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The European Monsoon (more commonly known as the return of the westerlies) is the result of a resurgence of westerly winds from the Atlantic, where they become loaded with wind and rain. [60] These westerly winds are a common phenomenon during the European winter, but they ease as spring approaches in late March and through April and May.
Alternatively, it can be categorized into two segments based on the direction of rain-bearing winds: Southwest (SW) monsoon; Northeast (NE) monsoon [Note 1] Based on the time of year that these winds bring rain to India, the monsoon can also be categorized into two periods: Summer monsoon (May to September) Winter monsoon (October to November)
Summer monsoon rain over eastern New Mexico. The North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon [1] is a term for a pattern of pronounced increase in thunderstorms and rainfall over large areas of the southwestern United States and northwestern Mexico.
Map legend: Date: March 2007: Source: Own work International Borders: University of Texas map library - India Political map 2001 Disputed Borders: University of Texas map library - China-India Borders - Eastern Sector 1988 & Western Sector 1988 - Kashmir Region 2004 - Kashmir Maps.
Onset dates and prevailing wind currents of the southwest summer monsoons in India. 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. The southwestern summer ...
Of the major monsoon systems, only the North American monsoon is expected to have substantial decreases in total precipitation, with the most likely outcome being a 1%-6% reduction in summer rainfall.
The Australian monsoon (AUM), also known as the Australian summer monsoon (ASM), [2] and the Australian-Indonesian monsoon (AIM), [3] is a monsoon system that increases thunderstorms and rainfall over many areas of Indonesia and northern Australia, from the far northern tropics of the region to the semi-arid zone of Australia, typically between ...
Monsoons play a vital role in managing wildfire threat by providing moisture at higher elevations and feeding desert streams. Heavy monsoon rain can lead to excess winter plant growth, in turn a summer wildfire risk. A lack of monsoon rain can hamper summer seeding, reducing excess winter plant growth but worsening drought.