Ginger Redlinger, July 22, 2007

NOAA Teacher at Sea
Ginger Redlinger
Onboard NOAA Ship Rainier
July 15 – August 1, 2007

Mission: Hydrographic Survey
Geographical Area: Baranof Island, Alaska
Date: July 22, 2007

One of five Geodetic Survey Benchmarks at Dorothy Cove
One of five Geodetic Survey Benchmarks at Dorothy Cove

Weather Data from the Bridge
Visibility:  4 Nautical Miles
Wind directions: 190°
Wind Speed: 6 Knots
Sea Wave Height:  0 – 1
Seawater Temperature: 12.8° C
Sea-level Pressure: 1010.0 millibars (mb)
Cloud cover: Cloudy &
Rain Temperature: 13.9° C

Mariner Words of the Day: Port & Starboard 

Port and starboard are directional words indicating the sides of the ship.  As you are facing the bow (front) of the ship, port is on the left side, and starboard on the right side. How to remember? Port and left both have four letters.

Science and Technology Log 

Position A
Position A

Today was the day that we wrapped things up in this area by re-surveying a few sections to improve the quality of the initial set of readings, took horizontal measurements of the water-level (by hand) in order to improve the accuracy of area mean tide (high and low) data, and prepared the ship to move south. I have written earlier about the attention to detail, safety, and teamwork in the day-to-day operations, the gathering and processing of data, and daily production of results.  Today I am adding the noticeable value of the work done by NOAA vessels as noted by a gentleman and his family who came to watch our tide gauge survey crew work this morning. He said, “You people with NOAA do a great job, and the folks in Sitka use your information all the time.  We are thankful that you have provided us with the information we need so we can enjoy navigating the waters around here.” That was a good way to start the day. I highly recommend that you read TAS Beth Carter’s description of mechanics and tools involved in Tide Gauge Surveys.

Position B
Position B

While it sounds easy, it is actually very challenging to collect accurate measurements to the specifications required for this work, which are to the millimeter. Everything has to be level and measured at precise locations using benchmark geodetic locaters installed. Using the same locations (the geodetic benchmarks) each time you take measurements ensures consistent use and interpretation of horizontal measurements. The horizontal measurements between the benchmarks tell us whether or not the land height has changed. This is important information to give context to any changes the tide gauge measures.  If the mean tide level has changed, you need to know if the land level has changed too! Much of the data we gathered today is also connected to the GPS (Global Positioning System.)  I have an old farmhouse and level is not a word I can use to describe most of it.  Making a precise measure by establishing a level place on a slippery, rocky beach makes taking measurements in my house seem like a piece of cake! The survey scopes at the benchmarks are looking across about 50 feet of water to their left at the picture on the left (below) – which is the rod at another benchmark.  The next picture is the rod at the third position, which would be on the beach about 90 degrees, and 50 feet to the left of the survey scope (and the same, but the right, of the rod on the other side.  When the lines connect, we have a triangle!

Position C
Position C

If you would like to see how challenging this can be, here is a simulation that reverses the location of the surveying scope eyepiece (with the crosshairs) and the rod (with the height indicators), but it will definitely give you an appreciation for the challenge of accurate measurement over distance: Imagine yourself with a standard size metric ruler and a piece of paper with a crosshair pen line about 10 cm long each direction. About one centimeter from the top and the bottom of the vertical line draw another crossing horizontal line 2 cm long, about 1cm on each side. Tape the paper to the wall across the room and walk to the other side facing the paper you just taped to the wall. Now hold up your ruler an arm’s length away, vertically, with the 0 on the bottom so you are reading the measure up from the bottom of the lines.  Close one eye.  Try to identify exactly the millimeter at each horizontal line, for each of the horizontal lines.  Could you line it up exactly? Was your ruler and paper both “level” so you could? Hard to see?  Hard to measure? Now you see how challenging this can be! Imagine making an accurate measurement over a distance of 50 to 75 feet! It is also important to note that multiple measures must be taken that have to agree on the same result, with allowance for a tiny margin of error (again, a two millimeter margin of error is allowed – that is one millimeter error for the upper half of the cross hair and one for the lower half).

