Indian Climate: Monsoon, Seasons, Rainfall & Climate Phenomena
Complete notes on India's monsoon mechanism, four seasons, rainfall distribution, climate regions, El Nino, and La Nina for Kerala PSC.
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India’s climate is primarily classified as “tropical monsoon” type. Understanding the monsoon mechanism, seasons, and rainfall distribution is essential for Kerala PSC exams. Climate questions appear in nearly every graduate-level paper.
Factors Influencing India’s Climate
| Factor | How it Affects |
|---|---|
| Latitude | Tropic of Cancer divides India into tropical (south) and subtropical (north) |
| Himalayas | Block cold Central Asian winds; trap monsoon moisture |
| Distribution of land and water | Differential heating drives monsoon winds |
| Distance from sea | Coastal areas are moderate; interior is extreme |
| Altitude | Temperature decreases ~6.5°C per 1,000 m rise |
| Relief/Topography | Western Ghats force orographic rainfall on windward side |
| Upper air circulation | Jet streams influence onset and withdrawal of monsoon |
The Four Seasons of India
| Season | Months | Key Features |
|---|---|---|
| Cold Weather (Winter) | December–February | NE monsoon winds; dry in most of India; Tamil Nadu gets rainfall |
| Hot Weather (Summer) | March–May | Rising temperatures; loo (hot winds) in north; pre-monsoon showers (mango showers in Kerala, Nor’westers/Kal Baisakhi in Bengal/Assam) |
| Advancing Monsoon (Rainy) | June–September | SW monsoon; bulk of India’s rainfall (about 75% of annual total) |
| Retreating Monsoon (Autumn) | October–November | Monsoon withdraws from NW to SE; cyclones in Bay of Bengal; NE monsoon brings rain to Tamil Nadu |
The Southwest Monsoon — Mechanism
Key Concepts
| Concept | Explanation |
|---|---|
| Differential heating | Land heats faster than sea in summer, creating low pressure over northern plains |
| ITCZ shift | Inter-Tropical Convergence Zone shifts northward to Ganga plains in summer |
| Trade winds | SE trade winds from Southern Hemisphere cross equator, deflect right (Coriolis force), become SW monsoon |
| Somali Jet / Low-Level Jet | Strong wind current crossing Arabian Sea; drives moisture to India |
| Tibetan Plateau heating | Creates upper-level high pressure; helps establish the monsoon circulation |
| Tropical Easterly Jet | Upper atmosphere jet stream over peninsular India during monsoon |
Two Branches of SW Monsoon
| Branch | Route | Areas Receiving Rainfall |
|---|---|---|
| Arabian Sea Branch | Hits Western Ghats first; one arm goes to Gujarat/Rajasthan; one to central India | Kerala (June 1), Karnataka, Maharashtra, Gujarat |
| Bay of Bengal Branch | Enters NE India (Meghalaya); deflected westward by Himalayas along Ganga plain | NE India, Bihar, UP, Punjab |
Monsoon Timeline
| Date (Approximate) | Event |
|---|---|
| June 1 | SW monsoon arrives in Kerala (onset) |
| June 10 | Reaches Mumbai |
| June 15 | Covers most of South and Central India |
| July 1 | Covers eastern India |
| July 15 | Reaches all of India including NW |
| September 1 | Begins retreat from NW India |
| October 15 | Withdraws from most of northern India |
| December | Fully withdrawn from India |
PSC Note: June 1 is the normal date of monsoon onset over Kerala. This is the single most tested date in Indian geography.
The Northeast Monsoon (Retreating Monsoon)
| Feature | Detail |
|---|---|
| Period | October–December |
| Wind direction | Northeast to Southwest |
| Moisture source | Bay of Bengal |
| Main beneficiary | Tamil Nadu and parts of Andhra Pradesh |
| Why Tamil Nadu? | Coast lies parallel to NE winds; winds pick up moisture over Bay of Bengal |
| Cyclone season | October–November cyclones in Bay of Bengal |
Rainfall Distribution
Annual Rainfall Zones
| Zone | Rainfall (cm/year) | Areas |
|---|---|---|
| Heavy rainfall (over 200 cm) | Western Ghats windward side, NE India (Meghalaya), Andaman-Nicobar | Cherrapunji, Mawsynram, Western coast |
| Moderate rainfall (100–200 cm) | Eastern plains, western coastal areas, parts of UP, Bihar, Bengal | Most of peninsular India |
| Low rainfall (50–100 cm) | Interior Deccan, parts of central India, Punjab, Haryana | Rain shadow regions |
| Very low rainfall (below 50 cm) | Western Rajasthan (Thar), Ladakh, parts of Gujarat | Arid/semi-arid zones |
Rainfall Records
| Record | Place | Detail |
|---|---|---|
| Wettest place (world, average annual) | Mawsynram (Meghalaya) | ~11,871 mm average annual |
| Second wettest / most rain in a single year | Cherrapunji (Sohra) | Held the record once; now second to Mawsynram |
| Driest in India | Leh (Ladakh) | About 10 cm per year |
Why Meghalaya gets so much rain: The funnel-shaped hills of the Khasi and Jaintia ranges force the Bay of Bengal branch of the monsoon sharply upward, causing intense orographic rainfall.
