1. . (i) Cold weather season normally takes place from December to February (ii) Temperature keeps on decreasing. (iii) Average temperature is between 10' to 20' C. (iv) Days are warm and nights are cold. (v) North East trade winds blow from land to sea, which are incidentally cold and dry. (vi) We preRead more

    . (i) Cold weather season normally takes place from December to February
    (ii) Temperature keeps on decreasing.
    (iii) Average temperature is between 10′ to 20′ C.
    (iv) Days are warm and nights are cold.
    (v) North East trade winds blow from land to sea, which are incidentally
    cold and dry.
    (vi) We prefer to wear woollen clothes and like to sit under the Sun.

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  2. (i) With the arrival of monsoon, the normal rainfall increases suddenly and carries on for several days. (ii) This is also known as 'burst of monsoon' and can be distinguished from the pre-monsoon showers. (iii) The monsoon arises at Southern tip of Indian peninsula generally, by the first week of JRead more

    (i) With the arrival of monsoon, the normal rainfall increases suddenly and
    carries on for several days.
    (ii) This is also known as ‘burst of monsoon’ and can be distinguished from
    the pre-monsoon showers.
    (iii) The monsoon arises at Southern tip of Indian peninsula generally, by the
    first week of June approximately.
    (iv) Then it gets divided into two-The Arabian sea branch and Bay of
    Bengal branch.
    (v) Then it starts moving upwards, the Arabian Sea branch reaches Madhya
    Pradesh/U.P. in about ten days.
    (vi) The Bay of Bengal branch also advances rapidly and arrives in Assam in
    the first week of June.

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  3. . (i) western Rajasthan and part of Gujarat are desert type regions with extreme climate. Intense thermal heating makes the desert land very dry. (ii) The Arabian Sea branch runs parallel to Aravallis, providing no barriers to the clouds, leaving it again a dry region. (iii) The Bay of Bengal branchRead more

    . (i) western Rajasthan and part of Gujarat are desert type regions with
    extreme climate. Intense thermal heating makes the desert land very
    dry.
    (ii) The Arabian Sea branch runs parallel to Aravallis, providing no barriers
    to the clouds, leaving it again a dry region.
    (iii) The Bay of Bengal branch is unable to reach up to western part and
    in winters even western disturbances also hardly give any rains to this
    region.
    (iv) The leeward side of the western Ghats also lies in the rain shadow of
    S.W. monsoon.
    (v) With the result, areas lying at the same latitude are unable to receive
    rains, if they are on the leeward side of the Western Ghats.

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  4. (i) The northern plains receive rains from the Bay of Bengal branch of the S.W. monsoons. (ii) It strikes the Myanmar's Arkan mountains and gets deflected westward along the Himalayas. (iii) Maximum precipitation is recorded in the north-eastern part of India and West Bengal. (iv) As the monsoon movRead more

    (i) The northern plains receive rains from the Bay of Bengal branch of the
    S.W. monsoons.
    (ii) It strikes the Myanmar’s Arkan mountains and gets deflected westward
    along the Himalayas.
    (iii) Maximum precipitation is recorded in the north-eastern part of India
    and West Bengal.
    (iv) As the monsoon moves westwards, they gradually lose moisture and
    rainfall decreases from east to west over the northern plains.
    (v)The clouds are almost exhausted by the time they reach western
    Rajasthan.

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  5. (i) Diurnal range of temperature is the difference between maximum and minimum temperature of a day. (ii) Diurnal range of temperature is high in desert regions like Rajasthan, Thar Desert and interior parts of Rann of Kutch. (iii) In these sandy areas, the day temperature may rise to 50' and drop dRead more

    (i) Diurnal range of temperature is the difference between maximum and
    minimum temperature of a day.
    (ii) Diurnal range of temperature is high in desert regions like Rajasthan,
    Thar Desert and interior parts of Rann of Kutch.
    (iii) In these sandy areas, the day temperature may rise to 50′ and drop
    down to near freezing point the same night’
    (iv) It is so because the sand absorbs heat very fast during day and loses heat
    very fast at night.

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