Deglaciation in high mountain areas signifies the transition from glacial to periglacial conditioned landscapes. Due to the reduced melt rate of debris-covered glacier ice, these areas of the glacier may persist long after the surrounding glacier has ...
Fabian Fleischer +5 more
doaj +1 more source
Origin and significance of 'dispersed facies' basal ice: Svínafellsjökull, Iceland [PDF]
Dispersed facies basal ice - massive (i.e. structureless) ice with dispersed debris aggregates - is present at the margins of many glaciers and, as a product of internal glacial processes, has the potential to provide important information about the ...
Nicholas G. Midgley (7190381) +15 more
core +1 more source
Spatial patterns in glacier characteristics and area changes from 1962 to 2006 in the Kanchenjunga–Sikkim area, eastern Himalaya [PDF]
This study investigates spatial patterns in glacier characteristics and area changes at decadal scales in the eastern Himalaya – Nepal (Arun and Tamor basins), India (Teesta basin in Sikkim) and parts of China and Bhutan – based on various satellite ...
A. E. Racoviteanu +3 more
doaj +1 more source
A number of glaciological observations on debris-covered glaciers around the globe have shown a delayed length and mass adjustment in relation to climate variability, a behavior normally attributed to the ice insulation effect of thick debris layers ...
Daniel Falaschi +11 more
doaj +1 more source
Brief communication: Thinning of debris-covered and debris-free glaciers in a warming climate [PDF]
Recent geodetic mass-balance measurements reveal similar thinning rates on glaciers with or without debris cover in the Himalaya–Karakoram region. This comes as a surprise as a thick debris cover reduces the surface melting significantly due to its ...
A. Banerjee
doaj +1 more source
Debris-covered glacier systems and associated glacial lake outburst flood hazards:Challenges and prospects [PDF]
Glaciers respond sensitively to climate variability and change, with associated impacts on meltwater production, sea-level rise and geomorphological hazards.
Glasser, N.F. +9 more
core +1 more source
GlacierNet: A Deep-Learning Approach for Debris-Covered Glacier Mapping [PDF]
Rising global temperatures over the past decades is directly affecting glacier dynamics. To understand glacier fluctuations and document regional glacier-state trends, glacier-boundary detection is necessary. Debris-covered glacier (DCG) mapping, however, is notoriously difficult using conventional geospatial technology methods.
Zhiyuan Xie +5 more
openaire +2 more sources
Glaciological results of the 2005 expedition to Inylchek Glacier, Central Tian Shan [PDF]
Like many other glaciers in Central Asia, Southern Inylchek glacier in the Kyrgyz Tian Shan is covered by supraglacial moraine, which drastically influences melt rates and complicates the estimation of ablation. The quantification of sub-debris melt from
Lambrecht, Astrid +4 more
core +1 more source
Landforms and sediments developed during the recent recession of debris-covered Ponkar Glacier, Nepal [PDF]
Understanding the evolution of debris-covered glaciers in High Mountain Asia, the physical processes governing the effect of debris cover on mass balance, and the response of debris-covered glaciers to climatic change are key for assessing water ...
Glasser, N.F. +11 more
core +1 more source
Representing moisture fluxes and phase changes in glacier debris cover using a reservoir approach
Due to the complexity of treating moisture in supraglacial debris, surface energy balance models to date have neglected moisture infiltration and phase changes in the debris layer.
Essery, Richard +17 more
core +1 more source

