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Other populous national languages include Indonesian million speakers , Bengali million speakers , Japanese million speakers , and Filipino 90 million speakers , though most other countries in Asia also have their own national languages. Select feedback type: The Southern sections of Asia are mild to hot, while far northeastern areas such as Siberia are very cold. This causes the cold wind to sweep down from the Himalayas and Indo-Gangetic Plain towards the vast spans of the Indian Ocean south of the Deccan peninsula. The Asian monsoons may be classified into a few sub-systems, such as the South Asian Monsoon which affects the Indian subcontinent and surrounding regions, and the East Asian Monsoon which affects southern China, Korea and parts of Japan. District Sirsa. From the north, Arctic air has unimpeded access into the continent.
Asia - Climate: The enormous expanse of Asia and its abundance of mountain barriers and inland depressions have resulted in great differences between regions in solar radiation, atmospheric circulation, precipitation, and climate as a whole. A continental climate, associated with large landmasses and characterized by an extreme annual range of temperature, prevails over a large part of Asia. Asia - Climatic regions: The distribution pattern of precipitation throughout the year is varied. Relatively uniform moisture is characteristic of the Asian equatorial zone. Maximum summer precipitation and minimum winter precipitation are the rule in the subequatorial zones and in other regions with monsoon climates, as well as in those areas where there is summer movement of the fronts—the. Climate patterns involving the Indian and Pacific Oceans cause much of East Asia to have temperate weather with a heavy monsoon season, particularly in Eastern China, Hong Kong, Macau, Taiwan, South Korea and most of southern Japan. Much of continental Southeast Asia has a savannah climate similar to some of the drier parts of South Asia, while.
The distribution pattern of precipitation throughout the year is varied. Relatively uniform moisture is characteristic of the Asian equatorial zone. Maximum summer precipitation and minimum winter precipitation are the rule in the subequatorial zones and in other regions asian climate map monsoon climates, as well as in those areas where there is summer movement of the fronts—the polar front in the mountains of southern Siberia and the Arctic front in the subarctic regions. Wet winters and dry summers are typical of the Mediterranean climatic region in West Asiawhere precipitation is associated with the winter activity of the polar front. Asian climate map polar-front activity, accompanied by maximum precipitation, occurs in asian climate map spring in the interior parts of the West Asian highlands. Summer and winter precipitation merges in some parts of Asia.