Type |
Article |
Date |
1993 |
Language |
English |
Author(s) |
Quadfasel D, Baudner H |
Affiliation(s) |
DEUTSCH WETTERDIENST,SEEWETTERAMT HAMBURG,W-2000 HAMBURG 36,GERMANY |
Source |
Oceanologica Acta (0399-1784) (Gauthier-Villars), 1993 , Vol. 16 , N. 3 , P. 221-229 |
WOS© Times Cited |
69 |
Keyword(s) |
RED SEA, CIRCULATION OF MARGINAL SEAS, TOPOGRAPHIC GYRES |
Abstract |
High resolution synoptic hydrographic surveys carried out during 1982 to 1987 are used to delineate the two-dimensional baroclinic flow pattern of the Red Sea. it is shown that the circulation can be characterized through a succession Of four gyres, some 200 km in diameter, the locations of which are linked to the major topographic basins of the Red Sea. The gyres have a transport almost an order of magnitude larger than the large-scale thermohaline driven flow. They appear to be forced by the strongly rotational wind field over the Red Sea. |
Full Text |
File |
Pages |
Size |
Access |
18675.pdf |
9 |
647 KB |
Open access |
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