Here is another view of the survey scope lining up with the rod. If you look at the bottom of the rod you can see Geodetic Benchmark.
Here is another view of the survey scope lining up with the rod. If you look at the bottom of the rod you can see Geodetic Benchmark.

In the case of Dorothy Harbor, there are five Geodetic benchmark markers.  When the line of sight is either obstructed, or too great to make an accurate reading, then a “turn point” is established.  The turn point is set on a turtle (not a real turtle) which is a heavy disk that serves as set location upon which to balance the rod so measurements can be taken. Measurements must be taken from, and at, each location that needs the turn point to ensure that the data is correct.  Since this data is used to ensure the accuracy of tidal data in this area, and to supply information to the GPS – it must be done correctly. In the natural environment, this is quite challenging.  The measurements are recorded on a PDA and returned to the ship for processing.  Right triangle geometry, simple algebra, or trigonometry can be used to determine the accuracy of the measurements at each point.  If you have the markers at two line-of-site points (say to your right and your left) and are measuring the distance from where you are to each of the two points, you can figure out from your findings what the distance is between the two line-of-site points. By moving the rods to each of the five markers, you can verify that the measurements made from each location are accurate.  Taking and using multiple measures is common sense to those who do it all the time like the NOAA crew.  For many people, learning why is important.  Some people learn it through building things — like the common sense rule to measure more than once before you decide to cut lumber, or to measure from two directions before you square a corner – you have to be sure you are right before you move to the next step!

Once we were done with our measurements we ate lunch, then began to disassemble the Tide Gauge measurement assembly. The divers came in later to remove the equipment anchored underwater, and everyone returned to the ship to prepare for the evening’s departure.  The crew was exhausted as we had to climb, wade, carry, move, hold, disassemble, dive, and concentrate intently on our tasks.  Tonight we head south at 2100 towards Ketchikan and begin surveying a different area tomorrow.

After helping the crew complete today’s work, I realized how difficult it is to gather precise measures by hand in dynamic, ever-changing conditions.  (The wind picking up in the middle of a read — moving the 15’ high rods just enough to throw off the desired accuracy – so you have to start all over, the trees interfering with the line-of-site between the benchmarks and rods – people pushing back tree branches, trying to triangulate points on an unstable rocky beach, you get the idea…) Despite all these challenges, the crew gets the job done. This is what the navigating public (and commercial navigators), appreciate about NOAA’s work.  As I heard, straight from the pilot and family of the Sitka-based pleasure craft anchored in Toy Harbor.

I also appreciated the seafloor mapping tools provided by the technology on the ship. What if we had to take seafloor readings by hand! (And hope that we had found all the submerged rocks!) I think technology for surveying has made mapping the seafloor easier, at least at the measurement stage : )

Question of the Day 

Topic 1: How are navigational charts, topographical maps, and road maps alike?  How are they different?  (The answer to this question will be explored in the next journal).

Topic 2: Where can you find a geodetic benchmarks in your area? Outside of your area: What is special about the markers that are used in Disneyland (not created by the USGS)?

Topic 3: What are the tools and techniques of surveying?

Beth Carter, June 27, 2007

NOAA Teacher at Sea
Beth Carter
Onboard NOAA Ship Rainier
June 25 – July 7, 2007

Mission: Hydrographic Survey
Geographical Area: Gulf of Esquibel, Alaska
Date: June 27, 2007

Weather Data from Bridge 
Visibility:  6 miles
Wind direction:  034 degrees
Wind speed:  5 mph
Sea Wave Height:  none
Swell Wave Height:  none
Seawater temperature:  12.2 degrees C
Sea level pressure:  1017.2 mb
Dry Bulb Temperature: 12.2
Wet Bulb Temp:  11.7
Cloud cover, type: 8/8, stratus and cumulus
Depths: 31 fathoms

Researchers are kneeling in a sitka spruce forest as they check the computer that is collects and records tidal data on a small island in Nossuk Bay, Alaska.
Researchers are kneeling in a Sitka spruce forest as they check the computer that is collects and records tidal data on a small island in Nossuk Bay, Alaska.

