10 Facts About Northeast monsoon

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

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

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

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

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

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

However, the Northeast 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 Northeast monsoon occurs in the southern summer when the Northeast monsoon trough develops over Northern Australia.

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