Mountain water resources are of particular importance for downstream populations but are
threatened by decreasing water storage in snowpack and glaciers. Groundwater …

Abstract Changes in the mountain cryosphere impact the water security of downstream
societies and the resilience of water-dependent ecosystems and their services. However …

The cryosphere is defined by the presence of frozen water in its many forms: glaciers, ice
caps, ice sheets, snow, permafrost, and river and lake ice. In the extended Hindu Kush …

Groundwater flow through coarse blocky landforms contributes to streamflow in mountain
watersheds, yet its role in the alpine hydrologic cycle has received relatively little attention …

The mountain cryosphere and groundwater play pivotal roles in shaping the hydrological
cycle, yet their connectivity remains incompletely understood. Current knowledge on …

The hydrological characteristics of debris-covered glaciers are known to be fundamentally
different from those of clean-ice glaciers, even within the same climatological, geological …

The young water fraction (F yw*), defined as the fraction of catchment outflow with transit
times of less than 2–3 months, is increasingly used in hydrological studies that exploit the …

Abstract High Mountain Asia (HMA) is among the most vulnerable water towers globally and
yet future projections of water availability in and from its high‐mountain catchments remain …

Abstract We used End-Member Mixing Analysis (EMMA) to investigate the spatiotemporal
variability of source water contributions to streamflow generation from three headwater …

Quantifying the contributions of runoff components (CRCs) to streamflow is of significant
importance for understanding the dynamics of water resources under changing climate in …