·The Hindu

‘El Nino may occur after July; clear picture to emerge after April’

In this note
  1. At a Glance
  2. Why in the News
  3. Background & Evolution
  4. Core Static Facts
  5. Multi-Dimensional Analysis
  6. Recent Developments (Last 12–18 Months)
  7. Prelims Hooks (High-Density Factual Bullets)
  8. Mains Relevance
  9. Related Topics to Study Next
  10. Common Errors / Trap Areas
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1. At a Glance

  • El Niño is a periodic warming of the central-eastern equatorial Pacific Ocean, part of the ENSO (El Niño–Southern Oscillation) cycle, with major teleconnections to India's Southwest Monsoon (SWM). [1]
  • IMD defines El Niño as sustained warming of the central equatorial Pacific by ≥ 0.5 °C above average for five consecutive overlapping three-month periods. [1]
  • Historically, 6 out of 10 El Niño years are associated with below-normal monsoon rainfall over India — making it the single most important oceanic driver for Indian agriculture and food security. [1]
  • A UPSC aspirant must understand the ENSO mechanism, its India-specific impacts, IMD's forecasting apparatus, and associated policy responses (drought declaration, crop insurance, MSP adjustments).

2. Why in the News

  • February 1, 2026: IMD Director-General M. Mohapatra, in his monthly weather briefing, stated that ENSO-neutral conditions were likely to persist until July 2026, but there was a probability of a shift to El Niño conditions thereafter. [1]
  • Latest climate models (as of early Feb 2026) show >50% probability of El Niño after June 2026, rising to ~70% probability during July–August–September — the peak months of the SWM. [1]
  • Skymet (private forecasting agency) Chairman Jatin Singh flagged "early" model signals of a 2026 El Niño, warning of a "sub-par monsoon and drought conditions." [1]
  • Clarity on El Niño formation expected only after April 2026, when boreal spring predictability barrier is overcome.

3. Background & Evolution

Year/Period Event
1950s ENSO identified as a coupled ocean-atmosphere phenomenon by Jacob Bjerknes
1982–83 One of the strongest El Niño events on record; major disruptions globally
1997–98 Most intense El Niño of the 20th century; severe global impacts
2002–03 El Niño linked to drought in India; below-normal monsoon
2009 El Niño year; India received ~23% below-normal SWM rainfall
2014–15 Moderate El Niño; partial monsoon deficiency in India
2015–16 Super El Niño (strongest since 1997–98); severe drought in parts of India
2023–24 Most recent El Niño; global temperatures hit record highs; below-normal rainfall in India [1]
2024–25 Transition to La Niña conditions
2026 ENSO-neutral → possible El Niño post-July (current forecast) [1]
  • Predecessors: Walker Circulation concept (Gilbert Walker, 1920s) laid the theoretical basis; Bjerknes (1969) formalized the feedback loop.

4. Core Static Facts

Definitions & Classification

Term Definition
El Niño Anomalous warming of central-eastern equatorial Pacific ≥ 0.5 °C for ≥5 consecutive overlapping 3-month periods [1]
La Niña Converse; anomalous cooling of central equatorial Pacific by ≥ 0.5 °C [1]
ENSO El Niño–Southern Oscillation; the coupled ocean-atmosphere cycle encompassing El Niño, La Niña, and neutral phases
ENSO-Neutral Neither El Niño nor La Niña conditions; SST anomalies within ±0.5 °C of average
Niño 3.4 Region Primary monitoring region (5°N–5°S, 120°–170°W) used to define ENSO state
ONI Oceanic Niño Index — the standard NOAA index; 3-month running mean of SST anomaly in Niño 3.4 region
SOI Southern Oscillation Index — atmospheric component; measures sea-level pressure difference between Tahiti and Darwin
IOD Indian Ocean Dipole — a separate but related phenomenon; Positive IOD offsets El Niño's impact on India

Implementing / Monitoring Bodies

  • India Meteorological Department (IMD) — under Ministry of Earth Sciences (MoES); issues seasonal forecasts [1]
  • NOAA/CPC (USA) — global ENSO monitoring; issues monthly ENSO outlooks
  • WMO — coordinates international ENSO monitoring via WCRP/CLIVAR
  • Skymet — private weather agency in India; issues independent seasonal forecasts [1]

Key Numbers (Examinable)

Fact Value
El Niño threshold (SST anomaly) +0.5 °C
Duration criterion 5 consecutive overlapping 3-month periods
Historical monsoon failure association 6 out of 10 El Niño years [1]
2026 El Niño probability (post-June) >50%
2026 El Niño probability (Jul–Sep) ~70% [1]
Last El Niño 2023–24 [1]
India's SWM period June–September
Peak SWM months July–August

5. Multi-Dimensional Analysis

Environmental

  • El Niño suppresses the Intertropical Convergence Zone (ITCZ) over the Indian Ocean, weakening the pressure gradient that drives monsoon winds into India.
  • Warmer Pacific SSTs alter the Walker Circulation — weakening rising air over the Indian Ocean, reducing convective rainfall.
  • Positive IOD (warm western Indian Ocean vs. cool east) can partially counteract El Niño's negative effect on Indian monsoon — as seen in 2019, when positive IOD rescued monsoon despite El Niño.
  • ENSO events have intensified in frequency and magnitude under anthropogenic climate change (IPCC AR6 finding), complicating seasonal forecasting.

