HIMALDOC 27 records found  1 - 10nextend  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: 2018
Abstract Debris surface temperature is a function of debris characteristics and energy fluxes at the debris surface
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Year: 2017
Over Saint-Sorlin Glacier in the French Alps (45° N, 6
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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
We present a basic ablation model combining a positive degree-day approach to calculate melting and a simple equation based on wind speed to compute sublimation
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Year: 2016
Three debris-free glaciers of various areas have been monitored for the last 5 to 8 years in Everest region (Central Himalaya, Nepal) and their annual glacier-wide mass balances (Ba) obtained from the glaciological method strongly differ
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Year: 2016
Approximately 25 % of the glacierized area in the Everest region is covered by debris, yet the surface mass balance of debris-covered portions of these glaciers has not been measured directly
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Year: 2016
We present the updated glaciological mass balance (MB) of Chhota Shigri Glacier, the longest continuous annual MB record in the Hindu-Kush Karakoram Himalaya (HKH) region
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Year: 2016
Debris-covered glaciers occupy more than 1/4 of the total glacierized area in the Everest region of Nepal, yet the surface mass balance of these glaciers has not been measured directly
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Year: 2015
Although vital for millions of inhabitants, Himalayan water resources remain currently poorly known, mainly because of uncertainties on hydro-meteorological measurements
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HIMALDOC 27 records found  1 - 10nextend  jump to record: Search took 0.00 seconds. 
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