Pakshal SecretryAIR 8 · CSE 2025 · 213 wordsTheir whole copy
Opening
India Monsoon is reversal of winds in month of June to September bringing 80% of rainfall across India.
Body
features
- Arrive in two branches in India
- firstly on Mainland in 1st week of June in Kerala.
- post September gradually withdrawal from the mainland.
- Most Rains from Bay of Bengal Branch of Monsoon
- Regional precipitation depends
on orography, convectional current cyclonic condition etc.
- Concentrated mostly in 3 months across India.
Causative factors
- Land Breeze due to subcontinental territory
Shifting of ITCZ to north due to intense summer heating
Coriolis force → convergence of equatorial wind on Indian subcontinent
Heating of Massacarine High → creates low pressure to attract winds
El-Nino → ENSO circulation negatively affect Indian Monsoon
Indian Ocean Diopole → support cloud formation and low pressure on Indian subcontinent
MJO (Jullian Oscillation) → gives interseasonal push to monsoon rains in period of trough on Indian area
La-Nina → positively support monsoon in India
India's orography → (eg) - Himalaya doesnt let monsoon to go beyond Indian Territory
Cyclonic condition → In month of June near Indian subcontinent → support monsoon
Close
Thus, monsoon depends on variety of factors, thus IMD also is able to give forecast with 70% probability