded as well as the position and a note is made on the chart where any changes need to be made to the chart. A relatively simple procedure, this type of shoreline research is critical for anyone planning to go on shore on any of these islands. Once again I was able to see how important this work is!

Personal Log

My morning was spent on the launch boat doing shoreline surveying. While the technology used was fascinating, I still did not hesitate to wonder at the naturally beauty of these islands. Almost completely uninhabited, these islands host wildflowers, puffin, gulls, and an occasional seal basking on a sandy or rocky beach. The green slopes are sharply cut by dramatic cliffs, creating a feeling of comfort and adventure at the same time. With the clouds dancing across these islands, I almost felt like I was about to see a dinosaur emerge from one of the cliffs—this looks very much like Hollywood’s rendition of “Jurassic Park”! This afternoon I plan on working on more lesson plans as well as a possible journey on another shoreline survey boat.

Sena Norton, July 13, 2004

NOAA Teacher at Sea
Sena Norton
Onboard NOAA Ship Rainier

July 6 – 15, 2004

Mission: Hydrographic Survey
Geographical Area:
Eastern Aleutian Islands, Alaska
Date:
July 13, 2004

Location: At anchor, Popof Strait, Shumagin Is. AK
Latitude: 55 deg 17.9’ N
Longitude: 160 deg 32.13’W
Visibility: 1nm
Direction: 116 deg
Wind Speed: 10 kts
Sea wave height: n/a
Swell wave height: 0-1 ft
Seawater temperature: 10.1 deg C
Sea level pressure: 1011.0 mb
Cloud Cover: 8/8 Fog
Weather: Foggy with drizzle and areas of rain 12.1 deg C (air temp)

Plan of the Day:
Four launches for shoreline verification and continuation of hydro in deeper water.

Science and Technology Log

I learned the process and background concerning shoreline verification. This process ties in nicely with my new understanding of the process of Laser Airborne Bathymetry and how the two connect together. Shoreline verification is a process where a launch surveys to the 4-meter line and in the process correctly locates any targets found close to shore. The launch actually touches the target, at times from multiple sides so that a true GPS tag can be attached to the feature. This process helps the survey crew make better sense of wide swath readings and discern between sonar “fluff” and true features. Sometimes kelp or other objects block the sonar from capturing an accurate image and in the case of larger objects they are required to be “eye ball” verified for all survey areas. Shoreline is also used to double check location of known targets for drift or geologic movement. In the case of these Alaskan waters, the bottom changes yearly and the same can be said for the shoreline. Rocks move, and sand drifts cause sediment build-ups in different areas and underwater features might not have been placed accurately on the chart in the first place. All these factors add in to the need for physical shoreline verification of the survey swaths.

The jet boat launches are able to go almost all the way into shore but are not used until a prop motor launch has already done a through evaluation of the grid. According to the coxswains, shoreline is one of the more nerve-racking operations that they conduct. They are in shallow water trying to find hazards to navigation and they are still asked to safely navigate themselves. At times they are going into pockets almost blind because of the initial survey information being a tad sketchy. After of day of shoreline the coxswain is mentally and physically worn out.

Personal Log

Last night was a fun night on board, a group of crew and corps officers played some board games and let off some steam. This really is a fun crew to be around they are ready to have a good time and I believe they genuinely enjoy each other’s company. (Even if at times I know they drive each other crazy!) I am feeling more a part of the ship now as ever before, everyone is a friendly face and people are interested in what I am doing and what I do on dry land. They are very supportive of teachers and education and that is a boost to my morale because I feel supported in what I am doing here.

I have also enjoyed the time made available by being on board to work with the other TAS and collaborate with lesson ideas and simply “talk” to each other. Many times the one thing that teachers starve for is a chance to really get down and work with their colleagues. We are already planning on linking our classrooms, like Sister Classes for projects, pen pal and even to track the weather on opposite sides of the U.S. An added benefit is that she also just finished her first year of teaching and teaches at the same middle school level and I do. We have our careers in common and seem to have similar ideas on the direction of science education and its benefit to our students. We have completely different experiences as an educator because I teach in public school and she teaches in a small private school, but hearing the experience of the other has put a perspective not only on education but also on my professional/personal goals for the future of my career.

Question of the Day:
What is a “gyro” and why is it used on a ship?

A “gyro” or gyroscopic compass is the ships compass that is always pointed at the North/South axis no matter what the ship is doing in the water. It can be compared to a child’s top in the way that it works. It is important for a ships compass to be oriented in the N/S axis to accurately navigate and find the exact lat/long point. A compass will always point toward magnetic North which is about 1,600 km south of the North Pole (where all the meridians of longitude converge).