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Main article: Tropical cyclones in India Vardah making landfall at the coast of Chennai, India. Satellite imagery of Cyclone 05B in the Bay of Bengal.In northwestern India region, virtually cloudless conditions prevail in October and November, resulting in wide diurnal temperature swings; as in much of the Deccan Plateau, they register at 16–20°C (29–36°F). However, from January to February, "western disturbances" bring heavy bursts of rain and snow. These extra-tropical low-pressure systems originate in the eastern Mediterranean Sea. [28] They are carried towards India by the subtropical westerlies, which are the prevailing winds blowing at North India's range of latitude. [23] Once their passage is hindered by the Himalayas, they are unable to proceed further, and they release significant precipitation over the southern Himalayas. Caviedes, C. N. (2001), El Niño in History: Storming Through the Ages (1sted.), University Press of Florida (published 18 September 2001), ISBN 978-0-8130-2099-0 Chouhan, T. S. (1992), Desertification in the World and Its Control, Scientific Publishers, ISBN 978-81-7233-043-9 During the post-monsoon or autumn months of October to December, a different monsoon cycle, the northeast (or "retreating") monsoon, brings dry, cool, and dense air masses to large parts of India. Winds spill across the Himalayas and flow to the southwest across the country, resulting in clear, sunny skies. [47] Though the India Meteorological Department (IMD) and other sources refers to this period as a fourth ("post-monsoon") season, [48] [49] [50] other sources designate only three seasons. [51] Depending on location, this period lasts from October to November, after the southwest monsoon has peaked. Less and less precipitation falls, and vegetation begins to dry out. In most parts of India, this period marks the transition from wet to dry seasonal conditions. Average daily maximum temperatures range between 25 and 34°C (77 and 93°F) in the Southern parts. The main factor behind this shift is the high summer temperature difference between Central Asia and the Indian Ocean. [41] This is accompanied by a seasonal excursion of the normally equatorial intertropical convergence zone (ITCZ), a low-pressure belt of highly unstable weather, northward towards India. [40] This system intensified to its present strength as a result of the Tibetan Plateau's uplift, which accompanied the Eocene– Oligocene transition event, a major episode of global cooling and aridification which occurred 34–49Ma. [42]

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Frigid winds from the Himalayas can depress temperatures near the Brahmaputra River. [33] The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan plateau by preventing frigid and dry Arctic winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from travelling northwards, and causing heavy rainfall in the Terai region instead. The Himalayas are indeed believed to play an important role in the formation of Central Asian deserts such as the Taklamakan and Gobi. The mountain ranges prevent western winter disturbances in Iran from travelling further east, resulting in much snow in Kashmir and rainfall for parts of Punjab and northern India. Despite the Himalayas being a barrier to the cold northerly winter winds, the Brahmaputra valley receives part of the frigid winds, thus lowering the temperature in Northeast India and Bangladesh. The Himalayas contain the greatest area of glaciers and permafrost outside of the poles, and account for the origin of ten of Asia's largest rivers. The two Himalayan states in the east, Sikkim and Arunachal Pradesh, receive substantial snowfall. The extreme north of West Bengal centred on Darjeeling experiences snowfall, but only rarely. Soil and Climate of Bihar, Government of Bihar, archived from the original on 28 September 2011 , retrieved 13 September 2011 Southwest Monsoon: Normal Dates of Onset, India Meteorological Department, archived from the original on 27 September 2011 , retrieved 1 October 2011 A relative later told police that Rodriguez-Singh told her mother that she sold Noel to someone at a 'Fiesta Market' store, according to a copy of the search warrant obtained by the Star-Telegram.Lori Loughlin, 59, and HUGE 90s boy band set to reunite for new tour in 2024 - but fans fume that they won't be performing in Europe East of the Thar Desert, the Punjab-Haryana-Kathiawar region experiences a tropical and sub-tropical steppe climate. Haryana's climate resembles other states of the northern plains: extreme summer heat of up to 50°C and winter cold as low as 1°C. May and June are hottest; December and January are coldest. Rainfall is varied, with the Shivalik Hills region being the wettest and the Aravali Hills region being the driest. About 80% of the rainfall occurs in the monsoon season of July–September, which can cause flooding. The Punjabi climate is also governed by extremes of hot and cold. Areas near the Himalayan foothills receive heavy rainfall whereas those eloigned from them are hot and dry. Punjab's three-season climate sees summer months that span from mid-April to the end of June. Temperatures typically range from–2°C to 40°C, but can reach 47°C (117°F) in summer and −4°C in winter. Most part of the nation doesn't experience temperatures below 10°C (50°F) even in winter. The zone, a transitional climatic region separating tropical desert from humid sub-tropical savanna and forests, experiences temperatures that are less extreme than those of the desert. Average annual rainfall is 300–650 millimetres (11.8–25.6in), but is very unreliable; as in much of the rest of India, the southwest monsoon accounts for most precipitation. Daily summer temperature maxima rise to around 40°C (104°F); this results in natural vegetation typically comprising short, coarse grasses. [ citation needed] Subtropical humid [ edit ]

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There is a huge variation in the climatic conditions of Himachal Pradesh due to variation in altitude (450–6500 metres). The climate varies from hot and subtropical humid (450–900 metres) in the southern low tracts, warm and temperate (900–1800 metres), cool and temperate (1900–2400 metres) and cold glacial and alpine (2400–4800 meters) in the northern and eastern elevated mountain ranges. By October, nights and mornings are very cold. Snowfall at elevations of nearly 3000 m is about 3 m and lasts from December start to March end. Elevations above 4500 m support perpetual snow. The spring season starts from mid February to mid April. The weather is pleasant and comfortable in the season. The rainy season starts at the end of the month of June. The landscape lushes green and fresh. During the season streams and natural springs are replenished. The heavy rains in July and August cause a lot of damage resulting in erosion, floods and landslides. Out of all the state districts, Dharamshala receives the highest rainfall, nearly about 3,400mm (134in). Spiti is the driest area of the state, where annual rainfall is below 50mm. [29] The five Himalayan states (Ladakh, Jammu and Kashmir in the extreme north, Himachal Pradesh, Uttarakhand, Sikkim and Arunachal Pradesh in far east) and Northern West Bengal experience heavy snowfall, Manipur and Nagaland are not located in the Himalayas but experience occasional snowfall; in Ladakh, Himachal Pradesh and Jammu and Kashmir, blizzards occur regularly, disrupting travel and other activities. India Records Double-Digit Growth", BBC News (published 31 March 2004), 2004, archived from the original on 16 December 2008 , retrieved 23 April 2007 Noddy Holder's wife Suzan discusses her husband's 'horrifying' oesophageal cancer diagnosis five years after he was 'given six months to live' All the secret signs Victoria Coren Mitchell, 51, was pregnant: From talking about taking a 'little sabbatical' to carefully planned TV appearancesJessica Alba sizzles in a racy semi-sheer top as she joins a very stylish Nicole Richie at Carlos Eric Lopez's Dia De Muertos celebration Pisharoty, P. R.; Desai, B. N. (1956), "Western Disturbances and Indian Weather", Indian Journal of Meteorological Geophysics, vol.7, pp.333–338 Singh, P.; Kumar, N. (1997), "Effect of Orography on Precipitation in the Western Himalayan Region", Journal of Hydrology, vol.199, no.1, pp.183–206, Bibcode: 1997JHyd..199..183S, doi: 10.1016/S0022-1694(96)03222-2