Mike Laird, August 1, 2005

NOAA Teacher at Sea
Mike Laird
Onboard NOAA Ship Rainier
July 24 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: North Pacific
Date: August 1, 2005

Weather Data

Time: 13:00
Latitude: 55° 53.4 ̍ N
Longitude: 158˚ 50.4 ̍ W
Visibility: 10 nautical miles (nm)
Wind Direction: 225˚
Wind Speed: 10kts
Sea Wave Height: 0-1΄
Swell Wave Height: 0-1΄
Sea Water Temperature: 11.7˚ C
Sea Level Pressure: 1009.5 mb
Cloud Cover: Sky 8/8 covered; Lower level: cumulus Mid-level: altostratus High level: cirrus

Science and Technology Log 

Operating the RAINIER in port—as she transits from site to site, and as she lies at anchor acting as home base for the survey operations—requires that each of the ship’s “departments” functions efficiently with a small margin for error.  When things do go wrong, they must be handled using the resources available on the ship so that operations continue with as little down time as possible.  Perhaps the greatest resource onboard the RAINIER is her personnel.  Situations, like those listed below, continually arise and require those involved to demonstrate patience, innovation, problem solving abilities and determination:

  • A cable getting caught in one of the pulleys on a gravity davit just after it has been used to lower a survey launch at 8:00 to begin its day of echo sounding. The cable must be replaced and the davit operational by the time the launch returns at 16:30.
  • A crack in the hull of a launch (welded and “fixed” while the RAINIER was in port for three days in Kodiak) is allowing water into the launch at the rate of about a gallon an hour. The engineering people use some magic red goop to temporarily stop the leak until a permanent solution can be devised.
  • Electronic equipment is very temperamental (cables jiggle loose during transits through rough seas, components can overheat, software glitches rear their heads, etc.) and continually requires TLC to keep it happy and functioning.
  • Established, recognized Differential Global Positioning Systems (latitude and longitude data) and primary control stations (tide data) may not provide data that meets required specifications (because of their distance from the work area, topographic features, etc) necessitating the installation of temporary DGPS and tide station sites.

As a crew member, you never know what is going to come up and must always be willing and prepared to meet unforeseen challenges!

Personal Log 

Last night, after a day of recording data on one of the survey launches, six of us had a chance to take one of the skiffs and go do a little fishing.  Our primary target was halibut.  We motored out to a site scouted earlier in the day during our survey ops, dropped our lines and began jigging right on the bottom.  It wasn’t long before I felt a tugging on my line, began reeling in, and pulled up a baby halibut (or “but” as my companions more versed in these matters call them).  Not wanting to be accused as a cradle robber, I released it. I dropped my line again and after a few minutes of jigging, felt the tug, and reeled in a larger halibut (maybe a 15 pounder – I know technically still a baby).  I released it also, because my companions assure me, “It’s still early you’ll get a bigger one.” I didn’t – of course. However, I did have success (a silver salmon, and four sea cod – I kept these). I also hooked a pea cod, an Irish Lord and two other small halibut – I didn’t keep these. Fun times!

Mike Laird, July 31, 2005

NOAA Teacher at Sea
Mike Laird
Onboard NOAA Ship Rainier
July 24 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: North Pacific
Date: July 31, 2005

Weather Data

Time: 13:00
Latitude: 55° 53.4 ̍ N
Longitude: 158˚ 50.4 ̍ W
Visibility: 10 nautical miles (nm)
Wind Direction: 225˚
Wind Speed: 10kts
Sea Wave Height: 0-1΄
Swell Wave Height: 0-1΄
Sea Water Temperature: 11.7˚ C
Sea Level Pressure: 1009.5 mb
Cloud Cover: Sky 8/8 covered; Lower level: cumulus Mid-level: altostratus High level: cirrus

Science and Technology Log 

The RAINIER’s crew of forty-nine (men (40) and women (9)) is divided into six work groups:

I) Officers and junior officers:  Responsible for overall ship operations including: navigation, horizontal and vertical control, damage control (ship safety), medical services, field  operations, etc.

II) Survey operations: Responsibilities include: data collection and analysis

III) Deck operations:  Responsibilities include: launch and de-launch of small boats (launches and skiffs), operation of the small boats, manning equipment and lines used during anchoring and mooring of the ship, maintenance (cleaning, rust removal, painting) and operation of the deck and deck equipment (cranes, gravity davits, hydraulic davit, the anchor windlass), etc.

IV) Engineering operations: Responsibilities include: maintenance and operation of the ships electrical and mechanical systems

V) Yeoman and Electronics: Yeoman – responsibilities similar to those of a business manager  (personnel, payroll, ship’s budget, etc.).  This position is slowly being  eliminated from the ships in NOAA’s fleet.

Electronics – responsible for the maintenance and operation of the electronic equipment onboard ship (computers, radios, GPS units, etc).

