A semi-arid wasteland near Tirunelveli, Tamil Nadu. In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering Tirunelveli (திருநெல்வேலி is a city in Tamil Nadu and was formed into a Municipal corporation in 1999 by merging three municipalities viz Tamil Nadu ( Tamil:, Country of the Tamils, t̪ɐmɨɻ n̪aːɽɯ is one of the 28 states of India. Monsoon clouds dump torrents of rain on lush forests that are only kilometres away in windward-facing Kerala, but are prevented from reaching Tirunelveli by the Agasthyamalai Range of the Western Ghats (background). Windward is the direction from which the wind is blowing at the time in question Kerala ( Malayalam: {{Kerala in Malayalam}}; For the Australian television series see Rain Shadow (TV series. Agastya Mala (also known as Agastyarkoodam or Agasthyakoodam) is a peak within Neyyar Wildlife Sanctuary in the Western Ghats of South

A scene in Uttarakhand's Valley of Flowers National Park. Uttarakhand ( Hindi: उत्तराखण्ड or उत्तराखंड Uttar + Akhand i Valley of Flowers National Park is an Indian national park, Nestled high in West Himalaya is renowned for its meadows of endemic alpine flowers and outstanding In contrast to Tirunelveli, the park receives ample orographic precipitation due to its location in a mountainous windward-facing region wedged between the Zanskars and the Greater Himalayas. Orographic lift occurs when an Air mass is forced from a low Elevation to a higher elevation as it moves over rising terrain Windward is the direction from which the wind is blowing at the time in question The Zanskar Range is a Mountain range in Indian state of Jammu and Kashmir that separates Zanskar from Ladakh. The Great Himalayas lie north of the Lower Himalayan Range. These mountains are bounded by the Indus River in the north and the west as the river takes a southward

The formation of the Himalayas (pictured) during the Early Eocene some 53 million years ago was a key factor in determining India's modern-day climate; global climate and ocean chemistry may have been impacted. The Ypresian is the first stage of the Eocene Epoch and usually corresponds to the Early Eocene subepoch though sometimes the Lutetian ^[1]

The climate of India comprises a wide range of weather conditions across a large geographic scale and varied topography, making generalisations difficult. Analysed according to the Köppen system, India hosts six major climatic subtypes, ranging from desert in the west, to alpine tundra and glaciers in the north, to humid tropical regions supporting rainforests in the southwest and the island territories. The Köppen climate classification is one of the most widely used climate classification systems It was developed by Wladimir Köppen, a German climatologist India, officially the Republic of India (भारत गणराज्य inc-Latn Bhārat Gaṇarājya; see also other Indian languages) is a country A desert is a Landscape or region that receives very little precipitation. In physical Geography, tundra is an area where the Tree growth is hindered by low temperatures and short growing seasons "Glacial" and "Glaciation" redirect here For the geological periods see Glacial period. Rainforests are Forests characterized by high Rainfall with definitions setting minimum normal annual rainfall between 1750–2000 mm (68-78 inches Many regions have starkly different microclimates. A microclimate is a local atmospheric zone where the Climate differs from the surrounding area The nation has four seasons: winter (January and February), summer (March to May), a monsoon (rainy) season (June to September), and a post-monsoon period (October to December). A monsoon is a seasonal prevailing wind which lasts for several months

India's unique geography and geology strongly influence its climate; this is particularly true of the Himalayas in the north and the Thar Desert in the northwest. The geography of India is diverse with landscape ranging from snow-capped mountain ranges to deserts plains rainforests hills and plateaus The geological history of India started with the geological evolution of rest of the Earth i The Thar Desert ( Hindi: थार मरुस्थल also known as the Great Indian Desert, is The Himalayas act as a barrier to the frigid katabatic winds flowing down from Central Asia. A katabatic wind, from the Greek word katabatikos meaning "going downhill" is the technical name for a drainage Wind, a wind Central Asia is a region of Asia from the Caspian Sea in the west to central China in the east and from southern Russia in the north to northern Pakistan in the south Thus, North India is kept warm or only mildly cold during winter; in summer, the same phenomenon makes India relatively hot. Geography Northern India lies mainly on continental India and a very small part of it lies on the Indian peninsula Although the Tropic of Cancer—the boundary between the tropics and subtropics—passes through the middle of India, the whole country is considered to be tropical. For the novel by Henry Miller, see Tropic of Cancer (novel. The Tropic of Cancer, or Northern tropic, is one of five

As in much of the tropics, monsoonal and other weather conditions in India are unstable: major droughts, floods, cyclones and other natural disasters are sporadic, but have killed or displaced millions. India's long-term climatic stability is further threatened by global warming. Global warming is the increase in the average measured temperature of the Climatic diversity in India makes the analysis of these issues complex.

History

During the Late Permian (some 260–251 million years ago), the Indian subcontinent was part of the vast supercontinent Pangaea. In Astronomy, Geology, and Paleontology, mya or " mya " is an abbreviation for "million years ago". This article deals with the geophysical region in Asia For geopolitical treatments see South Asia. In Geology, a supercontinent is a Landmass comprising more than one Continental core or Craton. Pangaea, Pangæa or Pangea (pænˈdʒiːə from παν pan, meaning entire, and Γαῖα Gaea, meaning Earth in Despite its position within a high-latitude belt at 55–75° S (as opposed to its current position between 5 and 35° N), latitudes now occupied by such places as Greenland and parts of the Antarctic Peninsula, India likely experienced a humid temperate climate with warm, frost-free weather, though with well-defined seasons. Greenland (Kalaallit Nunaat meaning "Land of the Greenlanders" Grønland is a self-governing Danish Province located between the The Antarctic Peninsula is the northernmost part of the mainland of Antarctica, and almost the only part of that continent that extends outside the Antarctic Circle ^[2] Later, India joined the southern supercontinent Gondwana, a process beginning some 550–500 mya. Gondwana (ɡɒnˈdwɑːnə originally Gondwanaland) was a southern Supercontinent that existed about 500 to 200 Ma ago During the Late Paleozoic, Gondwana extended from a point at or near the South Pole to near the equator, where the Indian craton (stable continental crust) was positioned, resulting in a mild climate favourable to hosting high-biomass ecosystems. The Paleozoic or Palaeozoic Era (from the Greek palaio (παλαιο "old" and zoe (ζωη "life" meaning "ancient life" The South Pole, also known as the Geographic South Pole or Terrestrial South Pole, is the southernmost point on the surface of the Earth. The geological history of India started with the geological evolution of rest of the Earth i The continental crust is the layer of granitic, Sedimentary, and Metamorphic rocks which form the Continents and the areas of shallow seabed Biomass refers to living and recently dead Biological material that can be used as fuel or for industrial production An ecosystem is a natural unit consisting of all plants animals and micro-organisms( Biotic factors in an area functioning together with all of the non-living physical ( This is underscored by India's vast coal reserves—much of it from the late Paleozoic sedimentary sequence—the fourth-largest reserves in the world. ^[3] During the Mesozoic, the world, including India, was considerably warmer than today. The Mesozoic Era is one of three geologic eras of the Phanerozoic eon. With the coming of the Carboniferous, global cooling stoked extensive glaciation, which spread northwards from South Africa towards India; this cool period lasted well into the Permian. The Carboniferous is a geologic period and system that extends from the end of the Devonian period about 359 Global cooling in general can refer to an overall cooling of the Earth. "Glacial" and "Glaciation" redirect here For the geological periods see Glacial period. The Republic of South Africa (also known by other official names) is a country located at the southern tip of the continent of Africa The Permian is a geologic period and system that extends from 299 ^[4]

