The Eddy Field of the Central North Atlantic

Sixty-eight satellite-tracked buoys were released in the western and central North Atlantic during 1981 and 1982. Mean velocity values and the variance about the mean were calculated for 20 selected areas. The mean velocities confirm the large-scale gyre circulation. The velocity variance decreases...

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Bibliographic Details
Main Author: Krauss,W.
Other Authors: KIEL UNIV (GERMANY F R) INST FUER MEERESKUNDE
Format: Text
Language:English
Published: 1983
Subjects:
*Ocean currents
North Atlantic Ocean
Eddies(Fluid mechanics)
Buoys
Drift
Velocity
Kinetic energy
Symposia
Component Reports
Mid-Atlantic Ridge
North Atlantic
Online Access:http://www.dtic.mil/docs/citations/ADP002664
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADP002664
Description
Summary:Sixty-eight satellite-tracked buoys were released in the western and central North Atlantic during 1981 and 1982. Mean velocity values and the variance about the mean were calculated for 20 selected areas. The mean velocities confirm the large-scale gyre circulation. The velocity variance decreases toward the east and south. East of the Mid-Atlantic Ridge the eddy kinetic energy reaches values of about 200 sq cm/s at 500 N, but only 50 sq cm/s at 30 N. This article is from 'The Role of Eddies in the General Ocean Circulation: Proceedings of 'Aha Huliko'a Hawaiian Winter Workshop Held at Manoa on January 5-7, 1983,' AD-A137 212, p275-282.

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