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3)Indian summer monsoon. The Indian summer monsoon typically lasts from June-September (Fig. 58d), with large areas of western and central India receiving more than 90% of their total annual precipitation during the period, and southern and northwestern India receiving 50%-75% of their total annual rainfall.
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1.) Pre monsoon showers are know as mango showers in telangana and Andhra.
3.) The south-west monsoon causes over 80% of the rainfall over the country from June to September. The south-west monsoon originates from the Indian Ocean. The south-west monsoon is divided into two branches: Arabian sea branch and Bay of Bengal branch.
2.) The eastern jet becomes powerful and is stationed at 15° N latitude. The easterly winds in the lower troposphere.
4.) Chennai Bay of Bengal sea is warmer. This would mean direct impacts on sea water current, atmospheric pressure, atmospheric temperature and uneven tropical rainfalls.
5.) the temperature gradient in each layer is determined by the heat source of the layer. most of the important progresses of the atmosphere take place in the lowest two layers: the temperature of the troposphere is highest near the surface of the earth and decrease with altitude.
6.) the surface air that flows from these subtropical high-pressure belts toward the equator is deflected toward the west in both hemispheres by the Coriolis effect. These winds blow predominantly from the the northeast in the Northern hemisphere and from the southeast in the southern hemisphere.
7 and 8 don't know....
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