Ratna Sagar Geography Solutions Solutions for Class 6 Social science Chapter 9 - India Climatic Conditions

Answer:

The correct answer is option (d).

Explanation: Water bodies exert a moderating influence on the climate of the places that are near them. Kochi lies in the southwest coast; therefore, it experiences equable climate.  

Answer:

The correct answer is option (b).

Explanation: Coastal areas experience equable climate because of the presence of water bodies around the peninsula. The interior parts of the country experience extreme climate. Lucknow, which is situated in the interior of India, witnesses extreme climatic conditions.

Answer:

The correct answer is option (d).

Explanation: From September to November, monsoon winds start retreating. Thus, the weather becomes extreme and is characterised by high heat and humidity. The cyclones arising in the Bay of Bengal cause rainfall in the Coromandel Coast of Tamil Nadu. Hence, Chennai receives most of its rainfall during the retreating monsoon.

Answer:

The correct answer is option (c).

​Explanation: Pre-monsoon showers are experienced during the end of the summer season. In Kerala and Karnataka, they cause the early ripening of mangoes. Hence, these showers are referred to as mango showers.

Answer:

The correct answer is option (a).

Explanation: In West Bengal, the pre-monsoon showers are characterised by strong winds and heavy rainfall. These are experienced with the approach of the summer season and are called kalbaisakhi.

Answer:

The correct answer is option (c).

Explanation: Monsoon in India starts from June; the whole country experiences the weather within a few weeks. It continues till the month of September. The time period varies depending on the location of a place.

Answer:

The correct answer is option (b).

Explanation: The distribution of rainfall depends upon a variety of factors like relief features, direction of winds and distance from a sea. The average annual rainfall in India, i.e. 120 cm, is the highest in the world.

Answer:

The correct answer is option (a).

Explanation: The distribution of rainfall varies from one place to another. Mawsynram near Cherrapunji in Meghalaya has recorded the highest annual rainfall of 1142 cm.

Answer:

1. Temperature and rainfall are two important elements of climate.

Explanation: The two elements of climate are temperature and rainfall. There is a considerable variation in both the elements not only from one place to another but also from one season to another.

2. January and February are the coldest months in many parts of India.

Explanation: During the cold weather season, most parts of the country witness a drop in temperature. January and February are the coldest months in most parts of the country. At some places, temperature goes below 0 ^oC.

3. â€‹Rainfall in India gradually decreases from south to north and east to west.

Explanation: The distribution of rainfall depends on a range of factors. India receives most of its rainfall from the southwest monsoon winds. But the amount of rainfall decreases as we move from south to north and from east to west. Also, reduction in rainfall is seen when we go from coastal areas to the interiors of the country.

4. â€‹The monsoon starts retreating from the month of mid-September.

Explanation: The monsoon winds start retreating from mid-September and continues till the month of November. The process is very slow. It causes rainfall in the Coromandel Coast of Tamil Nadu and some other areas.

Answer:

1. The given statement is true.

Explanation: India experiences tropical monsoon type of climate. It has distinct hot and cold weather seasons. The monsoon season starts roughly from May.

2. â€‹The statement is false.
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Explanation: Coastal areas experience moderate climate because of the presence of water bodies, but the interior parts of the country experience extreme climatic conditions.

3. â€‹The statement is false.
​
Explanation: During the cold weather season, the Northern Plains have a very low temperature. But at the same time, south India has equable climate. So, the temperature decreases from south to north.

4. â€‹The statement is false.
​
Explanation: Loo is a hot, dust-laden wind that blows over the Northern Plains. It is a very dry wind; hence, it does not bring any rainfall.

5. â€‹The statement is false.
​
Explanation: From September to November, monsoon winds start retreating. Thus, the weather becomes extreme with high heat and humidity. The cyclones arising from the Bay of Bengal cause rainfall in the Coromandel Coast of Tamil Nadu.

Answer:

The correct match is given as under:
 

Answer:

1. Temperature variance, rainfall distribution and monsoon winds cause four different season cycles in India. The names of the main seasons in India are as follows:

• Cold weather season - Mid-November to mid-March
• Hot weather season - Mid-March to May end
• Southwest monsoon season - June to September
• Retreating monsoon season - October to mid-November

Answer:

1. The winter cyclones originate in the Mediterranean Sea; they cause mild rainfall in the Northern Plains and snowfall in the Himalayas.

