HIMALDOC 19 records found  1 - 10next  jump to record: Search took 0.00 seconds. 
Year: 2019
Mass losses originating from supraglacial ice cliffs at the lower tongues of debris-covered glaciers are a potentially large component of the mass balance, but have rarely been quantified
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Year: 2016
We use high‐resolution digital elevation models (DEMs) from unmanned aerial vehicle (UAV) surveys to document the evolution of four ice cliffs on the debris‐covered tongue of Lirung Glacier, Nepal, over one ablation season
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Year: 2016
This study presents volume and mass changes of seven (five partially debris-covered, two debris-free) glaciers in the upper Langtang catchment in Nepal
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Year: 2016
Debris-covered glaciers are increasingly studied because it is assumed that debris cover extent and thickness could increase in a warming climate, with more regular rockfalls from the surrounding slopes and more englacial melt-out material
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Year: 2015
Meteorological studies in high-mountain environments form the basis of our understanding of catchment hydrology and glacier accumulation and melt processes, yet high-altitude (>4000 m above sea level, asl) observatories are rare
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Year: 2015
The hydrology of high-elevation watersheds of the Hindu Kush-Himalaya region (HKH) is poorly known
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Year: 2015
Debris-covered glaciers play an important role in the high-altitude water cycle in the Himalaya, yet their dynamics are poorly understood, partly because of the difficult fieldwork conditions
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Year: 2015
Air temperature is one of the most relevant input variables for snow and ice melt calculations
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Year: 2015
Debris-covered glaciers play an important role in the high-altitude water cycle in the Himalaya, yet their dynamics are poorly understood, partly because of the difficult fieldwork conditions
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Year: 2015
Spatial evolution of supraglacial debris cover on mountain glaciers is a largely unmonitored and poorly understood phenomenon that directly affects glacier melt
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HIMALDOC 19 records found  1 - 10next  jump to record: Search took 0.00 seconds. 
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