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Class 9 Geography Chapter 4 Climate NCERT Solution (English Medium)

NCERT Exercise

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?

(a) Silchar (c) Cherrapunji

(b) Mawsynram (d) Guwahati

Ans. (b) Mawsynram

(ii) The wind blowing in the northern plains in summers is known as:

(a) Kaal Baisakhi (c) Trade Winds

(b) Loo (d) None of the above

Ans. (b) Loo

(iii) Which one of the following causes rainfall during winters in north-western part of India.

(a) Cyclonic depression (c) Western disturbances

(b) Retreating monsoon (d) Southwest monsoon

Ans. (c) Western disturbances

(iv) Monsoon arrives in India approximately in:

(a) Early May (c) Early June

(b) Early July (d) Early August

Ans. (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

Ans. (b) Warm days and cold nights

2. Answer the following questions briefly.

(i) What are the controls affecting the climate of India?

Ans. India’s climate is strongly influenced by the Himalayas and the Thar Desert. Monsoon winds, geographical location of the country, winds blown from the West and other relief features of the earth plays a great role in directing the climate of India.

There are the following factors affecting the climate of India:


(i) Monsoon winds: India's climate is controlled by monsoon winds. In summer, monsoons are on shore winds. These winds give most of rainfall to the country. In winter the monsoon winds blow from land to sea as N.E. Monsoons. These are dry winds.


(ii) Extent of the country: India is a vast country. The northern part lies in the temperate region and experiences hot summers and cool winters. The southern part lies nearer the equator and has hot season throughout the year.


(iii) Location of the Himalayas: The Himalayas act as a climatic barrier. This mountain wall protects India from the cold winds of Central Asia in winter. The Himalayas check the on-shore. S.W. Monsoons and force these to give rainfall.


(iv) The Indian Ocean: India lies at the head of the Indian Ocean. S.W. Monsoons originate from this ocean in summer and give rainfall over most of the country. Cyclones also originate over this ocean.


(v) The western disturbances: The western disturbances (cyclones) originate from the Mediterranean Sea and enter India in winter. They are responsible rainfall in north-western parts of India in winter.


(vi) Distance from the sea: The coastal areas experience marine climate. Generally, these areas have equable climate, but the interior regions experience extreme or continental type of climate, e.g. north-west India.


(vii) Relief of the land: Relief influences the distribution of temperature and rainfall in India. Mountainous areas have low temperatures. The windward slopes such as Western Ghats receive heavy rainfall while the leeward slopes (Deccan Plateau) lie in the rain-shadow and are dry.

(ii) Why does India have a monsoon type of climate?

Ans. India has a monsoon type of climate because:

(i) It is strongly directed by the monsoon winds during June to September.

(ii) Monsoon season in India is further divided into Pre-monsoon, monsoon and post-monsoon seasons.

(iii) India exists in the tropical and sub-tropical area. Half of its area located at the south to the Tropic of Cancer 23°30’N.

(iv) The atmospheric conditions, surface winds, upper air circulation, western disturbances and tropical cyclones play a significant role in controlling the climate of the country.

(v) The climate of India is strongly influenced by monsoon winds. India has a monsoon type of climate due to its geographical location.

(iii) Which part of India does experience the highest diurnal range of temperature and why?

Ans. The north-western parts of India, like Haryana, Punjab, Rajasthan, UP., Delhi, experience diurnal temperature. Here the temperature goes up to 48 Celsius. This happens because the low-pressure conditions intensify the north-western parts during May-June. Hot, dry winds namely Loo, starts blowing and dust storms spurt as south-westerly winds blow violently to compensate the low pressure condition formed in north-western parts of the country.

The north-western India is surrounded by the desert. The desert sand becomes hot during the day and quickly cools down in the night which affects the daytime temperature of the neighboring regions.

(iv) Which winds account for rainfall along the Malabar Coast?

Ans. Malabar coast in the southwest of India received very high account about 250 cms of rainfall due to the Southwest monsoon (the Arabian Sea branch of monsoon). When the Southwest monsoon heat the Malabar coast, the western ghat’s elevation work as a barrier in the way of monsoon winds and clouds. So Malabar coast received the high amount of rainfall. Although the leeward side of the western ghat comes in rain shadow zone during the onwards of Southwest Monsoon winds.

(v) What are Jet streams and how do they affect the climate of India?

Ans. Jet streams are high-velocity westerly winds blowing through a narrow zone, around 12,000 meters over the troposphere. These are actually, westerly winds blowing at higher altitude. Their velocity (speed) recorded in summer is about 110 km/h and about 184 km/h. in winter. These blow at the mid-latitude and over sub-tropical regions (north half of India).

These streams are located over 27-30° north latitude. The westerly flows are responsible for western disturbances and the easterly flows cause tropical depressions during monsoon and even in early winter season.

(vi) Define monsoons. What do you understand by “break” in monsoon?

