← Resources · July 03, 2026
Environment & Ecology GSGS 5 min read

Union Home Minister and Minister and Cooperation Shri Amit Shah and Union Minister of Agriculture and Farmers Welfare Shri Shivraj Singh Chouhan reviews situation regarding below-normal rainfall and its impact in certain parts of country due to ‘El Niño’

What happened
01

The Union Home Ministry and the Ministry of Agriculture jointly convened a high-level review meeting to assess the impact of below-normal rainfall on parts of India during the 2026 southwest monsoon season.

02

India's June 2026 monsoon opened with a steep 40% rainfall deficit, driven by a strengthening El Niño, with central, eastern, and northeastern regions worst affected.

03

The India Meteorological Department (IMD) has forecast the 2026 monsoon season at approximately 90% of the Long Period Average (LPA) — classified as below-normal — with an 84% probability of deficient or below-normal rainfall.

04

Around 200 districts have been flagged as vulnerable to El Niño-related agricultural stress, with the Centre directing states to activate stage-wise crop and irrigation contingency plans.

05

The review examined both immediate drought relief measures and medium-term impact on kharif sowing, reservoir levels, groundwater recharge, and rural incomes.

Static topic 1 of 4 · Environment & Ecology

El Niño and the El Niño-Southern Oscillation (ENSO)

El Niño is the warm phase of the El Niño-Southern Oscillation (ENSO) — a periodic climate pattern driven by anomalous warming of sea surface temperatures (SSTs) in the central and eastern tropical Pacific Ocean. It operates on a 2–7 year cycle. The complementary cool phase, La Niña, has the opposite effect. The atmospheric component of ENSO — the pressure seesaw between the eastern and western Pacific — is called the Southern Oscillation; together they form ENSO.

Key Details

  • During El Niño, anomalously warm Pacific SSTs suppress convective activity over the Indian subcontinent, weakening the southwest monsoon.
  • During La Niña, cooler Pacific SSTs enhance convection over India, typically strengthening the monsoon.
  • El Niño years with significant Indian monsoon deficits include 2002, 2009, and 2015; La Niña years tend to bring excess rainfall.
  • The Southern Oscillation Index (SOI) measures atmospheric pressure differences between Tahiti and Darwin, Australia — a negative SOI indicates El Niño conditions.
Connection to this news

The 2026 El Niño is suppressing convective activity over the Indian subcontinent, directly causing the below-normal rainfall deficit flagged in the government's review.

Static topic 2 of 4 · Environment & Ecology

Indian Ocean Dipole (IOD) and Its Modulating Effect

The Indian Ocean Dipole (IOD) is a climate phenomenon defined by the difference in SSTs between the western Indian Ocean (Arabian Sea) and the eastern Indian Ocean (south of Indonesia). A positive IOD — warmer Arabian Sea, cooler eastern Indian Ocean — can partially counteract El Niño's negative effect on the Indian monsoon.

Key Details

  • A positive IOD historically counteracted El Niño in years like 1983, 1994, and 1997, producing near-normal monsoon rainfall despite El Niño conditions.
  • A negative IOD combined with El Niño creates the worst-case scenario — as in 2002 and 2015, when India recorded severe droughts.
  • The IOD develops from April–May and peaks in October, making its phase critical to seasonal monsoon forecasts.
  • IMD and the World Meteorological Organization (WMO) monitor both ENSO and IOD in issuing Long Range Forecasts (LRF).
Connection to this news

The forecast for below-normal 2026 rainfall indicates that IOD modulation is insufficient to offset the El Niño effect this season, heightening drought risk.

Static topic 3 of 4 · Environment & Ecology

India's Drought Management Framework

India classifies drought under the Disaster Management Act, 2005. The National Disaster Management Authority (NDMA) issues guidelines for drought management; states are responsible for declaration and relief. The Manual for Drought Management (2016) specifies drought declaration criteria, monitoring parameters, and permissible relief heads under SDRF/NDRF funding.

Key Details

  • Drought declaration triggers in India: States assess meteorological, hydrological, agricultural, and socio-economic indicators; formal declaration is by the state government.
  • State Disaster Response Fund (SDRF): Primary relief fund, maintained by states; Centre contributes 75% (90% for special category states) of the annual allocation.
  • National Disaster Response Fund (NDRF): Additional central support for disasters beyond state capacity, managed by the NDMA.
  • Pradhan Mantri Fasal Bima Yojana (PMFBY): Crop insurance scheme providing financial protection to farmers against crop loss from drought, flood, and other perils.
  • The IMD's Long Period Average (LPA) for annual rainfall is approximately 87 cm; below-normal is defined as 90–96% of LPA; deficient is below 90%.
Connection to this news

The government review directly invokes the NDMA-NDRF framework to assess which districts require central drought relief support, and whether PMFBY and contingency crop plans need activation.

Static topic 4 of 4 · Environment & Ecology

Kharif Agriculture and Monsoon Dependency

India's agricultural calendar is bifurcated into kharif (summer/monsoon) and rabi (winter) seasons. Kharif crops — sown in June–July and harvested in September–October — are almost entirely rain-fed and depend critically on the southwest monsoon. Major kharif crops include rice, maize, jowar, bajra, cotton, soybean, and sugarcane.

Key Details

  • Approximately 60% of India's net sown area is rain-fed; these farmers have no access to irrigation infrastructure.
  • A 10% decline in rainfall can reduce kharif output by 4–6%, with proportionally larger impacts on coarse cereals and pulses grown in rain-shadow regions.
  • Below-normal monsoon depresses rural incomes, increases food price inflation, and strains rural credit demand — channels through which agricultural stress transmits to the broader economy.
  • The government's contingency crop planning involves recommending alternative shorter-duration or drought-resistant varieties when sowing is delayed beyond threshold dates.
Connection to this news

The joint ministry review specifically examined kharif sowing prospects in 200 vulnerable districts — areas where delayed or deficient rainfall can lead to widespread crop failure and demand for drought relief.

Key facts & data
  • India's June 2026 monsoon deficit: approximately 40% below normal
  • IMD's 2026 seasonal forecast: approximately 90% of LPA (below-normal category)
  • Probability of below-normal or deficient 2026 rainfall: 84%
  • Number of districts flagged for El Niño vulnerability: approximately 200
  • Long Period Average (LPA) for Indian annual rainfall: approximately 87 cm
  • IMD definition of below-normal: 90–96% of LPA; deficient: below 90%
  • Drought Management Act framework: Disaster Management Act, 2005
  • NDMA (National Disaster Management Authority): established under Disaster Management Act, 2005, chaired by the Prime Minister
  • PMFBY (Pradhan Mantri Fasal Bima Yojana): crop insurance scheme covering kharif and rabi crops
  • El Niño cycle frequency: every 2–7 years
  • Major drought years linked to El Niño: 2002, 2009, 2015
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