EnvironmentGS3+ GS1

El Niño threat persists for rabi crops despite July monsoon revival

Indian Express·2026-08-11· Read original

"El Niño threat persists for rabi crops despite July monsoon revival"

Prelims Facts

  • •El Niño defined when SSTs in Niño 3.4 region exceed climatological mean by +0.5°C for five consecutive overlapping three-month periods
  • •India's Southwest Monsoon (June–September) delivers ~75% of annual rainfall; LPA ≈ 887 mm; below-normal threshold = <90% of LPA
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Key Terms

Low-Pressure System (LPS)

synoptic-scale weather system over Bay of Bengal that delivers concentrated monsoon rainfall inland

Long Period Average (LPA)

baseline average rainfall (~887 mm) against which seasonal monsoon performance is measured

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Study Note

BackgroundCore Concept

Background

India's Southwest Monsoon (June–September) is the agricultural lifeline of the country, delivering approximately 75% of annual rainfall against a Long Period Average (LPA) of ~887 mm. The monsoon's behaviour is critically shaped by the El Niño–Southern Oscillation (ENSO) — a naturally recurring ocean-atmosphere coupled phenomenon in the tropical Pacific. El Niño, the warm phase of ENSO, is defined when sea surface temperatures (SSTs) in the Niño 3.4 region of the central-eastern equatorial Pacific exceed the climatological mean by +0.5°C for five consecutive overlapping three-month periods. Historically, roughly 60% of strong El Niño years have coincided with below-normal monsoon rainfall in India, though modulating factors such as the Indian Ocean Dipole (IOD) and the Madden-Julian Oscillation (MJO) can offset or amplify this suppressive effect.

Kharif crops — sown with the onset of the monsoon and harvested in autumn — include rice, pulses, oilseeds, cotton, and soyabean, and are directly dependent on the June–September rainfall window. Rabi crops (wheat, mustard, potato), sown in October–November and harvested in spring, depend less on monsoon rain but are sensitive to winter temperatures, which El Niño is known to elevate. India's import dependence on oilseeds, pulses, and cotton means that domestic production shortfalls from weather shocks translate rapidly into import bills and global price exposure.

The Topic Explained

The mechanism by which El Niño suppresses Indian monsoon rainfall operates through the Walker Circulation — the zonal atmospheric loop in the tropical Pacific. Under normal conditions, strong easterly trade winds push warm surface water westward, sustaining rising moist air over the Indo-Pacific Warm Pool and driving monsoon convection over India. During El Niño, trade winds weaken or reverse, warm water shifts eastward toward the central-eastern Pacific, and the Walker Circulation weakens. This induces subsidence (sinking air) over the Indian Ocean, suppressing convective activity and reducing the moisture-laden winds that fuel the Southwest Monsoon.

A critical mechanism for monsoon variability within the season is the formation of Low-Pressure Systems (LPS) — synoptic-scale weather systems that develop over the Bay of Bengal and move inland, delivering concentrated rainfall across central and peninsular India. …

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Related PYQs

2014GS1 Prelims

The seasonal reversal of winds is the typical characteristic of

AEquatorial climate
BMediterranean climate
CMonsoon climate
DAll of the above climates
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2020GS1 Prelims

With reference to Ocean Mean Temperature (OMT), which of the following statements is/are correct?

1.OMT is measured up to a depth of 26°C isotherm which is 129 metres in the south-western Indian Ocean during January-March.

2.OMT collected during January-March can be used in assessing whether the amount of rainfall in monsoon will be less or more than a certain long-term mean.

Which of the statements given above is/are correct?

A1 only
B2 only
CBoth 1 and 2
DNeither 1 nor 2
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Practice MCQs

Environmentmedium

With reference to Low-Pressure Systems (LPS) and the Indian Southwest Monsoon, consider the following statements:

1.A normal June monsoon season witnesses approximately three LPS active over about 11 days.

2.LPS formation over the Bay of Bengal is the primary mechanism delivering rainfall to peninsular and central India during the monsoon season.

3.El Niño conditions directly suppress LPS formation by strengthening easterly trade winds over the Bay of Bengal.

Which of the statements given above is/are correct?

A1 and 2 only
B2 and 3 only
C1 and 3 only
D1, 2 and 3
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Environmenteasy

The FAO Food Price Index is best described as:

AA simple average of retail food prices in developing countries, updated annually by the UN
BA weighted average of world prices of a basket of food commodities, indexed to a base period value of 100 for 2014–16
CAn index measuring food price inflation in G20 economies, published quarterly by the World Bank
DA composite index of food production volumes and export prices, maintained by the WTO
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Environmentmedium

Consider the following statements about El Niño's impact on Indian agriculture:

1.El Niño's suppressive effect on Indian monsoon rainfall typically manifests with a lag of 1–2 months after the phenomenon intensifies.

2.El Niño raises global temperatures, which can shorten and warm Indian winters, adversely affecting wheat and mustard yields.

3.Historically, all strong El Niño years have resulted in below-normal monsoon rainfall in India.

Which of the statements given above is/are correct?

A1 only
B1 and 2 only
C2 and 3 only
D1, 2 and 3
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