Notes-Class 10-Geography-Chapter-4-Climate-Maharashtra Board

Climate

Class 10-Geography-Chapter-4 Maharashtra Board

Notes

Topics to be learn :

Details of climatic conditions & Comparative study of India and Brazil with reference to

  • Features of climate,
  • Factors affecting climate,
  • Features of temperatures
  • Features of rainfall.
  • Natural Disaster

Brazil :  Proximity to equator. Brazilian Highlands, the Great Escarpment are the main factors affecting climate of Brazil.

Features of Brazil’s climate : Because of the vast latitudinal extent of Brazil, it experiences wide range of climatic variations in climate.

Brazil’s extents lie mostly in the tropical region. The features of Brazil’s climate are as follows :

Variations :

  • Brazil’s latitudinal extents are very vast. As its effect, a wide range of climate, i.e. variations in climate are found in Brazil.
  • The climate is hot near equatorial region.
  • Temperate type of climate is in the areas near the Tropic of Capricorn.

Factors affecting climate of Brazil :

  • Due to proximity to equator, the temperatures in the northern part of Brazil is comparatively higher. On the other hand, the temperature in the southern part of Brazil is comparatively lower.
  • The temperature is comparatively low in the Brazilian highlands. Brazilian highlands receives moderate amount of rainfall, i.e. nearly 600 mm to 1200 mm.
  • The great Escarpment and the Brazilian Highlands obstruct the trade winds blowing from the southeast and the northeast directions. This leads to heavy rainfall in the windward sides of the Great Escarpment, i.e. in the eastern coastal region of Brazil.
  • The winds blowing beyond the Highlands become dry and therefore it rains less to the leeward side of the Great Escarpment and the Brazilian Highlands.

Possibilities of natural disasters occurring due to sudden change in climate :

  • In the northern coastal areas near equator the winds flow in the vertical direction.
  • Similarly, the convergence zone of the trade winds in this region is weak.
  • As a result, the possibility of cyclones in the coastal regions is very rare.

Features of temperatures in Brazil :

The features of temperatures in Brazil are as follows :

Northern part & Southern part of Brazil :

The northern part of Brazil :

  • The higher temperatures are found in the northern part of Brazil near equator.
  • In the coastal regions near the equator, the variations in temperatures are negligible.
  • The average temperature in the Amazon river valley is between 25°C and 28°C.

The southern part of Brazil : The lower temperatures are found in the southern part of Brazil to the south of the Tropic of Capricorn.

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Highlands : The cool climate is found in the highlands of Brazil.

Coastal regions : Mild and humid climate is found in the coastal regions of Brazil.

Features of rainfall in Brazil :

The features of rainfall in Brazil are as follows :

Rainfall occurring due to southeast trade winds : Brazil gets rainfall from the southeast as well as northeast trade winds.

  • The Great Escarpment and the Brazilian Highlands obstructs the northeast and southeast trade winds. As its effect, these winds move upwards along the slopes of the Great Escarpment and the Brazilian Highlands.
  • At higher altitude, the condensation process takes place and windward side receives more rain.
  • Thus, the windward side of the Great Escarpment and the Brazilian Highlands receive abundant rainfall and the rain shadow region is found to the other side.

Nature of rainfall in Brazil :

Nature of rainfall in Brazil :

  • Brazil has its rainy season from September to November as well as from March to May.
  • The amount of annual average rainfall in the Amazon river basin is nearly 2000 mm.
  • Every year, the Amazon river rises more than 9 metres flooding the surrounding forests.
  • The amount of annual average rainfall is nearly 1000 mm to 1200 mm in the southeast coastal region.
  • The amount of annual average rainfall is only 600 mm to the northeast of the
  • Brazilian Highlands. This region is known as ‘Drought Quadrilateral’.
  • The amount of annual average rainfall is around 1500 mm in Paraguay-Parana river basin.
  • In Brazil, the severity of floods is comparatively greater in the forests to the north of the equator.

