Southwest monsoon has arrived in Andaman and Nicobar

  • The India Meteorological Department announced that the Southwest Monsoon (SWM) advanced over the Andaman Sea and Andaman & Nicobar Islands on 16 May 2026 and is likely to reach Kerala by 26 May 2026, nearly six days earlier than the normal onset date of 1 June.
  • Despite the early onset, IMD has forecast below-normal seasonal rainfall at 92% of the Long Period Average (LPA), with a growing probability of El Niño conditions, which may suppress monsoon rainfall over India.

Relevance

  • GS Paper 1: Indian monsoon system, climatology, and oceanatmosphere interactions.
  • GS Paper 3: Agriculture, disaster management, water resources, and climate change.

Practice Question  

An early onset of the southwest monsoon does not necessarily guarantee above-normal rainfall. Discuss in the context of El Niño and its implications for Indias agriculture and economy. (15 Marks, 250 Words)

What is the Southwest Monsoon?
  • The Southwest Monsoon is India’s principal rainy season extending from June to September and contributes nearly 70% of annual rainfall. It is driven by seasonal reversal of winds caused by differential heating between land and ocean.
  • The monsoon typically reaches Kerala around 1 June and advances northward to cover most of India by mid-July, replenishing reservoirs, groundwater, and supporting agricultural sowing.
Branches of the Monsoon
  • The monsoon divides into the Arabian Sea Branch and the Bay of Bengal Branch. Together they deliver rainfall to the Western Ghats, Indo-Gangetic Plains, northeastern states, and peninsular India.
Early Arrival
  • The 2026 onset over Kerala is expected around 26 May (±4 days), making it an early arrival compared with the climatological date of 1 June.
Onset Does Not Determine Seasonal Rainfall
  • The timing of onset reflects atmospheric conditions over the southern coast, but it does not reliably predict the spatial distribution or total rainfall during the full four-month season.
Definition
  • El Niño is the warm phase of the El Niño–Southern Oscillation (ENSO), characterized by unusually warm sea surface temperatures in the central and eastern equatorial Pacific Ocean.
Impact on India
  • El Niño generally weakens the Walker Circulation and reduces moisture-bearing monsoon winds, increasing the probability of deficient rainfall and drought-like conditions.
El Niño Outlook for 2026
  • The National Oceanic and Atmospheric Administration estimated an 82% probability of El Niño development during MayJuly 2026 and a 96% probability of persistence through December 2026–February 2027.
  • Meteorological agencies indicate the possibility of a strong El Niño, which could intensify adverse impacts on rainfall, agriculture, and water availability.
  • IMD has projected seasonal rainfall at 92% of LPA, which falls in the below-normal category under official classification.
  • The forecast also suggests roughly a 35% probability of deficient rainfall, raising concerns regarding drought-prone and rain-fed regions.
Agriculture
  • Nearly 50–55% of India’s net sown area remains rain-fed, and a substantial share of farmers depend on timely monsoon rainfall for sowing crops such as rice, soybean, pulses, and cotton.
Water Security
  • Monsoon rainfall replenishes reservoirs, rivers, and aquifers that support drinking water, irrigation, and industrial use.
Energy and Economy
  • Hydropower generation, rural demand, inflation, and overall economic growth are closely linked to monsoon performance.
Agricultural Stress
  • Reduced rainfall can delay sowing, lower crop yields, and increase dependence on irrigation, especially in semi-arid and drought-prone regions.
Food Inflation
  • Lower production of cereals, pulses, and vegetables may raise food prices and affect household consumption.
Water Scarcity
  • Reservoir deficits and declining groundwater recharge can intensify rural and urban water stress.
Rural Distress
  • Crop losses may increase indebtedness and reduce incomes in rain-dependent farming areas.
  • The Indo-Gangetic Plain, parts of central India, and peninsular drought-prone regions are particularly vulnerable to rainfall deficits and long-term drying trends.
  • Coastal and northeastern regions may still experience localized heavy rainfall even in below-normal monsoon years.
  • Global warming is increasing the frequency of extreme rainfall events, longer dry spells, and greater variability in monsoon behavior.
  • Climate change can amplify the economic consequences of El Niño by increasing uncertainty in agriculture and water management.
  • India Meteorological Department provides extended-range forecasts and region-specific advisories to farmers.
  • Indian Council of Agricultural Research develops contingency crop plans for delayed or deficient rainfall.
  • Schemes such as Pradhan Mantri Fasal Bima Yojana and Pradhan Mantri Krishi Sinchai Yojana help reduce weather-related risks.
  • Normal onset date of the southwest monsoon over Kerala is 1 June.
  • IMD forecast for 2026 seasonal rainfall: 92% of LPA.
  • El Niño is associated with warming of the equatorial Pacific Ocean.
  • The Southwest Monsoon contributes about 70% of India’s annual rainfall.
  • ENSO stands for El Niño–Southern Oscillation.

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