UPSC Foundation 2026 and JPSC Mentorship admissions open Daily Current Affairs
learnpro Civil Services
LearnPro Menu
Home Current Affairs All Articles
UPSC
UPSC NOTES
STATE PSC
OPTIONAL SUBJECTS
CURRENT AFFAIRS
DAILY EDITORIAL
COURSES
DOWNLOAD NOTES
PYQ Papers Mains Answer Writing Online Courses

CA Topic

Early Onset of Indian Monsoon

Brief Context

In Context As per the IMD, there are chances of early onset of the southwest monsoon. The normal onset date of the monsoon over Kerala is June 1 and it usually takes about 10 days for the system to reach Kerala from the Nicobar islands. Mechanism of the Indian Monsoon: The Driving Forces Differential Heating of Land and Sea: In summer, India’s landmass heats faster than the ocean, creating low pressure over land and drawing in moisture-laden winds from the sea.

Source Content

Syllabus: GSI/ Indian Physical Geography

In Context

  • As per the IMD, there are chances of early onset of the southwest monsoon. The normal onset date of the monsoon over Kerala is June 1 and it usually takes about 10 days for the system to reach Kerala from the Nicobar islands.

Mechanism of the Indian Monsoon: The Driving Forces

  • Differential Heating of Land and Sea: In summer, India’s landmass heats faster than the ocean, creating low pressure over land and drawing in moisture-laden winds from the sea.
  • Inter-Tropical Convergence Zone (ITCZ): The ITCZ, where trade winds meet near the equator, shifts north during summer, intensifying low pressure over the Indo-Gangetic plain and drawing in monsoon winds.
  • Tibetan Plateau: Its high elevation heats up, creating an upper-air low-pressure zone that strengthens vertical circulation and attracts monsoon winds.
  • Tropical Easterly Jet: Develops during summer, strengthening monsoon trough and rainfall.
  • ENSO:
    • El Niño: Warms Pacific waters, usually weakening Indian monsoon.
    • La Niña: Cools Pacific, often strengthening monsoon.
  • Indian Ocean Dipole (IOD):
    • Positive IOD: Strengthens monsoon with warm western Indian Ocean.
    • Negative IOD: Weakens monsoon.

Onset and Advancement

  • Arabian Sea Branch: Hits Kerala around June 1, moves up the west coast, bringing heavy rain to Western Ghats and inland states.
  • Bay of Bengal Branch: Reaches Northeast India in early June, then moves westward along the Indo-Gangetic plain. India is usually fully covered by mid-July.
  • Retreat of the Monsoon: Retreat begins in October from northwest India. Clear skies and residual moisture cause hot, humid conditions called “October heat.”
  • Reversal of wind direction brings rain to the southeastern coast, notably Tamil Nadu and Andhra Pradesh.

Impact of the Monsoon

  • Agriculture: Essential for Kharif crops like rice and maize. A good monsoon improves yields; a poor one leads to drought.
  • Economy: Monsoon-linked agriculture influences GDP, rural income, and food prices.
  • Water Resources and Hydropower: Rains recharge rivers and reservoirs, crucial for drinking water, irrigation, and electricity.
  • Environment and Culture: Supports biodiversity and cultural traditions like festivals celebrating rain.
  • Disasters: Heavy rains can trigger floods, landslides, and other disasters, especially in vulnerable regions.

Recent Government Initiatives to Improve Monsoon Forecasting

  • Monsoon Mission: Launched in 2012 by the Ministry of Earth Sciences it was a major initiative aimed at enhancing the accuracy of monsoon forecasting.
  • National Supercomputing Mission: Aimed at enhancing computational infrastructure needed for running high-end dynamical weather models.
  • ICAR & IMD Collab: The IMD, in collaboration with the Indian Council of Agricultural Research (ICAR), provides Agromet Advisory Services.

Source: TH