Science and Technology Log 

On Tuesday afternoon, June 26, I went out with a crew of researchers to check the equipment that collects tidal data for Esquibel Bay. There are six main pieces of equipment used to collect this data: 1) a cylinder of nitrogen, 2) a hose attached to the nitrogen cylinder that emits small bubbles of nitrogen into the water, 3) a computer that collects and records data, 4) a solar collector to power the computer’s battery, 5) a  transmitter that sends the data to a satellite, and 6) the tide staff (an actual wooden staff in the water), and GPS benchmarks. The staff is set and readings taken so that the vertical measurements of the staff are linked to the benchmarks. The gage, which is officially a “tertiary” gage, is set up concurrent with a “primary” gage that has been acquiring data for over one epoch (19 years or more). Sitka, Alaska, is the site of NOAA’s primary gage, which has similar tidal characteristics to the area that we are working now. Thus, only an amplitude and phase differential must be applied to the Sitka gage to get a water level for this area.  Without the staff readings, there would be no way to tie the “bubbler” level to the ground surrounding the gage site, and thus no way to recover the actual local vertical datum (water level) relative to the gage in Sitka.

The nitrogen cylinder slowly leaks bubbles through the hose, which are released into the water. When the tide is high, there is more water and pressure above the hose which makes it more difficult for the bubbles to escape the hose. When the tide is low, there is less water above the hose, and therefore less pressure, which makes it easier for the bubbles to escape. Readings are recorded digitally every six minutes, averaged every six seconds. Staff-to-gage measurements are also recorded every six minutes whenever the site is visited, and 3 hours’ worth are recorded at  installation and removal, so that the vertical measurements of the station  are effectively “tied” to the measurements at the primary water level station at Sitka. (Good Working Question: Download data from both  stations and compare the two – are there differences? Next, compare Sitka and Ketchikan and Kodiak – are there bigger differences?).

ENS Meghan McGovern, Junior Officer of RAINIER, and Shawn Gendron, survey technician, position the tripod which will hold the transmitter to collect the GPS information needed by the RAINIER.
ENS Meghan McGovern, Junior Officer of RAINIER, and Shawn Gendron, survey technician, position the tripod which will hold the transmitter to collect the GPS information needed by the RAINIER.

For some reason, the transmitter is not emitting signals that can be read by the satellite, and therefore by the scientists at NOAA headquarters. This is why the skiff took several technicians over to check the equipment to see if it is still functioning and recording properly. They downloaded the water level data to send to headquarters via email while also setting up GPS equipment so that an ellipsoidal (GPSrelative) height can also be linked to the orthometric (gravitational) elevation determined through water level measurement, and will return to the ship and process the GPS data. The tides are important to hydrographic surveying, because obviously, the water is deeper at high tide than at low tide. The goal is to collect accurate information on tides, and then combine that with the data collected by the launches, in order to get accurate depth information.  The tide-corrected depths on the chart they want to show are relative to the mean low low water, which is the average of the lowest of daily tides taken over the last 19 years. On the Atlantic Ocean, tides are semi-diurnal. This means that there are two high tides and two low tides per 24 hours. But, on the Northeastern Pacific, tides are mixed.  See here for more details.

Today, (Wed. June 27), the crew returned to the small island to check on the HorCon station, which stands for Horizontal Controls.  The RAINIER established this water level station in April of 2007, and set into place 5 benchmarks which are tied into the international framework of benchmarks that make it possible to utilize GPS, or Global Positioning Satellites to determine one’s exact location. RAINIER’s researchers placed a receiver antenna on top of a tripod, which was positioned exactly above the center of the metal disc benchmark cemented into a rock.  The antenna receives from some of the 11 Global Positioning System satellites that orbit the earth and constantly change their relative positions. For a final position to be accurate, at least four satellites must be recorded in two different sessions of more than six hours duration separated by at least one day. They connected the cables, turned on the GPS receiver and then waited for the satellite constellation (also known as the ephemeris) to be downloaded so that all available satellites could be tracked. The first satellite was tracked around 1 hour later, and then we left the island, as the equipment was to be left in place for at least 6 hours.  When we returned 6 hours later, 8 satellites had made contact, and the recordings were noted and will be taken for evaluation onboard the ship.

