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9th April 2025 (9 Topics)

Monsoon Forecast 2025

Context

Private weather agency Skymet has released its first official forecast for the 2025 southwest monsoon, predicting ‘normal’ rainfall at 103% of the Long Period Average (LPA).

What is Monsoon?

  • The term monsoon refers to a seasonal reversal of winds, typically associated with heavy rainfall.
  • In India, the Southwest Monsoon (June–September) is the main rainy season, contributing 80–90% of the country’s annual rainfall.
  • Onset & Progress of Monsoon
  • The monsoon starts in Kerala around June 1st.
  • It then advances northwards, reaching Mumbai in ~10 days, Delhi by end of June, and entire India by mid-July.
  • The retreating monsoon (also called Northeast Monsoon) starts withdrawing from Rajasthan around September, fully withdrawing by mid-October.

Why Does the Monsoon Occur?

  • Differential Heating of Land and Sea: During summer, the land (especially North India) heats up faster than the sea. This creates a low-pressure zone over land and high pressure over the Indian Ocean. Moisture-laden winds from the ocean move toward the land to fill this void.
  • Inter-Tropical Convergence Zone (ITCZ): The ITCZ is a belt of low pressure near the equator where trade winds converge. In Indian summer, the ITCZ shifts northward (near the Tropic of Cancer) because the northern hemisphere is tilted toward the Sun. This pulls monsoon winds deep into the Indian subcontinent.
  • Coriolis Force: Due to Earth’s rotation, the winds deflect to the right in the northern hemisphere. This turns the southeast trade winds into southwest monsoon winds over India.
  • Other Climatic Factors Affecting Monsoon
    • El Niño: Warming in central/east Pacific Ocean ? Weakens Indian monsoon (can cause droughts)
  • La Niña: Cooling in the Pacific ? Strengthens monsoon
  • Indian Ocean Dipole (IOD): Positive IOD (warmer west Indian Ocean) ? Enhances monsoon
  • Equatorial Indian Ocean Oscillation: Affects monsoon build-up and variability
  • Western Disturbances: Interact with monsoon and winter weather over North India

Branches of Southwest Monsoon

Branch

Path

Impact

Arabian Sea Branch

Hits Western Ghats

Heavy rainfall in Kerala, Karnataka, Maharashtra, Goa

Bay of Bengal Branch

Moves toward Northeast and Indo-Gangetic Plains

Rain in Assam, West Bengal, Bihar, UP

Fact Box:

Key-Concepts

  • Long Period Average (LPA): LPA is the average rainfall India receives during the monsoon (June to September) over a long period — usually 50 years.
    • For India, LPA is 868.6 mm.
    • When rainfall is:
      • 96% to 104% of LPA: It’s called a normal monsoon
      • Above 104%: Above normal/excess
      • Below 96%: Below normal
      • Below 90%: Drought year
  • El Niño and La Niña (ENSO Phenomenon): El Niño-Southern Oscillation is a Pacific Ocean phenomenon that affects weather worldwide.
    • El Niño: Warm waters in the Pacific = Weak Indian monsoon =  Less rainfall
    • La Niña: Cold waters in the Pacific = Strong monsoon = More rainfall
    • Neutral: No significant warming or cooling = Monsoon behaves more naturally

  • Indian Ocean Dipole (IOD): It is the difference in sea surface temperatures between Western Indian Ocean (near Africa) and Eastern Indian Ocean (near Indonesia)
    • Positive IOD: Warmer west = Pulls moisture towards India = Good rainfall
    • Negative IOD: Warmer east = Moisture diverted away from India = Poor rainfall
    • Neutral IOD: No major impact

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