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Quantifying the controls of spatiotemporal variations in precipitation isotopes across Southeast Asia
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DOI：10.1016/j.epsl.2026.120248.png)
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Abstract
En 中文
• Integrated observations and isotope-enabled simulations in Southeast Asia. • Upstream rainout and source vapor δ¹⁸O are dominant controls. • Regional convection plays a stronger role than moisture source shifts. • Responses of precipitation δ¹⁸O to large-scale climate modes vary spatially.
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