The movement and strength of these jet streams have a direct impact on the Indian monsoon.
The Western Jet Stream (Subtropical Jet Stream): During winter, this jet stream is located south of the Himalayas. Its southward shift is associated with dry and cold weather in North India.
The Easterly Jet Stream (Tropical Easterly Jet): During the summer monsoon season, the Western Jet Stream shifts north of the Himalayas. Simultaneously, a new jet stream, the Tropical Easterly Jet, forms over peninsular India, blowing from east to west. This easterly jet is crucial for bringing monsoon rains to India.
The altitude of 9 to 13 km corresponds to the upper troposphere, where these jet streams are most prominent.