Monsoon Withdrawal 2026: IMD Retreating Monsoon Mechanism and El Nino Link for Exams
Geography12 min readSep 14, 2026Updated Sep 17, 2026

Monsoon Withdrawal 2026: IMD Retreating Monsoon Mechanism and El Nino Link for Exams

Monsoon Withdrawal 2026: IMD Retreating Monsoon Mechanism and El Nino Link for Exams
12 min read · 2,321 words

Monsoon Withdrawal 2026: IMD Retreating Monsoon Mechanism and El Nino Link for Exams

Quick Answer: What Is Monsoon Withdrawal 2026 and Why It Matters for Exams

In one line: Monsoon withdrawal 2026 is the IMD’s formal declaration of the southwest monsoon’s retreat — starting from west Rajasthan around 17 September and wrapping up nationwide by around 15 October — and every element of it is proven exam material.

Quick answer: Monsoon withdrawal is the process by which the India Meteorological Department (IMD) declares the end of the southwest monsoon over different parts of the country. It begins from west Rajasthan around 17 September and completes over the entire country by around 15 October. The IMD does not withdraw the monsoon on hunches — it applies fixed, science-based criteria: no rainfall for five continuous days, establishment of an anticyclone in the lower troposphere, and reduced moisture confirmed through satellite imagery. In 2026, as in recent years, Pacific ocean conditions — El Nino or La Nina — will influence both monsoon strength and withdrawal timing, which is exactly why examiners pair the two. Read the dates, the criteria, and the El Nino link once now and once before your exam: UPSC, SSC, Banking and CLAT have all lifted direct questions from each of these elements.

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What Is the Retreating Monsoon? Definition and Seasonal Timing

The retreating monsoon, also called the reversing monsoon or northeast monsoon, is the gradual withdrawal of the southwest monsoon winds from the Indian subcontinent between September and December. Commit the mechanism to memory as a chain: as the sun apparently moves southward after the summer solstice, the low-pressure system over northwest India weakens, the Inter-Tropical Convergence Zone (ITCZ) shifts south, and the moisture-laden southwest winds are replaced by dry continental winds blowing from land to sea. Examiners love to test this reversal — winds flip from sea-to-land to land-to-sea, and that single fact eliminates half the wrong options.

Memorise this timeline — it is the most examined part of the topic:

  • Mid-September (around 17 September): withdrawal begins from extreme west Rajasthan and parts of Kutch in Gujarat.
  • By end of September: withdrawal covers most of northwest India, including Punjab, Haryana, Delhi and west Uttar Pradesh.
  • First fortnight of October: withdrawal advances into central India and the northern peninsula.
  • Around 15 October: withdrawal from most of the country; the extreme southeastern peninsula (Tamil Nadu coast) now transitions to the northeast monsoon rains of October–December.

The withdrawal window — roughly September to November — is popularly called the season of retreating monsoon, or the “October heat” season over northern India. Note the phrasing: hot and humid conditions, not rain-bearing winds — a classic one-mark distinction.

IMD Withdrawal Criteria: The Science Behind the Declaration

Since 2006, the IMD declares withdrawal of the southwest monsoon from a region only when all of the following synoptic conditions are satisfied together:

  1. Continuous absence of rainfall over the region for five consecutive days.
  2. Establishment of an anticyclone in the lower troposphere (around 850 hPa) — roughly 1.5 km above sea level — signalling dry, subsiding air taking over.
  3. Sharp fall in moisture content, clearly visible in satellite water vapour imagery as dryness in the middle and lower troposphere.
  4. Persistence of these conditions, confirming that the monsoon circulation has genuinely weakened over the region and not merely paused.

These objective criteria exist for one reason: withdrawal is never declared just because of a temporary break in rainfall. Examiners exploit exactly this distinction — they will offer “no rain for a few days” as a withdrawal condition and expect you to reject it. Fix two numbers in your memory before the exam: 850 hPa and the five-day no-rainfall rule. Both are proven MCQ hooks. Verify details on the official IMD monsoon pages at mausam.imd.gov.in.