Anna-Liza Villard-Howe, the Navigation Officer of the RAINIER, explained to me that the GPS measurements of benchmarks are being conducted in order to get as precise a determination of sea level as is possible, so that all the hydrographic information collected by the RAINIER can be referenced to the ellipsoid. Sea level has changed in Alaska in the recent past due to glacial rebound, which means that as the glaciers recede, the land is actually rising. Also, many large earthquakes have occurred in Alaska in the last century, which also changed the shape of some landforms and affected sea level readings. Online Sea Floor Mapping Activity Targets Kids (CED, OCS). In celebration of World Hydrography Day, NOAA’s Ocean Service  Communications and Education Division, in cooperation with NOAA’s Office  of Coast Survey, launched a new educational offering — Sea Floor Mapping —  on the National Ocean Service Education Web site. It is designed for students at the 3rd – 5th grade level, and the media-rich activity teaches young people about mapping the seafloor and why it is important.  This activity also conveys information about NOAA’s missions of discovery and service. The Sea Floor Mapping Activity is available online here.

Questions of the Day 

  1. Why are tides in the Pacific and Atlantic different?  What are the factors that affect tidal changes?
  2. Look up a tidal chart for the inlet or beach nearest to your home.  How far apart are the high and low tides?
  3. Who (which country or countries/which agencies) is responsible for the maintenance of the 11 Global Positioning Satellites that are now orbiting the earth?  If a satellite fails, would it be replaced?  By what agency?

Personal Log 

While on the tiny island, one of the officers carried a shotgun…in case we met a bear!  I’m pleased to say we didn’t encounter a bear, but did discover animal scat, and two eagle feathers. One was a tail feather – beautifully white – and we didn’t collect the feathers because it is illegal to collect eagle feathers.  We also saw 7-8 harbor seals on a rock outcropping. We tried to sneak up on them to get good photographs, but they bobbed and rocked and slipped into the water before we got very close. Also, on the island I was surprised to find many clumps of saltwort, which Eastern coast students (and my first grade class!) should recognize from the mud flat near the salt marsh.  It tastes….salty! No surprise there.

On Wednesday, there were so many white gnats that we sent the skiff back to the ship for bug repellant. They were like No-See-Ems, only we could See Em and Feel Em!  We built a small, smoky fire, which made things somewhat better.   The highlight of the day for me was kayaking after dinner with the XO (Executive Officer) of the ship, and Ian Colvert, an assistant survey technician.  We saw a rainbow and paddled through a misty rain, then sunshine…a beautiful evening.

Barney Peterson, August 27, 2006

NOAA Teacher at Sea
Barney Peterson
Onboard NOAA Ship Rainier
August 12 – September 1, 2006

Mission: Hydrographic Survey
Geographical Area: Shumagin Islands, Alaska
Date: August 27, 2006

Intern Umeko Foster exploring the coastline of Cushing Bay on Mitrofania Island.
Intern Umeko Foster exploring the coastline of Cushing Bay on Mitrofania Island.

Weather Data from Bridge 
Visibility: 10+ nm
Wind :  light airs
Seawater temperature: 11.1˚C
Sea level pressure:1017.0 mb
Cloud cover: partly cloudy

Science and Technology Log 

The personnel aboard the RAINIER are from a wide variety of backgrounds and locations. They come from the southern states, America’s Heartland, cowboy country, the east coast, and the Pacific Northwest.  Many now call Seattle, RAINIER’s homeport, their home.  What follows are brief profiles with some officers and crew members that I spent time with on the ship.

