Explanations:The southwest monsoon in India is a significant climatic phenomenon that brings substantial rainfall to the subcontinent. However, the distribution of this rainfall is not uniform across all regions. The Tamil Nadu coast experiences a dry season during the southwest monsoon, which is contrary to the general expectation of heavy rainfall during this period. To understand this phenomenon, it is essential to consider the geographical position of Tamil Nadu and the nature of the monsoon winds.
The southwest monsoon originates from the Arabian Sea and moves towards the Indian subcontinent, bringing moisture-laden winds that result in heavy rainfall in regions like Kerala, Karnataka, and parts of Maharashtra. However, the Tamil Nadu coast is situated in a position that does not receive the full impact of these monsoon winds. The Arabian Sea branch of the southwest monsoon is the primary source of moisture for the Indian subcontinent during this season, and it does not directly affect the Tamil Nadu coast.
The Bay of Bengal branch of the southwest monsoon, on the other hand, primarily affects the eastern coast of India, including regions like Odisha and West Bengal. The Tamil Nadu coast is not influenced by this branch of the monsoon, and therefore, the statements in the question that refer to the Bay of Bengal branch are incorrect.
The rainshadow effect is a phenomenon where the windward side of a mountain range receives heavy rainfall, while the leeward side remains dry due to the blocking of moisture-laden winds. This effect is more relevant to regions like the Western Ghats, which block the monsoon winds coming from the Arabian Sea. The Tamil Nadu coast does not experience the rainshadow effect from the Bay of Bengal branch of the southwest monsoon, as it is not in the path of these winds.
Therefore, the dry season in Tamil Nadu during the southwest monsoon is not due to the factors mentioned in the statements. The correct understanding is that the Tamil Nadu coast is not directly affected by the Bay of Bengal branch of the southwest monsoon, and the rainshadow effect is not a significant factor in this region. The dryness is primarily due to the geographical position of Tamil Nadu relative to the Arabian Sea branch of the monsoon.