Editorial Summary The Hindu uses IMD’s below-normal 2026 monsoon projection to examine India’s structural agricultural vulnerabilities — rainfed dependence, groundwater depletion, low PMFBY coverage, and slow NDMA protocol activation. The editorial calls for automatic monsoon-response protocols triggered by IMD forecasts, rather than reactive crisis management.


El Niño and India’s Monsoon — The Mechanism

Central Pacific warms (El Niño event)
     ↓
Walker Circulation weakens
     ↓
Indian Ocean temperature gradient reduces
     ↓
Southwest Monsoon weaker inflow
     ↓
Below-normal rainfall in India (historically 8–12% deficit)

Modulating factor: A positive Indian Ocean Dipole (IOD) — warmer western Indian Ocean — can partially offset El Niño by independently strengthening monsoon inflow. The IOD’s status (announced April–May) determines El Niño’s actual impact on Indian monsoon.


Historical El Niño Drought Years in India

Year El Niño Intensity Monsoon Departure Impact
2002 Moderate −19% Severe drought; 21 states affected
2009 Moderate −23% Second worst in 35 years
2015 Strong −14% 12 states declared drought; MGNREGS surge
2023 Strong −6% Partial: spatial heterogeneity; SW below-normal

PMFBY — The Insurance Gap

Metric Value
Launch 2016 (replaced NAIS)
Coverage ~32% of sown area (FY24)
Premium subsidy 50% Central + 25% State + 2% farmer
Claim settlement time 45–60 days (often delayed to 90+)
States opted out AP, Bihar, West Bengal, Gujarat
Target Should cover 50%+ of sown area for meaningful risk transfer

UPSC Relevance

Paper Angle
GS1 — Geography El Niño mechanism; Indian Ocean Dipole; monsoon patterns
GS3 — Agriculture Rainfed agriculture; PMFBY; drought resilience; PMKSY
GS3 — Economy Food inflation; CPI linkage; FCI buffer stocks
GS2 — Governance NDMA drought manual; disaster preparedness protocols
Mains Keywords El Niño, Indian Ocean Dipole (IOD), IMD long-range forecast, Southwest Monsoon, PMFBY, PMKSY, NDMA drought manual, rainfed agriculture, groundwater depletion, FCI buffer stocks