Table of Contents
THE INDIAN CLIMATIC CALENDAR
- In the case of India, IMD has categorized the following four annual seasons:
- The Winter Season (January – February)
- The Summer season (March-May)
- The Rainy Season (Southwest Monsoon Season)(June – September)
- The Autumn season (October – December)
Classical theories
- Considered the monsoon as land and sea breeze on a continental scale.
- Based on the apparent movement of the sun towards the tropic of cancer,
- Results in the creation of low-pressure systems around
- These winds caused heavy rainfall over the Indian subcontinent.
- During winter, the apparent movement of the sun towards the tropic of Capricorn.
- High-pressure regions over the Indian subcontinent.
- There is a change in the direction of the winds which
- Adheres to the broader principles of the monsoon.
The modern theories
- Taking into consideration various aspects of the monsoon
- The variable heating of land and sea,
- The geographical shape of the sub-continent,
- Lower and upper air circulations(jet streams) etc.
- The modern theories are influenced by the following factors:
- Differential Heating of the landmass.
- Role of the Jet Streams.
- The movement of the ITCZ.
- The Indian branch of the walker cell.
- The Indian Ocean Dipole.
- All these factors affect the onset, the intensity, and the variability of the monsoon.
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