Economic

  • Below-normal monsoon directly depresses Kharif crop output (rice, pulses, oilseeds, sugarcane) — India's food security and agricultural GDP (≈14% of GDP) at risk.
  • Inflation risk: Deficient monsoon triggers vegetable and pulses price spikes — a key input to CPI food inflation monitored by the RBI for monetary policy.
  • Hydropower generation falls in El Niño years (reduced reservoir inflows), pushing up electricity prices and industrial costs.
  • Agriculture employs ~45% of India's workforce; monsoon failure triggers rural income shocks, distress migration, and reduced rural consumption.

Administrative / Policy

  • IMD's seasonal forecast (typically issued April) is the key trigger for government preparedness: procurement buffer stocking, NFSA operations, drought contingency plans.
  • NDMA (National Disaster Management Authority) activates drought protocols; state governments declare drought/scarcity under their respective State Disaster Management Acts.
  • PM-FASAL (Fasal Bima) and PMFBY (PM Fasal Bima Yojana) — crop insurance schemes that are central to farmer income protection in El Niño years.
  • Spring predictability barrier (March–May) makes early El Niño forecasts unreliable — explains IMD's caution that "clarity will only emerge after April." [1]

Scientific / Technological

  • Modern coupled General Circulation Models (CGCMs) — e.g., NCEP CFS, ECMWF SEAS, UK Met Office GloSea — are the tools producing the probabilistic outlooks cited by IMD. [1]
  • IMD uses Extended Range Prediction System (ERPS) for weekly-scale monsoon forecasts and Seasonal Prediction Model (Monsoon Mission CFS) for seasonal outlooks.
  • Argo floats, TAO/TRITON buoy array in the Pacific, and satellite altimetry (TOPEX/Jason series) provide real-time ocean monitoring underpinning ENSO forecasts.
  • Boreal spring predictability barrier: ENSO forecasts made before May are inherently less reliable due to high signal-to-noise ratio during spring; this is why IMD explicitly cites April as the clarity threshold. [1]

Geopolitical / Strategic

  • India's food export commitments (rice, wheat) are calibrated against domestic surplus projections — El Niño years may necessitate export restrictions (as in 2023 rice export ban).
  • Regional food security in South Asia and Southeast Asia is correlated with Indian production; El Niño-linked deficits have humanitarian ripple effects in Bangladesh, Nepal, Sri Lanka.
  • India's WTO agricultural commitments (Agreement on Agriculture) constrain subsidy and procurement responses to drought-induced production shortfalls.

Social

  • Drought in El Niño years historically drives farmer distress, debt defaults, and suicide clusters — particularly in Maharashtra, Karnataka, Telangana, Madhya Pradesh.
  • Tribal and dryland farming communities (Vidarbha, Bundelkhand, Marathwada) are disproportionately vulnerable given rain-fed agriculture dependence.
  • MGNREGS (Mahatma Gandhi National Rural Employment Guarantee Scheme) serves as the primary drought-relief employment buffer; demand spikes in El Niño years, testing fiscal headroom.

6. Recent Developments (Last 12–18 Months)

  • 2023–24: El Niño event caused record global temperatures (2024 hottest year on record per WMO); India experienced below-normal SWM rainfall and heat wave intensification. [1]
  • 2024–25 (La Niña transition): ENSO shifted to La Niña, associated with above-normal SWM 2024 for most of India; reservoirs above long-period average.
  • Early 2025: La Niña conditions; IMD forecast above-normal/normal monsoon for 2025.
  • Late 2025: Gradual transition back to ENSO-neutral; global models begin signalling possible 2026 El Niño.
  • February 1, 2026: IMD DG Mohapatra states >50% El Niño probability post-June; ~70% for Jul–Sep; final clarity after April. [1]
  • Skymet (early 2026): Independent forecast aligns with El Niño risk; warns of potential "sub-par monsoon and drought." [1]