Ans. Monsoons are generally rain bearing and directing winds. This term has been derived from the Arabic word "mausim” first used by the Arab traders who used to visit India for trading purposes through sea routes. It means season. We therefore, can state them seasonal reversal of the wind system in monsoon.

"Monsoon Break refers to the happening of wet and dry spells during the rainy season. Monsoon rains take place only for a few days at a time. They are interspersed with rainless intervals. The monsoon rains take place for a few days continuously with some rainless breaks. These wet and dry spells of the monsoon rains is termed as monsoon break.

(vii) Why is the monsoon considered a unifying bond?

Ans. The term "unifying bond" implies an attachment or affection of something with another. India has a unique combination of seasons. The different parts of the country experience different climates during the same time. The location of Himalayas in the northern India acts as a barrier that saves the country from the strong cold winds of the Central Asia. The other places with the same latitude experience extremely cold winds. In the same way, the peninsular India is covered by the seas from three sides. This arrangement also makes sure a moderate temperature in India. India is a country where people belonging to different ethnicities live together. India is an epitome of Unity in Diversity. Though different parts of the country have different climate in the same time, but Monsoon is a period which happens to come around the same time every years. The seasonal reversal of the wind system provides a rhythmic cycle of seasons. Indian festivities, plant and animal lives, agricultural calendar, etc. share close ties with the monsoon. Hence, monsoon acts as a unifying bond in India.

3. Why does the rainfall decrease from the east to the west in Northern India.

Ans. The rainfall decreases from east to the west in Northern India because monsoon rises from both the Arabian Sea and the Bay of Bengal, which causes heavy rainfall in the Brahmaputra valley and the Assam hills. As soon as they move toward Himalayas they take western turn and move up the Ganga valley, but due its westward approach it become drier and drier resulting in lesser rainfall North West India. The shrinking moisture levels results in decrease in rainfall from east to the west.

4. Give reasons as to why.

(i) Seasonal reversal of wind direction takes place over the Indian subcontinent?

Ans. In winters, the sun moves toward the south, the low pressure channel over the northern plains becomes feebler causing the monsoon wind to blow from northeast to south during this period. During summers, low pressure area develops in the interior of Asian continent impacting the North-Western India. Because of this sea begin to blow toward the landmasses. The shift in the progress of monsoon combined with the variation in season causes reversal of wind direction in the Indian sub-continent.

(ii) The bulk of rainfall in India is concentrated over a few months.

Ans. The bulk of rainfall in India is received during the four months of the rainy season i.e. June, July, August and September. This is the period of South-West Monsoons blowing from sea to land. These seas to land winds are the rain giver, as these moisture-laden winds are on-shore winds. The tropical cyclones add to the amount of rainfall. Easterly tropical jet stream, too, helps in the monsoonal rain during this period.

(iii) The Tamil Nadu coast receives winter rainfall.

Ans. Konkan Coast faces On-Shore South West Monsoons during summer. The moist laden winds cause heavy rainfall (more than 250 cms). But these winds do not result in heavy rainfall on the Coromandel Coast lies on the east of Eastern Ghats. Coromandel Coast also receives winter rainfall from North Eastern Monsoons, but on Konkan Coast these winds are off-shore and do not result in rainfall. Thus Coromandel Coast gets rainfall in both the seasons, but the total amount is less than that of Konkan Coast.

Tamil Nadu gets most of rain from North-Eastern Monsoons in October, November and December. These Winds after picking up moisture from Bay of Bengal fetch more rain on the eastern coast. This is why; Tamil Nadu receives rain in winter when the fury of monsoons is over in most parts of the country.

(iv) The delta region of the eastern coast is frequently struck by cyclones.

Ans. Tropical cyclones are depressions originating over Bay of Bengal. These tropical cyclones are often destructive. They cause heavy rains. These cyclones strike West Bengal and Bangladesh (Ganga Delta). They cross the Eastern coast and affect the states of Orissa, Andhra Pradesh, Tamil Nadu and Kerala. The thickly populated deltas of Mahanadi, Godavari, Krishna and Kaveri are the main targets of these tropical cyclones. Likely MOCHA Cyclone struck the eastern coast in May 2023.

(v) Parts of Rajasthan, Gujarat and the leeward side of the Western Ghats are drought-prone.

Ans. The western part of Rajasthan is desert. It gets an annual rainfall less than 20 cms. Rajasthan is under the influence of South West Summer monsoons. The Aravallis system lies parallel to the direction of South West monsoons coming from Arabian Sea. So these low mountain system is unable to check these winds, so western Rajasthan is practically dry. The southern parts get some rainfall. This area lies at a great distance from the Bay of Bengal. The Bay of Bengal monsoons become dry and lose their moisture when they reach Rajasthan. Also, Rajasthan and Gujarat are at a great distance from the Himalayan region so, they do not come under the influence of monsoons giving rain in the sub-Himalayan region. The leeward slopes of Western Ghats remain in rain-shadow, but there is no guarantee of rainfall hence, this area also comes under the drought prone areas of the country.