VI) Steward: Responsibilities include: operation of the galley, preparing three meals a day for the crew, preparing snacks for the morning and afternoon breaks, and preparing a picnic lunch and drinks to send with the three to four launch crews who are sent out on survey assignments.

I was able to work with the deck crew the other day, and I’ll share the experience in a future log!

Personal Log 

Today I did a lot of housekeeping kind of stuff.  I was getting pretty low on clean clothes, so I went down and used the ship’s laundry – three washing machines and three driers.  The only difficulty is trying to find open machines.  Either I hit it on a busy day or 49 crewmembers and four guests keep the machines busy.  I also caught up on my logs and did some background reading on tides and tidal datum.  Think I will try a little fishing tonight – still haven’t managed to pull one over the ship’s side.  Last night Jon, one of the crew, somehow caught a skate (looks like a ray).  He hooked it in one of the fins. We pulled it up took a look at it and then released it back over the side.  Very interesting!

Mike Laird, July 30, 2005

NOAA Teacher at Sea
Mike Laird
Onboard NOAA Ship Rainier
July 24 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: North Pacific
Date: July 30, 2005

Weather Data

Latitude: 55°37.1̍ N
Longitude: 156˚46.6 ̍ W
Visibility: 10 nautical miles (nm)
Wind Direction: 140˚
Wind Speed: 5 kts
Sea Wave Height: 0-1΄
Swell Wave Height: 2΄
Sea Water Temperature: 12.2˚ C
Sea Level Pressure: 1009.8 mb
Cloud Cover: Stratus

Science and Technology Log 

I would like to add some clarifying information to my log entry, Mike Laird, July 29, 2005.  In that entry, I discussed setting up two horizontal control-data collection stations, and in reading the entry, it appears that the purpose for both stations is to support the “fly-away” Differential Global Positioning System (DGPS).  This is not accurate.  Only the station we established on the point will be used to determine the exact location of the DGPS.

The purpose of the other station is to verify the accuracy of the existing benchmark at that site, so a tidal datum (“…a base elevation used as a reference from which to reckon heights or depths”) can be established for the tide station located there.  I mentioned in the previous log that the horizontal control team is responsible for establishing accurate latitude and longitude coordinates for each sounding taken by the RAINIER and the launches. In addition, the soundings are taken throughout the day at different stages of the tide, which means that water depth will vary.

It is the responsibility of the vertical control team to provide precise tide data for corrections that have to be applied to the soundings so that they meet NOAA’s Mean Lower Low Water (MLLW) guideline (ensures minimum water depth is charted).  Mean Lower Low Water means that an average is taken of the tide level at the lower of the two ebb periods in a semi-diurnal (two flood periods and two ebb periods every day) tidal day. The National Water Level Observation maintains primary control stations in many locations around the United States. These stations determine a tidal datum based on the average of observations over a nineteen-year period.

In many survey areas, the tidal datum received from a primary control station can be used to make the necessary corrections to the soundings.  However, the nearest station to the RAINIER’s current work area is located in Sand Point – a significant distance away.  Therefore, the vertical control team established the tertiary tidal station (one in operation for at least thirty consecutive days but less than a year) here in Cushing Bay, so that data more indicative of the local conditions can be collected and compared to the primary datum.  During this analysis, a decision will be made about any adjustments that need to be made to the primary datum before it is used to make corrections to the survey soundings.

Personal Log 

Our good fortune continues to hold – the weather is incredible.  Sun is shining brightly, temperature in the low 70’s.  We had been hearing whispers since lunch of a beach party tonight. The rumors were confirmed by an announcement following dinner that a skiff would be ferrying people to the shore and back from 18:30 until 23:30.  It was a time for the crew and guests to relax and hang out, enjoy a big driftwood bonfire, do a little beachcombing (the captain found a large whalebone – rib maybe), have some sodas and listen to a little music.  A lot of fun!

Mike Laird, July 29, 2005

NOAA Teacher at Sea
Mike Laird
Onboard NOAA Ship Rainier
July 24 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: North Pacific
Date: July 29, 2005

Weather Data

Latitude: 55° 53.36 ̍ N
Longitude: 158˚ 58.4 ̍ W
Visibility: 10 nautical miles (nm)
Wind Direction: Light Airs
Wind Speed: Light Airs
Sea Wave Height: 0΄
Swell Wave Height: 0΄
Sea Water Temperature: 12.2˚ C
Sea Level Pressure: 1013.5 mb
Cloud Cover: Sky 8/8 covered;
Lower-level: cumulus, stratocumulus
Mid-level: altostratus

Science and Technology Log 

Today I am on a team that is going ashore to set up two horizontal control-data collection stations. The horizontal control team is responsible for establishing accurate latitude and longitude coordinates for the location of the survey soundings. The RAINIER uses a Differential Global Positioning System (DGPS) to acquire precise readings for every collected depth sounding. The remote location of the Mitrofania Island work area has introduced an infrequently encountered challenge for the horizontal control team.  The two Coast Guard operated DGPS Beacon Stations that are closest to the work area (one on Kodiak Island and one in Cold Bay) are too far away (we are on the outer fringe of their transmitting capability) for the signal to reach the launches in some of the more isolated, shielded areas. As a result, we are out setting up the horizontal control data collection stations.

