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.

4 min read Updated Oct 2026 #quick revision#cgpsc#monsoon

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

FactDetail
MonsoonArabic mausim = season; seasonal reversal of winds
Climate typeTropical monsoon; Tropic of Cancer crosses the middle of India, including northern Chhattisgarh
Thermal conceptHalley (1686): land–sea heating contrast
Dynamic conceptITCZ shifts to 20°–25° N = monsoon trough (Flohn)
Westerly jetWinter, south of the Himalaya (western disturbances); moves north of the Himalaya before onset
Tropical easterly jetSummer, upper air over the peninsula
Somali (Findlater) jetLow-level cross-equatorial jet off East Africa
Mascarene HighHigh pressure near Madagascar
Kerala onset1 June (± about a week)
Whole country8 July (revised 2020; old value about 15 July)
Withdrawal beginsAbout 17 September, west Rajasthan (old value 1 September)
Withdrawal completeAbout 15 October
BurstSudden, heavy-rain onset
BreakMonsoon trough shifts to the Himalayan foothills; rain there and in the north-east, dry elsewhere

Branches

BranchKey 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 BengalMyanmar 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 NaduRain shadow in June–September; gets rain in October–December (north-east monsoon)

Seasons and Local Weather

Season / phenomenonDetail
Cold weatherDecember–February; western disturbances (Mediterranean; winter rain for wheat)
Hot weatherMarch–May; May hottest in north and central India
LooHot, dry afternoon winds, north-west India
Mango showersKerala and coastal Karnataka
Blossom showersCoffee areas of Kerala and Karnataka
Kalbaisakhi / nor’westersWest Bengal, Odisha, Assam; in Assam Bardoli Chheerha (tea showers)
Highest recorded temperature51.0 °C, Phalodi (Rajasthan), May 2016
Retreating monsoonOctober–November; October heat (hot and humid)
Cyclone seasonsApril–May and October–November; Bay of Bengal more active
IMD statistical seasonsWinter Jan–Feb; pre-monsoon Mar–May; SW monsoon Jun–Sep; post-monsoon Oct–Dec
Six ritusVasant, Grishma, Varsha, Sharad, Hemant, Shishir

Rainfall Numbers

FactDetail
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 shareAbout 75% of annual
IMD categories (all-India)<90% deficient; 90–95 below normal; 96–104 normal; 105–110 above normal; >110 excess
District / subdivision normalWithin ±19%
2023About 94% of LPA (El Niño + positive IOD)
2025About 108% of LPA
2026About 87% of LPA (759.4 mm): deficient, lowest since 2015
WettestMawsynram (average); Cherrapunji (historical records)
DriestLeh, western Rajasthan
Variability >50%Western Rajasthan, Ladakh, interior Deccan
RuleLow rainfall → high variability

Koeppen Types (NCERT)

TypeRegion
AmwWest coast south of Goa
AsCoromandel coast
AwMost of the peninsular plateau (most of Chhattisgarh)
BShwParts of Rajasthan, Haryana, Gujarat
BWhwExtreme western Rajasthan
CwgGanga plain, eastern Rajasthan, northern MP, most of the north-east
DfcArunachal Pradesh
EHigh Himalaya (J&K, Ladakh, HP, Uttarakhand)

ENSO and IOD

FactDetail
El NiñoWarm central/eastern Pacific; weak trades; Peru upwelling suppressed; usually weak Indian monsoon
La NiñaCool central/eastern Pacific; strong trades; usually good monsoon
Southern OscillationGilbert Walker, 1920s; SOI = Tahiti − Darwin; negative SOI = El Niño
ENSO couplingBjerknes, 1969
Niño 3.45° N–5° S, 170° W–120° W; El Niño at +0.5 °C or more
RONINOAA’s official ENSO index from February 2026 (anomaly relative to the tropical mean)
El Niño ModokiCentral-Pacific warming
Positive IODWestern Indian Ocean warmer; helps the monsoon (Saji–Yamagata, 1999)
MJOEastward pulse, 30–60 days; onset and active/break spells
1997Very strong El Niño, positive IOD, near-normal monsoon
2002, 2009El Niño droughts (deficits of about 19% and 22%)
2020–2022Triple-dip La Niña
2026NOAA El Niño Advisory (June 2026); monsoon about 87% of LPA

Chhattisgarh Angle

FactDetail
Annual rainfallAbout 1,200–1,300 mm; mostly June–September
Main rain sourceBay of Bengal branch and its depressions
WettestBastar plateau
DriestWestern plain (Kabirdham, Bemetara), in the lee of the Maikal range
Monsoon arrivalAround mid-June, Bastar first
RiskConcentration and July–August dry spells for rain-fed paddy

Don’t Confuse

ThisvsThat
Westerly jet (winter, western disturbances)vsEasterly jet (summer, monsoon depressions)
Mango showers (Kerala, Karnataka)vsKalbaisakhi (Bengal)
Mawsynram (highest average)vsCherrapunji (historical records)
LPA 87 cm (June–September)vsAbout 116 cm (annual)
Positive IOD (west warm, good)vsNegative IOD (east warm, bad)
Negative SOI (El Niño)vsPositive SOI (La Niña)
Old normal: whole country covered by 15 JulyvsCurrent 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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