2. Loo are the hot and dust-laden winds that blow in north India. They mostly originate in the state of Rajasthan. These winds are dry; hence, they do not cause any rainfall.

3. The branches of southwest monsoon winds are as follows:

• The Bay of Bengal branch
• The Arabian Sea branch

Answer:

1. The names of the main seasons in India are as follows:
     i) Cold weather season - Mid-November to mid-March
     ii) Hot weather season - Mid-March to May end
    iii) Southwest monsoon season - June to September
     iv) Retreating monsoon season - October to mid-November

2. During the winter season, temperature remains low throughout the country. This temperature is very low in the northern region and increases as we go towards the south. January and February witness the lowest temperature during this season. Also, the mountains of the north experience heavy snowfall.

3. The weather of the Northern Plains during the hot weather season is mostly dry and hot. The hot and dust-laden winds called loo blow in the Northern Plains. Towards the end of the season, few places receive pre-monsoon showers.

4. The monsoon season is hot and wet and extends from June to September. The retreating monsoon season is cold and dry and extends from the middle of September to November. Only few parts of the country receive rainfall in the retreating monsoon season; the monsoon season, on the other hand, brings rainfall to most parts of the country.

Answer:

The main factors that affect the climate of India are as follows:

1. Location: India is divided into almost two equal halves by the Tropic of Cancer. Hence, half part is tropical, while other half experiences subtropical climate. The Himalayas protect India from cold Siberian winds and is one of the reasons behind the rainfall here.
2. Relief: During summers, most of the country experiences high temperatures except the Himalayas, which experience a relatively low temperature. Also, the places that are near the sea experience moderate climate both in summers and winters.
3. Distance from the sea: The coastal areas experience moderate climate because of the presence of water bodies, but the interior parts of the country experience extreme climatic conditions.

Answer:

The Himalayas have a considerable influence on the climate of the Indian subcontinent. On one hand, they protect the Indian mainland from the chilly winds of Siberia. Had they not been there, the Indian lands would have been frozen and covered with snow throughout the year. The Himalayas also act as a barrier to the monsoon winds coming from seas. Hence, they are an important cause of rainfall in India. They help in maintaining both the elements of climate, i.e. temperature and rainfall.

Answer:

Monsoon winds are moisture-laden winds originating from a sea and moving towards the Indian peninsula. India experiences most of its rain from the southwest monsoon winds. They are divided by the Indian peninsula into two parts: the one that originates from the Arabian Sea and the other that originates from the Bay of Bengal. They bring a huge amount of moisture with them, which causes rainfall in most parts of the country. They are very irregular and erratic and causes floods and drought at two places at the same time.

Answer:

Rainfall is not evenly distributed across the Indian subcontinent. The fact that one part of the country experiences floods while the other experiences droughts proves unequal rainfall distribution across the country. The average annual rainfall is 120 cm. But the distribution depends on factors like relief features, direction of moisture-laden winds and the location of a place and its distance from the sea. Meghalaya receives more than 800 cm of annual rainfall, while some parts of Rajasthan receive only 10 cm of annual rainfall. 

Answer:

The distribution of rainfall is highly uneven in India. Meghalaya receives 800 cm of annual rainfall and Rajasthan receives 10 cm of annual rainfall. There are several reasons for the same. For example, Rajasthan has high temperature with low humidity, so the monsoon winds are not seen here in this season; this ultimately leads to droughts here. On the other hand, the northeastern states witness high humidity due to dense forests. So, they receive more rainfall. This is the reason some parts of India experience floods and droughts at the same time.

Answer:

Though most of the country gets rainfall during summers, the coastal areas of Tamil Nadu receive rainfall during winters. This is because of the retreating monsoon, which extends from the middle of September to the middle of November. During this period, cyclones originate in the Bay of Bengal, which make the weather oppressive, causing high humidity. These cyclones hit the Tamil Nadu coast after picking moisture from the Indian Ocean and cause rainfall.

Answer:

Winds move from a high-pressure region to a low-pressure zone. During summers, high pressure develops over the coastal lands, so the cold winds move from the sea to the land, reducing the temperature of the region. The reverse happens in winters when high pressure develops over the sea. This way an equable temperature is maintained in the coastal areas in which sea breeze plays a very important role.