Geography
Climate and the Indian Monsoon
Climate and the Indian Monsoon — Quick Revision
One-page CGPSC quick revision for Climate and the Indian Monsoon: dates, LPA figures, seasons, local winds, Koeppen types, El Niño, La Niña and IOD.
The monsoon mechanism, the seasons, rainfall distribution and ENSO on one page. For explanations, go back to the chapter.
How to use this sheet
Scan it top to bottom in the week before Prelims. Bold entries are the facts examiners return to most often.
Mechanism and Dates
| Fact | Detail |
|---|---|
| Monsoon | Arabic mausim = season; seasonal reversal of winds |
| Climate type | Tropical monsoon; Tropic of Cancer crosses the middle of India, including northern Chhattisgarh |
| Thermal concept | Halley (1686): land–sea heating contrast |
| Dynamic concept | ITCZ shifts to 20°–25° N = monsoon trough (Flohn) |
| Westerly jet | Winter, south of the Himalaya (western disturbances); moves north of the Himalaya before onset |
| Tropical easterly jet | Summer, upper air over the peninsula |
| Somali (Findlater) jet | Low-level cross-equatorial jet off East Africa |
| Mascarene High | High pressure near Madagascar |
| Kerala onset | 1 June (± about a week) |
| Whole country | 8 July (revised 2020; old value about 15 July) |
| Withdrawal begins | About 17 September, west Rajasthan (old value 1 September) |
| Withdrawal complete | About 15 October |
| Burst | Sudden, heavy-rain onset |
| Break | Monsoon trough shifts to the Himalayan foothills; rain there and in the north-east, dry elsewhere |
Branches
| Branch | Key facts |
|---|---|
| Arabian Sea (stronger) | Western Ghats (heavy rain, rain shadow on the Deccan); Narmada–Tapi corridor to central India; Saurashtra–Kachchh–Rajasthan (parallel to the Aravalli, little rain) |
| Bay of Bengal | Myanmar and Bangladesh; Garo–Khasi hills (Mawsynram, Cherrapunji); turned west by the Himalaya, so rain decreases east to west in the Ganga plain; depressions over Odisha–Chhattisgarh–MP |
| Tamil Nadu | Rain shadow in June–September; gets rain in October–December (north-east monsoon) |
Seasons and Local Weather
| Season / phenomenon | Detail |
|---|---|
| Cold weather | December–February; western disturbances (Mediterranean; winter rain for wheat) |
| Hot weather | March–May; May hottest in north and central India |
| Loo | Hot, dry afternoon winds, north-west India |
| Mango showers | Kerala and coastal Karnataka |
| Blossom showers | Coffee areas of Kerala and Karnataka |
| Kalbaisakhi / nor’westers | West Bengal, Odisha, Assam; in Assam Bardoli Chheerha (tea showers) |
| Highest recorded temperature | 51.0 °C, Phalodi (Rajasthan), May 2016 |
| Retreating monsoon | October–November; October heat (hot and humid) |
| Cyclone seasons | April–May and October–November; Bay of Bengal more active |
| IMD statistical seasons | Winter Jan–Feb; pre-monsoon Mar–May; SW monsoon Jun–Sep; post-monsoon Oct–Dec |
| Six ritus | Vasant, Grishma, Varsha, Sharad, Hemant, Shishir |
Rainfall Numbers
| Fact | Detail |
|---|---|
| Annual LPA (1971–2020) | 1,160.1 mm |
| June–September LPA (1971–2020) | 868.6 mm (87 cm); old (1961–2010) about 88 cm |
| Monsoon share | About 75% of annual |
| IMD categories (all-India) | <90% deficient; 90–95 below normal; 96–104 normal; 105–110 above normal; >110 excess |
| District / subdivision normal | Within ±19% |
| 2023 | About 94% of LPA (El Niño + positive IOD) |
| 2025 | About 108% of LPA |
| 2026 | About 87% of LPA (759.4 mm): deficient, lowest since 2015 |
| Wettest | Mawsynram (average); Cherrapunji (historical records) |
| Driest | Leh, western Rajasthan |
| Variability >50% | Western Rajasthan, Ladakh, interior Deccan |
| Rule | Low rainfall → high variability |
Koeppen Types (NCERT)
| Type | Region |
|---|---|
| Amw | West coast south of Goa |
| As | Coromandel coast |
| Aw | Most of the peninsular plateau (most of Chhattisgarh) |
| BShw | Parts of Rajasthan, Haryana, Gujarat |
| BWhw | Extreme western Rajasthan |
| Cwg | Ganga plain, eastern Rajasthan, northern MP, most of the north-east |
| Dfc | Arunachal Pradesh |
| E | High Himalaya (J&K, Ladakh, HP, Uttarakhand) |
ENSO and IOD
| Fact | Detail |
|---|---|
| El Niño | Warm central/eastern Pacific; weak trades; Peru upwelling suppressed; usually weak Indian monsoon |
| La Niña | Cool central/eastern Pacific; strong trades; usually good monsoon |
| Southern Oscillation | Gilbert Walker, 1920s; SOI = Tahiti − Darwin; negative SOI = El Niño |
| ENSO coupling | Bjerknes, 1969 |
| Niño 3.4 | 5° N–5° S, 170° W–120° W; El Niño at +0.5 °C or more |
| RONI | NOAA’s official ENSO index from February 2026 (anomaly relative to the tropical mean) |
| El Niño Modoki | Central-Pacific warming |
| Positive IOD | Western Indian Ocean warmer; helps the monsoon (Saji–Yamagata, 1999) |
| MJO | Eastward pulse, 30–60 days; onset and active/break spells |
| 1997 | Very strong El Niño, positive IOD, near-normal monsoon |
| 2002, 2009 | El Niño droughts (deficits of about 19% and 22%) |
| 2020–2022 | Triple-dip La Niña |
| 2026 | NOAA El Niño Advisory (June 2026); monsoon about 87% of LPA |
Chhattisgarh Angle
| Fact | Detail |
|---|---|
| Annual rainfall | About 1,200–1,300 mm; mostly June–September |
| Main rain source | Bay of Bengal branch and its depressions |
| Wettest | Bastar plateau |
| Driest | Western plain (Kabirdham, Bemetara), in the lee of the Maikal range |
| Monsoon arrival | Around mid-June, Bastar first |
| Risk | Concentration and July–August dry spells for rain-fed paddy |
Don’t Confuse
| This | vs | That |
|---|---|---|
| Westerly jet (winter, western disturbances) | vs | Easterly jet (summer, monsoon depressions) |
| Mango showers (Kerala, Karnataka) | vs | Kalbaisakhi (Bengal) |
| Mawsynram (highest average) | vs | Cherrapunji (historical records) |
| LPA 87 cm (June–September) | vs | About 116 cm (annual) |
| Positive IOD (west warm, good) | vs | Negative IOD (east warm, bad) |
| Negative SOI (El Niño) | vs | Positive SOI (La Niña) |
| Old normal: whole country covered by 15 July | vs | Current normal: 8 July (since 2020) |
Favourite MCQ trap
Old textbooks give 15 July for full coverage, 1 September for the start of withdrawal and 88 cm for the LPA. Current values are 8 July, 17 September and 87 cm (1971–2020). And remember: not every El Niño means drought (1997).
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