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Quick recap: the climate of India on one page
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.
ನಮ್ಮ ವಾಯುಗುಣ ಉಷ್ಣವಲಯದ ಮಾನ್ಸೂನ್ ಪ್ರಕಾರದ್ದು: ಚಳಿಗಾಲದಲ್ಲಿ ನೆಲದಿಂದ ಸಮುದ್ರಕ್ಕೆ, ಬೇಸಿಗೆಯಲ್ಲಿ ಸಮುದ್ರದಿಂದ ನೆಲಕ್ಕೆ ಗಾಳಿ ದಿಕ್ಕು ಬದಲಿಸುತ್ತದೆ — ಅದೇ ಮಳೆ ಯಾವಾಗ, ಎಲ್ಲಿ ಎಂದು ನಿರ್ಧರಿಸುತ್ತದೆ. ಅಕ್ಷಾಂಶ, ಹಿಮಾಲಯ, ಸಮುದ್ರದಿಂದ ದೂರ, ಭೂಸ್ವರೂಪ ಇದನ್ನು ರೂಪಿಸುತ್ತವೆ. ಹಿಮಾಲಯ ಮನೆಯ ಕಾಂಪೌಂಡ್ ಗೋಡೆಯಂತೆ ತಣ್ಣನೆಯ ಗಾಳಿ ತಡೆದು, ಬೇಸಿಗೆಯ ತೇವದ ಗಾಳಿಯನ್ನು ಒಳಗೇ ಇಡುತ್ತದೆ. ಮೂರು ಭಾಗಗಳು: ಯಂತ್ರ, ನಾಲ್ಕು ಋತುಗಳು, ಮಳೆಯ ಮಾದರಿ–ಮುನ್ಸೂಚನೆ. (→ English: monsoon; tropical monsoon climate · हिन्दी: मानसून; उष्णकटिबंधीय मानसूनी जलवायु)
ಭಾಗ 1: ಚಳಿಗಾಲದಲ್ಲಿ ವಾಯವ್ಯದಲ್ಲಿ ಅಧಿಕ ಒತ್ತಡ, ಒಣ ಗಾಳಿ, ಹಿಮಾಲಯದ ದಕ್ಷಿಣಕ್ಕೆ ಪಶ್ಚಿಮ ಜೆಟ್. ಬೇಸಿಗೆಯಲ್ಲಿ ವಾಯವ್ಯದಲ್ಲಿ ಕಡಿಮೆ ಒತ್ತಡ; ಅಂತರ ಉಷ್ಣವಲಯ ಸಂಗಮ ವಲಯ ಉತ್ತರಕ್ಕೆ ಸರಿದು ಗಂಗಾ ಬಯಲಿನಲ್ಲಿ ತಗ್ಗಾಗಿ; ಆಗ್ನೇಯ ವಾಣಿಜ್ಯ ಮಾರುತಗಳು ಸಮಭಾಜಕ ದಾಟಿ ನೈಋತ್ಯ ಗಾಳಿಯಾಗಿ. ಮೇಲೆ ಜೆಟ್ ಪ್ರವಾಹ ಹಿಮಾಲಯದ ಉತ್ತರಕ್ಕೆ, 15° ಬಳಿ ಪೂರ್ವ ಜೆಟ್, ಕಾದ ಟಿಬೆಟ್. ಕೇರಳಕ್ಕೆ ಜೂನ್ 1, ಇಡೀ ದೇಶಕ್ಕೆ ಜುಲೈ 8; ತಗ್ಗು ತಪ್ಪಲಿಗೆ ಸರಿದರೆ ಬಿಡುವು; ಎಲ್ ನಿನೊ ದುರ್ಬಲಗೊಳಿಸುತ್ತದೆ; ಸೆಪ್ಟೆಂಬರ್ 17ರಿಂದ ಅಕ್ಟೋಬರ್ 15ರವರೆಗೆ ಹಿಂದಿರುಗುವಿಕೆ. (→ English: Inter-Tropical Convergence Zone; jet stream; monsoon onset · हिन्दी: अंतःउष्णकटिबंधीय अभिसरण क्षेत्र; जेट धारा; मानसून का आगमन)
ಭಾಗ 2: ಚಳಿಗಾಲದಲ್ಲಿ ಉತ್ತರದಲ್ಲಿ ಹಿಮ, ಮಂಜು, ಶೀತ ಅಲೆ; ಪಶ್ಚಿಮ ಪ್ರಕ್ಷುಬ್ಧತೆ ಗೋಧಿಯಂತಹ ರಬಿ ಬೆಳೆಗಳಿಗೆ ಮಳೆ, ಹಿಮ ಕೊಡುತ್ತದೆ. ಬೇಸಿಗೆಯಲ್ಲಿ ಬಿಸಿಯ ಪಟ್ಟಿ ಡೆಕ್ಕನ್ನಿಂದ ವಾಯವ್ಯಕ್ಕೆ; ಬಿಸಿಗಾಳಿ, ಧೂಳಿನ ಬಿರುಗಾಳಿ; ಸಮಾಧಾನವಾಗಿ ಬಂಗಾಳ–ಅಸ್ಸಾಂ–ಒಡಿಶಾದಲ್ಲಿ ಕಾಲಬೈಶಾಖಿ, ಕೇರಳ–ಕರ್ನಾಟಕ ಕರಾವಳಿಯಲ್ಲಿ ಮಾವಿನ ಮಳೆ, ಕಾಫಿ ತೋಟಗಳಲ್ಲಿ ಹೂಮಳೆ. ನೈಋತ್ಯ ಋತುವಿನಲ್ಲಿ ಅರಬ್ಬಿ ಶಾಖೆ ಘಟ್ಟಗಳ ಮೇಲೆ ಪರ್ವತ ಮಳೆ, ಡೆಕ್ಕನ್ ಮಳೆನೆರಳಿನಲ್ಲಿ; ಕೊಲ್ಲಿ ಶಾಖೆ ಮೇಘಾಲಯವನ್ನು ತೋಯಿಸಿ ಕೋಲ್ಕತ್ತಾದಿಂದ ದೆಹಲಿಯತ್ತ ದುರ್ಬಲವಾಗುತ್ತದೆ. (→ English: western disturbance; kalbaisakhi (nor'wester); orographic rainfall · हिन्दी: पश्चिमी विक्षोभ; काल बैसाखी; पर्वतीय वर्षा)
