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English · हिन्दी · తెలుగు · தமிழ் · മലയാളം · मराठी · ಕನ್ನಡ

Quick recap: the climate of India on one page

తెలుగులో వివరణ

Climate of India · Quick recap · Fact-checked on · how we check

Written with AI from the sources listed at the bottom of this page, then fact-checked by a separate AI.

All three parts condensed for quick revision: how the monsoon works; the four seasons, local storms and cyclones; and rainfall, its variability, climatic regions and IMD's forecasts.

Each idea is explained first in Telugu (తెలుగు), ending with the English and Hindi exam terms, followed by the same point in exam English. UPSC Prelims is in English or Hindi, so understand it in Telugu and revise it in English.

మన వాతావరణం ఉష్ణమండల రుతుపవనాల రకం: చలికాలంలో నేల నుంచి సముద్రానికి, వేసవిలో సముద్రం నుంచి నేలకు గాలులు తిరగబడతాయి — అవే వాన ఎప్పుడు, ఎక్కడ అని నిర్ణయిస్తాయి. అక్షాంశం, హిమాలయాలు, సముద్రం నుంచి దూరం, ఎత్తుపల్లాలు దీన్ని మలుస్తాయి. హిమాలయాలు ఇంటి ప్రహరీ గోడలా చలిగాలిని ఆపి, వేసవి తేమ గాలులను లోపలే ఉంచుతాయి. మూడు భాగాలు: యంత్రాంగం, నాలుగు కాలాలు, వాన తీరు–అంచనా. (→ English: monsoon; tropical monsoon climate · हिन्दी: मानसून; उष्णकटिबंधीय मानसूनी जलवायु)

In exam EnglishIndia has a tropical monsoon climate: a seasonal reversal of winds, from land to sea in winter and from sea to land in summer, decides when and where the country gets its rain. Latitude, the Himalaya, distance from the sea and relief shape it. The Himalaya keep out Central Asian cold in winter and hold the moist winds in during summer, which is why South Asia behaves as one climatic unit. The chapter moves in three steps: how the monsoon works (Part 1), the four seasons it creates (Part 2), and the resulting pattern of rainfall, its reliability and its forecasting (Part 3).

పార్ట్ 1: చలికాలంలో వాయవ్యంలో అధిక పీడనం, పొడి గాలులు, హిమాలయాలకు దక్షిణంగా పశ్చిమ జెట్. వేసవిలో వాయవ్యంలో అల్పపీడనం; అంతర ఉష్ణమండల అభిసరణ మండలం ఉత్తరానికి జరిగి గంగా మైదానంపై ద్రోణిగా; ఆగ్నేయ వాణిజ్య పవనాలు భూమధ్యరేఖ దాటి నైరుతి గాలులుగా. పైన జెట్ ప్రవాహం హిమాలయాల ఉత్తరానికి, 15° దగ్గర తూర్పు జెట్, వేడెక్కిన టిబెట్. కేరళకు జూన్ 1, దేశమంతా జూలై 8; ద్రోణి కొండల పాదాలకు జరిగితే విరామం; ఎల్ నినో బలహీనపరుస్తుంది; సెప్టెంబర్ 17 నుంచి అక్టోబర్ 15 దాకా వెనక్కి. (→ English: Inter-Tropical Convergence Zone; jet stream; monsoon onset · हिन्दी: अंतःउष्णकटिबंधीय अभिसरण क्षेत्र; जेट धारा; मानसून का आगमन)

In exam EnglishPart 1, how the monsoon works: in winter, high pressure over north-west India sends dry winds off the land while the westerly jet flows south of the Himalaya. In summer a strong low forms over the north-west, the Inter-Tropical Convergence Zone is pulled north into the monsoon trough over the Ganga plain, and the south-east trades cross the equator and are turned into south-westerlies by the Coriolis force, helped by the Somali jet. Aloft, the westerly jet stream shifts north of the Himalaya, a tropical easterly jet appears near 15°N, and the heated Tibetan plateau strengthens the circulation. The monsoon reaches Kerala about 1 June and covers India by about 8 July (2020 normal dates); breaks come when the trough moves to the foothills; El Niño tends to weaken it and a positive Indian Ocean Dipole to help; withdrawal runs from about 17 September to 15 October.

పార్ట్ 2: చలికాలంలో ఉత్తరాన మంచు, పొగమంచు, చలిగాలులు; పశ్చిమ విక్షోభం గోధుమ వంటి రబీ పంటలకు వాన, మంచు ఇస్తుంది. వేసవిలో వేడి పట్టీ దక్కన్ నుంచి వాయవ్యానికి; వడగాలి, దుమ్ము తుపానులు; ఊరటగా బెంగాల్–అస్సాం–ఒడిశాలో కాలబైశాఖి, కేరళ–కర్ణాటక తీరంలో మామిడి జల్లులు, కాఫీ తోటల్లో పూల జల్లులు. నైరుతి కాలంలో అరేబియా శాఖ కనుమలపై భారీ వాన, దక్కన్ వర్షచ్ఛాయలో; బంగాళాఖాత శాఖ మేఘాలయను తడిపి, కోల్‌కతా నుంచి ఢిల్లీ వైపు బలహీనపడుతుంది. (→ English: western disturbance; kalbaisakhi (nor'wester); orographic rainfall · हिन्दी: पश्चिमी विक्षोभ; काल बैसाखी; पर्वतीय वर्षा)

