Match the atmospheric pressure systems and circulation features associated with the Indian monsoon mechanism listed in List-I with their corresponding meteorological characteristics and roles described in List-II. Which of the following represents the correct set of pairings?
- Mascarene HighSemi-permanent subtropical high-pressure cell located near 30°S in the southern Indian Ocean, serving as the primary source region for cross-equatorial monsoon flow.
- Tibetan AnticycloneWarm-core upper-tropospheric high-pressure system generated by intense summertime sensible heating and latent heat release over the plateau.
- Somali Jet (Findlater Jet)Low-level cross-equatorial wind stream off the East African coast that accelerates moisture transport into the Arabian Sea branch.
- Tropical Easterly Jet (TEJ)Upper-tropospheric wind stream centered around 13°N latitude whose strength directly modulates monsoon rainfall intensity over peninsular India.
Cevap
Mascarene High pairs with the semi-permanent subtropical high-pressure cell near 30°S in the southern Indian Ocean; Tibetan Anticyclone pairs with the warm-core upper-tropospheric high-pressure system over the plateau; Somali Jet pairs with the low-level cross-equatorial wind stream off East Africa; and Tropical Easterly Jet pairs with the upper-tropospheric wind stream at 13°N latitude.
The correct pairings accurately link each monsoon circulation component to its distinct altitude layer and physical role: the Southern Hemisphere Mascarene High drives low-level cross-equatorial flow; the Tibetan Anticyclone provides upper-level divergence; the Somali Jet serves as the low-level moisture highway across the Arabian Sea; and the Tropical Easterly Jet maintains upper-tropospheric easterly momentum over peninsular India.
Adım Adım Çözüm
Anahtar Kavram
Indian Monsoon Atmospheric Driving Mechanisms and Pressure Systems
Tahmini Süre:2m 0s