(i) Which one of the following places receives the highest rainfall in the world?
(a) Silchar
(b) Mawsynram
(c) Cherrapunji
(d) Guwahati
Ans: (b) Mawsynram
(ii) The wind blowing in the northern plains in summers is known as:
(a) Kaal Baisakhi
(b) Loo
(c) Trade Winds
(d) None of the above
Ans: (b) Loo
(iii) Monsoon arrives in India approximately in:
(a) Early May
(b) Early July
(c) Early June
(d) Early August
Ans: (c) Early June
(iv) Which one of the following characterises the cold-weather season in India?
(a) Warm days and warm nights
(b) Warm days and cold nights
(c) Cool days and cold nights
(d) Cold days and warm nights
Ans: (b) Warm days and cold nights
(i) What are the controls affecting the climate of India?
Ans: There are six major controls of the climate of any place. They are:
(ii) Why does India have a monsoon type of climate?
Ans: India has a monsoon type of climate because the climate of India is governed by the monsoon winds which are limited between 20° North and 20° South.
(iii) Which part of India does experience the highest diurnal range of temperature and why?
Ans: The Indian desert, located in the north-western part of India experiences the highest diurnal range of temperature because of the sand which is present there, quickly becomes hot during the day and cools down rapidly during night.
(iv) Which winds account for rainfall along the Malabar Coast?
Ans: Malabar Coast gets rains from South-West Monsoon Winds.
(v) Define monsoons. What do you understand by “break” in monsoon?
Ans:
(vi) Why is the monsoon considered a unifying bond?
Ans: The monsoon is considered a unifying bond because:
Q3. Why does the rainfall decrease from the east to the west in Northern India?
Ans:
(i) Seasonal reversal of wind direction takes place over the Indian subcontinent?
Ans: Seasonal reversal of wind direction over the Indian subcontinent takes place due to pressure differential. El Nino has major role to play in the seasonal reversal of wind direction over the Indian subcontinent.
(ii) The bulk of rainfall in India is concentrated over a few months.
Ans: The monsoon begins from the first week of June and advances quite rapidly to cover almost the whole country by mid-July. Hence, the bulk of rainfall in India concentrated over the months of a few months; mainly June to August.
(iii) The Tamil Nadu coast receives winter rainfall.
Ans: The Tami Nadu coast receives winter rainfall because of movement of low-pressure conditions to the Bay of Bengal.
(iv) The delta region of the eastern coast is frequently struck by cyclones.
Ans: The Bay of Bengal is the centre of various pressure changes and hence there is always a chance of development of cyclone. Due to this, the delta region of the eastern coast is frequently struck by cyclones.
(v) Parts of Rajasthan, Gujarat and the leeward side of the Western Ghats are drought-prone.
Ans:
Q5. Describe the regional variations in the climatic conditions of India with the help of suitable examples.
Ans:
Q6. Give an account of weather conditions and characteristics of the cold season.
Ans: Following are the features of the cold season:
Q7. Give the characteristics and effects of the monsoon rainfall in India.
Ans: Characteristics of the monsoon rainfall in India:
Effects of the monsoon rainfall in India:
Q. On an outline map of India, show the following.
(i) Areas receiving rainfall over 400 cm.
(ii) Areas receiving less than 20 cm of rainfall.
(iii) The direction of the south-west monsoon over India.
Ans:
(i) The Western Coast and North Eastern India receives rainfall over 400 cm. Mawsynram and Cherrapunji in Meghalaya are known for receiving maximum rainfall in the world. The Andaman Islands and Lakshadweep Islands are also known to receive annual rainfall above 400 cm.
(ii) The parts of Northern Kashmir, Western Rajasthan, Deccan plateau and Punjab are known to be the areas that receive scanty rainfall that is less than 20 cm. In Northern part of India, rainfall decreases toward the west, while in the peninsular region except for Tamil Nadu, the rainfall decreases eastwards.
(iii) South west monsoon is a compound and a self-evolved weather system unique to Indian subcontinent. The south west monsoon in India moves in south-west direction. In India there are only south-west and north-east monsoons. Because of the corol is effect, the south-east monsoon becomes south west trade winds.
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