Climate warming on the cryosphere could change catchment precipitation‐runoff relation by
additional water from glacier melting and more energy absorbed at the ground surface …

Uncertainty and parameter equifinality are important issues for hydrological models,
especially in cold mountainous regions where multiple runoff components enhance the …

This study integrated a water isotope module into the hydrological model THREW (Tsinghua
Representative Elementary Watershed) which has been successfully used in high and cold …

Issues related to large uncertainty and parameter equifinality have posed big challenges for
hydrological modeling in cold regions where runoff generation processes are particularly …

The southeastern part of the Tibetan Plateau (TP), one of the regions with the largest glacier
distribution on the plateau, has been experiencing a significant loss in glacier mass balance …

Tracer-aided hydrological models integrating water isotope modules into the simulation of
runoff generation are useful tools to reduce uncertainty of hydrological modeling in cold …

In cold and high-elevation mountainous catchments, climate and landscape vary with
elevation, which leads to elevational variability in runoff. The short-term variation and long …

Quantitative analysis of changes in Lhasa River runoff components was significant to local
water resources management. This study constructed the spatial processes in hydrology …

The major rivers on the Tibetan Plateau supply important freshwater resources to riparian
regions but have been undergoing significant climate change in recent decades …

Snowmelt runoff is an essential runoff component in alpine watersheds. On the Tibetan
Plateau, the complex hydrometeorological and underlying surface conditions make a single …