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Timescale-dependent Westerlies-Monsoon interactions regulate holocene humidity and dust variability on the northeastern Tibetan Plateau
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DOI：10.1016/j.gr.2026.06.018.png)
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Abstract
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• Qaidam dust and humidity show timescale-dependent circulation controls. • Multi-millennial Qaidam humidity and dust is controlled by East Asian monsoon. • Qaidam humidity is influenced by the westerlies on millennial-scale. • Qaidam dust is forced by high-latitude forcing on millennial-scale. • Future decadal Qaidam humidity and dust is dominated by East Asian monsoon.
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