Stages of Monsoon Withdrawal Across India

Withdrawal follows a clear southwest-to-southeast retreat — the exact mirror image of the onset. Examiners love this reversal, so fix the direction first, then the dates. Read the five stages in order below; they are the most examined sequence in retreating monsoon questions.

  1. Stage 1 – Extreme west Rajasthan and Kutch: withdrawal begins here around 17 September. Remember this date — it is the single most asked figure in this topic.
  2. Stage 2 – Northwest India: Punjab, Haryana, Delhi, Uttarakhand, west Uttar Pradesh and Jammu — cleared by late September.
  3. Stage 3 – Central India and Gujarat: Madhya Pradesh, Chhattisgarh, Odisha, Maharashtra and Telangana — from the first week to mid-October.
  4. Stage 4 – Interior peninsula and northeast India: by around 15 October, including Vidarbha, Andhra Pradesh and the northeastern states.
  5. Stage 5 – Extreme southeastern peninsula: the final withdrawal does not end in silence — it merges with the onset of the northeast monsoon rains over Tamil Nadu, coastal Andhra, Kerala and south interior Karnataka. This overlap is a classic statement-based trap in UPSC and SSC papers.

Memory hook — learn it once and the whole map falls into place: onset begins from Kerala, withdrawal begins from west Rajasthan, and withdrawal runs as the mirror image of onset in direction.

Retreating Monsoon Weather: Why Tamil Nadu Gets Rain in October–December

During October–December, the prevailing winds reverse: they blow from the land (northeast) towards the sea. These dry continental winds pick up moisture while crossing the Bay of Bengal and then strike the Coromandel Coast (Tamil Nadu) and coastal Andhra Pradesh, where the Eastern Ghats force the moist air to rise — classic orographic lifting, and examiners love asking exactly where this lifting happens. Key exam points:

  • Tamil Nadu draws about 48% of its annual rainfall from the northeast monsoon — the single most examined statistic here — which is why Chennai’s wettest months are October–December.
  • Read this as a two-season pair: the windward side of the Western Ghats gets rain from the southwest monsoon (June–September), while Tamil Nadu, sitting in the rain shadow during those months, compensates during the retreating monsoon. This contrast is the most common trap in MCQs on Indian rainfall distribution.
  • October heat: after the southwest monsoon withdraws, clear skies and high humidity make northern India oppressive and stifling — the phenomenon labeled “October heat.” Remember the two ingredients: clear skies + trapped humidity.
  • Tropical cyclones: the retreat season overlaps with peak cyclonic activity in the Bay of Bengal (October–December), because warm sea surface temperatures (above 26.5°C) and low wind shear favour cyclogenesis. The landfalling systems batter the Odisha, Andhra Pradesh and Tamil Nadu coasts — a favourite current-affairs-to-geography link in exams.

El Nino and Its Effect on Monsoon Withdrawal and Strength

El Nino is the abnormal warming of sea surface temperatures (SSTs) over the central and eastern equatorial Pacific Ocean. Its effects on the Indian monsoon work through these mechanisms:

  • Warm Pacific SSTs shift convection eastward from the Indonesian region, weakening the Walker circulation (the east–west atmospheric circulation over the Pacific).
  • This weakens the southwest monsoon circulation and typically brings below-normal all-India rainfall — historically, about 60% of El Nino years have been drought years in India.
  • El Nino years often show a delayed onset, long breaks, and delayed or erratic withdrawal, because the monsoon trough and cross-equatorial flow remain disturbed.
  • El Nino years are also associated with suppressed Bay of Bengal cyclone activity during the monsoon season but sometimes enhanced post-monsoon storms over the Arabian Sea region, as noted in research cited by the Ministry of Earth Sciences (PIB).

For 2026: the IMD’s operational position, as issued in its seasonal forecasts and updated ENSO bulletins on mausam.imd.gov.in and press releases on PIB, should be quoted as the authoritative source. The IMD consistently states that ENSO (El Nino/La Nina) is one of several factors influencing monsoon strength, alongside the Indian Ocean Dipole (IOD), Madden–Julian Oscillation (MJO) and mid-latitude weather systems; its impact on withdrawal timing varies year to year. Candidates should always cite the latest IMD statement rather than assuming a fixed outcome.

