In many areas of the Loess Plateau, groundwater is too deep to extract, making meteoric water (snow and rain) the only viable water resource. Here we traced the rainwater and water vapor sources using the δ2H and δ18O signature of precipitation in the northern mountainous region of Yuzhong on the Loess Plateau. The local meteoric water line in 2016 and 2017 was defined as δ2H = 6.8 (±0.3)∙δ18O + 4.4 (±2.0) and δ2H = 7.1 (±0.2)∙δ18O + 1.5 (±1.6), respectively. The temperature and precipitation amount are considered to be the main factor controlling the δ2H and δ18O variation of precipitation, and consequently, relationships were first explored between δ18O and local surface air temperature and precipitation amount by linear regression analys...
The precipitation δ18O-elevation gradients are important for paleoclimate, hydrology, and paleo...
δ18O variability in daily precipitation at two stations (Lanzhou and Zhangye) north of the Qinling M...
Potential evapotranspiration (ET0) is an important part of regional hydrological cycle and energy cy...
In many areas of the Loess Plateau, groundwater is too deep to extract, making meteoric water (snow ...
In many areas of the Loess Plateau, groundwater is too deep to extract, making meteoric water (snow ...
A prerequisite for using isotopic techniques to study the regional water cycle of a mountainous area...
Stable water isotopes (delta O-18 and delta H-2) are an important source signature for understanding...
Evidence has indicated an overall wetting trend over the Three-Rivers Headwater Region (TRHR) in the...
textThe Loess Plateau in China is located in a typical summer rain region with a rainfall season. It...
National Natural Science Fund of China 50239050;State Key Laboratory of Soil Erosion and Dryland Fa...
Seasonal and interannual variations in precipitation stable isotopes are crucial for clarifying comp...
The variation in rainy season precipitation and its associated atmospheric water vapor transport dur...
National Natural Science Fund of China 50239050;State Key Laboratory of Soil Erosion and Dryland Fa...
Hydrological processes produce effects on water resources in inland mountainous regions. To perform ...
δ18O variability in daily precipitation at two stations (Lanzhou and Zhangye) north of the Qinling M...
The precipitation δ18O-elevation gradients are important for paleoclimate, hydrology, and paleo...
δ18O variability in daily precipitation at two stations (Lanzhou and Zhangye) north of the Qinling M...
Potential evapotranspiration (ET0) is an important part of regional hydrological cycle and energy cy...
In many areas of the Loess Plateau, groundwater is too deep to extract, making meteoric water (snow ...
In many areas of the Loess Plateau, groundwater is too deep to extract, making meteoric water (snow ...
A prerequisite for using isotopic techniques to study the regional water cycle of a mountainous area...
Stable water isotopes (delta O-18 and delta H-2) are an important source signature for understanding...
Evidence has indicated an overall wetting trend over the Three-Rivers Headwater Region (TRHR) in the...
textThe Loess Plateau in China is located in a typical summer rain region with a rainfall season. It...
National Natural Science Fund of China 50239050;State Key Laboratory of Soil Erosion and Dryland Fa...
Seasonal and interannual variations in precipitation stable isotopes are crucial for clarifying comp...
The variation in rainy season precipitation and its associated atmospheric water vapor transport dur...
National Natural Science Fund of China 50239050;State Key Laboratory of Soil Erosion and Dryland Fa...
Hydrological processes produce effects on water resources in inland mountainous regions. To perform ...
δ18O variability in daily precipitation at two stations (Lanzhou and Zhangye) north of the Qinling M...
The precipitation δ18O-elevation gradients are important for paleoclimate, hydrology, and paleo...
δ18O variability in daily precipitation at two stations (Lanzhou and Zhangye) north of the Qinling M...
Potential evapotranspiration (ET0) is an important part of regional hydrological cycle and energy cy...