Yarlung Tsangpo’s Rainfall Paradox: Orographic Asymmetry and Monsoon Boundary Instability
雅鲁藏布江降水悖论:地形不对称性与季风边界不稳定性
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While southern slopes receive over 4,500 mm annually, the northern Yarlung Tsangpo valley averages less than 300 mm—yet recent decades show reversed precipitation anomalies in winter months.
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This inversion stems from weakened Himalayan thermal forcing, allowing mid-latitude cyclones to penetrate deeper than historically recorded.
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