Q1. Which of the following statements most accurately explains the nature, dynamics, and regional implications of jet streams, particularly in the context of South Asian monsoon behavior and extreme weather events?
- (a) Jet streams are permanent low-level winds flowing parallel to the equator, and their seasonal shift has no significant influence on Indian monsoon onset or withdrawal.
- (b) The Tropical Easterly Jet (TEJ) and Subtropical Westerly Jet (STWJ) are upper tropospheric winds whose seasonal dominance over the Indian subcontinent strongly influences the monsoon cycle, with the STWJ facilitating active monsoon conditions.
- (c) The Subtropical Westerly Jet retreats northward during summer, allowing the Tropical Easterly Jet to dominate, which aids monsoon onset, whereas the presence of STWJ over India during summer can suppress monsoon activity.
- (d) Jet streams have no role in mid-latitude cyclones or upper-air divergence, and their impact is confined to aviation and turbulence rather than synoptic-scale weather systems.
Answer & solution
Answer: (c) The Subtropical Westerly Jet retreats northward during summer, allowing the Tropical Easterly Jet to dominate, which aids monsoon onset, whereas the presence of STWJ over India during summer can suppress monsoon activity.
The Subtropical Westerly Jet sits south of the Himalayas in winter; its shift north of the Himalayas by early June lets the Tropical Easterly Jet establish itself and is the trigger for the monsoon burst.
Option 2 fails on its last clause — the STWJ suppresses, not facilitates, the monsoon when it lingers over north India.
Revision note — Jet streams and the Indian monsoon
• A jet stream is a narrow band of fast upper-tropospheric westerly wind at about 9–14 km height, blowing west to east at more than 120 km/h.
• The Subtropical Westerly Jet (STWJ) lies at about 25°–30° N, south of the Himalayas, in winter; it steers western disturbances from the Mediterranean into north-west India.
• In summer the STWJ moves north of the Tibetan plateau.
• The Tropical Easterly Jet (TEJ) then forms at about 15° N over peninsular India at 14–16 km, blowing east to west, strengthened by the heating of the Tibetan plateau.
• The return of the STWJ south of the Himalayas in autumn induces subsidence over north-west India and helps the monsoon withdraw.
• The Somali (Findlater) jet is a low-level cross-equatorial jet that carries moisture across the Arabian Sea toward the Kerala coast.
• The role of jet streams in the monsoon was stressed by Koteswaram and Flohn; jet streams also feed upper-air divergence that deepens mid-latitude cyclones.
Do not mix these up
• STWJ vs TEJ — the STWJ blows west to east and dominates winter; the TEJ blows east to west and dominates the summer monsoon.
• Western disturbances vs monsoon rain — western disturbances bring winter rain to north-west India along the westerly jet; the monsoon is a summer system.
Also asked from this topic: the direction of jet streams over India in winter (west to east); how the subtropical jet aids monsoon withdrawal (subsidence over land).