4 Geography · 4.2.4 Climate and monsoon
4.2.4.4 Monsoon mechanism: classical theory, ITCZ, jet streams and the Tibetan Plateau
The south-west monsoon is a seasonal reversal of winds driven by the shift of the ITCZ over India, the heating of the Tibetan Plateau, the arrival of the tropical easterly jet and the cross-equatorial flow from the Mascarene High.
- APPSC Group 1
- Advanced level
- 4 min read
- Full course
Key terms
- monsoon
- ITCZ
- monsoon trough
- jet stream
- tropical easterly jet
- Tibetan Plateau
- Mascarene High
- Somali jet
- Coriolis
What this note covers
- Core factsFoundation
- ExplainedStandard
- DeeperAdvanced
- Mains writingMains writing
- Common trapsFoundation
- Quick revisionFoundation
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