![]() |
|
![]() |
| Home | Calendar | Contacts | Publications |
Real-time results
4-days+ results |
High-res. surveys |
Turbulence |
Moorings & NDBC |
Aircraft |
Coastal radar |
Atmospheric modeling |
Satellite data |
Data assimilation |
From: Pat Wheeler
Subject: Revelle Report Jan 17-20
In the previous report I forgot to mention that Rob Pinkel had two people on board during our loading to add software so that we could use his high resolution ADCP system. This tested out well and we plan to use it.
Jan 17 transit north continued, no in water testing of gear, fog at night
Jan 18 continued transit, very smooth ride, beautiful weather
Jan 19 arrival at CH-6 03:00We completed a 12 depth "pump station" with all chemistry and optics on-line. The afternoon was devoted to setting up and deploying Moum's bottom mooring (lander). Murray's mooring were all sighted, as was the met buoy. Moum's anchor and float are at 45 00.419 N 124 12.206 W (124 m) and the bottom lander is at 45 00.256 N 124 12.205 W (123 m).
We ran inshore along 45 0.6 N and scouted 3-4 lines of crab pots between the 70 m and 50 m. The plan was to run a 5 depth pump station at CH-1 but CTD on Hale's sled failed. Several attempts of repair were not successful so we remained inshore until daylight.
WECOMA is within a mile of our mooring site and Jack and I made radio contact.
At daylight we moved south to 45 00 N, and noted locations of several crab pot lines again between 50 m and 80 m and completed two ADCP transects along 45 N. Hales' CTD was succesfully repaired and we started our first profiling transect at 13:00. Our plan is to pull Hales' sled and Moum's Chameleon to the suface to cross the crab pot lines. So far we've been successful. To be safe we may restrict our inshore towing work for daylight hours. We plan to run the profiling transect to CH-7 today which should take 16 h. Then we will return to CH-6 for a 12 depth pump station.
We had radio contact with the WECOMA again just as they finished their small box survey.
We see interesting temperature inversions and a weak subsurface fluorescence signal near the bottom across the inner shelf. We also see the strong fresh water signal that Jack reported.
On our profiling transect (moving westward) we lose internet connections and e-mail so we will not be able to download data until we head back inshore.
Pat Wheeler
Chief Scientist
RV Revelle