The distribution of rainfall across India during the southwest monsoon season is notably uneven. This variation is influenced by several geographical and atmospheric factors. Let's analyze the options to understand the primary reasons for this unevenness.
The southwest monsoon, typically occurring from June to September, brings the majority of India's annual rainfall. However, the amount of rain received varies significantly from region to region. Some areas receive heavy rainfall, while others experience moderate or scanty rainfall.
This statement accurately explains a major reason for uneven rainfall distribution. India has significant mountain ranges like the Western Ghats and the Himalayas. The Western Ghats intercept the moisture-laden southwest monsoon winds coming from the Arabian Sea. This causes intense orographic rainfall on the western (windward) side of the Ghats, while the eastern (leeward) side receives much less rainfall. Similarly, the Himalayas affect the path and intensity of the monsoon winds moving northward, influencing rainfall patterns in the northern plains and the Himalayan foothills.
This is incorrect. The very concept of uneven distribution implies that monsoon winds do not bring the same amount of rain to all parts of the country. Factors like topography, distance from the sea, and atmospheric conditions cause significant variations.
This is an exaggeration and is incorrect. While the Himalayas significantly influence the monsoon, they do not stop all rainfall. They are crucial for generating rainfall on their southern slopes and play a role in determining the monsoon's extent and intensity over the subcontinent.
This is factually incorrect. Rainfall during the southwest monsoon is received across large parts of India, including the north, central, and northeastern regions, not just the southern states. The distribution is uneven, but not confined to one region.
Based on the analysis, the influence of major mountain ranges on the direction and intensity of monsoon winds is a key factor causing the uneven distribution of rainfall experienced in India during the southwest monsoon season. These geographical features create distinct rainfall patterns, leading to wet windward sides and dry leeward sides, significantly impacting regional climates.