Abstract
Recent observations of satellite-tracked drogued buoys in the Gulf of Carpentaria indicate a slow, clockwise mean circulation, which appears to be a permanent feature in the Gulf. Residual currents, derived from 3-5 months of recent current-meter observations, and from a numerical tidal model of the Gulf, are compared with the motions deduced from the buoys. North-west monsoon winds and density-induced currents enhance the clockwise circulation. However, application of the south-east trade-wind stress at neap tides drives a counterclockwise circulation, and at spring tides, a weak clockwise circulation. The large annual variation of mean sea level in the Gulf is a maximum in the south-east corner (75 cm): 70% of this can be accounted for by the effects of winds, atmospheric pressure, and steric variations, all of which exhibit marked seasonality, are approximately in phase, and are thus additive.
Subject
Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics,Oceanography
Cited by
40 articles.
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