The Western Ghats, particularly the windward side, receives the highest rainfall during the southwest monsoon due to orographic uplift.

The distance from the sea plays a significant role in determining the amount of rainfall received in different regions during the monsoon.

North-Eastern India, particularly the state of Meghalaya, experiences the longest monsoon season due to its proximity to the Bay of Bengal.

The sudden onset of the monsoon in India is commonly referred to as the 'monsoon burst'.

North-Western India, particularly the state of Rajasthan, receives the lowest rainfall during the southwest monsoon due to its distance from the sea.

The southwest monsoon in India typically lasts for about 4 months, from June to September.

North-Western India, particularly the state of Rajasthan, experiences the highest variability in monsoon rainfall due to its location in the rain shadow region of the Western Ghats.

The gradual withdrawal of the monsoon from India is commonly referred to as the 'monsoon retreat'.

North-Eastern India, particularly the state of Meghalaya, receives the highest rainfall during the northeast monsoon due to its proximity to the Bay of Bengal.

The northeast monsoon in India typically lasts for about 2 months, from October to November.

The Western Ghats, particularly the windward side, experiences the lowest variability in monsoon rainfall due to its consistent exposure to the southwest monsoon winds.

The phenomenon of monsoon failure in India is commonly referred to as 'monsoon failure'.

North-Eastern India, particularly the state of Assam, is most prone to monsoon floods due to its location in the path of the southwest monsoon winds and the presence of major rivers.

The phenomenon of delayed onset of the monsoon in India is commonly referred to as 'monsoon delay'.

North-Eastern India, particularly the state of Assam, experiences the highest frequency of monsoon depressions due to its location in the path of the southwest monsoon winds.