In a monsoon circulation, wind flow reverses seasonally with the migration of the ITCZ.

Name: In a monsoon circulation, wind flow reverses seasonally with the migration of the ITCZ.
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During the monsoon season, the wind flow reverses direction in response to the migration of the Intertropical Convergence Zone (ITCZ). In summer, when the ITCZ moves northward, winds become southerly, while in winter, when the ITCZ moves southward, winds become northerly.

In a Monsoon Circulation, Wind Flow Reverses Seasonally with the Migration