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Drought Quadrilateral in Brazil :

Drought Quadrilateral in Brazil :

  • The winds that reach the top of the Great Escarpment and the Brazilian Highlands become dry. The capacity of holding moisture of these winds increases.
  • As its effect it rains less to the leeward side of the Great Escarpment and the Brazilian Highlands.
  • Thus, the northeast part of Brazil receives the minimum rainfall.
  • The amount of annual average rainfall is only nearly 600 mm in this region. This region is a rain shadow region.
  • It is known as ‘Drought Quadrilateral’. The higher temperature is found in this region.

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Features of winds in Brazil :

Towards Brazil winds are flowing from different directions. The following could be the reasons behind it.

  • The equator passes through the northern part of Brazil. The low pressure belt is found near equatorial region in Brazil.
  • The winds from high pressure belt from southern and northern hemisphere flow towards this region in Brazil.
  • As its effect, in the northern part of Brazil, the northeast trade winds flow.
  • Similarly, in the southern part of Brazil, the southeast trade Winds flow.

Climate of Manaus, Belem, Porto Alegre, Rio de Janeiro :

Climate of Manaus, Belem, Porto Alegre, Rio de Janeiro

Manaus : Manaus has the maximum range of temperature. It is nearly from 23°C (minimum temperature) to 33°C (maximum temperature). In Manaus, the highest temperature is found in the months from August to October. Here rains is most in the month of March

Belem : In Belem the highest temperature is found in the months of June to December. Here rains is most in the month of March

Porto Alegre : In Porto Alegre the highest temperature is found in the months of January and February. Here rains is most in the month of August and September

Rio de Janeiro : In Rio de Janeiro the highest temperature is found in the month of February. Here rains is most in the month of January and March. Humid and moderate type of climate will be found in Rio de Janeiro.

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Features of India’s climate : India's climate is 'monsoon' type. The sunrays are perpendicular upto the Tropic of Cancer, which passes through the middle of the country. As a result, average temperatures are higher throughout the year.

India is included in the tropical region. The features of India’s climate are as follows :

Type : Monsoon

Nature : Higher temperatures almost throughout the year.

Seasons : There are following four seasons as per the Indian Meteorological Department :

  • The hot weather season
  • The season of rainfall (Monsoon)
  • The season of Retreating Monsoon and
  • The cold weather season.

 The main factors affecting climate :

  • The Indian Ocean
  • Himalayan ranges.

Impact of Indian Ocean and the Himalayas on the origin monsoons :

Impact of Indian Ocean and the Himalayas on the origin  monsoons :

The Indian Ocean and Himalayan ranges play an important role in formation of southeast monsoon winds.

  • In summers, the temperature in Punjab Plains and the Thar desert is found to be high. As its effect, the areas of low pressure are developed.
  • On the other hand, the areas of high pressure are found in the Indian Ocean. This leads to formation and flowing of southeast monsoon winds from the Indian Ocean to the mainland of India.
  • These winds are moisture-laden and so they bring rainfall in India.
  • Himalayas saves India by obstructing the passage of very cold winds from the north into India in winter.
  • The southwest monsoon winds flow from the south to the north and reaches towards the Himalayas.
  • These winds are obstructed by the Himalayas. Due to obstruction, these winds change their direction and start flowing from the northeast to the Indian Ocean.
  • The return journey of these winds bring the retreating monsoon in peninsular region of India.

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 Reasons for diversity in climatic conditions :

  • The latitudinal location
  • The altitude of the place.

 Natural calamities occurring due to sudden change in climate :

  • Erratic rainfall
  • Droughts
  • Cyclones
  • Floods. etc.

 Features of temperatures in India :

The Tropic of Cancer passes through the middle of India. As its effect, the differences in the temperatures found in the northern and the southern part of India are as follows :

Thar desert in Rajasthan and the peninsular regions in the south are the regions of the maximum temperature and the Himalayan regions in the north are the regions of the minimum temperatures.

Southern part & Northern part of India :

The southern part of India : The southern part of India (regions to the south of the Tropic of Cancer) receives comparatively perpendicular sunrays. As its effect, the temperature in the southern part of India is comparatively higher.

