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 hydrological regimes for the major river basins in the Tibetan Plateau (TP), including the
source regions of the Yellow (UYE), Yangtze (UYA), Mekong (UM), Salween (US) …

A large number of Himalayan glacier catchments are under the influence of humid climate
with snowfall in winter (November–April) and south-west monsoon in summer (June …

The effect of climate change on snow water equivalent, snowmelt runoff, glacier melt runoff
and total streamflow and their distribution is examined for the Spiti river. This is a high …

Streamflow in the Himalayan rivers is generated from rainfall, snow and ice. The distribution
of runoff produced from these sources is such that the streamflow may be observed in these …

In the present study, degree–day factors for snow and ice were determined over Dokriani
Glacier located in the Garhwal Himalayas. The field experiments were made at an altitude of …

Discharge measurements, precipitation observations and hydrochemical samples from
catchments of the Callejon de Huaylas watershed draining the Cordillera Blanca to the Rio …

The contribution of snow and glacier-melt runoff to Himalayan rivers is significant and an
estimation of the amount is necessary for the development, planning, and management of …

The continuous increase in the emission of greenhouse gases has resulted in global
warming, and substantial changes in the global climate are expected by the end of the …

Diurnal variations in discharge and suspended sediment concentration (SSC), including
runoff delaying characteristics, have been studied for the Gangotri Glacier, the largest …