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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). West-central Asia experiences some of the largest diurnal ...
This is a list of countries and sovereign states by temperature. Average yearly temperature is calculated by averaging the minimum and maximum daily temperatures in the country, averaged for the years 1991 – 2020, from World Bank Group , derived from raw gridded climatologies from the Climatic Research Unit .
By 1975, land temperatures across Asia have already increased since the preindustrial period. ... Köppen climate classification map for Central Asia for 1980–2016.
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [ 1 ][ 2 ] with several later modifications by Köppen, notably in 1918 and 1936. [ 3 ][ 4 ] Later, German climatologist Rudolf Geiger (1894–1981 ...
4 Asia's changing climate. ... A 1916 physical map of Asia by Tarr and McMurry. Medieval Europeans considered Asia as a continent, a distinct landmass.
Mean annual temperatures in the coastal areas are around 23 °C (73 °F) in which the coldest month has a mean temperature of 16 to 17 °C (61 to 63 °F) and the hottest month has a mean temperature of 28 to 30 °C (82 to 86 °F). 17 Average annual rainfall in coastal areas is approximately 1,600 to 1,700 mm (63 to 67 in). 17.
Climate of China. Owing to tremendous differences in latitude, longitude, and altitude, the climate of China is extremely diverse. It ranges from tropical in the far south to subarctic in the far north, and alpine in the higher elevations of the Tibetan Plateau. Monsoon winds, caused by differences in the heat-absorbing capacity of the ...
Southeast Asia map of Köppen climate classification. Most of Southeast Asia have a tropical climate that is hot and humid all year round with plentiful rainfall. The majority of Southeast Asia has a wet and dry season caused by seasonal shifts in winds or monsoons.