ಜೂನ್–ಸೆಪ್ಟೆಂಬರ್ನಲ್ಲಿ ತಮಿಳುನಾಡು ಕರಾವಳಿ ಸುಮಾರು ಒಣ — ಘಟ್ಟಗಳ ಹಿಂದೆ, ಕೊಲ್ಲಿ ಶಾಖೆಗೆ ಸಮಾನಾಂತರ. ಹಿಂದಿರುಗುವ ಮಾನ್ಸೂನ್ ಕಾಲದಲ್ಲಿ ಕಡಿಮೆ ಒತ್ತಡ ಕೊಲ್ಲಿಗೆ; ಉತ್ತರದಲ್ಲಿ 'ಅಕ್ಟೋಬರ್ ಬಿಸಿ'; ಅಕ್ಟೋಬರ್–ಡಿಸೆಂಬರ್ ಈಶಾನ್ಯ ಮಳೆಯೇ ಕೋರಮಂಡಲ ಕರಾವಳಿಯ ಮುಖ್ಯ ಮಳೆ. ಉಷ್ಣವಲಯದ ಚಂಡಮಾರುತ ಏಪ್ರಿಲ್–ಮೇ ಅಥವಾ ಹೆಚ್ಚಾಗಿ ಅಕ್ಟೋಬರ್–ಡಿಸೆಂಬರ್ನಲ್ಲಿ; ಕೊಲ್ಲಿಯಲ್ಲೇ ಹೆಚ್ಚು; ಅಲೆಯೇರಿಕೆಯೇ ದೊಡ್ಡ ಹಾನಿ; ದೆಹಲಿಯ IMD ಕೇಂದ್ರ ಹೆಸರಿಡುತ್ತದೆ. (→ English: retreating monsoon; north-east monsoon; tropical cyclone · हिन्दी: लौटता मानसून; उत्तर-पूर्व मानसून; उष्णकटिबंधीय चक्रवात)
| Season | Months | Key features |
|---|---|---|
| Cold weather | December–February | High pressure in the north-west, dry offshore winds; western disturbances bring rain and snow; fog, frost, cold waves |
| Hot weather | March–May | Heat low from the Thar; loo and dust storms; kalbaisakhi, mango and blossom showers |
| South-west monsoon | June–September | Onset in Kerala about 1 June; Arabian Sea and Bay of Bengal branches; rain shadow in the Deccan; dry Tamil Nadu coast |
| Retreating monsoon | October–November | October heat in the north; north-east monsoon on the Coromandel coast (to December); main cyclone season |
ಭಾಗ 3: 200 ಸೆಂ.ಮೀ.ಗಿಂತ ಹೆಚ್ಚು ಪಶ್ಚಿಮ ಕರಾವಳಿ–ಘಟ್ಟ, ಮೇಘಾಲಯ–ಈಶಾನ್ಯ, ಪೂರ್ವ ಹಿಮಾಲಯದ ತಪ್ಪಲು; 50ಕ್ಕಿಂತ ಕಡಿಮೆ ಪಶ್ಚಿಮ ರಾಜಸ್ಥಾನ, ಕಚ್, ಲಡಾಖ್. ವ್ಯತ್ಯಯ ಗುಣಾಂಕ ತೇವದ ಕಡೆ ಕಡಿಮೆ, ಒಣ ಕಡೆ 50%ಕ್ಕಿಂತ ಹೆಚ್ಚು. 25%ಕ್ಕೂ ಹೆಚ್ಚು ಕೊರತೆ = ಹವಾಮಾನ ಬರ. ಬಯಲಿನಲ್ಲಿ ಬಿಸಿ ಅಲೆ 40°C + 4.5°C ಅಥವಾ 45°C; ಮೇಘಸ್ಫೋಟ ಗಂಟೆಗೆ 100 ಮಿ.ಮೀ. ಕೊಪೆನ್: ಪಶ್ಚಿಮ ಕರಾವಳಿ Amw, ಕೋರಮಂಡಲ As, ಪರ್ಯಾಯದ್ವೀಪ Aw. ದೀರ್ಘಾವಧಿ ಸರಾಸರಿ ಸುಮಾರು 87 ಸೆಂ.ಮೀ.; ಸಾಮಾನ್ಯ 96–104%, ಕೊರತೆ 90ಕ್ಕಿಂತ ಕೆಳಗೆ, ಹೆಚ್ಚುವರಿ 110ಕ್ಕಿಂತ ಮೇಲೆ; ಮೊದಲ ಮುನ್ಸೂಚನೆ ಏಪ್ರಿಲ್ ಮಧ್ಯದಲ್ಲಿ. (→ English: long period average (LPA); coefficient of variation · हिन्दी: दीर्घावधि औसत; विचरण गुणांक)
Exam traps
- In winter the westerly jet is SOUTH of the Himalaya and brings western disturbances; in summer it moves NORTH. The tropical easterly jet appears only in the monsoon months.
