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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.
Print/export Download as PDF; Printable version; ... File:Blank Asia.png: Map of Asia without national borders. Asia98.svg: national primary level divisions as of 1998.
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 ...
Blue = Central Asia; Yellow = East Asia (China, Mongolia, Korea, Japan) Brown = West Asia/Middle East; Green = South Asia (India, Pakistan, Bangladesh, Nepal, Bhutan) Red = South East Asia (10 ASEAN countries + East Timor) Date: 5 May 2007 (original upload date) Source: Own work based on the blank world map: Author
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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.
The Asiatic Low is a low-pressure trough which lies over southern Asia, during early summer. It is located roughly over India, heading over the Bay of Bengal. It is a major action centre for the Northern Hemisphere during that time of the year. [1] It is created by more intense July sun, causing desert land areas of Northern Africa and Asia to ...