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Monsoon

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A monsoon () is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation, but now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone, specifically between its limits to the north and south of the equator. Usually, the term monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is a dry phase.

Monsoon of South AsiaMonsoon of South AsiaThe Monsoon of South Asia is among several geographically distributed global monsoons. It affects the Indian subcontinent, where it is one of the oldest and most anticipated weather phenomena, and an economically important pattern every year from June through September, but it is only partly understood and notoriously difficult to predict.North American monsoonNorth American monsoonThe North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon is a pattern of pronounced seasonal increase in thunderstorms and rainfall over large areas of the southwestern United States and northwestern Mexico.Australian monsoonAustralian monsoonThe Australian monsoon (AUM), also known as the Australian summer monsoon (ASM), and the Australian-Indonesian monsoon (AIM), is a monsoon system that increases thunderstorms and rainfall over many areas of Indonesia and northern Australia, from the far northern tropics of the region to the semi-arid zone of Australia, typically between November and mid-March, which is the wet season of many parts of northern Australia and Indonesia.RainRainRain or rainfall is a form of atmospheric precipitation composed of droplets of water aerosols that have condensed from atmospheric water vapor and fall by gravity. Depending on the intensity, rain can be described as a drizzle (very light, sporadic rainfall), a shower (brief, moderate rainfall), a cloudburst (brief heavy rainfall) or a downpour (prolonged heavy or "torrential" rainfall).Indian subcontinentIndian subcontinentThe Indian subcontinent is a physiographic region of Asia below the Himalayas which projects into the Indian Ocean between the Bay of Bengal to the east and the Arabian Sea to the west. It is now divided amongst Bangladesh, India, and Pakistan.PrecipitationPrecipitationCondensed water vapor that falls from clouds30-year (1991–2020) mean annual total precipitation based on ERA5 reanalysis data.In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls from clouds due to gravitational pull. The main forms of precipitation include drizzle, rain, rain and snow mixed ("sleet" in Commonwealth usage), snow, ice pellets, graupel and hail.Arabian SeaArabian SeaMax. width2,400 km (1,500 mi)Surface area3,862,000 km (1,491,000 sq mi) (3,600,000–4,600,000 km in various sources)Max.Bay of BengalBay of BengalThe Bay of Bengal forms the northeastern part of the Indian Ocean, located between the Indian subcontinent and the Indochinese peninsula, south of the Bengal region. Spread across an area of 2,600,000 km (1,000,000 sq mi), it is bordered by many of the countries in South Asia and Southeast Asia.Atmosphere of EarthAtmosphere of EarthThe atmosphere of Earth consists of a layer of mixed gas (commonly referred to as air) that is retained by gravity, surrounding the Earth's surface. It contains variable quantities of suspended aerosols and particulates that create weather features such as clouds and hazes. The atmosphere serves as a protective buffer between the Earth's surface and outer space.Glossary of the British RajThe British Raj adopted a range of Indian terms in the administration of British India. The following list is based on a glossary attached to the fifth Report of the Committee of the House of Commons on Indian Affairs, appointed in 1810, comprising Hindustani words commonly used in the administration of the country.Wet seasonWet seasonThe wet season (sometimes called the rainy season or monsoon season) is the time of year when most of a region's average annual rainfall occurs. Generally, the season lasts at least one month. The term green season is also sometimes used as a euphemism by tourist authorities. Areas with wet seasons are dispersed across portions of the tropics and subtropics.Intertropical Convergence ZoneIntertropical Convergence ZoneThe Intertropical Convergence Zone (ITCZ , or ICZ), known by sailors as the doldrums or the calms because of its monotonous windless weather, is the area where the northeast and the southeast trade winds converge. It encircles Earth near the thermal equator, though its specific position varies seasonally. When it lies near the geographic equator, it is called the near-equatorial trough.Special:Search/monsoonSpecial:Search/monsoonRelated word or term.

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