- Revised normal dates (2020): onset over Kerala about 1 June; all India covered by about 8 July (not 15 July); withdrawal starts about 17 September and ends about 15 October.
- Winter rain in Punjab and Haryana comes from western disturbances; winter rain on the Tamil Nadu coast comes from north-east winds over the Bay of Bengal.
- Kalbaisakhi belongs to West Bengal, Assam and Odisha; mango showers to the Kerala and Karnataka coasts; the loo to the north-western plains.
- The Tamil Nadu coast is dry in the south-west monsoon; its main rain comes from the north-east monsoon, October to December.
- The Bay of Bengal has many more cyclones than the Arabian Sea; the main season is October to December, not July–August.
- The coefficient of variation is HIGHEST where rainfall is LOWEST. 'Normal' monsoon = 96–104% of the LPA (about 87 cm, 1971–2020).
Recap
- Tropical monsoon climate: seasonal reversal of winds; the Himalaya block cold air and trap the monsoon.
- Summer: low over the north-west, ITCZ pulled north into the monsoon trough, cross-equatorial south-westerlies, Somali jet, easterly jet, heated Tibet.
- Kerala onset about 1 June, all India about 8 July; breaks when the trough reaches the foothills; El Niño tends to weaken, positive IOD to help.
- Cold season: western disturbances; hot season: loo, dust storms, kalbaisakhi, mango and blossom showers.
- Arabian Sea branch: Western Ghats rain and Deccan rain shadow; Bay branch: Meghalaya, then rain falls off from Kolkata to Delhi.
- Retreating monsoon: October heat; north-east monsoon on the Coromandel coast; cyclones mainly October–December, mostly in the Bay.
- Over 200 cm on the west coast, Meghalaya and the north-east; under 50 cm in western Rajasthan, Kachchh and Ladakh; variability highest in dry areas.
- IMD (1875): LPA about 87 cm; normal 96–104%; first forecast mid-April; Köppen: Amw west coast, As Coromandel, Aw most of the Peninsula.
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 only
- 2 only
- Both 1 and 2
- 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 June
- 15 June
- 8 July
- 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:
- The retreating south-west monsoon
- Western disturbances
- North-east trade winds from the Bay of Bengal
- 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:
- A-2, B-3, C-1
- A-3, B-2, C-1
- A-2, B-1, C-3
- 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?
- Western disturbances reach the far south in these months
- North-easterly winds pick up moisture over the Bay of Bengal, aided by depressions and cyclones
- The Arabian Sea branch crosses the Western Ghats at full strength
- 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 only
- 2 only
- Both 1 and 2
- 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?
- Western Rajasthan
- Meghalaya
- Konkan coast
- 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:
- 90 to 110 per cent of the LPA
- 96 to 104 per cent of the LPA
- 100 per cent of the LPA exactly
- 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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- India Meteorological Department, Ministry of Earth Sciences: monsoon reports, revised normal dates of onset and withdrawal (2020), the seasons of India, cyclone reports of the Regional Specialised Meteorological Centre, New Delhi, rainfall statistics, long-range forecasts and the long period average (1971–2020) — https://mausam.imd.gov.in
- Indian Institute of Tropical Meteorology, Pune: monsoon dynamics, jet streams, ENSO, the Indian Ocean Dipole and monsoon variability — https://www.tropmet.res.in
- National Disaster Management Authority: guidelines on cyclones, droughts, floods and heat waves — https://ndma.gov.in
- Ministry of Earth Sciences: the National Monsoon Mission and monsoon forecasting — https://moes.gov.in