The first station is set up over an existing benchmark and will record data transmitted directly from a GPS satellite.  The receiver will record readings for six hours, shut down for twenty-four hours, and resume recording for a final six-hour time period. Finished with the first station, we travel across the bay to a point that extends out into the ocean. We will set up the second horizontal control data collection station at this location. However, there is not an existing benchmark, so we must establish one.  First, we drive three-foot sections of metal rod into the ground (normally benchmarks are fixed in rock but there is none at this site).  We sink two sections and decide that is enough to hold the benchmark in place for the two months that it will be in use (for a permanent benchmark the rod is driven until it can go no further).  The brass cap is then stamped with a name (SPIT) and date (2005) and affixed to the top of the rod.  We are now able to set up the second station. The receiver will follow the same collection pattern: collecting signals for six hours, resting for twenty-four hours, and collecting for another six hours.

At the end of the collection period, the data from the sensors will be uploaded to an onboard computer and transmitted to the National Geodetic Survey in Washington D.C. where corrections to account for error introduced by things such as the atmosphere are applied. The corrected data, returned to the ship, will establish very accurately (within cm) the latitude and longitude for the site.  One final correction is made to the data before the site can be used. This error source is the satellite itself and comes from the satellite’s perceived position (where it thinks it is in the sky) as compared to its actual position.  The precise location is monitored by the United States Air Force.  Final corrections using this information will provide pinpoint accuracy (within mm) of the benchmark’s location. A temporary, or “fly-away”, DGPS station can now be placed at this benchmark and transmit signals easily received by the launches.

Personal Log 

Yet another beautiful day! Once on shore the mosquitoes were terrible – swarming in clouds around our heads.  A little bug dope, the warm sun, and cool breeze soon took care of this problem.  A great day to be out working!

Mike Laird, July 28, 2005

NOAA Teacher at Sea
Mike Laird
Onboard NOAA Ship Rainier
July 24 – August 13, 2005

Mission: Hydrographic Survey
Geographical Area: North Pacific
Date: July 28, 2005

Weather Data

Latitude: 55°37.1̍ N
Longitude: 156˚46.6 ̍ W
Visibility: 10 nautical miles (nm)
Wind Direction: 140˚
Wind Speed: 5 kts
Sea Wave Height: 0-1΄
Swell Wave Height: 2΄
Sea Water Temperature: 12.2˚ C
Sea Level Pressure: 1009.8 mb
Cloud Cover: Stratus

Science and Technology Log 

Another beautiful day in the Gulf of Alaska – partially cloudy with lots of sun!  Today I remained aboard the RAINIER and had an opportunity to talk with Ensign Olivia Hauser about the map sheets.  The sheets are prepared to guide the launches on their echo sounding runs. The whole area to be mapped on this leg of the mission is subdivided into zones called sheets.  At the beginning of the workday, each launch is assigned a sheet for the crew to follow for that day. However prior to distribution to the launch crews, the sheets must be developed.

Each sheet (there are six sheets for our current assignment) is the responsibility of a single sheet manager who takes care of the initial preparation of the sheet, sheet revisions, and the beginning phases of data analysis.  In developing the sheet, the manager attempts to achieve 100% coverage of the seafloor.  This means that the manager attempts to determine the optimum distance between the lines the launch will follow during its sounding runs. In areas like the waters around Mitrofania where there is little or no existing data, the first run of a sheet is a best guess plot.  In essence, the launches are conducting reconnaissance runs.

The data collected during these runs, may reveal some error in the initial line plots.  One problem is called a “holiday” which is a gap between the lines (unsounded seafloor).  This happens when the lines are spaced too far apart for the depth of the water (the water is shallower than expected), and the footprint scanned becomes too narrow leaving a gap between it and the footprint of the neighboring line(s).  A second type of problem is excessive noise in the scan results. In reconnaissance work, this is often the result of a greater than expected water depth in a launch not equipped to handle soundings at that depth. When these types of errors are identified, the sheet manager will revise the sheet plotting a new set of lines to be run. If necessary, a different launch (one with appropriate echo sounding equipment) will be assigned to run the new lines.  Once a complete set of good lines is established for a sheet and seafloor data for the entire sheet is collected, initial analysis begins. Computer programs take cast data (conductivity, pressure, and temperature), tide information, GPS readings (corrected for error), data accounting for the pitch and roll of the launch and process the soundings.  The result is a first look at the bottom!  Subtle changes in shading reveal changes in floor depth and other bottom features. The soundings run by the RA5 launch so far have indicated a mostly flat floor with a few rock outcroppings and small ridges.

Personal Log 

The day was fantastic warm and sunny!  One of the crew caught a halibut, which the galley cooked–a special treat for dinner tonight!