Assay on floods and dought
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Answer:
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eastern states of Assam, Arunachal Pradesh, Meghalaya, and Nagaland, etc. receive very heavy rainfall.
The Indian sub-continent has a distinct geographical and historical identity. Its territories extend 3,214 kilometers between the extremes of the north and the south, and 2,933 kilometers between those of the east and the west. This vast landmass called India has been a playground of the monsoon from times immemorial. Monsoon is the seasonal wind of the Indian Ocean. By the end of the month of May, a low pressure is formed in the coastal plains in the west of India which attracts the monsoon winds and then there are occasional rains. In early June, the low pressure builds up heavily over north-western parts of the country and then the south-west rain bearing winds rush to the area with thunder, lightning and showers. By the beginning of July, these monsoon winds cover almost the entire country.
The intense heat of northern plains creates a low pressure area but the oceanic region maintains its low temperature and high pressure centre. Consequently, rain bearing winds, originating in the Indian Ocean, start blowing from the high pressure zone to the low pressure region over the vast landmass of India and then there are rains till September. The part of the monsoon winds from the Bay of Bengal move towards the plains of Ganga and Brahmaputra and cause heavy rains in West Bengal, Assam, Arunachal Pradesh and other neighboring states of the sub-Himalayan region and the northern plains. But the distribution of rainfall is highly unequal. The Indian rains are erratic and ill-distributed,, which causes frequent floods and droughts.
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Free sample essay on Drought and Flood in India. The rainfall in India varies from place to place and year to year. The north-eastern states of Assam, Arunachal Pradesh, Meghalaya, and Nagaland, etc. receive very heavy rainfall.
The Indian sub-continent has a distinct geographical and historical identity. Its territories extend 3,214 kilometers between the extremes of the north and the south, and 2,933 kilometers between those of the east and the west. This vast landmass called India has been a playground of the monsoon from times immemorial. Monsoon is the seasonal wind of the Indian Ocean.
By the end of the month of May, a low pressure is formed in the coastal plains in the west of India which attracts the monsoon winds and then there are occasional rains. In early June, the low pressure builds up heavily over north-western parts of the country and then the south-west rain bearing winds rush to the area with thunder, lightning and showers. By the beginning of July, these monsoon winds cover almost the entire country.
The intense heat of northern plains creates a low pressure area but the oceanic region maintains its low temperature and high pressure centre. Consequently, rain bearing winds, originating in the Indian Ocean, start blowing from the high pressure zone to the low pressure region over the vast landmass of India and then there are rains till September.
The part of the monsoon winds from the Bay of Bengal move towards the plains of Ganga and Brahmaputra and cause heavy rains in West Bengal, Assam, Arunachal Pradesh and other neighboring states of the sub-Himalayan region and the northern plains. But the distribution of rainfall is highly unequal. The Indian rains are erratic and ill-distributed,, which causes frequent floods and droughts.