Tectonic movement by the Indian Plate caused it to pass over a geologic hotspot—the Réunion hotspot—now occupied by the volcanic island of Réunion. Plate tectonics (from Greek τέκτων tektōn "builder" or "mason" describes the large scale motions of Earth 's Lithosphere The India or Indian Plate is a Tectonic plate that was originally a part of the ancient continent of Gondwanaland from which it split off eventually In Geology, a hotspot is a location on the Earth's surface that has experienced active volcanism for a long period of time The Réunion hotspot is a Volcanic hotspot which currently lies under the Island of Réunion in the Indian Ocean. Réunion ( French: Réunion or formally La Réunion; previously Île Bourbon) is an island located in the Indian Ocean, east of This resulted in a massive flood basalt event that laid down the Deccan Traps some 60–68 mya,^[5][6] at the end of the Cretaceous period. A flood basalt or trap basalt is the result of a giant Volcanic eruption or series of Eruptions that coats large stretches of land or the Ocean floor The Deccan Traps are a Large igneous province located on the Deccan Plateau of west-central India (between 17-24N 73-74E and one of the largest Volcanic The Cretaceous (kriːˈteɪʃəs, usually abbreviated 'K' for its German translation "Kreide" is a geologic period and system, reaching from the end of This may have contributed to the global Cretaceous-Tertiary (K-T) extinction event, which caused India to experience significantly reduced insolation. The Cretaceous–Tertiary extinction event, which occurred approximately ( Ma) was a large-scale mass extinction of animal and plant species in a geologically Insolation is a measure of Solar radiation energy received on a given surface area in a given time Elevated atmospheric levels of sulphur gases formed aerosols such as sulfur dioxide and sulfuric acid, similar to those found in the atmosphere of Venus; these precipitated as acid rain. Technically an aerosol is a suspension of fine solid particles or liquid droplets in a gas Sulfuric (or sulphuric acid, H 2 S[[oxygen O]]4 is a strong Mineral acid. Structure and composition Composition The atmosphere of Venus is composed mainly of Carbon dioxide, along with a small amount of Nitrogen and other Acid rain is Rain or any other form of precipitation that is unusually Acidic It has harmful effects on plants aquatic animals and infastructure Elevated carbon dioxide emissions also contributed to the greenhouse effect, causing warmer weather that lasted long after the atmospheric shroud of dust and aerosols had cleared. Carbon dioxide ( Chemical formula:) is a Chemical compound composed of two Oxygen Atoms covalently bonded to a single The Greenhouse effect refers to the change in the Thermal equilibrium temperature of a planet or moon by the presence of an Atmosphere containing gas that absorbs Climate change is any long-term significant change in the “average weather” that a given region experiences Further climatic changes 20 million years ago, long after India had crashed into the Laurasian landmass, were severe enough to cause the extinction of many endemic Indian forms. Laurasia (lɔˈreɪʃiə lɔˈreɪʒə was a Supercontinent that most recently existed as a part of the split of the Pangaean supercontinent in the late Mesozoic ^[7] Meanwhile, the formation of the Himalayas resulted in blockage of frigid Central Asian air, preventing it from reaching India; this made its climate significantly warmer and more tropical in character than it would otherwise have been.

Regions

Main article: Climatic regions of India

Average annual temperatures across India:      Below 20. Tropical rainy climatic group The regions belonging to this group experience persistent high temperatures which normally do not go below 18°C even in the coolest month 0 °C (< 68. 0 °F)      20. 0–22. 5 °C (68. 0–72. 5 °F)      22. 5–25. 0 °C (72. 5–77. 0 °F)      25. 0–27. 5 °C (77. 0–81. 5 °F)      Above 27. 5 °C (> 81. 5 °F)

Climatic zones in India, based on the Köppen classification system:      Alpine E (ETh)      Humid subtropical C (Cfa)      Tropical wet and dry A (Aw)      Tropical wet A (Am)      Semi-arid B (BSh)      Arid B (BWh)

India is home to an extraordinary variety of climatic regions, ranging from tropical in the south to temperate and alpine in the Himalayan north, where elevated regions receive sustained winter snowfall. The Köppen climate classification is one of the most widely used climate classification systems It was developed by Wladimir Köppen, a German climatologist For the climate of the mountains named the Alps, see Climate of the Alps. Humid subtropical climate ( Köppen Cfa or Cwa) is a climate zone characterized by hot humid summers and chilly to mild winters A tropical climate is a kind of Climate typical in the Tropics. A tropical climate is a kind of Climate typical in the Tropics. A Semi-arid climate or steppe climate generally describes climatic regions that receive low annual Rainfall (250-500 mm or 10-20 in In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering The nation's climate is strongly influenced by the Himalayas and the Thar Desert. ^[8] The Himalayas, along with the Hindu Kush mountains in Pakistan, prevent cold Central Asian katabatic winds from blowing in, keeping the bulk of the Indian subcontinent warmer than most locations at similar latitudes. The Hindu Kush is a Mountain range located between Afghanistan and Pakistan. Pakistan () officially the Islamic Republic of Pakistan, is a country located in South Asia, Southwest Asia, Middle East and Latitude, usually denoted symbolically by the Greek letter phi ( Φ) gives the location of a place on Earth (or other planetary body north or south of the ^[9] Simultaneously, the Thar Desert plays a role in attracting moisture-laden southwest summer monsoon winds that, between June and October, provide the majority of India's rainfall. ^[8][10] Four major climatic groupings predominate, into which fall seven climatic zones that, as designated by experts, are defined on the basis of such traits as temperature and precipitation. ^[11] Groupings are assigned codes (see chart) according to the Köppen climate classification system.

Tropical wet

A tropical rainy climate covers regions experiencing persistent warm or high temperatures, which normally do not fall below 18 °C (64 °F). The Celsius Temperature scale was previously known as the centigrade scale. Fahrenheit is a temperature scale named after Daniel Gabriel Fahrenheit (1686–1736 a German Physicist who proposed it in 1724 India hosts two climatic subtypes that fall under this group. The most humid is the tropical wet monsoon climate that covers a strip of southwestern lowlands abutting the Malabar Coast, the Western Ghats, and southern Assam. The Malabar Coast also known as the Malabarian Coast, is a long and narrow south-western shore line of the mainland Indian subcontinent. The Western Ghats ( Kannada ಸಹ್ಯಾದ್ರಿ Marathi / Konkani - सह्याद्री Sahyadri Malayalam സഹ്യപര്‍വ്വതം Assam) ( Assamese: অসম Ôxôm) is a northeastern state of India with its capital at Dispur, a suburb of the city India's two island territories, Lakshadweep and the Andaman and Nicobar Islands, are also subject to this climate. Lakshadweep ( (ലക്ഷദ്വീപ്,) the smallest Union territory of India, is a group of islands 200 to 300 km off of the coast of The Andaman & Nicobar Islands is a Union territory of India. Informally the territory's name is often abbreviated to A & N Islands, or ANI Characterised by moderate to high year-round temperatures, even in the foothills, its rainfall is seasonal but heavy—typically above 2,000 millimetres (79 in) per year. ^[12] Most rainfall occurs between May and November; this is adequate for the maintenance of lush forests and other vegetation throughout the remainder of the year. December to March are the driest months, when days with precipitation are rare. The heavy monsoon rains are responsible for the extremely biodiverse tropical wet forests of these regions.

