The monsoon trough is a significant weather phenomenon associated with the Asian monsoon system. It is essentially a low-pressure area that extends across the Indian subcontinent and parts of Southeast Asia, where the southwest monsoon winds meet the northeast trade winds. Key characteristics of the monsoon trough include: 1. **Location**: The monsoon trough typically lies approximately along the latitude of the Himalayas, but its position can vary and shift throughout the monsoon season.
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