AS Leslie Abrahamson and I talked while she was splicing lines (working on ropes to keep the ends from fraying or unraveling).  That is a fairly specialized skill and Leslie had ample time to practice while working for several years on Tall Ships. She was a teacher for over 5 years working with high school aged youths, in programs including  widely respected Outward Bound. Following graduation from high school in Long Island, New York, Leslie attended Stanford University in Palo Alto, California to study theater arts. At the end of her 3rd year she went to Shanghai and spent six months discovering the joys of outdoor life: hiking, camping, and trekking.  Meeting new people and having new experiences helped form her into an adventurous, self-reliant young woman.  She returned, finished college, got into SCUBA diving and boats, and began working on dive and whale watching boats. After working 24/7 with high school students in expeditionary learning projects, Leslie was ready for a change. She was hired as an Able Bodied Seaman working for NOAA.  Leslie has been accepted for graduate school and is considering an advanced degree in marine affairs and coastal zone management, but the training opportunities through NOAA are really attractive to her right now. She is enjoying working in the waters of the Pacific Northwest.

Survey Technician Matt Boles (right) locating tide gauge markers on Olga Island.
Survey Technician Matt Boles (right) locating tide gauge markers on Olga Island.

Umeko Foster is a second-year intern aboard RAINIER from California Maritime Academy. Raised in southern California, Umeko is looking forward to the challenges and opportunities of working aboard ships, either with NOAA or in merchant shipping. She spent this summer and last learning first-hand about living and working aboard an ocean-going vessel.  Umeko has worked in a variety of jobs aboard RAINIER. I most often found her standing watch on the bridge, or working on deck duties around the ship. She has worked on the hydrography survey launches, but hasn’t acquired specialized knowledge of the highly technical equipment used in surveying.  Her background at the Maritime Academy will qualify her as a 3rd Mate for work on ships.

Survey Technician Matt Boles comes from Tennessee.  With an Associate degree in Geographic Information Systems (GIS) he joined NOAA 18 months ago to gain some practical experience in that field before committing to a 4 year study program. One of the things that influenced his decision was his experience in an internship he did in 2004: the teamwork and positive attitudes of the crew he worked with made him want to become a part of the organization.  Matt feels that being in Alaska, far from his family has helped him to become more aware of possibilities and to develop a new set of values about environmental stewardship. His internship aboard the fisheries ship was his first ocean experience and gave him an appreciation for a new part of the world.

TAS Peterson with Lt. Ben Evans atop Olga Island.
TAS Peterson with Lt. Ben Evans atop Olga Island.

He has fine-tuned his goals toward a degree in aerospace science so he will be able to use his skills in remote sensing surveying in other applications such as aerial survey work.  He is strongly motivated toward helping people learn more about the world we live in and how to live in it wisely, hopefully avoiding future tragedies like the Exxon Valdez oil spill.  Matt, who got married just three months ago, says the hardest parts of his life at sea are being away from family for long periods of time and the lack of physical activity space aboard ships. As a musician (bass guitar player), outdoor enthusiast, and with a strong interest in aviation, Matt likes to spend his free time actively.  There isn’t much room to hike on the ship.

AS Leslie Abrahamson splicing lines aboard NOAA ship RAINIER.
AS Leslie Abrahamson splicing lines aboard NOAA ship RAINIER.

Personal Log 

I got a really good workout today. I went ashore on Olga Island with Field Operations Officer Ben Evans and Survey Technician Matt Boles.  Our job was to locate and document five brass survey monuments for positioning a temporary tide gauge on the Island next season. I served as photographer and we all scrambled around on the rocks looking for the brass plates fixed onto the rocks.

When we finished documenting locations we took a few minutes to climb to the top of the island for the view. ST Boles and I went straight up through the brush at about a 50˚angle and met Lt Evans on top.  He had found a better slope and walked right up. There was a pair of Bald Eagles circling and calling above the summit and the view was wonderful. After taking pictures we headed back down. Who would have ever thought I would be climbing like this in rubber boots?

You have to love these “XtraTuf’s!”

