Coastal upwelling in the South Eastern Arabian Sea is a phenomenon characterized by the rising of deeper, colder, and nutrient-rich water to the surface along the coast. This process is driven primarily by wind patterns and ocean currents. Here's a more detailed explanation of the dynamics and significance of this phenomenon: ### Mechanism of Upwelling 1. **Wind Patterns**: The South Eastern Arabian Sea is affected by the monsoon winds, particularly during the southwest monsoon season (June to September).

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