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Climatic Regions of India : Koeppen’s Classification | |||
Climate Type | Climatic Region | Annual Rainfall in the Region | |
Amw (Monsoon type with shorter dry winter season) | Western coastal region, south of Mumbai | over 300 cm | |
As (Monsoon type with dry season in high sun period) | Coromandel coast = Coastal Tamil Nadu and adjoining areas of Andhra Pradesh | 75 – 100 cm [wet winters, dry summers] | |
Aw (Tropical Savanah type) | Most parts of the peninsular plateau barring Coromandel and Malabar coastal strips | 75 cm | |
BShw (Semi-arid Steppe type) | Some rain shadow areas of Western Ghats, large part of Rajasthan and contiguous areas of Haryana and Gujarat | 12 to 25 cm | |
BWhw (Hot desert type) | Most of western Rajasthan | less than 12 cm | |
Cwg (Monsoon type with dry winters) | Most parts of the Ganga Plain, eastern Rajasthan, Assam and in Malwa Plateau | 100 – 200 cm | |
Dfc (Cold, Humid winters type with shorter summer) | Sikkim, Arunachal Pradesh and parts of Assam | ~200 cm | |
Et (Tundra Type) | Mountain areas of Uttarakhand The Average temperature varies from 0 to 10°C | Rainfall varies from year to year. | |
E (Polar Type) | Higher areas of Jammu & Kashmir and Himachal Pradesh in which the temperature of the warmest month varies from 0° to 10°C | Precipitation occurs in the form of snow | |
Climatic Regions of India : Trewartha’s Classification
Climate Type | Climatic Region | Other Cliamatic Condtions |
Am (Tropical Rain Forest) | Western coastal region, Sahayadris and parts of Assam | 200 cm annual rainfall & 18.2 C to 29 C temperature |
Aw (Tropical Savanna) | Peninsular India except the semi arid zone | 150 cm annual rainfall & 18 C-32 C temperature |
Aw (Tropical Savanah type) | Most parts of the peninsular plateau barring Coromandel and Malabar coastal strips | 75 cm |
BS (Semi-arid Steppe type) | Runs southwards from central Maharashtra to Tamilnadu, Andhra Pradesh | 40-75 cm annual rainfall & 20-32 C temperature |
BSh (Tropical and subtropical Steppe) | Ranges from Punjab to Kutch | Annual temperature 35 C & 30-60 cm annual rainfall |
BWh (Tropical Desert) | Western parts of Barmer, Jaiselmer and Bikaner and parts of Kutch | Annual Temperature 35 C & annual rainfall 25 cm |
Caw (Humid Subtropical Climate with dry winters) | It ranges from Punjab to Assam | Rainfall from 100-150 cm |
H (Mountain Climate) | Mountain areas of Himalayas including Jammu & Kashmir, Uttarakhand, Himachal Pradesh, Sikkim, Arunachal Pradesh | The average temperature varies from 0 to 10°C. |
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The Köppen climate classification is a system that classifies climates into five main climate groups: tropical, dry, temperate, continental, and polar. Each group is then divided into sub-groups based on temperature and precipitation.
The Köppen climate classification is one of the most widely used climate classification systems in the world. It was developed by German-Russian climatologist Wladimir Köppen in the early 20th century. The system is based on the annual and monthly mean temperature and precipitation of a location.
The five main climate groups in the Köppen climate classification are:
- Tropical: A climate with an average temperature of 18°C (64°F) or higher throughout the year. Tropical climates are found near the equator, where the sun’s rays are most direct.
- Dry: A climate with an average annual precipitation of less than 25 cm (10 in). Dry climates are found in areas where there is little rainfall, such as deserts and semi-deserts.
- Temperate: A climate with an average annual temperature between 10°C (50°F) and 18°C (64°F). Temperate climates are found in areas between the tropics and the poles.
- Continental: A climate with a large difference between the summer and winter temperatures. Continental climates are found in areas that are far from the ocean, such as the interior of North America and Eurasia.
- Polar: A climate with an average annual temperature below 10°C (50°F). Polar climates are found in the Arctic and Antarctic regions.
Each of the five main climate groups is then divided into sub-groups based on temperature and precipitation. For example, the tropical climate group is divided into the tropical rainforest climate, the tropical savanna climate, and the tropical monsoon climate.
The Köppen climate classification is a useful tool for understanding the Earth’s climate. It can be used to identify areas with similar climates, to track changes in climate over time, and to predict future Climate Change.
The Thornthwaite climate classification is a system that classifies climates based on the amount of water that is available for Plants to use. The system divides climates into three main groups: humid, sub-humid, and arid. Each group is then divided into sub-groups based on the amount of precipitation and potential evapotranspiration.