Difference Between Southwest and Northeast Monsoon: Exam Comparison Table

FeatureSouthwest MonsoonNortheast (Retreating) Monsoon
Wind directionSea to land (southwest)Land to sea (northeast)
Onset/Withdrawal monthsOnset ~1 June (Kerala); withdraws Sept–OctSets in mid-October; active till December
Main rainfall regionsWest coast, Western Ghats windward side, Ganga plains, northeast IndiaTamil Nadu, coastal Andhra, Rayalaseema, south interior Karnataka, Kerala, Andaman & Nicobar
Dominant pressure systemLow pressure over north/northwest India; ITCZ shifted north; Tibetan Plateau heatingHigh pressure over land (cold Asian landmass); ITCZ shifted south of equator
Moisture sourceArabian Sea and Bay of Bengal branchesMoisture picked up over Bay of Bengal
Share of annual rainfallAbout 75% of India’s annual rainfallSmall nationally, but ~48% of Tamil Nadu’s annual rainfall

Climatic Regions and Retreating Monsoon: Geography Fundamentals

This topic connects directly to NCERT Class 11 Fundamentals of Physical Geography (Chapter: Climate) and covers:

  • Seasonal reversal of winds: differential heating of land and sea reverses pressure gradients between summer (thermal low over Asia) and winter (high pressure/cold Siberian anticyclone).
  • ITCZ shift: the monsoon trough (ITCZ) lies over the Ganga plain in July and shifts south of the equator in winter, driving the reversal.
  • Jet streams: the Subtropical Westerly Jet shifts south of the Himalayas in winter (bringing western disturbances), while the Tropical Easterly Jet (linked to Tibetan Plateau heating) strengthens the southwest monsoon.
  • Tibetan plateau heating: summer heating of the plateau acts as an elevated heat source, intensifying the monsoon circulation; its cooling in autumn aids withdrawal.
  • Climatic region link: the Coromandel Coast’s “rainfall in October–December” regime, and the semi-arid/monsoon regimes elsewhere, are classified in Koppen-based regionalisations used in Indian geography syllabi.

2026 Withdrawal News: Key Headlines and Data Points to Remember

For current-affairs accuracy, always anchor answers to official announcements:

  • The normal (long-period) withdrawal dates issued by IMD: 17 September from west Rajasthan; 15 October for the entire country.
  • IMD press releases on withdrawal milestones and seasonal rainfall (as % of the long-period average of ~87 cm) are published via PIB and mausam.imd.gov.in — quote the exact date and percentage given in the release of the day.
  • Track the ENSO bulletin (IMD’s monthly El Nino/La Nina update) for the 2026 season, and the IOD status, since both are cited in IMD’s seasonal outlooks.
  • Recent years show withdrawal has often been delayed by one to two weeks against normal dates, which itself becomes a headline data point for exams.

Note: Since 2026-specific dates are announced progressively during the season, verify the exact day of withdrawal declarations from the IMD release before writing them in an exam.

Previous Year Questions (PYQs) on Indian Monsoon

  • UPSC Prelims (2012): “The seasonal reversal of winds is the typical characteristic of — (a) Equatorial climate (b) Mediterranean climate (c) Monsoon climate (d) All of the above.” Answer: (c) Monsoon climate.
  • UPSC Prelims: Questions on the normal date of withdrawal of the southwest monsoon from extreme west Rajasthan (17 September) and on Tamil Nadu’s northeast monsoon rainfall regime have appeared repeatedly in one form or another.
  • SSC CGL: “Which state receives most rainfall from the northeast monsoon?” — Answer: Tamil Nadu.
  • SSC/Banking GA: “El Nino is associated with the warming of which ocean?” — Answer: The Pacific Ocean (central and eastern equatorial Pacific).

