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Stable isotopes of water are widely used in scientific research to reconstruct paleoclimate and paleoenviron- ment variations[1―4]. Atmospheric water vapor plays a keyrole in the precipitation events. Therefore, the isotopic composition of atmospheric water vapor has a direct effect upon that of precipitation[5,6]. Observation of stable isotope variation of atmospheric water vapor has an important significance to indicate the moisture origins andmoisture transport in the study area. Based on …  相似文献   

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