Alpine catchments are important sources of fresh water but compared to lower altitude
catchments our understanding of the hydrological functioning of these catchments during …

We analysed contributions to run‐off using hourly stream water samples from seven
individual melt‐induced run‐off events (plus one rainfall event) during 2011, 2012 and 2013 …

Assessing temporal variations in soil water flow is important, especially at the hillslope scale,
to identify mechanisms of runoff and flood generation and pathways for nutrients and …

Climatic trends and anthropogenic changes in land cover and land use are impacting the
hydrology and water quality of streams at the field, watershed, and regional scales in …

Alpine shrubs and soils in catchments of the headwaters of the Yangtze River in west China
are very important for reducing flooding and sustaining base flow during the summer …

The transmission of water through soil is one of the critical links to reflect the hydrological
process. At present, there are controversies about the infiltration of farmland irrigation water …

Precipitation infiltration and evaporation are the main controlling factors on soil water
content (SWC) in the Chinese Loess Plateau (CLP). However, the temporal and spatial …

Shallow saturated subsurface flow is a dominant runoff mechanism on hillslopes of
headwater catchments under humid temperate climate. Its timing and magnitude is …

The prevailing opinion on the temporal origin of water in a hillslope stormflow hydrograph is
that the pre-event water represents a dominant fraction. Such conclusion is usually based on …

We examined the contributions of bedrock groundwater to the upscaling of storm‐runoff
generation processes in weathered granitic headwater catchments by conducting detailed …