In India, a tropical wet and dry climate is more common. Significantly drier than tropical wet zones, it prevails over most of inland peninsular India except for a semi-arid rain shadow east of the Western Ghats. In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering Winter and early summer are long, dry periods with temperatures averaging above 18 °C (64 °F). Summer is exceptionally hot; temperatures in low-lying areas may exceed 50 °C (122 °F) during May, leading to heat waves that can each kill hundreds of Indians. ^[13] The rainy season lasts from June to September; annual rainfall averages between 750–1500 millimetres (30–59 in) across the region. Once the dry northeast monsoon begins in September, most precipitation in India falls on Tamil Nadu, leaving other states comparatively dry. ^[14]

Tropical dry

A tropical arid and semi-arid climate dominates regions where the rate of moisture loss through evapotranspiration exceeds that from precipitation; it is subdivided into three climatic subtypes. In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering Evapotranspiration (ET is a term used to describe the sum of Evaporation and Plant Transpiration from the earth's land surface to Atmosphere The first, a tropical semi-arid steppe climate, predominates over a long stretch of land south of Tropic of Cancer and east of the Western Ghats and the Cardamom Hills. In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering The Cardamom Hills are part of the southern Western Ghats located in southeast Kerala and Southwest Tamil Nadu in South India. The region, which includes Karnataka, inland Tamil Nadu, western Andhra Pradesh, and central Maharashtra, gets between 400–750 millimetres (16–30 in) annually. Karnataka (ಕರ್ನಾಟಕ pronounced) is a state in the southern part of India Maharashtra ( Marathi: mahārāṣṭra, IPA) is a state located on the western coast of India. It is drought-prone, as it tends to have less reliable rainfall due to sporadic lateness or failure of the southwest monsoon. ^[15] North of the Krishna River, the summer monsoon is responsible for most rainfall; to the south, significant post-monsoon rainfall also occurs in October and November. This article is about an Indian river For other meanings of this river names see Krishna (disambiguation and Krishnaveni. In December, the coldest month, temperatures still average around 20–24 °C (68–75 °F). The months between March to May are hot and dry; mean monthly temperatures hover around 32 °C, with 320 millimetres (13 in) precipitation. Hence, without artificial irrigation, this region is not suitable for permanent agriculture.

The Rann of Kutch, a vast salt marsh south of the Thar Desert in Gujarat. The Rann of Kutch is a seasonally marshy region located in the Thar Desert biogeographic province in Gujarat state of northwestern India A salt marsh is a type of Marsh that is a transitional intertidal between land and salty or Brackish water (e Gujarat (ગુજરાત Gujǎrāt, pronounced) is a state in western India. During the monsoon season, the region fills with standing waters.

Most of western Rajasthan experiences an arid climatic regime. Rājasthān ( Devanāgarī: राजस्थान raːdʒəst̪ʰaːn is the largest state of the Republic of India in terms of area In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering Cloudbursts are responsible for virtually all of the region's annual precipitation, which totals less than 300 millimetres (12 in). A cloudburst is an extreme form of Rainfall sometimes mixed with Hail and Thunder, which normally lasts no longer than a few minutes but is capable of creating Such bursts happen when monsoon winds sweep into the region during July, August, and September. Such rainfall is highly erratic; regions experiencing rainfall one year may not see precipitation for the next couple of years or so. Atmospheric moisture is largely prevented from precipitating due to continuous downdrafts and other factors. An updraft or downdraft ( air pocket) is the vertical movement of Air as a Weather related phenomenon ^[16] The summer months of May and June are exceptionally hot; mean monthly temperatures in the region hover around 35 °C (95 °F), with daily maxima occasionally topping 50 °C (122 °F). During winters, temperatures in some areas can drop below freezing due to waves of cold air from Central Asia. There is a large diurnal range of about 14 °C (57 °F) during summer; this widens by several degrees during winter.

East of the Thar Desert, the region running from Punjab and Haryana to Kathiawar experiences a tropical and sub-tropical steppe climate. Punjab (ਪੰਜਾਬ पंजाब pəɲdʒaːb is a state in northwest India. Haryana (हरियाणा Punjabi: ਹਰਿਆਣਾ hərɪjaːɳaː is a state in northern India. Kathiawar or Kathiawad ( Gujarati: કાઠીયાવાડ; kaʈʰijaʋaɽ is a Peninsula in western India. In physical Geography, a steppe ( German, from степь - "a flat and arid land" степ - /stɛp/ тал - tal дала - /dɑlɑ/ pronounced 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 30–65 centimetres (12-26 in), 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). The resulting natural vegetation typically comprises short, coarse grasses.

Subtropical humid

Most of Northeast India and much of North India are subject to a humid sub-tropical climate. Though they experience hot summers, temperatures during the coldest months may fall as low as 0 °C (32 °F). Due to ample monsoon rains, India has only one subtype of this climate, Cfa (under the Köppen system). ^[17] In most of this region, there is very little precipitation during the winter, owing to powerful anticyclonic and katabatic (downward-flowing) winds from Central Asia. Due to the region's proximity to the Himalayas, it experiences elevated prevailing wind speeds, again from the influence of Central Asian katabatic movements.

Humid subtropical regions are subject to pronounced dry winters. Winter rainfall—and occasionally snowfall—is associated with large storm systems such as "Nor'westers" and "Western disturbances"; the latter are steered by westerlies towards the Himalayas. Western Disturbance is the term used in India, Pakistan, Afghanistan and Nepal to describe an Extratropical storm that brings sudden The Westerlies or the Prevailing Westerlies are the prevailing winds in the Middle latitudes between 30 and 60 degrees Latitude, blowing from ^[18] Most summer rainfall occurs during powerful thunderstorms associated with the southwest summer monsoon; occasional tropical cyclones also contribute. A tropical cyclone is a storm system characterized by a low pressure center and numerous Thunderstorms that produce strong winds and Flooding Annual rainfall ranges from less than 1,000 millimetres (39 in) in the west to over 2,500 millimetres (98 in) in parts of the northeast. As most of this region is far from the ocean, the wide temperature swings more characteristic of a continental climate predominate; the swings are wider than in those in tropical wet regions, ranging from 24 °C (75 °F) in north-central India to 27 °C (81 °F) in the east. Continental climate is a Climate that is characterized by Winter Temperatures cold enough to support a fixed period of Snow cover each Year

Montane

Pangong Lake in Ladakh, an arid montane region lying deep within the Himalayas. Pangong Tso (or Pangong Lake; Tso: Ladakhi for lake is a Lake in the Himalayas situated at a height of about 4250 m (13900 ft Ladakh ( Ladakhi lad̪ɑks लदाख لدّاخ "land of high passes" is a region in the Indian state of Jammu and Kashmir between In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering

India's northernmost fringes are subject to a montane, or alpine, climate. In the Himalayas, the rate at which an air mass's temperature falls per kilometre (3,281 ft) of altitude gained (the adiabatic lapse rate) is 5. The lapse rate is defined as the negative of the rate of change in an atmospheric variable usually Temperature, with height in an atmosphere 1 °C/km. ^[19] In terms of environmental lapse rate, ambient temperatures fall by 0. The lapse rate is defined as the negative of the rate of change in an atmospheric variable usually Temperature, with height in an atmosphere 6 °C (1. 1 °F) for every 100 metres (328 ft) rise in altitude. Thus, climates ranging from nearly tropical in the foothills to tundra above the snow line can coexist within several dozen miles of each other. The snow line is the point above which or poleward of which snow and ice cover the ground throughout the year Sharp temperature contrasts between sunny and shady slopes, high diurnal temperature variability, temperature inversions, and altitude-dependent variability in rainfall are also common. The northern side of the western Himalayas, also known as the trans-Himalayan belt, is a region of barren, arid, frigid, and wind-blown wastelands. In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering Most precipitation occurs as snowfall during the late winter and spring months.

