The Indian summer monsoon circulation features several characteristic jet streams: the low-level Somali Jet, the upper-tropospheric Tropical Easterly Jet (TEJ), and the Subtropical Westerly Jet, each with distinct heights, source regions, and latitudinal positions.
The Somali Jet is indeed centred near 1.5 km height (low-level jet), the Subtropical Westerly Jet is climatologically located near 25 degrees N, and the...
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