The empirical classification of Koeppen's Climatic Regions is based on mean annual and mean monthly temperature and precipitation data. The spread of plants and climate, according to Koeppen, are inextricably linked. Classification took certain temperature and precipitation values and related them to vegetation distribution, then used these values to classify climates. This article will explain to you the Climatic Regions of India according to Koeppen's Scheme which will be helpful in Geography preparation for the UPSC Civil service exam.
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| Jet Streams | Indian Monsoon |
| Seasons in India | El-Nino |
| Factors Affecting the Climate of India | Indian Ocean Dipole |
| Group | Characteristics |
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| A-Tropical | The coldest month's average temperature is 18° C or higher. |
| B-Dry Climates | The amount of potential evaporation is greater than the amount of precipitation. |
| C- Warm Temperate | The average temperature of the coldest month of the year in the (Mid-latitude) climates is greater than minus 3°C but lower than 18°C. |
| D-Cold Snow forest | The coldest month's average temperature is minus 3° C or below. |
| E-Cold Climates | The average monthly temperature is below 10° C. |
| H-Highlands | Cold due to elevation |
| Group | Type | Letter code | Characteristics |
|---|---|---|---|
| A-Tropical Humid Climate | Tropical Wet Tropical Monsoon Tropical wet and dry | Af Am Aw | No dry season Monsoonal, Short dry season Winter dry season |
| B-Dry Climate | Subtropical Steppe Subtropical Desert Mid-latitude Steppe Mid-latitude Desert | BSh BWh BSk BWk | Low-latitude semi-arid or dry Low-latitude arid or dry Mid-latitude semi-arid or dry Mid-latitude arid or dry |
| C-Warm temperate Climates | Humid subtropical Mediterranean Marine west coast | Cfa Cs Cfb | No dry season Dry hot summer No dry season, warm and cool summer, Precipitation varies 50- 250cm |
| D-Cold Snow-forest Climates | Humid Continental Subarctic | Df Dw | No dry season, severe winter Winter dry and very severe |
| E-Cold climates | Tundra Polar ice cap | ET EF | No true summer Perennial ice |
| H-highland | Highland | H | Highland with snow cover |
| Climate Type | Region | Annual Rainfall |
|---|---|---|
| Amw (Monsoon type with short dry winter season) | South of Mumbai, on the western shore. | Over 300 cm |
| As (Monsoon type with dry season in high sun period) | Coromandel coast - Coastal Tamil Nadu and bordering Andhra Pradesh regions | 75 – 100 cm (wet winters, dry summers) |
| Aw (Tropical Savanna type) | Most of the peninsular plateau, with the exception of the Coromandel and Malabar coastal regions. | 75cm |
| BShw (Semi-arid Steppe type) | Some rain shadow portions of the Western Ghats, a considerable portion of Rajasthan, and adjoining areas of Haryana and Gujarat | 12cm to 25cm |
| BWhw (Hot desert type) | The majority of western Rajasthan | Less than 12cm |
| Cwg (Monsoon type with dry winters) | Most of the Ganga Plain, eastern Rajasthan, Assam, and the Malwa Plateau are affected. | 100cm to 200cm |
| Dfc (Cold, Humid winters type with shorter summer) | Sikkim, Arunachal Pradesh, and portions of Assam | Approximately 200cm |
| Et (Tundra Type) | Uttarakhand's mountainous terrain. The average temperature ranges from 0 to 10 degrees Celsius. | The amount of rain that falls fluctuates from year to year. |
| E (Polar Type) | Higher portions of Jammu and Kashmir and Himachal Pradesh, where the hottest month's temperature ranges from 0° to 10° C. | Snow is the most common kind of precipitation. |

The most extensively used climatic classification is Koeppen's Climate Classification. In 1884, Wladimir Peter Koeppen developed this climate classification system. He recognized that plant spread and climate were intricately related. The categories are determined by annual and monthly temperature and precipitation averages. Most geographers have prioritized rainfall above temperature when defining Indian climatic areas since changes in rainfall are far more pronounced than those in temperature.
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| Geography Notes | Physical Geography |
| India's Physiographic Divisions | Indian Drainage Systems |
| Climatology | Natural Disasters |
| Water Resources in India | Major Lakes in India |
Question: What is the Köppen Climate Classification?
Answer: The Köppen Climate Classification is a system used to classify the world's climates based on temperature and precipitation patterns. It categorizes climates into major types such as tropical, dry, temperate, and polar.
Question: What type of climate is found in the Thar Desert region of India?
Answer: The Thar Desert region of India has an arid climate (BWh, BWk), characterized by low rainfall and extreme temperatures.
Question: Which regions in India experience a tropical wet climate?
Answer: Regions such as Kerala, West Bengal, and the Andaman and Nicobar Islands experience a tropical wet climate (Am, Af), with high temperatures and heavy rainfall throughout the year.
Question: What climate type is associated with the Himalayan region?
Answer: The Himalayan region experiences a montane climate (ET, EF) in high-altitude areas and a temperate climate (Cwb, Cfb) in the lower elevations.
