Abstract
In the Qaidam Basin, a harsh environment limits precipitation observations, which hinders the understanding of the hydrological cycle. This study compared and discerned the applicability of 11 general circulation models (GCMs) simulating δ18O and δ2H in precipitation in the Qaidam basin and tracked the water vapor backward trajectory by the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT). The LDMZ (nudged) model is most applicable in the study area. The moisture sources are the Westerlies and inland recycled moisture. This study can improve the understanding of the adaptability of GCMs in the arid alpine zone and the hydrological cycle in the Tibetan Plateau.
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Data availability
All meteorological data used during this study are available from the China Meteorological Data Service Center at http://data.cma.cn/. Simulations of hydrogen and oxygen stable isotopes in precipitation used during this study can be downloaded from https://data.giss.nasa.gov/swing2/. Observations of hydrogen and oxygen stable isotopes in precipitation used during this study are available from Tibetan Network for Isotopes in Precipitation dataset as cited by Yao et al. (2013). GDAS1 data from NCEP/NCAR are available from National Oceanic and Atmospheric Administration at https://www.noaa.gov/.
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This work was funded by the National Natural Science Foundation of China (Grant/Award Number: 517037511 and 42101021).
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Conceptualization, XZ and TW; methodology and analysis, XZ, TW, FM, and LH; writing-original draft preparation, XZ; writing-review and editing, JC, JC, and TW; supervision, JC. All authors have read and agreed to the published version of the manuscript.
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Zhang, X., Chen, J., Chen, J. et al. Simulating precipitation stable isotopes and tracking moisture sources in Qaidam Basin combining GCMs and HYSPLIT. J Radioanal Nucl Chem 332, 4877–4888 (2023). https://doi.org/10.1007/s10967-023-09180-0
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DOI: https://doi.org/10.1007/s10967-023-09180-0