Climate Regions of India (Koppen Classification)
| Type | Code | Areas | Features |
|---|---|---|---|
| Tropical Wet (Rainforest) | Af | Western coast, NE India, Andaman | Heavy rain throughout year |
| Tropical Monsoon | Am | Most of Western Ghats, West Bengal | Seasonal heavy rain, short dry season |
| Tropical Wet and Dry (Savanna) | Aw | Most of peninsular India | Distinct wet and dry seasons |
| Semi-arid (Steppe) | BSh | Rajasthan, Gujarat, parts of Karnataka, TN | Low rainfall, hot |
| Hot Desert | BWh | Western Rajasthan (Thar) | Very low rainfall, extreme heat |
| Humid Subtropical | Cwa | Northern plains (UP, Bihar, Punjab, Haryana) | Hot summers, cold winters, monsoon rain |
| Montane/Alpine | H | Himalayas, high-altitude areas | Cold, varies with altitude |
Important Local Winds and Weather Phenomena
| Phenomenon | Region | Description |
|---|---|---|
| Loo | Northern plains (UP, Rajasthan, Punjab) | Hot, dry summer winds (May–June) |
| Mango Showers | Kerala, Karnataka | Pre-monsoon showers in April–May helping mango ripening |
| Cherry Blossoms / Blossom Showers | Karnataka (coffee-growing areas) | Pre-monsoon showers helping coffee flowering |
| Nor’westers / Kal Baisakhi | West Bengal, Assam | Violent thunderstorms in April–May; beneficial for tea and jute |
| Bardoli Chheerha | Assam | Pre-monsoon thundershowers |
| October Heat | Northern India | Oppressive heat and humidity during retreating monsoon |
| Western Disturbances | North India (Punjab, J&K, HP) | Winter rainfall caused by Mediterranean weather systems traveling eastward |
El Nino and La Nina
El Nino (ENSO — El Nino Southern Oscillation)
| Feature | Detail |
|---|---|
| What it is | Periodic warming of sea surface temperature (SST) in central and eastern tropical Pacific Ocean |
| Normal condition | Warm water in western Pacific (near Indonesia); cold water in eastern Pacific (near Peru) |
| During El Nino | Warm water shifts to eastern Pacific; trade winds weaken |
| Effect on Indian monsoon | Generally weakens the SW monsoon, leading to drought or below-normal rainfall |
| Frequency | Every 2–7 years |
| Name meaning | ”The Christ Child” (usually appears around Christmas off Peru’s coast) |
La Nina
| Feature | Detail |
|---|---|
| What it is | Abnormal cooling of SST in eastern Pacific |
| Effect on Indian monsoon | Generally strengthens the SW monsoon, leading to above-normal or heavy rainfall |
| Relation to El Nino | Opposite phase of ENSO cycle |
| Name meaning | ”The Girl” |
Indian Ocean Dipole (IOD)
| Feature | Detail |
|---|---|
| What it is | Difference in SST between western and eastern Indian Ocean |
| Positive IOD | Western Indian Ocean warmer; enhances Indian monsoon rainfall |
| Negative IOD | Eastern Indian Ocean warmer; weakens Indian monsoon |
| Interaction | Positive IOD can counteract El Nino’s negative impact on Indian monsoon |
Jet Streams and Indian Monsoon
| Jet Stream | Season | Location | Effect |
|---|---|---|---|
| Subtropical Westerly Jet | Winter | South of Himalayas (over northern plains) | Brings western disturbances; winter rain in north India |
| Tropical Easterly Jet | Summer (monsoon) | Over peninsular India (at about 14°N) | Associated with strong SW monsoon |
Key fact: The onset of SW monsoon coincides with the withdrawal of the Subtropical Westerly Jet from over northern India and the establishment of the Tropical Easterly Jet.
Climate Change and India
| Observation | Detail |
|---|---|
| Temperature trend | Average temperature has risen by about 0.7°C over the past century |
| Monsoon trend | Increased variability; more extreme rainfall events |
| Glaciers | Himalayan glaciers retreating |
| Sea level | Rising about 1.3 mm per year along Indian coast |
| Extreme events | Increasing frequency of cyclones, floods, and droughts |
Frequently Asked PSC Questions
Q: Normal date of monsoon onset over Kerala? A: June 1
Q: Wettest place in the world? A: Mawsynram, Meghalaya
Q: Which state gets rainfall from NE monsoon? A: Tamil Nadu (also parts of Andhra Pradesh)
Q: What is Loo? A: Hot dry winds blowing in northern plains during summer
Q: El Nino effect on Indian monsoon? A: Weakens the monsoon (leads to drought/below-normal rainfall)
Q: Mango showers occur in which state? A: Kerala and Karnataka (pre-monsoon showers in April–May)
Q: About 75% of India’s annual rainfall is received during? A: Southwest monsoon season (June–September)
Q: Western disturbances bring rainfall to which region? A: North India (Punjab, J&K, HP) during winter
Q: Tropic of Cancer passes through how many Indian states? A: 8 states (Gujarat, Rajasthan, MP, Chhattisgarh, Jharkhand, West Bengal, Tripura, Mizoram)
Exam Tips
- June 1 (monsoon onset in Kerala) is the single most asked date — never forget it
- El Nino = drought, La Nina = excess rain — this one-line distinction scores marks
- Mawsynram vs Cherrapunji — PSC still asks “wettest place” — answer is Mawsynram (for average annual), not Cherrapunji
- Know the two branches of SW monsoon and which areas each covers
- Tamil Nadu’s NE monsoon rainfall is a frequently asked “exception” question
- The Tropic of Cancer passing through 8 states is asked as both “name them” and “how many”
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