Explanation:

India's climate is strongly influenced by the Himalayas and the Thar Desert. The Himalayas along with the Hindu Kush mountains in Pakistan prevent cold Central Asian katabatic winds from blowing in keeping the bulk of the Indian subcontinent warmer than most locations at the similar latitudes. Simultaneously the Thar Desert plays a role in attracting moisture-laden southwest summer monsoon winds that, between June and October provide the majority of India's rainfall.