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Observations of the Leeuwin Current off Western Australia
Leeuwin Current Western Australia
2009/1/19
Shipboard observations made in May 1982 showed a definite poleward surface flow (the Leeuwin Current) over the West Australian shelf from 22°S to 28°S. The surface current was relatively fresh, warm, ...
The Large-Scale Environment of the Poleward-Flowing Leeuwin Current, Western Australia：Longshore Steric Height Gradients, Wind Stresses and Geostrophic Flow
Large-Scale Environment Poleward-Flowing Leeuwin Current Wind Stresses Geostrophic Flow
2009/1/15
Steric heights have been estimated using T–S relationships for all available XBTs within 10–40°S, 105–130°E to 1980, and merged with steric heights from hydrology data. These data were subdivided into...
Two models, one numerical and one analytical, are used to investigate mechanisms for the generation and flow of the Leeuwin Current observed off the west coast of Australia. Three numerical experiment...
Modeling Studies of Eddies in the Leeuwin Current：The Role of Thermal Forcing
primitive equation Leeuwin Current North West
2008/12/27
A high resolution, multilevel, primitive equation (PE) model is used to investigate the generation and stability of the Leeuwin Current and eddies off the west coast of Australia. Two numerical experi...
The Leeuwin Current off Western Australia, 1986–1987
Leeuwin Current Leeuwin Current Interdisciplinary Experiment Western Australia
2008/12/23
The Leeuwin Current in the Indian Ocean off Western Australia differs from the other major eastern boundary currents, e.g., California Current, since it flows rapidly poleward against the prevailing e...
Modeling Studies of the Leeuwin Current off Western and Southern Australia
Modeling Studies Leeuwin Current Western and Southern Australia
2008/10/23
The Leeuwin Current strengthens considerably from February to May each year, following the slackening of southerly coastal winds; strong eddies develop. A high-resolution, multilevel, primitive equati...
The outflow from the Indonesian seas empties approximately 5–7 Sv of surface warm (and low salinity) Indonesian Throughflow water into the southern Indian Ocean (at roughly 12°S). Using a nonlinear 1&...