Monsoon type of climate is found in India, the word monsoon is derived from the word which means the direction of the winds, today according to the weather,
the change of the Arabian Sea and Bengal in India.The climate of India is of that monsoon type, but the fact to be noted is that the northern part of India which is located north of the Tropic of Cancer is in the temperate zone and the part located south of the Tropic of Cancer is in that zone.
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Indian Monsoon
The Indian monsoon is mainly related to the changes in atmospheric circulation during the summer season.
From the beginning of summer, the sun begins to turn north.
With the north of the sun, the inter-tropical convergence zone ITCZ also begins to turn north, due to its effect, the paschimi jet stria It starts flowing in the north of the Himalayas and in the Indian subcontinent, due to the high temperature, low air pressure develops.
After the displacement of the western jet stream to the north of the Himalayas, the eastern jet stream develops in India, its position varies according to the season in about 15 to 30 degrees north latitude, it is considered as Indian.It is believed to be mainly responsible for the Bharti monsoon blast.
Due to the influence of the easterly jet stream, high pressure develops in the south Indian Ocean near the island of Madagascar, from this center of high air pressure, the southwest monsoon originates.
स्थानापन्न वस्तु/substitute goods
अपूर्ण प्रतियोगिता/कीमत नेतृत्व मॉडल/imperfect competition
वैदिक काल|महावीर (वर्धमान)|महात्मा बुद्ध/Vedic Period ,
Intertropical Convergence Zone (ITCZ)
Intertropical Convergence Zone (ITCZ) The Trans-tropical Convergence Zone on the equator is a low pressure area where trade winds are found in the month of July around ITC Z 20 to 25 Arms North Latitudes.It is situated in the surrounding Gangetic plain,
it is also sometimes called monsoon trough.This monsoon trough encourages the development of thermal low pressure over north and northwest India.
Due to the northward movement of ITCZ, the trade winds of the Southern Hemisphere cross the middle of the 40 degrees east longitude Under the influence of the Coriolis force, the direction of these trade winds crossing the equator becomes from southwest to northeast.This is the South West Monsoon. In winter,
ITCZ shifts to the South, according to this, the direction of the winds changes from South-West to North-East. This is the North East Monsoon.
