Water stable isotopes (18O and 2H) are widely used as ideal tracers to track water through
the soil and to separate evaporation from transpiration. Due to the technical developments in …

The theoretical basis for application of stable isotope mass balance of lakes is described for
a range of climatic situations including low latitude, high latitude, high altitude, continental …

Renewable fresh water over continents has input from precipitation and losses to the
atmosphere through evaporation and transpiration. Global-scale estimates of transpiration …

Groundwater recharged by meteoric water supports human life by providing two billion
people with drinking water and by supplying 40% of cropland irrigation. While annual …

Global warming is considered a major threat to Earth's lakes water budgets and quality.
However, flow regulation, over-exploitation, lack of hydrological data, and disparate …

Stable water isotopes are widely used in ecohydrology to trace the transport, storage, and
mixing of water on its journey through landscapes and ecosystems. Evaporation leaves a …

Accurate quantification of evaporative losses to the atmosphere from surface water bodies is
essential for calibration and validation of hydrological models, particularly in remote arid and …

Understanding the influence of vegetation on water storage and flux in the upper soil is
crucial in assessing the consequences of climate and land use change. We sampled the …

Climate change is expected to alter hydrological and biogeochemical processes in high-
latitude inland waters. A critical question for understanding contemporary and future …

Stable isotope ratios of H and O are widely used to identify the source of water, eg, in
aquifers, river runoff, soils, plant xylem, and plant-based beverages. In situations where the …