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iss073e1025732
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iss073e1025732 (Oct. 18, 2025) --- The Himalayas separate mainland Asia from the Indian subcontinent, revealing an arid, desert-like terrain on the Asian side, known as the Tibetan Plateau. On the southern slopes of the mountain range, moist air rises, cools, and condenses, producing rainfall that supports a humid, subtropical climate. As the air descends on the northern slopes, it warms and dries, creating barren conditions due to the rain shadow effect.
NASA Image and Video Library’s own descriptionCredit lineiss073e1025732. NASA/JSC, 2025-10-18. Public domain. ID: iss073e1025732.