Results 51 to 60 of about 5,892 (191)
Debris-cover impact on glacier melting in the Upper Indus Basin
Out of 4530 glaciers covering ∼4770 km2 in the Upper Indus Basin, viz., Chenab, Zanaskar and Suru sub-basins, we selected topographically and morphologically homogeneous set of 98 glaciers; 56 debris-covered and 42 clean to assess the impact of debris ...
Dar, Reyaz Ahmad +2 more
core +1 more source
Many of the glaciers in the Nepalese Himalaya are partially covered in a layer of loose rock known as debris cover. In the Dudh Koshi River Basin, Nepal, approximately 25% of glaciers are debris‐covered.
Emily R. Potter +4 more
doaj +1 more source
Reduced melt on debris-covered glaciers: investigations from Changri Nup Glacier, Nepal [PDF]
Abstract. 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. In this study, ground-based measurements of surface elevation and ice depth are combined with terrestrial photogrammetry and unmanned aerial vehicle (UAV ...
Christian Vincent +10 more
openaire +9 more sources
Air temperature distribution and energy balance modelling of a debris-covered glacier
Near-surface air temperature is an important determinant of the surface energy balance of glaciers that is often represented by constant linear temperature gradients in models.
Brock, B.W. +13 more
core +1 more source
Many debris-covered glaciers are broadly distributed across High Mountain Asia and have made a number of contributions to water circulation for Qinghai-Tibet Plateau (QTP).
Liye Yang +4 more
doaj +1 more source
Debris-covered glacier energy balance model for Imja–Lhotse Shar Glacier in the Everest region of Nepal [PDF]
Debris thickness plays an important role in regulating ablation rates on debris-covered glaciers as well as controlling the likely size and location of supraglacial lakes.
D. R. Rounce +2 more
doaj +1 more source
Debris‐covered glaciers and rock glaciers in the nanga parbat himalaya, pakistan [PDF]
The origin and mobilization of the extensive debris cover associated with the glaciers of the Nanga Parbat Himalaya is complex. In this paper we propose a mechanism by which glaciers can form rock glaciers through inefficiency of sediment transfer from glacier ice to meltwater.
John F. Shroder +3 more
openaire +1 more source
Debris-covered glaciers present significant challenges for accurately mapping and monitoring glacier dynamics, particularly in regions like the Eastern Pamir Plateau.
Aamir Feroz +5 more
doaj +1 more source
Pluri-decadal (1955–2014) evolution of glacier–rock glacier transitional landforms in the central Andes of Chile (30–33° S) [PDF]
Three glacier–rock glacier transitional landforms in the central Andes of Chile are investigated over the last decades in order to highlight and question the significance of their landscape and flow dynamics.
S. Monnier, C. Kinnard
doaj +1 more source
Modelling climate sensitivity of debris-covered glaciers
The common occurrence of debris-covered glaciers in high-mountain areas makes their response to climate change relevant. The insulating effect of debris cover on surface melt causes debris-covered glaciers behave differently from debris-free glaciers, warranting the use of a specialized model for predictions.
openaire +1 more source

