The climate of India is influenced by a combination of factors, including latitude, altitude, distance from the sea, and the presence of mountain ranges.

Southern India, particularly the Malabar Coast, experiences a tropical wet and dry climate, characterized by heavy rainfall during the monsoon season and dry conditions during the rest of the year.

The Thar Desert is a hot desert climate zone, characterized by extremely high temperatures, low precipitation, and sparse vegetation.

The Himalayas act as a barrier to the cold winds from Central Asia, preventing them from reaching Northern India and influencing its climate.

Cherrapunji in Meghalaya is renowned for receiving the highest rainfall in the world, making it a region with exceptionally heavy rainfall.

Shimla, located in the foothills of the Himalayas, experiences a Mediterranean climate, characterized by hot, dry summers and mild, wet winters.

The climate of the Andaman and Nicobar Islands is influenced by the Bay of Bengal, which brings heavy rainfall during the monsoon season.

North-Eastern India, particularly the states of Sikkim and Arunachal Pradesh, experiences a temperate oceanic climate, characterized by moderate temperatures and abundant rainfall.

The Western Ghats act as a barrier to moisture-carrying winds from the Arabian Sea, causing heavy rainfall on the windward side and a rain shadow effect on the leeward side.

Fog formation in the Ganga-Brahmaputra plains during winter is influenced by a combination of high humidity, low temperatures, and lack of wind.

The Lakshadweep Islands experience a tropical monsoon climate, characterized by heavy rainfall during the monsoon season and moderate temperatures throughout the year.

Rajasthan, Gujarat, and Madhya Pradesh experience a semi-arid climate, characterized by low rainfall and high temperatures.

The climate of the Eastern Ghats is influenced by the Bay of Bengal, which brings heavy rainfall during the monsoon season.

North-Eastern India, particularly the state of Assam, experiences a humid subtropical climate, characterized by hot, humid summers and mild, dry winters.

The climate of the Andaman and Nicobar Islands is influenced by the Bay of Bengal, which brings heavy rainfall during the monsoon season.