The hydrological roles of glaciers and seasonal snow in the Indus, Ganges, Brahmaputra, Amu Darya, Syr Darya and Mekong basins are, for the first time, assessed comprehensively at a major river basin scale in this paper. Contribution of glacier runoff, subdivided into renewable and nonrenewable components, and seasonal snowmelt to mean annual flow is evaluated for two time slices: 1961-1990 and 2001-2010. The recent changes of the hydrological roles of glaciers and snow, and the most likely changes of those under future climate change are analyzed
River flow from glacierized areas in the Himalaya is influenced both by intra-annual variations in p...
Snow and ice in high mountains represent and important water resource in many parts of the world, es...
Himalayan headwaters supply large quantities of runoff derived from snowmelt and monsoon rainfall to...
This paper presents a comprehensive assessment of the water storage properties of glaciers and seaso...
A large number of Himalayan glacier catchments are under the influence of humid climate with snowfal...
Rivers originating in the high mountains of Asia are among the most meltwater-dependent river system...
Rising temperatures and changing precipitation patterns across the Hindu Kush–Himalaya (HKH) region ...
The spatial variation in observed and projected climate change is large and mountain ranges and thei...
In Asia, water resources largely depend on water generated in the mountainous upstream parts of seve...
The present study sets out to investigate the sensitivity of water availability to climate change fo...
Climate records for locations across the southern slope of the Himalaya between 77°E and 91°E were s...
The upper Indus River basin has large masses of glaciers that supply meltwater in the summer. Water ...
Streamflow in the Himalayan rivers is generated from rainfall, snow and ice. The distribution of run...
This is the publisher's version, also available electronically from http://onlinelibrary.wiley.com/d...
River flow from glacierized areas in the Himalaya is influenced both by intra-annual variations in p...
Snow and ice in high mountains represent and important water resource in many parts of the world, es...
Himalayan headwaters supply large quantities of runoff derived from snowmelt and monsoon rainfall to...
This paper presents a comprehensive assessment of the water storage properties of glaciers and seaso...
A large number of Himalayan glacier catchments are under the influence of humid climate with snowfal...
Rivers originating in the high mountains of Asia are among the most meltwater-dependent river system...
Rising temperatures and changing precipitation patterns across the Hindu Kush–Himalaya (HKH) region ...
The spatial variation in observed and projected climate change is large and mountain ranges and thei...
In Asia, water resources largely depend on water generated in the mountainous upstream parts of seve...
The present study sets out to investigate the sensitivity of water availability to climate change fo...
Climate records for locations across the southern slope of the Himalaya between 77°E and 91°E were s...
The upper Indus River basin has large masses of glaciers that supply meltwater in the summer. Water ...
Streamflow in the Himalayan rivers is generated from rainfall, snow and ice. The distribution of run...
This is the publisher's version, also available electronically from http://onlinelibrary.wiley.com/d...
River flow from glacierized areas in the Himalaya is influenced both by intra-annual variations in p...
Snow and ice in high mountains represent and important water resource in many parts of the world, es...
Himalayan headwaters supply large quantities of runoff derived from snowmelt and monsoon rainfall to...