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During the Triassic period of 251–199.6 Ma, the Indian subcontinent was the part of a vast supercontinent known as Pangaea.Despite its position within a high-latitude belt at 55–75° S—latitudes now occupied by parts of the Antarctic Peninsula, as opposed to India's current position between 8 and 37° N—India likely experienced a humid temperate climate with warm and frost-free weather ...
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The average temperature in summer is about 15 °C (59 °F), and winter temperature is about 2 °C (36 °F). Snowfall occurs in some parts of this region. Being obstructed by the Himalayas, the region receives heavy rainfall. Due to the scenic beauty and temperate climate of the region, a huge number of tourists visit the areas.
Primarily a summer phenomenon, the Bay of Bengal branch of the Indian Monsoon is the major bearer of rain in most parts of Uttar Pradesh. It is the south-west monsoon which brings most of the rain, although rain due to western disturbances [5] and the north-east monsoon also contribute small quantities towards the overall rain in the state. [4]
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The seasonally reversing open ocean currents that pass south of India are referred to as the Winter Monsoon Current and the Summer Monsoon Current (alternately, the Northeast Monsoon Current and the Southwest Monsoon Current). [1] The cold Somali Current, which is strongly linked to the Indian monsoon, is also discussed in this article.