In exam EnglishPart 2, the seasons: the cold season (December to February) brings frost, fog and cold waves to the north, while each western disturbance, steered from the Mediterranean region by the westerly jet, gives rain and snow valuable for rabi crops. The hot season (March to May) moves the heat belt from the Deccan to the north-west and brings the loo and dust storms; local storms give relief: kalbaisakhi (nor'wester) in West Bengal, Assam and Odisha ('bardoli chheerha' in Assam), mango showers on the Kerala and Karnataka coasts and blossom showers in the coffee areas. In the south-west monsoon season (June to September) the Arabian Sea branch drops orographic rain on the Western Ghats and leaves the Deccan in rain shadow; the Bay of Bengal branch drenches Meghalaya and then weakens westward along the Ganga plain, from Kolkata to Delhi.

జూన్–సెప్టెంబర్‌లో తమిళనాడు తీరం దాదాపు పొడి — కనుమల వెనక, బంగాళాఖాత శాఖకు సమాంతరం. తిరోగమన రుతుపవనాలు కాలంలో అల్పపీడనం బంగాళాఖాతానికి; ఉత్తరాన 'అక్టోబర్ వేడి'; అక్టోబర్–డిసెంబర్ ఈశాన్య వానలే కోరమాండల్ తీరానికి ప్రధాన వాన. ఉష్ణమండల తుపాను ఏప్రిల్–మే లేదా ఎక్కువగా అక్టోబర్–డిసెంబర్‌లో; బంగాళాఖాతంలోనే ఎక్కువ; ఉప్పెనే పెద్ద నష్టం; దిల్లీ IMD కేంద్రం పేర్లు పెడుతుంది. (→ English: retreating monsoon; north-east monsoon; tropical cyclone · हिन्दी: लौटता मानसून; उत्तर-पूर्व मानसून; उष्णकटिबंधीय चक्रवात)

In exam EnglishThe Tamil Nadu coast stays fairly dry from June to September, being on the leeward side of the Ghats and parallel to the Bay branch. In the retreating monsoon season (October and November) the low moves to the Bay of Bengal, north India feels 'October heat', and the north-east monsoon brings the Coromandel coast its main rain from October to December. A tropical cyclone can strike in April–May or, more often, October–December; the Bay of Bengal has far more than the Arabian Sea, storm surge does most of the damage, and IMD's Regional Specialised Meteorological Centre in New Delhi names the cyclones of the north Indian Ocean.
Climate of India at a glance
SeasonMonthsKey features
Cold weatherDecember–FebruaryHigh pressure in the north-west, dry offshore winds; western disturbances bring rain and snow; fog, frost, cold waves
Hot weatherMarch–MayHeat low from the Thar; loo and dust storms; kalbaisakhi, mango and blossom showers
South-west monsoonJune–SeptemberOnset in Kerala about 1 June; Arabian Sea and Bay of Bengal branches; rain shadow in the Deccan; dry Tamil Nadu coast
Retreating monsoonOctober–NovemberOctober heat in the north; north-east monsoon on the Coromandel coast (to December); main cyclone season

పార్ట్ 3: 200 సెం.మీ. పైగా పశ్చిమ తీరం–కనుమలు, మేఘాలయ–ఈశాన్యం, తూర్పు హిమాలయ పాదాల్లో; 50 లోపు పశ్చిమ రాజస్థాన్, కచ్, లద్దాఖ్‌లో. విచలన గుణకం తడి ప్రాంతాల్లో తక్కువ, పొడి ప్రాంతాల్లో 50% పైగా. 25% పైగా లోటు = వాతావరణ కరువు. మైదానాల్లో వడగాలుల హెచ్చరిక 40°C + 4.5°C లేదా 45°C; మేఘ విస్ఫోటనం గంటకు 100 మి.మీ. కొప్పెన్: పశ్చిమ తీరం Amw, కోరమాండల్ As, ద్వీపకల్పం Aw. దీర్ఘకాలిక సగటు సుమారు 87 సెం.మీ.; సాధారణం 96–104%, లోటు 90 లోపు, అధికం 110 పైన; మొదటి అంచనా ఏప్రిల్ మధ్యలో. (→ English: long period average (LPA); coefficient of variation · हिन्दी: दीर्घावधि औसत; विचरण गुणांक)

In exam EnglishPart 3, rainfall and forecasting: over 200 cm falls on the west coast and Western Ghats, in Meghalaya and the north-east and along the eastern sub-Himalaya; under 50 cm in western Rajasthan, Kachchh and Ladakh. The coefficient of variation is lowest where rain is heaviest and above 50 per cent in the driest areas. IMD calls a shortfall of more than 25 per cent a meteorological drought. On the plains a heat wave means at least 40°C and 4.5°C above normal, or 45°C; a cloudburst is about 100 mm or more in an hour over a small area. In Köppen's scheme the west coast is Amw, the Coromandel coast As and most of the Peninsula Aw. IMD (1875) forecasts the season against the long period average (LPA) of about 87 cm (1971–2020): normal is 96–104 per cent, deficient below 90 and excess above 110; the first forecast comes in mid-April.

