11 Facts About Southwest monsoon

Usually, the term Southwest monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is a dry phase.

The English Southwest monsoon came from Portuguese ultimately from Arabic, "perhaps partly via early modern Dutch monson".

The Southwest monsoon has varied significantly in strength since this time, largely linked to global climate change, especially the cycle of the Pleistocene ice ages.

The North American monsoon is known to many as the Summer, Southwest, Mexican or Arizona monsoon.

Influence of the Southwest Monsoon is felt as far north as in China's Xinjiang.

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The effects extend westwards to the Mediterranean, where however the impact of the Southwest monsoon is to induce drought via the Rodwell-Hoskins mechanism.

Meanwhile, a low pressure system known as a Southwest monsoon trough develops over South-East Asia and Australasia and winds are directed toward Australia.

East Asian Southwest monsoon affects large parts of Indochina, the Philippines, China, Taiwan, Korea and Japan.

However, the Southwest monsoon is not a simple response to heating but a more complex interaction of topography, wind and sea, as demonstrated by its abrupt rather than gradual withdrawal from the region.

The Australian Southwest monsoon occurs in the southern summer when the Southwest monsoon trough develops over Northern Australia.

The European Southwest monsoon is not a Southwest monsoon in the traditional sense in that it doesn't meet all the requirements to be classified as such.