5. Describe the regional variations in the climatic conditions of India with the help of suitable examples.

Ans. In India, there are perceptible regional variations in climatic conditions within the country.

(i) In summer, the temperature may be 50°C or more in some parts of Rajasthan desert, whereas it may be around 20°C in Pahalgam in Jammu and Kashmir. On a winter night, the temperature at Dassin Jammu and Kashmir may be as low as -45°C, while Thiruvananthapuram may have a temperature of +20°C.

(ii) In certain places there is a wide difference between day and night temperatures. In the Thar Desert, the day temperature may be 50°C and drops down to near freezing point the same night. On the other hand, there is hardly any difference between day and night temperatures in the Andaman and Nicobar Islands or in Kerala.

(iii) While precipitation is mostly in the form of snowfall in the upper parts of Himalayas, it only rains over the rest of the country.

(iv) The annual precipitation varies from 400 cm in Meghalaya to less than 10 cm in Ladakh and Western Rajasthan.

(v) Most parts of the country receive rainfall from June to September, but Tamil Nadu coast receives rainfall during autumn and early winter.

6. Discuss the mechanism of monsoons.

Ans. To understand the mechanism of monsoons the following facts are important:

(i) The difference in the rate of heating and cooling of land and sea on a large scale. During summers a low pressure area develops on the Indian landmass while the seas around experience comparatively high pressure.

(ii) The shift of the position of the Inter-Tropical Convergence Zone. This is the equatorial trough normally positioned about 5°N of the equator, also known as the monsoon trough during the monsoon season.

(iii) The presence of high pressure area, east of Madagascar approximately at 20°S over the Indian Ocean. The intensity and position of this high pressure area affects the Indian monsoons.

(iv) The Tibetan high level plateau gets intensely heated during summers which results in strong vertical currents and formation of high pressure over the plateau at about 9 kilometers above sea level.

(v) The movement of the westerly jet to the north of the Himalayas and the presence of the tropical easterly jet over the Indian peninsula during summers.

Apart from this, it has also been noticed that changes in the pressure conditions over the southern Oceans also affect the monsoons.

7. Give an account of weather conditions and characteristics of the cold season.

Ans. The temperature, atmospheric pressure, wind, humidity and precipitation usually determine the weather conditions at any point of time (a day or a week) and the space. Weather is generally expressed as cool, hot, windy, calm, cloudy, bright, wet or dry. Actually, atmospheric conditions are called the weather. We experience hot weather in summers, cold weather in winters, wet weather in rainy season and cool and dry during October-November and the March and April respectively.

Weather phenomenon changes rapidly. Any day may have different weather conditions. We just feel suffocated due to humidity and scorching heat of July month. Suddenly clear sky is covered with clouds and it starts raining with lightning and strong wind. Something of such strange happens when cyclonic depression cause damages in deltas of the Mahanadi, Kaveri, Godavari and Krishna rivers.

Following are the characteristics of the cold season.

(i) It begins from mid-November in Northern India and pervades here till February. The mid-months, i.e., December and January are the coldest months.

(ii) The temperature gradually decreases during this period from south to the north. For example, in Chennai 20°-25°C while it is 10°15°C in northern plains.

(iii) Days are experienced warm while the nights are cold. Days are cut short while nights are longer.

(iv) Most part of the country remains dry (i.e., without winter rain) during this period and only Tamil Nadu coast including Coromandel coast receive heavy winter rains.

(v) Coastal areas enjoy moderate temperature throughout the year while the rest of the country experiences cold, heat, humid and moderate according to the cycle of the seasonal change. It means reversal of winds or monsoon type climate has more seasonal variations to experience.

8. Give the characteristics and effects of the monsoon rainfall in India.

Ans. The characteristics of Monsoon season is discussed below:

a. It gives water into most of the parts of the country except some leeward sides’ rain shadow regions and desert areas.

b. Early in the season, the windward side of the Western Ghats receives heavy rainfall of more than 250 cm.

c. The rain shadow areas of Deccan Plateau and parts of Madhya Pradesh also get scanty rains.

d. The maximum rainfall is recorded in the north-eastern parts of the country. Mawsynram happens to be the wettest place in the world.

e. Indian monsoon takes “breaks” viz. sprinkled with rainless intervals. This happens because of the monsoon trough, caused due to spatial distribution of rainfall.

f. The frequency and intensity of tropical depressions also determine the amount and duration of monsoons.

g. The monsoon trough over the northern plains becomes weaker causing the months of October-November, a period of transition from hot rainy season to dry winter conditions.

The effects of Monsoon season is discussed below:

a. When the rains are heavy, the rivers get flooded causing heavy damage in the plains year after year.

b. A dry spell would cause as much misery as the river floods.

c. The characteristic of monsoon has a very destabilizing effect on Indian economy that continues to be predominantly agricultural and severely dependent on rained irrigation.