Areas south of the Himalayas are largely protected from cold winter winds coming in from the Asian interior. The leeward side (northern face) of the mountains receives less rain while the southern slopes, well-exposed to the monsoon, get heavy rainfall. Areas situated at elevations of 1,070–2,290 metres (3,510–7,510 ft) receive the heaviest rainfall, which decreases rapidly at elevations above 2,290 metres (7,513 ft). The Himalayas experience their heaviest snowfall between December and February and at elevations above 1,500 metres (4,921 ft). Snowfall increases with elevation by up to several dozen millimetres per 100 metre (~2 in; 330 ft) increase. Elevations above 5,000 metres (16,404 ft) never experience rain; all precipitation falls as snow. ^[20]

Seasons

The India Meteorological Department (IMD) designates four official seasons:^[21]

A winter scene in Bandhavgarh National Park, Madhya Pradesh. The India Meteorological Department (IMD also referred to as the Met Office is a Government of India organisation that is responsible for meteorological observations weather Bandhavgarh National Park ( Devanagari: बांधवगढ राष्ट्रीय उद्दान is one of the largest national parks in India Madhya Pradesh (abbreviated as MP) ( Hindī: मध्य प्रदेश pronounced, Translation: Middle Province) often

• Winter, occurring between January and March. The year's coldest months are December and January, when temperatures average around 10–15 °C (50–59 °F) in the northwest; temperatures rise as one proceeds towards the equator, peaking around 20–25 °C (68–77 °F) in mainland India's southeast.
• Summer or pre-monsoon season, lasting from March to June (April to July in northwestern India). In western and southern regions, the hottest month is April; for northern regions, May is the hottest month. Temperatures average around 32–40 °C (90–104 °F) in most of the interior.
• Monsoon or rainy season, lasting from June to September. The season is dominated by the humid southwest summer monsoon, which slowly sweeps across the country beginning in late May or early June. Monsoon rains begin to recede from North India at the beginning of October.
• Post-monsoon season, lasting from October to December. South India typically receives more precipitation. Monsoon rains begin to recede from North India at the beginning of October. In northwestern India, October and November are usually cloudless. Parts of the country experience the dry northeast monsoon.

The Himalayan states, being more temperate, experience an additional two seasons: autumn and spring. Traditionally, Indians note six seasons, each about two months long. These are the spring (Sanskrit: vasanta), summer (grīṣma), monsoon season (varṣā), early autumn (śarada), late autumn (hemanta), and winter (śiśira). Sanskrit (sa संस्कृता वाक् saṃskṛtā vāk, for short sa संस्कृतम् saṃskṛtam) is a historical These are based on the astronomical division of the twelve months into six parts. The ancient Hindu calendar also reflects these seasons in its arrangement of months. The Hindu calendar used in ancient times has undergone many changes in the process of regionalization and today there are several regional Indian Calendars, as

Winter

Once the monsoons subside, average temperatures gradually fall across India. As the Sun's vertical rays move south of the equator, most of the country experiences moderately cool weather; temperatures change by about 0. 6 °C (1. 35 °F) per degree of latitude. December and January are the coldest months, with mean temperatures of 10–15 °C (50–59 °F) in Indian Himalayas. Mean temperatures are higher in the east and south, where they reach 20–25 °C (68–77 °F).

In northwestern India, virtually cloudless conditions prevail in October and November, resulting in wide diurnal temperature swings; as in much of the Deccan Plateau, they range between 16–20 °C (61–68 °F). However, from March to May, "western disturbances" bring heavy bursts of rain and snow. These extra-tropical low-pressure systems originate in the eastern Mediterranean Sea. A low pressure area, or " low " is a region where the Atmospheric pressure is lower in relation to the surrounding area ^[22] They are carried towards India by the subtropical westerlies, which are the prevailing winds blowing at North India's range of latitude. The Westerlies or the Prevailing Westerlies are the prevailing winds in the Middle latitudes between 30 and 60 degrees Latitude, blowing from The prevailing winds are the trends in speed and direction of Wind over a particular point on the Earth 's surface ^[18] Once their passage is hindered by the Himalayas, they are unable to proceed further, and they release significant precipitation over the southern Himalayas. ^[23] The three Himalayan states (Jammu and Kashmir in the extreme north, Himachal Pradesh, and Uttarakhand) experience heavy snowfall; in Jammu and Kashmir, blizzards occur regularly, disrupting travel and other activities. Himachal Pradesh ( Hindi: हिमाचल प्रदेश Punjabi: ਹਿਮਾਚਲ ਪ੍ਰਦੇਸ਼ pronounced) is a state in the Uttarakhand ( Hindi: उत्तराखण्ड or उत्तराखंड Uttar + Akhand i "Snowfall" redirects here For other uses see Snow (disambiguation or Snowfall (disambiguation. A blizzard is a severe Winter storm condition characterized by low Temperatures strong Winds and heavy blowing Snow Blizzards are formed when

A winter scene by a lake in Nainital, Uttarakhand. Nainital is a town in the Indian state of Uttarakhand and headquarters of Nainital district in the Kumaon Foothills Uttarakhand ( Hindi: उत्तराखण्ड or उत्तराखंड Uttar + Akhand i

The rest of North India, including the Indo-Gangetic Plain, almost never receives snow. Geography Northern India lies mainly on continental India and a very small part of it lies on the Indian peninsula The Indo-Gangetic Plain also known as the Northern plains and the North Indian River Plain is a large and fertile plain encompassing most of northern and eastern India, However, in the plains, temperatures occasionally fall below freezing, though never for more one or two days. Winter highs in Delhi range from 16 °C (61 °F) to 21 °C (70 °F). Nighttime temperatures average 2–8 °C (36–46 °F). In the Punjab plains, lows can fall below freezing, dropping to around −6 °C (21 °F) in Amritsar. Punjab (ਪੰਜਾਬ पंजाब pəɲdʒaːb is a state in northwest India. Amritsar (ਅੰਮ੍ਰਿਤਸਰ meaning The Lake of the Holy Nectar, is the administrative headquarters of the Amritsar District in the state Frost sometimes occurs, but the hallmark of the season is the notorious fog, which frequently disrupts daily life; fog grows thick enough to hinder visibility and disrupt air travel 15–20 days annually. Fog is a cloud that is in contact with the ground Stratus clouds are usually the only clouds that touch the ground ^[24] Eastern India's climate is much milder, experiencing moderately warm days and cool nights. Highs range from 23 °C (73 °F) in Patna to 26 °C (79 °F) in Kolkata (Calcutta); lows average from 8 °C (46 °F) in Patna to 14 °C (57 °F) in Kolkata. Paṭnā ( Hindi: पटना is the capital of the Indian state of Bihar, and one of the oldest continuously inhabited Frigid winds from the Himalayas can depress temperatures near the Brahmaputra River. The Brahmaputra, also called Tsangpo-Brahmaputra is a Trans-boundary river and one of the major Rivers of Asia. ^[25] The two Himalayan states in the east, Sikkim and Arunachal Pradesh, receive substantial snowfall. Sikkim ( Nepali:, also Sikhim) is a Landlocked Indian state nestled in the Himalayas It is the least populous state in India Arunachal Pradesh (अरुणाचल प्रदेश   Aruṇācal Pradeś is the easternmost state of India The extreme north of West Bengal, centred around Darjeeling, also experiences snowfall, but only rarely. West Bengal ( Bengali: পশ্চিমবঙ্গ Poshchim Bônggo poʃtʃim bɔŋgo is a state in eastern India. Darjeeling ( Nepali:) is a town in the Indian state of West Bengal.

