While ocean currents can influence local climate patterns, they are not a primary determinant of India's overall climate, which is primarily shaped by latitude, altitude, and distance from the sea.

The Tropical Monsoon climate zone, found in much of India, experiences hot and humid summers due to the influence of the monsoon winds, while winters are generally mild.

Southern India, particularly the state of Tamil Nadu, experiences a Mediterranean climate due to its proximity to the Arabian Sea and the influence of the Western Ghats mountain range.

The Thar Desert region in India experiences a hot and dry climate throughout the year, with minimal rainfall and high temperatures.

The Temperate Continental climate zone, found in parts of North India, experiences distinct seasons, with warm summers and cold winters due to its distance from the moderating influence of the sea.

Ladakh, a region in the northern part of India, experiences a cold desert climate due to its high altitude and distance from the sea.

The differential heating of land and sea surfaces during summer months is a primary factor contributing to the formation of the Indian monsoon.

Mawsynram, a town in Meghalaya, holds the record for receiving the highest annual rainfall in the world.

The Tropical Wet and Dry climate zone, found in parts of Southern India, experiences moderate temperatures throughout the year and abundant rainfall during the monsoon season.

Kolkata, West Bengal, experiences a humid subtropical climate due to its proximity to the Bay of Bengal and the influence of the monsoon winds.

While the Indian monsoon can influence crop production, it is not a direct consequence of the monsoon itself.

The Deccan Plateau region in India experiences a semi-arid climate due to its distance from the sea and the rain-shadow effect of the Western Ghats.

The Temperate Continental climate zone, found in parts of North India, experiences cold winters and mild summers, with moderate rainfall throughout the year.

The Andaman and Nicobar Islands experience a tropical rainforest climate due to their proximity to the equator and the influence of the monsoon winds.

Blizzards are not a characteristic of the Indian monsoon, which is primarily associated with heavy rainfall, thunderstorms, and seasonal wind reversals.