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Characteristics of the Indo‐Pacific Throughflow in the eastern Indian Ocean

Identifieur interne : 002513 ( Istex/Checkpoint ); précédent : 002512; suivant : 002514

Characteristics of the Indo‐Pacific Throughflow in the eastern Indian Ocean

Auteurs : N. A. Bray [États-Unis] ; S. E. Wijffels [Australie] ; J. C. Chong [États-Unis] ; M. Fieux [France] ; S. Hautala [États-Unis] ; G. Meyers [Australie] ; W. M. L. Morawitz [États-Unis]

Source :

RBID : ISTEX:8DF70B68E0E00E44B9AC6BD6852934E1DACF404B

English descriptors

Abstract

Five hydrographic sections across the Indonesian throughflow from the World Ocean Circulation Experiment (WOCE) and the Java Australia Dynamic Experiment (JADE) are used to examine seasonal water mass and density distributions, including semiannual variation of the South Java Current. Altimetric sea surface height variations match dynamic height along each WOCE cruise track remarkably well. They also reveal energetic eddies and meanders of the current system south of Java with intraseasonal (60‐day) changes in surface dynamic height comparable in magnitude to seasonal and interannual variations. Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.

Url:
DOI: 10.1029/97GL51793


Affiliations:


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ISTEX:8DF70B68E0E00E44B9AC6BD6852934E1DACF404B

Le document en format XML

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<div type="abstract">Five hydrographic sections across the Indonesian throughflow from the World Ocean Circulation Experiment (WOCE) and the Java Australia Dynamic Experiment (JADE) are used to examine seasonal water mass and density distributions, including semiannual variation of the South Java Current. Altimetric sea surface height variations match dynamic height along each WOCE cruise track remarkably well. They also reveal energetic eddies and meanders of the current system south of Java with intraseasonal (60‐day) changes in surface dynamic height comparable in magnitude to seasonal and interannual variations. Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.</div>
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