In South India, particularly the hinterland of Maharashtra, Madhya Pradesh, parts of Karnataka, and Andhra Pradesh, somewhat cooler weather prevails. South India is the area encompassing India 's states of Andhra Pradesh, Karnataka, Kerala and Tamil Nadu as well as the union Madhya Pradesh (abbreviated as MP) ( Hindī: मध्य प्रदेश pronounced, Translation: Middle Province) often Minimum temperatures in western Maharashtra, Madhya Pradesh and Chhattisgarh hover around 10 °C (50 °F); in the southern Deccan Plateau, they reach 16 °C (61 °F). Chhattisgarh ( Chhattisgarhi / Hindi: छत्तीसगढ़ tʃʰət̪t̪iːsgəɽʰ, a state in central India, formed when the sixteen Coastal areas, especially those near the Coromandel Coast, and low-elevation interior tracts are warm, with daily high temperatures of 30 °C (86 °F) and lows of around 21 °C (70 °F). The Coromandel Coast is the name given to the southeastern coast of the Indian peninsula The Western Ghats, including the Nilgiri Range, are exceptional; there, lows can fall below freezing. The Nilgiri (Tamil: நீலகிரி or literally Blue Mountains) often referred to as the Nilgiri Hills, are a range of mountains with at least 24 peaks above ^[26] This compares with a range of 12–14 °C (54–57 °F) on the Malabar Coast; there, as is the case for other coastal areas, the Indian Ocean exerts a strong moderating influence on weather. ^[9]

Summer

A summer view of Khajjiar, a hill station in Himachal Pradesh. Khajjiar is a small Hill station in Chamba District, Himachal Pradesh, India. Himachal Pradesh ( Hindi: हिमाचल प्रदेश Punjabi: ਹਿਮਾਚਲ ਪ੍ਰਦੇਸ਼ pronounced) is a state in the

Summer in northwestern India lasts from April to July, and in the rest of the country from March to June. The temperatures in the north rise as the vertical rays of the Sun reach the Tropic of Cancer. The hottest month for the western and southern regions of the country is April; for most of North India, it is May. Temperatures of 50 °C (122 °F) and higher have been recorded in parts of India during this season. ^[13] In cooler regions of North India, immense pre-monsoon squall-line thunderstorms, known locally as "Nor'westers", commonly drop large hailstones. A squall is a sudden sharp increase in wind speed which is usually associated with active weather such as rain showers thunderstorms or heavy snow ^[27] Near the coast the temperature hovers around 36 °C (97 °F), and the proximity of the sea increases the level of humidity. In southern India, the temperatures are higher on the east coast by a few degrees compared to the west coast.

By May, most of the Indian interior experiences mean temperatures over 32 °C (90 °F), while maximum temperatures often exceed 40 °C (104 °F). In the hot months of April and May, western disturbances, with their cooling influence, may still arrive, but rapidly diminish in frequency as summer progresses. ^[28] Notably, a higher frequency of such disturbances in April correlates with a delayed monsoon onset (thus extending summer) in northwest India. In eastern India, monsoon onset dates have been steadily advancing over the past several decades, resulting in shorter summers there. ^[18]

Altitude affects the temperature to a large extent, with higher parts of the Deccan Plateau and other areas being relatively cooler. Hill stations, such as Ootacamund ("Ooty") in the Western Ghats and Kalimpong in the eastern Himalayas, with average maximum temperatures of around 25 °C (77 °F), offer some respite from the heat. Hill station is a term used for a town usually at somewhat higher elevations WikipediaWikiProject Indian cities for details --> Ooty, short for Ootacamund (officially Udhagamandalam Tamil: உதகமண்டலம் Kalimpong (कालिम्पोङ is a Hill station (a hill town nestled in the Shiwalik Hills (or Lower Himalaya in the Indian state of West At lower elevations, in parts of northern and western India, a strong, hot, and dry wind known as the Loo blows in from the west during the daytime; with very high temperatures, in some cases up to around 45 °C (113 °F); it can cause fatal cases of sunstroke. Loo is a strong hot and dry wind which blows over Northern and parts of Western India during the day time in summer Hyperthermia, in its advanced state referred to as heat stroke or sunstroke, is an acute condition which occurs when the Body produces or absorbs more Tornadoes may also occur, concentrated in a corridor stretching from northeastern India towards Pakistan. A tornado is a violent rotating column of air which is in contact with both the surface of the earth and a Cumulonimbus cloud or in rare cases the base of a Cumulus They are rare, however; only several dozen have been reported since 1835. ^[29]

Monsoon

Onset dates and prevailing wind currents of the southwest summer and northeast winter monsoons.

Regional variation in rainfall across India. The monsoon season delivers four-fifths of the country's precipitation.

The southwest summer monsoon, a four-month period when massive convective thunderstorms dominate India's weather, is Earth's most valuable wet season. ^[30] It results from the southeast trade winds originating from a high-pressure mass centered over the southern Indian Ocean; attracted by a low-pressure region centered over South Asia, it gives rise to surface winds that ferry humid air into India from the southwest. The trade winds (also called trades) are the prevailing pattern of easterly winds found in the Tropics near the Earth's Equator. ^[31] These inflows ultimately result from a northward shift of the local jet stream, which itself results from rising summer temperatures over Tibet and the Indian subcontinent. Definitions of Tibet See also Definitions of Tibet Name In English The English word Tibet, like the word for Tibet in most European The void left by the jet stream, which switches from a route just south of the Himalayas to one tracking north of Tibet, then attracts warm, humid air. ^[32]

The main factor behind this shift is the high summer temperature difference between Central Asia and the Indian Ocean. ^[33] 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. The Intertropical Convergence Zone (ITCZ, also known as the Intertropical Front, Monsoon trough, Doldrums or the Equatorial ^[32] 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 34–49 mya. The Tibetan Plateau, also known as the Qinghai-Tibetan (Qingzang Plateau is a vast elevated Plateau in Central Asia covering most of the Tibet Autonomous Orogeny (Greek for "mountain generating" is the process of natural Mountain building and may be studied as a tectonic structural event as a geographical event and The Eocene epoch (558 ± 02 - 339 ± 01 Ma) is a major division of the Geologic timescale and the second epoch of the Palaeogene period in The Oligocene is a geologic epoch of the Paleogene period and extends from about 33 Aridification is the process of a region becoming increasingly dry. ^[34]