Question: How does Köppen’s classification help in understanding India’s climate?
Answer: Köppen’s classification provides a framework to categorize India’s diverse climate patterns, helping in the study of regional climatic impacts on agriculture, water resources, and settlement patterns.
1. Which climate classification is found in the coastal regions of Kerala and West Bengal according to Köppen’s system?
A. Tropical Wet Climate (Am, Af)
B. Arid Climate (BWh)
C. Temperate Climate (Cwb)
D. Polar Climate (ET)
Answer: (A) See the Explanation
The coastal regions of Kerala and West Bengal experience a tropical wet climate (Am, Af), with high temperatures and heavy rainfall throughout the year.
2. Which region in India has an arid climate (BWh, BWk) under Köppen’s classification?
A. Kerala
B. Gujarat
C. Himachal Pradesh
D. Uttarakhand
Answer: (B) See the Explanation
The arid climate (BWh, BWk) is found in regions like the Thar Desert in Rajasthan and parts of Gujarat, characterized by very low rainfall and extreme temperatures.
3. Which type of climate is prevalent in the Himalayan region at high altitudes?
A. Montane Climate (ET, EF)
B. Tropical Wet Climate (Af)
C. Arid Climate (BWh)
D. Temperate Climate (Cwb)
Answer: (A) See the Explanation
The high-altitude regions of the Himalayas experience a montane climate (ET, EF), characterized by cold temperatures and snow throughout the year.
4. What is the characteristic feature of the tropical dry climate (Aw) in India?
A. Heavy rainfall throughout the year
B. Winter dry season and high summer temperatures
C. Cold temperatures year-round
D. High-altitude snow and frost
Answer: (B) See the Explanation
The tropical dry climate (Aw) in central and western India is characterized by a dry season during winters and high temperatures in the summer.
5. What type of climate does the region of Himachal Pradesh experience according to Köppen’s classification?
A. Arid Climate (BWh)
B. Temperate Climate (Cwb)
C. Tropical Wet Climate (Af)
D. Montane Climate (ET)
Answer: (B) See the Explanation
The region of Himachal Pradesh experiences a temperate climate (Cwb) with moderate temperatures and winter rainfall due to western disturbances.
Q1: Explain the Köppen Climate Classification and its relevance in understanding India’s diverse climatic regions.
Answer: The Köppen Climate Classification is a globally recognized system that categorizes the world’s climates based on temperature and precipitation patterns. It divides climates into broad categories like tropical, dry, temperate, and polar. In India, Köppen’s classification helps in understanding the diverse climatic regions, from the tropical wet conditions of the Western Ghats to the arid conditions of the Thar Desert and the montane climate of the Himalayas.
This classification is crucial for studying the impact of climate on agriculture, water resources, and settlement patterns in India. It provides valuable insights into regional variations and helps policymakers design climate-adaptive strategies for development.
Q2: Discuss the characteristics and distribution of the tropical wet and dry climate in India according to Köppen’s classification.
Answer: The tropical wet climate (Am, Af) in India is found in the coastal regions of Kerala, West Bengal, and the Andaman and Nicobar Islands. This climate is characterized by high temperatures and heavy rainfall throughout the year, influenced by the monsoon winds.
The tropical dry climate (Aw) is prevalent in central and western India, including regions like Madhya Pradesh and Maharashtra. It experiences a distinct dry season during winters and high temperatures during summers. These regions rely on the monsoon rains for agriculture and face challenges related to water scarcity during the dry season.
Q3: How does Köppen’s climate classification help in understanding the challenges faced by regions with arid climates in India?
Answer: The arid climate (BWh, BWk) in India, found in the Thar Desert and parts of Gujarat, is characterized by very low rainfall and extreme temperatures. Köppen’s classification helps in identifying the unique challenges these regions face, such as water scarcity, drought, and limited agricultural potential.
Understanding the arid climate is crucial for developing sustainable water management practices, improving irrigation techniques, and promoting drought-resistant crops. It also aids in planning infrastructure development that can withstand the harsh climatic conditions of these regions.
Question: According to Köppen’s classification, which type of climate is found in the Thar Desert region of India?
A. Tropical Wet Climate
B. Arid Climate
C. Temperate Climate
D. Montane Climate
Answer: B
Explanation: The Thar Desert region of India has an arid climate (BWh), characterized by very low rainfall and extreme temperatures. This climate type is typical of desert regions.
Question: Analyze how Köppen’s classification of climates helps in understanding the climatic diversity of India and its impact on agriculture and water resources.
Explanation: Köppen’s climate classification provides a systematic approach to understanding the climatic diversity of India. By categorizing regions into tropical, temperate, and arid climates, it helps in analyzing the varying climatic conditions and their impact on agriculture and water resources. For example, regions with tropical wet climates benefit from monsoon rains, which support rice cultivation, while arid regions like Rajasthan struggle with water scarcity and rely on irrigation for agriculture. Understanding these climatic zones is crucial for climate-adaptive agricultural planning, efficient use of water resources, and addressing the challenges posed by climate change.
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