5 Conclusion
The water vapor content of the
air mass has a decisive influence on the evaporation of the reservoir.
The humid air mass from the southeast monsoon affects the area when the
evaporation is weak, and the dry air mass from the westerly wind affects
the area with strong evaporation. Evaporation from the reservoir has
obviously affected the precipitation in the area around the reservoir.
The impact range is related to the local atmospheric movement mode,
Evaporating water vapor affects the precipitation in high altitude areas
in the Xiying River Basin. Although the calculations regarding the
contribution of reservoir evaporation to local precipitation still has
significant uncertainties associated with the use of the stable isotope
algorithm, these uncertainties will be further reduced with an increase
of observation data and improvement of the algorithm itself.
Acknowledgements This research was financially supported by
National Natural Science Foundation of China (41661005, 41867030),
National Natural Science Foundation innovation research group science
foundation of China (41421061). We sincerely thank Marit Greenwood for
the writing suggestions and Language modification.
Data Availability The datasets generated and/or analyzed during
the current study are available from the corresponding author on
request.