Detailed Summary
The Southwest Monsoon Season stretches from June to September and is a critical period in India’s climatic calendar. The season commences with the onset of monsoon winds originating from the Indian Ocean, which gives rise to heavy rainfall across most parts of the country. This season is notably divided into two main branches: the Arabian Sea branch and the Bay of Bengal branch.
The Arabian Sea branch primarily affects the western coast, bringing substantial rains to states like Kerala and Maharashtra, while the Bay of Bengal branch influences the eastern regions, impacting states such as Odisha and West Bengal.
A significant aspect of the monsoon phenomenon is the orographic rainfall experienced along the Western Ghats. As moist air ascends over these mountains, it cools and condenses, resulting in heavy precipitation on the windward side. The intricate relationship between these wind patterns and the region's topography is crucial in determining rainfall distribution during this season. Understanding the dynamics of the Southwest Monsoon is essential due to its significant impact on agriculture, water supply, and local economies.