The southwest monsoon arrives in two branches: the Bay of Bengal branch and the Arabian Sea branch. The Bay of Bengal is a bay that forms the northeastern part of the Indian Ocean. The Arabian Sea ( Arabic: بحر العرب transliterated: Baḥr al-'Arab Sanskrit: सिन्धु सागर transliterated: The latter extends toward a low-pressure area over the Thar Desert and is roughly three times stronger than the Bay of Bengal branch. The monsoon usually breaks over Indian territory by around 25 May, when it lashes the Andaman and Nicobar Islands in the Bay of Bengal. Events 1085 - Alfonso VI of Castile takes Toledo Spain back from the Moors. The Andaman & Nicobar Islands is a Union territory of India. Informally the territory's name is often abbreviated to A & N Islands, or ANI It strikes the Indian mainland around 1 June,^[35] supplies over 80% of India's annual rainfall. Events 193 - Roman Emperor Didius Julianus is Assassinated 987 - Hugh Capet is elected ^[36] first appearing near the Malabar Coast of Kerala. The Malabar Coast also known as the Malabarian Coast, is a long and narrow south-western shore line of the mainland Indian subcontinent. By 9 June, it reaches Mumbai; it appears over Delhi by 29 June. Events 53 - Roman Emperor Nero marries Claudia Octavia 62 - Claudia Octavia commits Mumbai ( Marathi:,, IPA: formerly Bombay, is the capital of the Indian state of Maharashtra and the financial Delhi (दिल्ली ਦਿੱਲੀ دلی d̪ɪlːiː sometimes referred to as Dilli) is the second largest metropolis of India, with a population Events 512 - A Solar eclipse is recorded by a monastic chronicler in Ireland. The Bay of Bengal branch, which hugs the Coromandal Coast between Cape Comorin and Orissa, swerves to the northwest. For other uses of Kanyakumari, please see Kanyakumari (disambiguation. Orissa (ଓଡ଼ିଶା is a state located on the east coast of India, by the Bay of Bengal. The Arabian Sea branch moves northeast towards the Himalayas. By the first week of July, the entire country experiences monsoon rain; on average, South India receives more rainfall than North India. However, Northeast India receives the most precipitation. North-East India refers to the easternmost region of India consisting of the contiguous Seven Sister States and Sikkim. Monsoon clouds begin retreating from North India by the end of August; it withdraws from Mumbai by 5 October. Events 869 - The Fourth Council of Constantinople is convened to decide about what to do about Patriarch Photius of Constantinople As India further cools during September, the southwest monsoon weakens. By the end of November, it has left the country. ^[32]

Pre-monsoon clouds, as they appear in Mumbai, western Maharashtra. Mumbai ( Marathi:,, IPA: formerly Bombay, is the capital of the Indian state of Maharashtra and the financial

Monsoon rains impact the health of the Indian economy; as Indian agriculture employs 600 million people and composes 20% of the national GDP,^[37] good monsoons correlate with a booming economy. The economy of India, measured in USD exchange-rate terms is the twelfth largest in the world with a GDP of around $1 trillion (2008 Indian agriculture began by 9000 BCE as a result of early cultivation of plants and domestication of crops and animals Weak or failed monsoons (droughts) result in widespread agricultural losses and substantially hinder overall economic growth. ^[38][39][40] The rains reduce temperatures and replenish groundwater tables, rivers, and lakes.

Post-monsoon

During the post-monsoon months of October to December, a different monsoon cycle, the northeast (or "retreating") monsoon, brings dry, cool, and dense Central Asian 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. ^[41] Though the India Meteorological Department (IMD) and other sources refers to this period as a fourth ("post-monsoon") season,^[21][42][43] other sources designate only three seasons. The India Meteorological Department (IMD also referred to as the Met Office is a Government of India organisation that is responsible for meteorological observations weather ^[44] 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 28 °C and 34 °C (82–93 °F).

The northeast monsoon, which begins in September, lasts through the post-monsoon seasons, and only ends in March, carries winds that have already lost their moisture while crossing central Asia and the vast rain shadow region lying north of the Himalayas. For the Australian television series see Rain Shadow (TV series. They cross India diagonally from northeast to southwest. However, the large indentation made by the Bay of Bengal into India's eastern coast means that the flows are humidified before reaching Cape Comorin and rest of Tamil Nadu, meaning that the state, and also some parts of Kerala, experience significant precipitation in the post-monsoon and winter periods. For other uses of Kanyakumari, please see Kanyakumari (disambiguation. ^[14] However, parts of West Bengal, Orissa, Andhra Pradesh, Karnataka and North-East India also receive minor precipitation from the northeast monsoon. The state of Karnataka in India has a bittersweet relationship with rains ^[45]

Statistics

Shown below are temperature and precipitation data for selected Indian cities; these represent the full variety of major Indian climate types. Figures have been grouped by the four-season classification scheme used by the IMD;^[α] year-round averages and totals are also displayed.

Temperature

Precipitation

Disasters

Main article: Natural disasters in India

Disaster-prone regions in India. Cyclones Tropical cyclones which are severe storms spun off from the Intertropical Convergence Zone, may affect thousands of Indians living in coastal

Map showing winds zones, shaded by distribution of average speeds of prevailing winds.

Climate-related natural disasters cause massive losses of Indian life and property. Droughts, flash floods, cyclones, avalanches, landslides brought on by torrential rains, and snowstorms pose the greatest threats. Other dangers include frequent summer dust storms, which usually track from north to south; they cause extensive property damage in North India^[50] and deposit large amounts of dust from arid regions. In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering Hail is also common in parts of India, causing severe damage to standing crops such as rice and wheat.

Floods and landslides

In the Lower Himalaya, landslides are common. The young age of the region's hills result in labile rock formations, which are susceptible to slippages. Lability refers to something that is constantly undergoing change or something that is likely to undergo change Rising population and development pressures, particularly from logging and tourism, cause deforestation. The result, denuded hillsides, exacerbates the severity of landslides, since tree cover impedes the downhill flow of water. ^[51] Parts of the Western Ghats also suffer from low-intensity landslides. Avalanches occur in Kashmir, Himachal Pradesh, and Sikkim.

Floods are the most common natural disaster in India. The heavy southwest monsoon rains cause the Brahmaputra and other rivers to distend their banks, often flooding surrounding areas. The Brahmaputra, also called Tsangpo-Brahmaputra is a Trans-boundary river and one of the major Rivers of Asia. Though they provide rice paddy farmers with a largely dependable source of natural irrigation and fertilisation, the floods can kill thousands and displace millions. Excess, erratic, or untimely monsoon rainfall may also wash away or otherwise ruin crops. ^[52][53] Almost all of India is flood-prone, and extreme precipitation events, such as flash floods and torrential rains, have become increasingly common in central India over the past several decades, coinciding with rising temperatures. Mean annual precipitation totals have remained steady due to the declining frequency of weather systems that generate moderate amounts of rain. ^[54] (See 2007 South Asian floods. This article refers to the multiple concurrent floods in South Asia between July 3 and August 15 2007 (Dartmouth Flood Observatory numbers DFO115121124129136143153155157 and )

Cyclones

Satellite imagery of Cyclone 05B in the Bay of Bengal. The Bay of Bengal is a bay that forms the northeastern part of the Indian Ocean.

