Add to ORKGThe stable hydrogen and oxygen of lake, river, rain and snow waters were investigated to understand the water cycle characteristics of the drainage basin of Manasarovar Lake in Tibet. Both δD and δ <sup>18</sup>O of river water are larger than those of lake water and the effect of altitude on both δD and δ <sup>18</sup>O is not very significant. This phenomenon was suggested to occur because Manasarovar basin is located in Qinghai-Tibet Plateau which has low latitude, high altitude, abundant glaciers, thin air and intensive solar radiation, resulting in higher evaporation in lake water. © 2008 Springer-Verlag
Hydrogen isotope ratios of sedimentary biomarkers are known to record the climatic variability in te...
Lake level fluctuations are important features in paleo-reconstructions that can be linked to past c...
Although stable isotopes of hydrogen and oxygen in surface waters (especially in river waters) are u...
Abstract The stable hydrogen and oxygen of lake, river, rain and snow waters were investigated to un...
The stable hydrogen and oxygen of lake, river, rain and snow waters were investigated to understand ...
The integrated use of isotopic and hydrochemical tracers is an effective way to investigate hydrolog...
Qinghai Lake is one of China's national nature reserves and supports the ecological security of ...
The use of isotopic tracers is an effective approach for characterizing the moisture sources of prec...
The use of stable isotopes is a practical tool in the study of the lake water budget. This is an one...
Hydrological processes produce effects on water resources in inland mountainous regions. To perform ...
Stable water isotopes (delta O-18 and delta H-2) are an important source signature for understanding...
Lakes are regarded as important nodes in water resources, playing pivotal roles in the regional hydr...
Runoff generation and dynamics is an important issue in watershed and water resource management, but...
The integrated use of isotopic and hydrochemical tracers is an effective approach for investigating ...
On the Qinghai-Tibet Plateau (QTP), salinity, area, and altitude are the three main environmental gr...
Hydrogen isotope ratios of sedimentary biomarkers are known to record the climatic variability in te...
Lake level fluctuations are important features in paleo-reconstructions that can be linked to past c...
Although stable isotopes of hydrogen and oxygen in surface waters (especially in river waters) are u...
Abstract The stable hydrogen and oxygen of lake, river, rain and snow waters were investigated to un...
The stable hydrogen and oxygen of lake, river, rain and snow waters were investigated to understand ...
The integrated use of isotopic and hydrochemical tracers is an effective way to investigate hydrolog...
Qinghai Lake is one of China's national nature reserves and supports the ecological security of ...
The use of isotopic tracers is an effective approach for characterizing the moisture sources of prec...
The use of stable isotopes is a practical tool in the study of the lake water budget. This is an one...
Hydrological processes produce effects on water resources in inland mountainous regions. To perform ...
Stable water isotopes (delta O-18 and delta H-2) are an important source signature for understanding...
Lakes are regarded as important nodes in water resources, playing pivotal roles in the regional hydr...
Runoff generation and dynamics is an important issue in watershed and water resource management, but...
The integrated use of isotopic and hydrochemical tracers is an effective approach for investigating ...
On the Qinghai-Tibet Plateau (QTP), salinity, area, and altitude are the three main environmental gr...
Hydrogen isotope ratios of sedimentary biomarkers are known to record the climatic variability in te...
Lake level fluctuations are important features in paleo-reconstructions that can be linked to past c...
Although stable isotopes of hydrogen and oxygen in surface waters (especially in river waters) are u...