Exam traps

Recap

Practice questions

Q1. Consider the following statements about the jet streams over India:
1. In winter the subtropical westerly jet flows south of the Himalaya.
2. The tropical easterly jet is present over the Peninsula throughout the winter.
Which of the statements given above is/are correct?

  1. 1 only
  2. 2 only
  3. Both 1 and 2
  4. Neither 1 nor 2
Show answer

Answer: A. 1 only

Statement 1 is correct. Statement 2 is wrong: the tropical easterly jet appears only in the monsoon months. So '2 only' and 'both' are wrong, and 'neither' is wrong because statement 1 is true.

Q2. Under the normal dates revised by IMD in 2020, the south-west monsoon covers the whole of India by about:

  1. 1 June
  2. 15 June
  3. 8 July
  4. 15 July
Show answer

Answer: C. 8 July

The revised normal date is about 8 July. 1 June is the onset over Kerala; 15 June is not a normal date for covering the country; 15 July was the old date before the 2020 revision.

Q3. The winter rainfall of Punjab and Haryana, useful for the wheat crop, is caused mainly by:

  1. The retreating south-west monsoon
  2. Western disturbances
  3. North-east trade winds from the Bay of Bengal
  4. Kalbaisakhi storms
Show answer

Answer: B. Western disturbances

Western disturbances from the Mediterranean region, steered by the westerly jet, bring this winter rain. The retreating monsoon gives rain mainly to the south-east coast; north-east winds over the Bay give winter rain to Tamil Nadu; kalbaisakhi are hot-season storms of eastern India.

Q4. Match List I with List II:
List I (Local storm or shower) — List II (Region)
A. Kalbaisakhi — 1. Coffee areas of Karnataka
B. Mango showers — 2. West Bengal
C. Blossom showers — 3. Kerala coast
Select the correct answer using the code given below:

  1. A-2, B-3, C-1
  2. A-3, B-2, C-1
  3. A-2, B-1, C-3
  4. A-1, B-3, C-2
Show answer

Answer: A. A-2, B-3, C-1

Kalbaisakhi strikes West Bengal (A-2), mango showers fall on the Kerala coast (B-3) and blossom showers make coffee flower in Karnataka (C-1). Option (b) swaps kalbaisakhi and mango showers; (c) swaps the two kinds of shower; (d) puts kalbaisakhi in the coffee areas.

Q5. Which one of the following best explains why the Coromandel coast receives its main rainfall between October and December?

  1. Western disturbances reach the far south in these months
  2. North-easterly winds pick up moisture over the Bay of Bengal, aided by depressions and cyclones
  3. The Arabian Sea branch crosses the Western Ghats at full strength
  4. The ITCZ moves north over the Ganga plain
Show answer

Answer: B. North-easterly winds pick up moisture over the Bay of Bengal, aided by depressions and cyclones

The north-east monsoon winds gather moisture over the Bay and, with depressions and cyclones, bring rain to Tamil Nadu. Western disturbances affect the north-west; the Arabian Sea branch is a June–September feature and leaves this coast in rain shadow; the ITCZ is over the Ganga plain in July, not in October–December.

Q6. Consider the following statements about tropical cyclones affecting India:
1. The main cyclone season is October to December.
2. The Arabian Sea produces more cyclones than the Bay of Bengal.
Which of the statements given above is/are correct?

  1. 1 only
  2. 2 only
  3. Both 1 and 2
  4. Neither 1 nor 2
Show answer

Answer: A. 1 only

Statement 1 is correct. Statement 2 is wrong: the Bay of Bengal produces far more cyclones. So '2 only' and 'both' are wrong, and 'neither' is wrong because statement 1 is true.

Q7. Which one of the following regions has both low annual rainfall and the least reliable rainfall in India?

  1. Western Rajasthan
  2. Meghalaya
  3. Konkan coast
  4. Lower Ganga plain
Show answer

Answer: A. Western Rajasthan

Western Rajasthan gets under 50 cm and has a coefficient of variation above 50 per cent. Meghalaya, the Konkan coast and the lower Ganga plain all receive heavy rain with low variability.

Q8. IMD classifies a south-west monsoon season as 'normal' when all-India rainfall is:

  1. 90 to 110 per cent of the LPA
  2. 96 to 104 per cent of the LPA
  3. 100 per cent of the LPA exactly
  4. Above 110 per cent of the LPA
Show answer

Answer: B. 96 to 104 per cent of the LPA

Normal is 96–104 per cent of the LPA. 90–110 per cent mixes in the below-normal and above-normal bands; an exact 100 per cent is too narrow to be a category; above 110 per cent is 'excess'.

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