Q1. The Indian monsoon is primarily responsible for seasonal rainfall in India. What is the main cause behind the reversal of wind direction during monsoon?
- (a) Coriolis effect
- (b) Differential heating of land and sea
- (c) Young fold mountains
- (d) Dissected rivers and valleys
Answer & solution
Answer: (b) Differential heating of land and sea
⚠️ Note: the official sheet marks option 3; the correct answer is option 2 because the seasonal reversal of the monsoon winds is caused by the differential heating of land and sea, not by mountains.
In summer the Indian landmass heats faster than the Indian Ocean, so low pressure forms over north-west India and winds blow from sea to land (south-west monsoon).
In winter the land cools faster, high pressure builds over it, and the winds reverse to blow from land to sea (north-east monsoon).
Revision note — Mechanism of the Indian monsoon
• The word monsoon comes from the Arabic mausim (season); it means a seasonal reversal of wind direction.
• By late May intense heating of the north-western plains deepens the monsoon trough (a low-pressure belt) and the ITCZ shifts north to about 20–25 degrees N.
• The south-east trade winds of the southern hemisphere then cross the equator and arrive as the south-west monsoon.
• The Coriolis force only deflects the crossing winds to the right, turning south-east trades into south-westerlies; it is not the cause of the reversal.
• The Tibetan plateau heats strongly in summer, the sub-tropical westerly jet shifts north of the Himalaya, and the tropical easterly jet helps the burst of the monsoon.
• The monsoon has two branches — the Arabian Sea branch (west coast, Western Ghats) and the Bay of Bengal branch (eastern and north-eastern India).
• Normal onset over Kerala is 1 June; the season lasts June to September and brings about three-fourths of India's annual rain.
• The monsoon withdraws first from north-west India in September and last from the Tamil Nadu coast, which gets most of its rain from the north-east monsoon (October–December).
• El Niño years are linked with a weak monsoon; La Niña years with a strong one.
Do not mix these up
• Sea breeze vs monsoon — both come from differential heating of land and water, but a sea breeze reverses daily and a monsoon reverses seasonally.
• South-west vs north-east monsoon — the south-west monsoon (June–September) rains on most of India; the north-east monsoon (October–December) rains mainly on Tamil Nadu.
Also asked from this topic: the cause of the summer monsoon pressure gradient (differential heating of land and sea); the branch that rains on the west coast (Arabian Sea branch).