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The 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.
The East Asian monsoon is a monsoonal flow that carries moist air from the Indian Ocean and Pacific Ocean to East Asia.It affects approximately one-third of the global population, influencing the climate of Japan, the Korean Peninsula, Taiwan, China, the Philippines and Mainland Southeast Asia but most significantly Vietnam.
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. The southwestern ...
Image:China blank map-1.png – People's Republic of China; Image:China blank map-2.png – People's Republic of China; Image:Hong Kong District Locator (template map).png – Hong Kong Special Administrative Region of the People's Republic of China. Image:BlankMap-Philippines.png
For a detailed map of all disputed regions in South Asia, see Image:India disputed areas map.svg Internal borders The borders of the state of Meghalaya, Assam and Arunachal Pradesh are shown as interpreted from the North-Eastern Areas (Reorganisation) Act, 1971, but has yet to be verified.
Manchurian or monsoon continental climate in the world. The Monsoon continental climate, also known as Manchurian climate, is a continental climate sub-type. It is a monsoon climate with large thermal range. It is located mainly in East Asia, Korea and Manchuria. Its dry season happens during the winter ("Dw" meaning "Dry Winter").
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A monsoon (/ m ɒ n ˈ s uː n /) is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation [1] but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator.