Question

what is the difference between monsoon trough and monsoon axis​

Answer 1

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The monsoon trough is a portion of the Intertropical Convergence Zone in the Western Pacific, as depicted by a line on a weather map showing the locations of minimum sea level pressure, and as such, is a convergence zone between the wind patterns of the southern and northern hemispheres.

Answer 2

Answer:

Explanation:

Monsoon troughing in the western Pacific reaches its zenith in latitude during the late summer when the wintertime surface ridge in the opposite hemisphere is the strongest. It can reach as far as the 40th parallel in East Asia during August and the 20th parallel in Australia during February. Its poleward progression is accelerated by the onset of the summer monsoon which is characterized by the development of lower air pressure over the warmest part of the various continents.[4][5][6] In the Southern Hemisphere, the monsoon trough associated with the Australian monsoon reaches its most southerly latitude in February,[7] oriented along a west-northwest/east-southeast axis.