Long-Term Movement of Satellite-Tracked Buoys in the Beaufort Sea.

Trajectories of five free-drifting satellite-tracked buoys released during the summer of 1979 in open water in the Beaufort Sea north of the Tuktoyaktuk Peninsula indicate a pronounced east-to-west near-surface flow along the northern Alaskan coast. The direction of the buoy movement is in general a...

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Bibliographic Details
Main Authors: Murphy,D L, Tebeau,P A, Lissauer,I M
Other Authors: COAST GUARD RESEARCH AND DEVELOPMENT CENTER GROTON CT
Format: Text
Language:English
Published: 1981
Subjects:
Physical and Dynamic Oceanography
*OCEAN CURRENTS
*BUOYS
POSITION(LOCATION)
WIND
DRIFT
SURFACE WATERS
DATA ACQUISITION
SEA ICE
BEAUFORT SEA
TRACKS
Chukchi Sea
Tuktoyaktuk
Tuktoyaktuk Peninsula
Wrangel Island
Beaufort Sea
Chukchi
Point Barrow
Sea ice
Online Access:http://www.dtic.mil/docs/citations/ADA126344
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA126344
Description
Summary:Trajectories of five free-drifting satellite-tracked buoys released during the summer of 1979 in open water in the Beaufort Sea north of the Tuktoyaktuk Peninsula indicate a pronounced east-to-west near-surface flow along the northern Alaskan coast. The direction of the buoy movement is in general agreement with the direction of the flow in the southern portion of the Beaufort Sea Gyre as previously calculated from dynamic topography. The buoy tracks and speeds differ from the surface circulation calculated from the dynamic topography in two respects. First, the average buoy speeds (approx. 20 cm/s) were approximately 3 times larger than calculated surface currents. Second, three of the buoys moved onto the Chukchi Sea shelf near Wrangel Island instead of turning to the northwest near Point Barrow with the Beaufort Sea Gyre. The remaining two buoys stopped transmitting before reaching Point Barrow. Analysis of the available wind data suggests that the surface currents as indicated by the motions of the buoys were strongly influenced by the local wind. For surface wind speeds, or = 5 m/s the buoys moved 22 deg to the right of the wind at 3.8% of the wind speed. (Author)

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