Monsoon depressions are synoptic-scale (not mesoscale) low-pressure systems embedded within the monsoon trough, characterized by strong cyclonic vorticity, convergence ahead of the system, and maximum rainfall typically in the southwest quadrant relative to the system center.
Monsoon depressions are synoptic-scale disturbances (spanning hundreds of km, larger than mesoscale systems) with strong cyclonic (not anticyclonic) relative vorticity. Convergence ahead of the moving...
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