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Thornthwaite climate classification of India| Climatic regions UPSC | Geography of India| UPSC | UP-PCS | State PCS

Thornthwaite climate classification of India:

The following are the important points of Thornthwaite climatic classification:

  • Thornthwaite presented climate classification in 1931, 1933, and 1948.
  • In his 1933 presentation; gave the concept o precipitation effectiveness and temperature effectiveness.
  • In his 1948 concept; gave the potential evapotranspiration concept

Evapotranspiration:
 Combined, evaporation from the soil and transpiration from vegetation is called Evapotranspiration.

Precipitation effectiveness:

Plants' growth is not only dependent on precipitation but precipitation effectiveness.
Precipitation effectiveness P/E ratio=total monthly precipitation/ Evapotranspiration
P/E index= sum of 12-month P/E ratio.


Based on the P/E index, Thornthwaite classified five humidity regions:

  • A ( P/E index>128)- Wet- Rainforest.
  • B( P/E Index 64 to 127) - Humid- Forest
  • C( P/E index 32 to 63)- Subhumid - Grassland.
  • D(P/E index 16-32)- Semi Arid-Steppe
  • E(P/E index less than 16)- Arid-Desert

Rainfall variation measures in the following alphabet:
r= rainfall all the year
s= rainfall deficient in summer
w= rainfall deficient in winter
d=rainfall deficient all over the year.

Temperature efficiency:

Temperature efficiency is calculated mean average temperature through the years.

Based on Temperature efficiency:

  • A' tropical: T/E index more than 128.
  • B' Subtropical: T/E index 64-127.
  • C' Temperate: T/E index 32 - 63
  • D' Taiga: T/E index 16-31
  • E' Tundra: T/E index 1-15.
  • F' Frost: T/E index 0.

Based on the above three-category variable:

  • Precipitation effectiveness, rainfall variation, and temperature effectiveness, there are 32 main climatic regions and 120 subs climatic regions of the world. 
  • India has been divided into 12 climatic regions.
Thornthwait was criticized for making climatic classification complex. To make it simple,  Thornthwait gave the evapotranspiration concept to derive a climatic region in 1948
The main concept of Thornthwaite's climate classification of evapotranspiration is water balance. Rainforest and humid regions are water-surplus regions and semi-arid and arid regions are water-deficient regions.
  • A: Per humid
  • B: Humid
  • C1: Moist Sub Humid
  • C2: Dry Sub Humid
  • D: Semi-Arid
  • E: Arid
Thornthwaite climate classification of India



The following are the climatic division of India as per the Thornthwaite concept of Evapotranspiration.
Per Humid( A) region of India:
  • Western Ghats
  • Most parts of the NorthEastern States
Humid(B) region of India:
  • Adjoining region of the Perhumid region
Moist Sub Humid(C1) climatic region
  • Narrow belt Adjoining region of the humid region of Western Ghats.
  • Eastern India comprises West Bengal and Orissa
Dry Sub Humid(C2) regions:
  • Northern Narrow belt of the Ganga basin.
  • Part of Uttar Pradesh, Bihar, MP, Chhattisgarh, Jharkhand
  • Western Maharastra and Southern Gujarat
Semi-Arid(D) climatic region:
  • Part of Punjab and Haryana
  • Eastern part of Rajasthan, Maharashtra, Karnataka, Lenangna
  • Western Pat of Tamilnadu.
Arid climatic( E) region of India:

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