Potential evapotranspiration is the amount of water that would evaporate from a surface if there were no restrictions on the water supply. The Thornthwaite climate classification is based on the idea that the amount of water that is available for plants to use is determined by the difference between precipitation and potential evapotranspiration.
The three main climate groups in the Thornthwaite climate classification are:
- Humid: A climate with an average annual precipitation that is greater than the potential evapotranspiration. Humid climates are found in areas where there is more rainfall than Evaporation.
- Sub-humid: A climate with an average annual precipitation that is less than the potential evapotranspiration, but greater than half of the potential evapotranspiration. Sub-humid climates are found in areas where there is more evaporation than rainfall, but the rainfall is still sufficient to support plant Growth.
- Arid: A climate with an average annual precipitation that is less than half of the potential evapotranspiration. Arid climates are found in areas where there is very little rainfall and evaporation is high.
Each of the three main climate groups is then divided into sub-groups based on the amount of precipitation and potential evapotranspiration. For example, the humid climate group is divided into the humid continental climate, the humid subtropical climate, and the humid tropical climate.
The Thornthwaite climate classification is a useful tool for understanding the Earth’s climate. It can be used to identify areas with similar climates, to track changes in climate over time, and to predict future climate change.
What is climate?
Climate is the average weather conditions in a place over a long period of time. It is affected by factors such as latitude, altitude, and proximity to water.
What are the different Types of Climate?
There are many different ways to classify climates. One common system is the Köppen climate classification system, which divides climates into five main types: tropical, dry, temperate, continental, and polar.
What are the characteristics of each type of climate?
Tropical climates are warm and wet year-round. Dry climates are hot and dry in the summer and cold and dry in the winter. Temperate climates have four distinct seasons: spring, summer, fall, and winter. Continental climates have hot, humid summers and cold, dry winters. Polar climates are cold and dry year-round.
What are the Causes of Climate Change?
Climate change is caused by human activities such as burning fossil fuels, deforestation, and agriculture. These activities release greenhouse gases into the Atmosphere, which trap heat and cause the planet to warm.
What are the effects of climate change?
Climate change is causing a number of changes to the planet, including rising sea levels, more extreme weather events, and changes in plant and animal life. These changes are having a significant impact on people and the Environment.
What can we do to address climate change?
There are a number of things we can do to address climate change, including reducing our reliance on fossil fuels, investing in RENEWABLE ENERGY, and protecting forests. We can also make changes to our own lifestyles, such as driving less, using less energy, and eating less meat.
What is the future of climate change?
The future of climate change is uncertain. If we do not take action to reduce greenhouse gas emissions, the planet will continue to warm. This could have devastating consequences for people and the environment. However, if we take action now, we can still avoid the worst effects of climate change.
Which of the following is not a type of climate according to the Köppen climate classification system?
(A) Tropical rainforest
(B) Mediterranean
(C) Continental
(D) PolarWhich of the following is not a type of climate according to the Thornthwaite climate classification system?
(A) Humid subtropical
(B) Mediterranean
(C) Semiarid
(D) Tropical rainforestThe Köppen climate classification system is based on which of the following factors?
(A) Temperature and precipitation
(B) Vegetation
(C) Soil type
(D) LandformThe Thornthwaite climate classification system is based on which of the following factors?
(A) Temperature and precipitation
(B) Vegetation
(C) Soil type
(D) LandformThe Köppen climate classification system is more widely used than the Thornthwaite climate classification system because it is:
(A) More accurate
(B) More comprehensive
(C) Easier to use
(D) More widely acceptedThe Thornthwaite climate classification system is more accurate than the Köppen climate classification system because it takes into account:
(A) The amount of potential evapotranspiration
(B) The amount of actual evapotranspiration
(C) The length of the growing season
(D) The amount of precipitationThe Köppen climate classification system is more comprehensive than the Thornthwaite climate classification system because it includes:
(A) More climate types
(B) More detailed information about each climate type
(C) A wider range of climate variables
(D) A more sophisticated statistical modelThe Thornthwaite climate classification system is easier to use than the Köppen climate classification system because it:
(A) Is based on simpler criteria
(B) Has fewer climate types
(C) Is less complex
(D) Is more intuitiveThe Köppen climate classification system is more widely accepted than the Thornthwaite climate classification system because it:
(A) Is older
(B) Is based on more rigorous scientific principles
(C) Is used by more governments and organizations
(D) Is more widely taught in schools and universitiesThe Thornthwaite climate classification system is more widely used in the United States than the Köppen climate classification system because it:
(A) Is better suited to the climate of the United States
(B) Is based on data that is more readily available in the United States
(C) Is more widely taught in schools and universities in the United States
(D) Is used by more governments and organizations in the United States