The Himalayas act as a barrier, preventing cold winds from Central Asia from entering India, resulting in a warmer climate.

The Western Ghats receive heavy rainfall due to the orographic effect, where moisture-laden winds from the Arabian Sea are forced to rise and condense.

The Thar Desert is located in a rain shadow region, where the Himalayas block the moisture-carrying winds from the Bay of Bengal, resulting in arid conditions.

Jaipur, located in the state of Rajasthan, is known for its hot and dry climate, with temperatures often exceeding 45 degrees Celsius during the summer months.

The differential heating between the land and sea creates a pressure gradient, causing winds to flow from the cooler ocean to the warmer land, resulting in the monsoon winds.

The Himalayas, being at a high altitude, experience cold temperatures throughout the year, with some regions even experiencing snowfall.

High sea surface temperatures in the Bay of Bengal provide the necessary energy for the formation and intensification of cyclones.

Kerala, located on the Malabar Coast, experiences high humidity due to its proximity to the Arabian Sea and the Western Ghats, which trap moisture-laden winds.

Low temperatures during the winter months cause water vapor in the air to condense, forming fog.

Mumbai, located on the west coast of India, receives heavy rainfall during the monsoon season due to its proximity to the Arabian Sea.

The Western Ghats were formed as a result of the collision between the Indian Plate and the Eurasian Plate.

The Thar Desert, being a dry and arid region, experiences low humidity.

The Gangetic Plain was formed by the deposition of sediments by the Ganges River and its tributaries.

Odisha, located on the east coast of India, experiences a high frequency of thunderstorms due to its proximity to the Bay of Bengal and the Western Ghats.

The Deccan Plateau was formed as a result of volcanic eruptions that occurred over millions of years.