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India — Climate and the Monsoon

4 seasons, SW monsoon mechanism, branches, El Niño, climatic regions.

India — Climate and the Monsoon

Climate of India & the Monsoon

What you'll learn

  • Climate vs weather — long-term averages vs day-to-day conditions.
  • Factors controlling India's climate: latitude, altitude, distance from sea, wind systems.
  • Four seasons of India.
  • Monsoon — the most important climatic feature; its mechanism and retreat.
  • El Niño and its effect on Indian monsoon.

Key concepts

Climate vs Weather

TermMeaningTime scale
WeatherDay-to-day state of atmosphere (temp, rainfall, wind)Hours to days
ClimateAverage weather over 30+ years for a regionDecades

Factors controlling India's climate

FactorEffect
LatitudeSouthern India closer to equator → hotter; northern India has continental climate
AltitudeMountains cooler (Shimla vs Delhi, same latitude)
Distance from seaCoastal areas moderate temp; interiors have extreme hot/cold
HimalayasBlock cold Central Asian winds; force monsoon to give heavy rain
Western GhatsWindward (west) side gets heavy rain; leeward (east) side — rain shadow
Jet streamsFast-moving air currents in upper atmosphere influence rain patterns

Four seasons of India

SeasonMonthsFeatures
Cold WeatherNov–FebCool/cold; NE trade winds blow; North India foggy; Tamil Nadu gets rain (NE monsoon)
Hot Weather (Summer)Mar–MayVery hot; dust storms; loo winds (hot dry winds in North India); temperatures 40–48°C in Rajasthan
South-West Monsoon (Rainy)Jun–Sep75–90% of India's annual rainfall; most important season
Retreating Monsoon (Autumn)Oct–NovMonsoon withdraws; cyclones in Bay of Bengal → Tamil Nadu & AP coast

The South-West Monsoon — mechanism

Cause: Differential heating of land and sea.

  1. In summer, Indian landmass heats up rapidly → low pressure over land.
  2. Indian Ocean remains cooler → high pressure over sea.
  3. Moist winds blow from high pressure (sea) to low pressure (land) = monsoon winds.
  4. Moisture-laden winds rise over Western Ghats and Himalayas → cool → condense → heavy rainfall.

Two branches:

  • Arabian Sea branch: hits Western Ghats first (Malabar coast, Mumbai); then crosses Deccan; reaches Central India.
  • Bay of Bengal branch: hits NE India (Meghalaya, Assam) → moves west along Ganga plain.

Mawsynram (Meghalaya) — wettest place on Earth; ~11,870 mm/year; windward side of Khasi Hills.

Onset and retreat

EventTiming
Monsoon arrives Kerala~June 1
Covers entire India~July 15
Begins retreating from NW India~September
Fully withdrawn~December

Break in monsoon

  • Monsoon doesn't rain continuously — has wet spells and breaks (dry spells).
  • During break, jet stream shifts; can last 1–3 weeks.

El Niño effect

  • El Niño = unusual warming of Pacific Ocean surface waters every 2–7 years.
  • Weakens Indian monsoon → drought in India.
  • La Niña (cooling) → stronger monsoon → floods.
  • 2002, 2009, 2014 droughts in India linked to El Niño.

Climatic regions of India (brief)

RegionClimate typeExample
North-West (Rajasthan)Hot desert / aridJaisalmer (<100 mm rain)
North India plainsSemi-arid to sub-humidDelhi
North-EastHumid subtropicalShillong, Assam
Western coastTropical monsoonMumbai, Kerala
Deccan interiorTropical savannaPune, Hyderabad (rain shadow)
HimalayasAlpine / mountainShimla, Leh

Quick check

  • What is the difference between weather and climate?
  • Name four factors that control India's climate.
  • What causes the South-West Monsoon to blow towards India?
  • Name the two branches of the monsoon and which regions they affect first.
  • What is El Niño and how does it affect India?

Open the Practice tab for graded questions on Climate.

Key Takeaways (TL;DR)

  • What you'll learn
  • Key concepts
  • Quick check

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