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The 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. [1] Generally, the season lasts at least one month. [2] The term green season is also sometimes used as a euphemism by tourist authorities. [3]
The rainy season occurs from September to February and it is a major source of energy for the Hadley circulation during boreal winter. It is associated with the development of the Siberian High and the movement of the heating maxima from the Northern Hemisphere to the Southern Hemisphere.
Tropical monsoon climates have monthly mean temperatures above 18 °C (64 °F) in every month of the year and a dry season. [ 1 ] : 200–1 The tropical monsoon climate is the intermediate climate between the wet Af (or tropical rainforest climate ) and the drier Aw (or tropical savanna climate ).
The "Dry" and Hot Season (a relative term as the city does not truly have a dry season) occurs when seasonal south-west winds blow from Sumatra toward the West Coast of Peninsular Malaysia but are blocked by the Titiwangsa Mountain Range. The temperature may reach 40 degrees Celsius. The Rainy season usually occurs between October and March.
The Southern sections of Asia are mild to hot, while far northeastern areas such as Siberia are very cold, and East Asia has a temperate climate. The highest temperature recorded in Asia was 54 °C (at Ahvaz Airport, Iran on June 29, 2017, and at Tirat Zvi, Israel on June 21, 1942).
After a dry start to winter, California's rainy season is finally well under way. December downpours sent water racing through streets in coastal Ventura County and the city of Santa Barbara.
The Köppen climate classification is the most widely used climate classification system. [2] It defines a tropical climate as a region where the mean temperature of the coldest month is greater than or equal to 18 °C (64 °F) and does not fit into the criteria for B-group climates, classifying them as an A-group (tropical climate group). [3]
Over India, a subtropical westerly jet develops in the winter season and is replaced by the tropical easterly jet in the summer season. The high temperature during the summer over the Tibetan Plateau, as well as over Central Asia in general, is believed to be the critical factor leading to the formation of the tropical easterly jet over India.