The monsoon season in India typically lasts from June to September and is known for its heavy rainfall and thunderstorms.

The seasonal reversal of wind patterns, known as the monsoon winds, is the primary factor responsible for the formation of monsoons in India.

North-Eastern India, particularly the states of Meghalaya and Arunachal Pradesh, receives the highest rainfall during the monsoon season.

The term 'Rising Temperatures' is used to describe the gradual increase in temperature during the summer season in India.

Rajasthan, particularly the city of Churu, experiences the hottest summer temperatures in India.

The term 'Cold Front' is used to describe the cold wave that affects North India during the winter season.

Jammu and Kashmir, particularly the city of Leh, experiences the coldest winter temperatures in India.

The term 'Post-Monsoon' is used to describe the transition period between the monsoon season and the winter season in India.

Coastal Karnataka, particularly the city of Mangalore, experiences the most pleasant weather during the post-monsoon season.

The term 'Loo' is used to describe the warm wind that blows from the Arabian Sea during the summer season in India.

Mumbai, due to its coastal location, experiences the highest humidity levels during the monsoon season.

The term 'Cold Snap' is used to describe the sudden drop in temperature that occurs during the winter season in India.

Himachal Pradesh, particularly the city of Shimla, experiences the most snowfall during the winter season.

The term 'Frost' is used to describe the phenomenon that occurs when the temperature drops below the freezing point and water vapor in the air condenses directly into ice crystals.

Punjab, particularly the city of Amritsar, experiences the most fog during the winter season.