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Stable isotope composition of precipitation in the south and north slopes of Wushaoling Mountain, northwestern China
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文摘

Spatial-temporal difference for isotope caused by altitude and sub-cloud evaporation.

Temperature effect and altitude effect are both significant with seasonal variations.

Quantified the sub-cloud evaporation's influence on δ18O composition.

Some depleted δ18O and δD caused by monsoonal moisture and rainout process.

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