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Answer: The Himalayas and the Indian Ocean are the two great controls of the climate of India.
The Himalayas:
- They stop the very cold winds of Central Asia from entering India, so the north Indian plains do not have very severe winters.
- They obstruct the south-west monsoon winds and force them to rise, causing heavy rainfall on their southern slopes and over the northern plains; Ladakh and Tibet remain dry (rain-shadow).
- Because the monsoon winds are held back by the Himalayas, rainfall extends over the whole of north India.
- Their snow and glaciers feed the Indus, Ganga and Brahmaputra, which are perennial.
The Indian Ocean:
- In summer the Indian landmass gets intensely heated and a low-pressure area develops over it (especially over north-west India), while the pressure over the Indian Ocean is relatively high. Hence moisture-laden south-west monsoon winds blow from the ocean towards the land and bring most of India's rainfall.
- In winter the land cools and high pressure forms over it, while pressure over the ocean is lower, so the dry north-east winds blow from land to sea; they pick up moisture over the Bay of Bengal and give rain to the Tamil Nadu coast.
- It moderates the temperature of the coastal and peninsular parts, so the range of temperature there is small.
- Tropical cyclones form over the Bay of Bengal and the Arabian Sea and affect the east and west coasts.
The importance of Himalayas and the Indian Ocean with respect to the climate of India can be explained as follows :
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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