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The Gascoyne continental shelf extends from North West Cape (21.3°S) to Shark Bay (26.5°S), Western Australia, and is dominated by the Leeuwin Current (LC), an anomalous oligotrophic eastern boundary current that transports tropical water poleward and generates large-scale downwelling. In summer, shelf dynamics are influenced by wind-generated countercurrents (the Ningaloo and Capes Currents) that...
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