Linda Armwood, May 1, 2006

NOAA Teacher at Sea
Linda Armwood
Onboard NOAA Ship Fairweather
April 25 – May 5, 2006

Mission: Hydrographic Survey
Geographical Area: Aleutian Islands, Alaska
Date: May 1, 2006

Weather Data from Bridge 
Visibility:  10 nautical miles (nm)
Wind direction:  182°
Wind speed: 14 kt
Sea wave height: 1 ft.
Swell wave direction: 235
Swell wave height: 1
Sea water temp: 7.5
Sea level pressure:  1029.6 mb
Present weather: Partly cloudy
Temperature:  °C~ 7.5 dry/6.0 wet

Science and Technology Log 

The ship performed a procedure for collecting data from a selected area of the Gulf of Esquibel analogously compared to ‘mowing the lawn.’  In this process the ship actually sails up and down the selected area within the Gulf collecting various data.  As the ship sails, parallel lines are produced on the hydrography chart.  The hydrography chart is viewed via the DELPHMAP system during this entire process in the pilot’s house and the plotroom.  In the plotroom, rotating survey technicians monitor the area being covered with four computer screens and communicate with the pilot’s room when data collection is paused and when it is resumed.

The ship performs this process rather than the launches because the ship works in deeper water than the launches. Sound data was collected today with an instrument called the Seacat. In order to collect sound data with the Seacat the ship has to come to a complete stop. The Seacat is manually attached to cable that is housed with a structure called the ‘J’ frame.  The cable travels through two rotating blocks and the Seacast is manually deployed into the water until it reaches the bottom of the water.  It is immediately pulled back onto the ship, detached from the cable, and attached to a computer for prompt reading of the data known as a Conductivity, Temperature, and Density (CTD) caste.

Personal Log 

Thanks to FAIRWEATHER shipmates for answering all of my questions either verbally, with hand-drawn illustrations, or through demonstrations.  The tide staff stop observations that Ensign Gonsalves and I made were consistent with the automatic tide gauge readings. I’ve got the results to prove it!

Question of the Day 

Geospatial Semester and Environmental Science Students 

Give the length and width of the Gulf of Esquibel.  Also, include the name and geographic location of its land boundaries.

Mrs. Armwood

Stephanie Wally, August 31, 2005

NOAA Teacher at Sea
Stephanie Wally
Onboard NOAA Ship Rainier
August 29 – September 10, 2005

Mission: Hydrographic Survey
Geographical Area: Eastern Prince William Sound, Alaska
Date: August 31, 2005

Tide Staff Installation
Tide Staff Installation

Weather Data from Bridge 

Time: 1400
Cloud Cover: Low Clouds
Visibility: 10 nm (nautical miles)
Wind: 340°, 4 knots
Sea Wave Height: 0’
Swell Wave Height: 0’
Sea Water Temperature: 5.0°C
Sea Level Pressure: 1009.2 mb (millibars)
Temp: 11.7°C

Science and Technology Log 

The crew of RAINIER has been upbeat since yesterday’s successful installation of a tide gauge on an island close to the face of the Columbia Glacier.  Data from the temporary tide gauge will be collected to analyze changes in water level.  It is important to know the water level since other portions of the ship’s current mission depend on surveying the bottom in shallow depths.

The officers, surveyors, divers, coxswains, and crew worked together to ensure all aspects of the gauge were installed and operating correctly.  The weather proved to be the biggest challenge in the installation procedure.  We had periods of heavy rain, stormy seas, and near-freezing temperatures.  Thanks to our foul-weather gear, snack supply, alternating breaks, and sheer dedication of the team, we all returned safe and sound to RAINIER. We were welcomed by the CO, XO, and a warm meal from the galley crew.

Today we returned to the island in fairer weather to take bearings of the NOAA bench marks we laid in the rock.  By triangulating the position of each disc, their location can be recorded for future surveying and exploration.  Even though Global Positioning System (GPS) technology provides the station location, it is important to have a back up means of finding these bench marks in the future.  Who will look after our tidal gauge and bench marks while we continue our transit toward Valdez?  Hopefully the harbor seals, otters, and bald eagles!

Answer to yesterday’s question: 180° = South