Question

How is the Air Mass Theory related to the monsoon winds?

Answer 1

Hint: Noticed at first by mariners in the Arabian Seagoing between Africa, India, and Southeast Asia, the rainstorm can be classified into two branches dependent on their spread over the subcontinent: Arabian Sea branch Bay of Bengal branch.

Complete answer:
The southeast exchange winds the southern half of the globe and the upper east exchange winds the northern half of the globe meet each other close to the equator. The gathering spot of these breezes is known as the Inter-Tropical Convergence Zone (ITCZ).
Satellite symbolism uncovers that this is the area of rising air, the greatest mists, and substantial precipitation. The area of ITCZ moves north and south of the equator with the difference in the season. In the mid-year season, the sun sparkles vertically over the Tropic of Cancer, and the ITCZ moves northwards.
The southeast exchange winds of the southern half of the globe cross the equator and begin moving from southwest to upper east bearing affected by Coriolis power These uprooted exchange winds are called south-west rainstorm when they blow over the Indian sub-landmass. The front where the south-west rainstorm meets the north-east exchange winds is known as the Monsoon Front
Storms normally happen in tropical territories.
One zone that rainstorms sway enormously in India. In India storms make a whole season wherein the breezes turn around totally. The precipitation is an aftereffect of the combination of wind stream from the Bay of Bengal and converse breezes from the South China Sea. The beginning of the storm happens over the Bay of Bengal in May, showing up at the Indian Peninsula by June, and afterward, the breezes move towards the South China Sea.

Note:The southwest exchange twists over the southern half of the globe, crosses the equator and begins moving from Southwest toward the upper east heading affected by Coriolis power. These uprooted exchange winds are called southwest storms when they blow over India's subcontinent.