7. Prelims Hooks (High-Density Factual Bullets)

  1. El Niño is defined as central equatorial Pacific SST warming of ≥ 0.5 °C above average for five consecutive overlapping three-month periods. [1]
  2. Historically, 6 out of 10 El Niño years have been associated with below-normal monsoon rainfall in India. [1]
  3. The last El Niño before the 2026 forecast was the 2023–24 event, which caused below-normal rainfall in India. [1]
  4. La Niña is the converse of El Niño — a cooling of the central Pacific by ≥ 0.5 °C; El Niño and La Niña are cyclical phenomena. [1]
  5. IMD's seasonal forecast is typically issued in April, coinciding with overcoming the spring predictability barrier.
  6. ENSO-neutral conditions are expected to persist until July 2026 before possible El Niño onset. [1]
  7. Climate models (Feb 2026) show >70% probability of El Niño during July–August–September 2026 — the peak SWM months. [1]
  8. The Niño 3.4 region (5°N–5°S, 120°–170°W) is the standard monitoring zone for ENSO classification.
  9. The Oceanic Niño Index (ONI) — 3-month running mean of SST anomaly in Niño 3.4 — is NOAA's standard ENSO metric.
  10. IMD is under the Ministry of Earth Sciences (MoES), not the Ministry of Environment — a common confusion.
  11. Positive IOD can partially offset El Niño's suppressive effect on India's monsoon (e.g., 2019 rescue effect).
  12. The Southern Oscillation Index (SOI) measures sea-level pressure difference between Tahiti and Darwin — the atmospheric signature of ENSO.
  13. Skymet is a private weather forecasting company; IMD is the government agency under MoES. [1]
  14. M. Mohapatra is the Director-General of IMD (as of the February 2026 briefing). [1]
  15. July and August are identified as the "most important months" of India's summer monsoon season. [1]

8. Mains Relevance

GS Paper Mapping:

GS Paper Syllabus Heading
GS-I Important Geophysical phenomena — cyclones, earthquakes, tsunamis, volcanoes; climatic changes
GS-III Indian Economy — agriculture, food security; Disaster management — drought
GS-III Environment — climate change; conservation

Plausible Mains Question Stems:

  1. "El Niño events are becoming more frequent and intense under climate change. Examine the mechanisms through which El Niño affects India's monsoon and the policy preparedness required to mitigate its socio-economic impact." (GS-III)

  2. "Despite El Niño conditions in 2023-24, India's agricultural output remained resilient. Critically analyse the factors that can buffer India against El Niño-induced monsoon deficits." (GS-III)

  3. "Discuss the role of the Indian Ocean Dipole (IOD) in modulating El Niño's impact on the Indian monsoon. How does this complicate seasonal weather forecasting?" (GS-I)


9. Related Topics to Study Next

Topic Connection
Indian Ocean Dipole (IOD) Direct modulator of El Niño's India-monsoon teleconnection
Southwest Monsoon — Mechanisms & Variability El Niño's primary Indian impact pathway
PM Fasal Bima Yojana (PMFBY) Policy instrument activated in drought/El Niño years
MGNREGS Demand-side drought buffer; spikes in El Niño years
National Action Plan on Climate Change (NAPCC) Broader framework under which ENSO risk adaptation falls
Walker Circulation & Hadley Cell Atmospheric mechanisms linking Pacific SST to global rainfall
WMO & WCRP/CLIVAR International bodies coordinating ENSO monitoring and research
Drought Management in India (NDMA guidelines) Administrative response to El Niño-induced monsoon deficits

10. Common Errors / Trap Areas

  1. IMD vs. IMD / Ministry confusion: IMD is under Ministry of Earth Sciences (MoES), NOT Ministry of Environment, Forests and Climate Change (MoEFCC). Frequently confused.

  2. El Niño = bad monsoon (always): WRONG — historically only 6/10 El Niño years see below-normal monsoon. Positive IOD (2019) or favourable MJO can rescue the monsoon even during El Niño.

  3. El Niño vs. La Niña directional confusion: El Niño = warming (→ weak monsoon risk for India); La Niña = cooling (→ generally better/above-normal monsoon for India). Candidates sometimes invert this.

  4. ENSO = Pacific only: Trap — ENSO is a coupled ocean-atmosphere phenomenon. The atmospheric component (Walker Circulation, SOI) is equally important. IOD is a separate Indian Ocean phenomenon, not part of ENSO.

  5. Spring predictability barrier misunderstood: Forecasts issued before April–May for the monsoon season are inherently less reliable — not a data failure but a fundamental property of ENSO dynamics. IMD's "clarity after April" statement reflects this scientific constraint, not institutional limitation. [1]


Sources

  1. 1'El Nino may occur after July; clear picture to emerge after April' — Jacob Koshy, The Hindu, February 1, 2026 — `thehindu.com · tier 4
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