The northern part of India: The northern part of India (regions to the north of the Tropic of Cancer) receives comparatively less perpendicular stunrays. As its effect, the temperature in the northern part of India is comparatively lower. (In winters, the temperatures drop to - 40° Celsius in Jammu and Kashmir and mountainous regions of Himalayas in the north.

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Q. Why, the average annual temperature in India is generally high ?

Answer

  • The Tropic of Cancer passes through the middle of India.
  • India is included in the tropical region.
  • In winters, the temperatures drop below 0° Celsius in some parts of India.
  • However, during summers, the temperature increases up to 50° Celsius in some parts of India.
  • Thus, the average annual temperature in India is generally high.

Features of rainfall in India :

India receives rainfall mainly due to southwest monsoon winds. India experiences the highest rainfall in the month of June.

The features of rainfall in India are as follows :

Rainfall occurring due to southwest monsoon winds :

  • In summers, the low pressure areas are developed in Punjab Plains and the Thar Desert of Rajasthan.
  • As its effect, winds start blowing from the high pressure region in the Indian Ocean to the mainland of India.

Nature of rainfall in India :

Nature of rainfall in India :

  • Due to the obstruction caused by the Western Ghats (mountainous region) and the Eastern Ghats (mountainous region), the amount of rainfall is more in the coastal regions.
  • Semiarid conditions are found to the east of the Western Ghats of peninsular India. This region is a rain shadow region. Therefore semiarid climatic conditions are found here.
  • The southern part of western coastal region and the northeastern region get more than 4000 mm of rainfall
  • The rain shadow regions are found in leeward sides of mountains.
  • The southwest monsoon winds then blow parallel to the Aravalis. As a result, the amount of rainfall is found to be less in parts of Gujarat and Rajasthan.
  • These winds further move towards Himalayas. These winds return from the
  • Himalayas and begin their return journey from the northeast direction to the Indian Ocean.
  • During their return journey, these winds bring retreating monsoon in some parts of the peninsula.

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Q. What could be reason for some part of Raiasthan is under desert ?

Answer

  • The Aravali range is spread in the southwest - northeast direction in the central part of Rajasthan.
  • The Aravali range obstructs the southwest winds. As its effect, these winds flow to the north along with the Aravali range. This results in more rainfall to the windward side of the Aravali range,
  • When these winds cross the mountain top of Aravali range, go to other side of the mountain, these winds are dry.
  • As its effect, the leeward side of the Aravali range gets less rainfall. Therefore, some part of Raiasthan, i.e. the northwest part of Rajasthan is under desert.

Winds blow from the Bay of Bengal towards Meghalaya plateau. Cherrapunji and Mawsynram are located to the windward side of Meghalaya plateau. As its effect, these places receive maximum rainfall,

Shillong is located to the leeward side of Meghalaya plateau. This region is a rain shadow region. Therefore Shillong receives only 1000 mm of rainfall.

Climate of Delhi, Kolkata, Mumbai and Chennai :

Climate of Delhi, Kolkata, Mumbai and Chennai :

  • Delhi : The average range of minimum and maximum temperature of Delhi is between 6°C and 41°C. The range is maximum in Delhi. It indicates that Delhi has extreme climate.
  • Kolkata : The average range of minimum and maximum temperature of Kolkata is between 9°C and 37°C. The range is maximum in Kolkata. It indicates that Kolkata has extreme climate.
  • Mumbai : The average range of minimum and maximum temperature of Mumbai is between 16°C and 34°C. On the basis of temperature range, it can be concluded that the climate of Mumbai is hot and humid. Mumbai has equable climate. In Mumbai, the amount of average rainfall in the month of June is nearly 450 mm and it is nearly 720 mm in the month of July. On the basis of the amount of rainfall, it can be concluded that it rains heavily in the month of July in Mumbai.
  • Chennai : The average range of minimum and maximum temperature of Chennai is between 21°C and 39°C. The range is minimum in Chennai. It indicates that Chennai has equable climate.

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Useful links :


Main Page : - Maharashtra Board Class 10 -Geography  - All chapters notes, solutions, videos, test, pdf.

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