Tropical cyclones, which are severe storms spun off from the Intertropical Convergence Zone, may affect thousands of Indians living in coastal regions. A tropical cyclone is a storm system characterized by a low pressure center and numerous Thunderstorms that produce strong winds and Flooding The Intertropical Convergence Zone (ITCZ, also known as the Intertropical Front, Monsoon trough, Doldrums or the Equatorial Tropical cyclogenesis is particularly common in the northern reaches of the Indian Ocean in and around the Bay of Bengal. Tropical cyclogenesis is the technical term describing the development and strengthening of a Tropical cyclone in the Atmosphere. The Indian Ocean is the third largest of the world's Oceanic divisions covering about 20% of the water on the Earth 's surface Cyclones bring with them heavy rains, storm surges, and winds that often cut affected areas off from relief and supplies. Storm surge or tidal surge is an offshore rise of water associated with a low pressure weather system typically a Tropical cyclone. In the North Indian Ocean Basin, the cyclone season runs from April to December, with peak activity between May and November. ^[55] Each year, an average of eight storms with sustained wind speeds greater than 63 km/h (39 mph) form; of these, two strengthen into true tropical cyclones, which have sustained gusts greater than 117 km/h (73 mph). (For the South African airport with IATA code "KMH" see Johan Pienaar Airport. On average, a major (Category 3 or higher) cyclone develops every other year. The Saffir-Simpson Hurricane Scale is a classification used for most Western Hemisphere Tropical cyclones that exceed the intensities of Tropical depressions ^[55][56]

During summer, the Bay of Bengal is subject to intense heating, giving rise to humid and unstable air masses that produce cyclones. The Bay of Bengal is a bay that forms the northeastern part of the Indian Ocean. Many powerful cyclones, including the 1737 Calcutta cyclone, the 1970 Bhola cyclone, and the 1991 Bangladesh cyclone, have led to widespread devastation along parts of the eastern coast of India and neighboring Bangladesh. The years before 1980 featured the Pre-1980 North Indian Ocean cyclone seasons. The 1970 Bhola cyclone was a devastating Tropical cyclone that struck East Pakistan (now Bangladesh) and India 's West Bengal on The 1991 Bangladesh cyclone was among the deadliest tropical cyclones on record ( Bengali: বাংলাদেশ inc-Latn Bangladesh) officially Widespread death and property destruction are reported every year in exposed coastal states such as Andhra Pradesh, Orissa, Tamil Nadu, and West Bengal. Orissa (ଓଡ଼ିଶା is a state located on the east coast of India, by the Bay of Bengal. India's western coast, bordering the more placid Arabian Sea, experiences cyclones only rarely; these mainly strike Gujarat and, less frequently, Kerala. Gujarat (ગુજરાત Gujǎrāt, pronounced) is a state in western India. Kerala ( Malayalam: {{Kerala in Malayalam}};

In terms of damage and loss of life, Cyclone 05B, a supercyclone that struck Orissa on 29 October 1999, was the worst in more than a quarter-century. The 1999 Orissa cyclone, also known as Cyclone 05B and Paradip cyclone, was the deadliest Indian Ocean Tropical cyclone since the 1991 Bangladesh Events 437 - Valentinian III, Western Roman Emperor, marries Licinia Eudoxia, daughter of his cousin Theodosius II Year 1999 ( MCMXCIX) was a Common year starting on Friday (link will display full 1999 Gregorian calendar) With peak winds of 160 miles per hour (257 km/h), it was the equivalent of a Category 5 hurricane. The Saffir-Simpson Hurricane Scale is a classification used for most Western Hemisphere Tropical cyclones that exceed the intensities of Tropical depressions ^[57] Almost two million people were left homeless;^[58] another 20 million people lives were disrupted by the cyclone. ^[58] Officially, 9,803 people died from the storm;^[57] unofficial estimates place the death toll at over 10,000. ^[58]

Droughts

Main article: Drought in India

The dry bed of the Niranjana River, Bihar. Drought in India has resulted in tens of millions of deaths over the course of the 18th 19th and 20th centuries Bihar ( Hindi:बिहार Urdu: بہار bɪhaːr) is a state in eastern India.

Indian agriculture is heavily dependent on the monsoon as a source of water. In some parts of India, the failure of the monsoons result in water shortages, resulting in below-average crop yields. This is particularly true of major drought-prone regions such as southern and eastern Maharashtra, northern Karnataka, Andhra Pradesh, Orissa, Gujarat, and Rajasthan. In the past, droughts have periodically led to major Indian famines. Owing to its almost entire dependence upon the Monsoon rains India is more liable These include the Bengal famine of 1770, in which up to one third of the population in affected areas died; the 1876–1877 famine, in which over five million people died; the 1899 famine, in which over 4. The Bengal famine of 1770 (Bengali ৭৬-এর মন্বন্তর Chhiattōrer monnōntór; lit The Famine of '76) was a catastrophic Famine between 5 million died; and the Bengal famine of 1943, in which over five million died from starvation and famine-related illnesses. The Bengal famine of 1943 is one amongst the several Famines that occurred in British administered Bengal. ^[59][60]

All such episodes of severe drought correlate with El Niño-Southern Oscillation (ENSO) events. El Niño-Southern Oscillation ( ENSO; commonly referred to as simply El Niño) is a global coupled ocean-atmosphere phenomenon ^[61][62] El Niño-related droughts have also been implicated in periodic declines in Indian agricultural output. ^[63] Nevertheless, ENSO events that have coincided with abnormally high sea surfaces temperatures in the Indian Ocean—in one instance during 1997 and 1998 by up to 3 °C (5 °F)—have resulted in increased oceanic evaporation, resulting in unusually wet weather across India. Such anomalies have occurred during a sustained warm spell that began in the 1990s. ^[64] A contrasting phenomenon is that, instead of the usual high pressure air mass over the southern Indian Ocean, an ENSO-related oceanic low pressure convergence center forms; it then continually pulls dry air from Central Asia, desiccating India during what should have been the humid summer monsoon season. This reversed air flow causes India's droughts. ^[65] The extent that an ENSO event raises sea surface temperatures in the central Pacific Ocean influences the degree of drought. Sea surface temperature (SST is the water Temperature close to the surface The Pacific Ocean is the largest of the Earth 's Oceanic divisions ^[61]

Extremes

Alwar, on the fringes of the Thar Desert, registered a temperature of 50. 6 °C (123 °F), India's highest.

India's lowest recorded temperature reading was −45 °C (−49 °F) in Dras, Ladakh, in eastern Jammu and Kashmir; however, the reading was taken with non-standard equipment. WikipediaWikiProject Indian cities for details --> Drass is a tiny town in the Kargil District of Jammu and Kashmir, India. Further south, readings as low as −30. 6 °C (−23 °F) have been taken in Leh, also in Ladakh. Leh ( was the capital of the Himalayan kingdom of Ladakh, now the Leh District in the state of Jammu and Kashmir, India However, temperatures on the Indian-controlled Siachen Glacier near Bilafond La (5,450 metres (17,881 ft)) and Sia La (5,589 metres (18,337 ft)) have fallen below −55 °C (−67 °F),^[66] while blizzards bring wind speeds in excess of 250 km/h (155 mph),^[67] or hurricane-force winds ranking at 12 (the maximum) on the Beaufort scale. see Siachen conflict for the military conflict over this area The Siachen Glacier is located in the eastern Karakoram range in the Himalaya Bilafond La (meaning "Pass of the Butterflies" also known as the Saltoro Pass, is a Mountain pass situated on Saltoro Ridge, which sits Sia La is a Mountain pass situated on Saltoro Ridge, which sits immediately west of the vast Siachen Glacier. A tropical cyclone is a storm system characterized by a low pressure center and numerous Thunderstorms that produce strong winds and Flooding The Beaufort scale (ˈboʊfət is an Empirical measure for describing Wind speed based mainly on observed sea conditions It was those conditions, not actual military engagements, that were responsible for more than 97% of the roughly 15,000 casualties suffered by India and Pakistan over the course of conflict in the region. ^[67][68][66] The highest reliable temperature reading was 50. 6 °C (123 °F) in Alwar, Rajasthan in 1955. History "Alwar" was formerly known as "Ulwar" This mark was also reached at Pachpadra in Rajasthan. Pachpadra is a town in Indian state of Rajasthan. One of the famous attractions in the city is the Pachpadra lake, which is known for salt collection around it Recently, claims have been made of temperatures touching 55 °C (131 °F) in Orissa;^[69] these have been met with some skepticism by the India Meteorological Department (IMD), which has questioned the methods used in recording such data. The India Meteorological Department (IMD also referred to as the Met Office is a Government of India organisation that is responsible for meteorological observations weather

