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The climate of Asia is dry across its southwestern region. Some of the largest daily temperature ranges on Earth occur in the western part of Asia . The monsoon circulation dominates across the southern and eastern regions, due to the Himalayas forcing the formation of a thermal low which draws in moisture during the summer.
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The Köppen climate classification divides climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are A (tropical), B (arid), C (temperate), D (continental), and E (polar). Each group and subgroup is represented by a letter.
A map of Central Asia showing Köppen climate classification. 此文件中描述的项目 depicts. Central Asia. Köppen climate classification ...
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A subarctic climate has little precipitation, [21] and monthly temperatures which are above 10 °C (50 °F) for one to three months of the year, with permafrost in large parts of the area due to the cold winters. Winters within subarctic climates usually include up to six months of temperatures averaging below 0 °C (32 °F).
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Climate of Asia by country (22 C, 2 P) C. Climate change in Asia (12 C, 31 P) Pages in category "Climate of Asia" The following 17 pages are in this category, out of ...