History of Asia

How are the seasons on Indian subcontinent marked?

The seasons on the Indian subcontinent, comprising India, Pakistan, Bangladesh, and parts of Nepal and Bhutan, are traditionally marked by changes in weather patterns, rainfall, and temperatures. The subcontinent experiences three significant seasons:

1. Winter (December to February):

- The winter season is characterized by generally pleasant and mild weather, with temperatures ranging from 10 to 25°C (50 to 77°F) in most regions.

- Northern parts of India experience cooler temperatures, with some areas even facing frost and snowfall, particularly in the Himalayan regions.

- Rainfall is minimal during this time, creating a dry spell across much of the subcontinent.

2. Summer (March to May):

- Summer brings rising temperatures, with averages ranging from 25 to 45°C (77 to 113°F) in many regions.

- Hot and dry winds known as "loo" prevail in Northern India, further elevating temperatures and causing discomfort.

- This season is relatively rain-free, except for isolated thunderstorms and occasional heat bursts.

3. Monsoon (June to September):

- The arrival of the southwest monsoon marks the start of the monsoon season, bringing with it heavy rainfall.

- Monsoon winds typically enter the subcontinent through the state of Kerala in Southern India and gradually spread across the entire region.

- The monsoon brings copious amounts of rainfall, creating lush greenery and providing water for agriculture. However, excessive rains sometimes result in flooding and disruptions.

- The monsoon tends to retreat from the subcontinent by September or October, leading to the transition into post-monsoon or autumn.

In between these primary seasons, the subcontinent experiences short transitional periods known as "spring" and "autumn" (or post-monsoon), which generally exhibit more moderate weather conditions.