The average annual precipitation of 11,871 millimetres (467 in) in the village of Mawsynram, in the hilly northeastern state of Meghalaya, is the highest recorded in Asia, and possibly on Earth. Mawsynram is a village in the Khasi Hills of Meghalaya state in north-eastern India, 56 kilometers from Shillong. ^[70] The village, which sits at an elevation of 1,401 metres (4,596 ft), benefits from its proximity to both the Himalayas and the Bay of Bengal. However, since the town of Cherrapunji, 5 kilometres (3 mi) to the east, is the nearest town to host a meteorological office (none has ever existed in Mawsynram), it is officially credited as being the world's wettest place. ^[71] In recent years, the Cherrapunji-Mawsynram region has averaged 9,296 millimetres (366 in) of rain annually, though Cherrapunji has had at least one period of daily rainfall that lasted almost two years. ^[72] India's highest recorded one-day rainfall total occurred on 26 July 2005, when Mumbai received more than 650 millimetres (26 in);^[73] the massive flooding that resulted killed over 900 people. Events 657 - Battle of Siffin. 811 - Battle of Pliska; Byzantine Emperor Nicephorus Year 2005 ( MMV) was a Common year starting on Saturday (link displays full calendar of the Gregorian calendar. ^[74][75]

In terms of snowfall, regions of Jammur and Kashmir, such as Baramulla district in the east and the Pir Panjal Range in the southeast, experience exceptionally heavy snowfall. Baramulla is a District in the state of Jammu and Kashmir in north India. The Pir Panjal Range is a range of mountains that form a part of the Middle Himalayas across the states of Jammu and Kashmir and Himachal Pradesh in the Kashmir's highest recorded monthly snowfall occurred in February of 1967, when 8. 4 metres (331 in) fell in Gulmarg, though the IMD has recorded snowdrifts up to 12 metres (39 ft) in several Kashmiri districts. WikipediaWikiProject Indian cities for details --> Gulmarg (or "Meadow of Flowers" is a town a Hill station and a Notified area committee In February of 2005, more than 200 people died when, in four days, a western disturbance brought up to 2 metres (7 ft) of snowfall to parts of the state. ^[76]

Global warming

Main article: Effects of global warming on India

See also: 2007 South Asian heat wave

Lakshadweep, comprising tiny low-lying islands, are at risk of being inundated by sea level rises associated with global warming. The 2007 Asian Heat wave affected the South Asian countries of India, Pakistan, Bangladesh, and Nepal, as well as Russia

Several effects of global warming, including steady sea level rise, increased cyclonic activity, and changes in ambient temperature and precipitation patterns, have impacted or are projected to impact India. effects of Global warming on the environment and human life are numerous varied accelerating and taking scientists studying global warming by surprise Sea-level rise is an increase in Sea level. Multiple complex factors may influence this change Ongoing sea level rises have submerged several low-lying islands in the Sundarbans, displacing thousands of people. The Sundarbans (সুন্দরবন Shundorbôn) is the largest single block of tidal halophytic Mangrove forest in the world ^[77] Temperature rises on the Tibetan Plateau, which are causing Himalayan glaciers to retreat, may reduce the flow rate of the Ganges, Brahmaputra, Yamuna, and other major rivers; hundreds of thousands of farmers depend on these rivers. whitechuck glacier 2006jpg|right|thumb|320px|The same view as seen in 2006 where this branch of glacier retreated 1 The volumetric flow rate in Fluid dynamics and Hydrometry, (also known as volume flow rate or rate of fluid flow) is the volume of fluid which For the goddess of the river who is sometimes called Yamuna see Yami The Yamuna (Sanskrit यमुना ^[78] According to a 2007 World Wide Fund for Nature (WWF) report, the Indus River may run dry for the same reason. The Indus River { Sanskrit: सिन्धु Sindhu; Urdu: urd {{Nastaliq سندھ}} Sindh; Sindhi: snd ^[79]

Increased landslides and flooding are projected to impact such states as Assam. ^[80] Ecological disasters, such as a 1998 coral bleaching event that killed off more than 70% of corals in the reef ecosystems off Lakshadweep and the Andamans, and was brought on by elevated ocean temperatures tied to global warming, are also projected to become increasingly common. Coral bleaching is the loss of color of Corals due to stress-induced expulsion of symbiotic Unicellular Algae or due to the loss of pigmentation within Corals are Marine organisms from the class Anthozoa and exist as small Sea anemone –like Polyps typically in colonies of many ^[81][82][83]

The Indira Gandhi Institute of Development Research has reported that, if the predictions relating to global warming made by the Intergovernmental Panel on Climate Change come to fruition, climate-related factors could cause India's GDP to decline by up to 9%. The Indira Gandhi Institute of Development Research is a research institution dedicated to promoting scientific research on the developmental issues facing India. Contributing to this would be shifting growing seasons for major crops such as rice, production of which could fall by 40%. Around seven million people are projected to be displaced due to, among other factors, submersion of parts of Mumbai and Chennai, if global temperatures were to rise by a mere 2 °C (36 °F). ^[84] Such shifts are not new. Earlier in the Holocene epoch (4,800–6,300 years ago), parts of what is now the Thar Desert were wet enough to support perennial lakes; researchers have proposed that this was due to much higher winter precipitation, which coincided with stronger monsoons. The Holocene is a Geological epoch which began approximately 10000 years ago (about 8000 BC The geologic time scale is a chronologic schema (or idealized Model) relating Stratigraphy to time that is used by Geologists and other ^[85] Similarly, Kashmir, which once had a warm subtropical climate, shifted to a substantially colder temperate climate 2. 6–3. 7 mya; it was then repeatedly subjected to extended cold spells starting 600,000 years ago. ^[86]

On the other hand, Al Gore has said India can lead the world in climate change solution ^[87]

Atmospheric pollution

Clouds of thick haze and smoke form along the Ganges River Basin. Albert Arnold Gore Jr (born March 31 1948 is an American environmental Activist, author Businessperson, former Politician, and former

Thick haze and smoke, originating from burning biomass in northwestern India^[88] and air pollution from large industrial cities in northern India,^[89] often concentrate inside the Ganges Basin. The Ganga basin is a part of the composite Ganga - Brahmaputra - Meghna basin which drains an area of 1086000 square kilometres Prevailing westerlies carry aerosols along the southern margins of the steep-faced Tibetan Plateau to eastern India and the Bay of Bengal. The Bay of Bengal is a bay that forms the northeastern part of the Indian Ocean. Dust and black carbon, which are blown towards higher altitudes by winds at the southern margins of the Himalayas, can absorb shortwave radiation and heat the air over the Tibetan Plateau. Black carbon or BC is formed through the incomplete combustion of fossil fuels biofuel and biomass and is emitted in both anthropogenic and naturally occurring soot The net atmospheric heating due to aerosol absorption causes the air to warm and convect upwards, increasing the concentration of moisture in the mid-troposphere and providing positive feedback that stimulates further heating of aerosols. Convection in the most general terms refers to the movement of molecules within Fluids (i The troposphere is the lowest portion of Earth's atmosphere. It contains approximately 75% of the atmosphere's mass and almost all of its Water vapor and ^[89]

See also

• List of wettest known tropical cyclones in India

Notes

References

Late-season monsoon clouds during a sunset over the Coromandel Coast. The Coromandel Coast is the name given to the southeastern coast of the Indian peninsula

Citations

Further reading

External links