NCERT Solutions for Class 9 Geography Chapter 4 Climate
NCERT Solutions for Class 9 Social Science Geography Chapter 4 Climate contain answers to the textbook exercise questions. The NCERT solutions are easy and accurate that helps with the questions asked in the examinations. These solutions cover all the questions of the chapter in detail. NCERT Solutions for Class 9 Social Science Geography Chapter 4 are prepared by our subject experts in very easy language. All our solutions are updated as per the latest CBSE Syllabus and Guidelines.
Class 9 Social Science Geography Chapter 4 NCERT Solutions
Question 1: Choose the correct answer from the four alternatives given below.
(i) Which one of the following places receives the highest rainfall in the world?
Answer: (b) Mawsynram
(ii) The wind blowing in the northern plains in summers is known as:
(a) Kaal Baisakhi
(c) Trade Winds
(d) None of the above
Answer: (b) Loo
(iii) Which one of the following causes rainfall during winters in north-western part of India.
(a) Cyclonic depression
(b) Retreating monsoon
(c) Western disturbances
(d) Southwest monsoon
Answer: (a) Cyclonic depression
(iv) Monsoon arrives in India approximately in:
(a) Early May
(b) Early July
(c) Early June
(d) Early August
Answer: (c) Early June
(v) 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
Answer: (c) Cool days and cold nights
Question 2: Answer the following questions briefly.
(i) What are the controls affecting the climate of India?
Answer: The elements affecting the climate are temperature, atmospheric pressure, wind, humidity and precipitation.
(ii) Why does India have a monsoon type of climate?
Answer: India comes in the Inter Tropical Convergence Zone (ITCZ) also with various other factors, like the El Nino, Jet Stream and Coriolois Force are the reasons for monsoon type of climate in India.
(iii) Which part of India does experience the highest diurnal range of temperature and why?
Answer: Northwestern part of India experiences the highest diurnal range of temperature. This happens because of the presence of the Thar Desert and also because this region does not have the moderating influence of the ocean.
(iv) Which winds account for rainfall along the Malabar coast?
Answer: Malabar Coast gets rains from depressions and cyclones.
(v) What are Jet streams and how do they affect the climate of India?
Answer: Jet streams are high velocity westerly winds blowing through a narrow zone in the upper troposphere. The westerly flows are responsible for the western disturbances experienced in the north and north-western parts of the country. The easterly jet streams cause tropical depressions during the monsoon as well as October-November months.
(vi) Define monsoons. What do you understand by “break” in monsoon?
Answer: Monsoon refers to the seasonal reversal in the wind direction. Monsoon ‘break’ refers to the happening of wet and dry spells during the rainy season. The monsoon rains take place only for a few days at a time.
(vii) Why is the monsoon considered a unifying bond?
Answer: Although there are wide variations in weather patterns across India, the monsoon brings some unifying influences on India. The Indian landscape, its flora and fauna, etc. are highly influenced by the monsoon. The entire agricultural calendar in India is governed by the monsoon. Most of the festivals in India are related to agricultural cycle. These festivals may be known by different names in different parts of the country, but their celebration is decided by the monsoon.
Question 3: Why does the rainfall decrease from the east to the west in Northern India.
Answer: The Bay of Bengal branch of the monsoon winds moves towards northeast and return westwards covering the northern plains. While they move towards west, their moisture contains tends to reduce with subsequent rains. Hence the rainfall decreases from east to west in northern India.
Question 4: Give reasons as to why.
(i) Seasonal reversal of wind direction takes place over the Indian subcontinent?
Answer: 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.
Answer: 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 is concentrated over the months of a few months; mainly June to August.
(iii) The Tamil Nadu coast receives winter rainfall.
Answer: 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.
Answer: 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.
Answer: The parts fall in the rain shadow area of the Aravalli. Hence, they are drought prone and don’t receive much of rainfall.
Question 5: Describe the regional variations in the climatic conditions of India with the help of suitable examples.
Answer: Indian Peninsular shows wide variations in climatic conditions across various regions. For example; during winter season, the temperature goes into negative in the Himalayan region. In the northwestern India, temperatures can range between zero degree to 15°C during winter. During the same season, the temperature in Chennai remains a comfortable 25°C. The same variation can be seen in summer as well, while the temperature in Rajasthan can hover around 47°C, it is a comfortable 30°C in Chennai.
Question 6: Discuss the mechanism of monsoons.
Answer: The low-pressure condition over the northern plains intensifies by the beginning of June. It attracts the trade winds from the southern hemisphere. These south-east trade winds cross the equator and blow in a south-westerly direction to enter the Indian peninsula as the south-west monsoon. These winds bring abundant moisture to the subcontinent.
Following are the factors responsible for the mechanism of monsoon:
- The Sun causes differential heating and cooling of land and water. This creates low pressure on the landmass of India and high pressure over the ocean surface.
- The Inter Tropical Convergence Zone (ITCZ) is normally positioned about 5°N of the equator. It shifts over the Ganga plains during summer. It is also known as the monsoon trough during the monsoon season.
- The high pressure area, east of Madagascar is approximately 20°S over the Indian Ocean. This area affects the Indian Monsoon.
- The Tibetan plateau gets intensely heated during summer. This results in strong vertical air currents and formation of high pressure over the plateau. This high pressure zone is about 9 km above the sea level.
- The westerly jet stream move to the north of the Himalayas, and the tropical easterly jet stream moves over the Indian Peninsula during summer.
- The periodic change in pressure conditions between Pacific Ocean and the Indian Ocean that is known as the Southern Oscillation or SO also affects the monsoon.
- The difference in pressure over Tahiti and Darwin is computed to predict the intensity of the monsoons. Tahiti (18°S/149°W) lies in the Pacific Ocean and Darwin (12°30’S/131°E) lies in northern Australia. If the pressure differences are negative, it means a below average and late monsoon.
Question 7: Give an account of weather conditions and characteristics of the cold season.
Answer: The temperature ranges between 10°-15°C in the northern plains. The weather is usually marked by clear sky, low temperatures and low humidity and feeble variable winds. The inflow of the cyclonic disturbances from the west and the northwest is a characteristic feature of the cold weather over the northern plains. These low-pressure systems originate over the Mediterranean Sea and Western Asia and move into India. They cause winter rains over the plains and snowfall in the mountains.
Question 8: Give the characteristics and effects of the monsoon rainfall in India.
Answer: Characteristics of the monsoon rainfall in India:
- The duration of the monsoon varies from 100 to 120 days from early June to mid- September.
- Around the time of its arrival, the normal rainfall increases suddenly and continues regularly for several days. This is called the ‘burst’ of the monsoon.
- They are distinguished from the pre-monsoon showers because of their increase in rainfall amount and regularity.
- The monsoon arrives at the southern tip of the Indian Peninsular generally by the first week of June.
- The rainfall is unevenly distributed across the country.
Effects of the monsoon rainfall in India:
- Agriculture in India largely depends on Indian monsoons for water. Late, Low or excessive rains have a negative impact upon crops.
- Due to uneven distribution of rainfall across the country, there are few places that are drought prone and few are flood affected.
- The monsoon provides India with a diverse climatic pattern. Hence, in spite of the presence of great regional variations, it has a unifying influence upon the country and its people.