Deuterium‐excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling

@article{Cui2017DeuteriumexcessDO,
  title={Deuterium‐excess determination of evaporation to inflow ratios of an alpine lake: Implications for water balance and modeling},
  author={Jiangpeng Cui and Lide Tian and Trent Wade Biggs and Rong Wen},
  journal={Hydrological Processes},
  year={2017},
  volume={31},
  pages={1034 - 1046}
}
  • J. CuiL. Tian R. Wen
  • Published 28 February 2017
  • Environmental Science
  • Hydrological Processes
The numerous lakes on the Tibetan Plateau play an important role in the regional hydrological cycle and water resources, but systematic observations of the lake water balance are scarce on the Tibetan Plateau. Here, we present a detailed study on the water cycle of Cona Lake, at the headwaters of the Nujiang‐Salween River, based on 3 years (2011–2013) of observations of δ18O and δ2H, including samples from precipitation, lake water, and outlet surface water. Short‐term atmospheric water vapor… 

Figures and Tables from this paper

Insight into the stable isotopic composition of glacial lakes in a tropical alpine ecosystem: Chirripó, Costa Rica

Tropical high‐elevation lakes are considered sentinels of global climate change. This work characterizes the hydrological conditions of tropical alpine glacial lakes located in the highlands of

Variability of Stable Isotope in Lake Water and Its Hydrological Processes Identification in Mt. Yulong Region

Lakes are regarded as important nodes in water resources, playing pivotal roles in the regional hydrological cycle. However, the systematic study on lake water balance is scarce in Mt. Yulong region.

Hydrogen and Oxygen Isotope Composition and Water Quality Evaluation for Different Water Bodies in the Ebinur Lake Watershed, Northwestern China

Wetlands are sensitive indicators of climate change and have a profound impact on the supply of water resources in surrounding areas. In this study, the hydrochemical, isotopic characteristics (δ18O

Estimation of evaporation losses based on stable isotopes of stream water in a mountain watershed

Water stable isotopes (δ2H and δ18O) can record surface water evaporation, which is an important hydrological process for understanding watershed structure and function evolution. However, the

Identifying evaporation fractionation and streamflow components based on stable isotopes in the Kaidu River Basin with mountain–oasis system in north‐west China

Based on stable isotopes in stream water, groundwater, and meltwater in the Kaidu River Basin, NW China, we estimated the evaporation enrichment of stable oxygen isotopes in different types of water

Using stable isotopes to illuminate thermokarst lake hydrology in permafrost regions on the Qinghai‐Tibet plateau, China

Thermokarst lakes are widespread and developing on the Qinghai‐Tibet Plateau (QTP), and they have modified hydrological processes and water balance in the region. Despite increasing attention, our

Identifying surface water evaporation loss of inland river basin based on evaporation enrichment model

Accurately quantifying the evaporation loss of surface water is essential for regional water resources management, especially in arid and semi‐arid areas where water resources are already scarce. The

References

SHOWING 1-10 OF 68 REFERENCES

Evaporative enrichment of oxygen-18 and deuterium in lake waters on the Tibetan Plateau

Stable isotopes (δ18O and δD) are useful tracers for investigating hydrologic and climatic variability on a variety of temporal and spatial scales. Since the early isotopic studies on mountainous

Lake Water Isotope Variation Linked with the In-Lake Water Cycle of the Alpine Bangong Co, Arid Western Tibetan Plateau

ABSTRACT Water isotopes play an important role in the study of the alpine lake water budget and the hydrological cycle in the arid, far western Tibetan Plateau. These isotope records, derived from

Isotopic variation in the lake water balance at the Yamdruk‐tso basin, southern Tibetan Plateau

The use of stable isotopes is a practical tool in the study of the lake water budget. This is an one way to study the hydrological cycle in the large numbers of inland lakes on the Tibetan Plateau,

Evaporative enrichment of stable isotopes (δ18O and δD) in lake water and the relation to lake-level change of Lake Qinghai, Northeast Tibetan Plateau of China

Stable isotopic compositions (δ18O and δD) have been utilized as a useful indicator for evaluating the current and historical climatic and environmental changes. Therefore, it is vital to understand

Estimation of Evaporation from Cona Lake in the Central Tibetan Plateau Using an Isotope-based Method

The isotope-based methods are often used for estimating water balance of a lake.Such isotope-based methods,which primarily rely on water sampling and isotopic analysis,require regional background

Tracing contributions to hydro‐isotopic differences between two adjacent lakes in the southern Tibetan Plateau

Hydrological processes of lakes in the Tibetan Plateau are an important indicator of climate change. Due to the high elevation, inaccessibility and limited availability of historical observations,

Quantifying groundwater dependence of a sub-polar lake cluster in Finland using an isotope mass balance approach

A stable isotope study of 67 kettle lakes and ponds situated on an esker aquifer (90 km 2 ) in northern Finland was carried out to determine the role and extent of groundwater inflow in

Comparisons of observed and modelled lake δ18O variability

...