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This study uses a 3D ocean model to simulate circulation in the Pearl River Estuary under different tidal and wind conditions. Model results agree well with observational data. Simplified runs without winds show strong spring-neap variation in estuarine circulation. Additional runs including up-estuary and down-estuary winds reveal winds can modify circulation more than tidal straining alone by altering stratification and mixing. Response to winds depends on tidal stage, with weak response during spring tid

Author

Arfena Deah Lestari

Language

EN