Rapid Revision: One-Page Fact Sheet for Exam Day

  • Withdrawal begins: west Rajasthan, ~17 September; complete over India: ~15 October.
  • IMD criteria (2006): 5 consecutive dry days + anticyclone at 850 hPa + dryness in water vapour imagery + reduced moisture.
  • Retreating monsoon = northeast monsoon; winds blow land to sea.
  • Tamil Nadu gets ~48% of annual rainfall in October–December.
  • October heat: hot, humid conditions over north India after withdrawal.
  • Bay of Bengal cyclones peak in October–December.
  • El Nino: warm central/eastern Pacific SSTs → weak Walker circulation → weaker monsoon; ~60% of El Nino years are Indian drought years.
  • Drivers of reversal: differential land–sea heating, ITCZ shift, Tibetan Plateau heating, jet streams.
  • Southwest monsoon = ~75% of India’s annual rainfall.

Practice MCQs on Monsoon Withdrawal

Q1. The IMD declares monsoon withdrawal from a region when there has been an absence of rainfall for how many consecutive days?
(a) 3 (b) 5 (c) 7 (d) 10
Answer: (b) 5

Q2. The normal date of commencement of southwest monsoon withdrawal is:
(a) 1 September from Kerala (b) 17 September from west Rajasthan (c) 15 October from Punjab (d) 1 October from Gujarat
Answer: (b) 17 September from west Rajasthan

Q3. Which of the following states receives the bulk of its rainfall during the retreating monsoon?
(a) Kerala (b) Punjab (c) Tamil Nadu (d) Assam
Answer: (c) Tamil Nadu

Q4. El Nino weakens the Indian monsoon primarily by:
(a) Cooling the Arabian Sea (b) Weakening the Walker circulation due to warm eastern Pacific SSTs (c) Strengthening the ITCZ over the Ganga plain (d) Increasing Tibetan Plateau snowfall in summer
Answer: (b) Weakening the Walker circulation

Q5. As per IMD criteria, the anticyclone signalling withdrawal is identified at which atmospheric level?
(a) 500 hPa (b) 200 hPa (c) 850 hPa (d) Sea level only
Answer: (c) 850 hPa

Frequently Asked Questions

Q: When does the monsoon usually withdraw from India?

Withdrawal of the southwest monsoon begins from west Rajasthan around 17 September and is normally completed over the entire country by around 15 October, as per IMD’s normal withdrawal dates.

Q: Does El Nino delay monsoon withdrawal?

El Nino can weaken monsoon circulation, and El Nino years have often seen delayed or erratic withdrawal — but the effect varies each year. For 2026, cite the IMD’s latest ENSO bulletin and seasonal outlook (mausam.imd.gov.in / PIB) as its stated position; IMD treats ENSO as one of several influencing factors, not the sole determinant.

Q: What is the northeast monsoon?

It is the October–December wind system blowing from land to sea, which picks up moisture over the Bay of Bengal and brings rain mainly to Tamil Nadu, coastal Andhra Pradesh, Rayalaseema and south interior Karnataka.

Q: What are IMD’s withdrawal criteria?

No rainfall for 5 consecutive days, establishment of an anticyclone at 850 hPa, dryness in satellite water vapour imagery, and a marked reduction in atmospheric moisture.

Q: Is monsoon withdrawal important for competitive exams?

Yes. It appears in UPSC Prelims (geography), SSC CGL general awareness, Banking GA, CLAT GK and current-affairs sections, often combined with El Nino and IMD announcements.

Sources: India Meteorological Department (mausam.imd.gov.in), Press Information Bureau (pib.gov.in), NCERT Class 11 Fundamentals of Physical Geography.

Quick revision

  • Mid-September (around 17 September): withdrawal begins from extreme west Rajasthan and parts of Kutch in Gujarat.
  • By end of September: withdrawal covers most of northwest India, including Punjab, Haryana, Delhi and west Uttar Pradesh.
  • First fortnight of October: withdrawal advances into central India and the northern peninsula.
  • Around 15 October: withdrawal from most of the country; the extreme southeastern peninsula (Tamil Nadu coast) now transitions to the northeast monsoon rains of…
  • Continuous absence of rainfall: over the region for five consecutive days.
  • Establishment of an anticyclone in the lower troposphere (around 850 hPa) — roughly 1.5 km above sea level — signalling dry, subsiding air taking over.
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