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Akademický článek
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Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Debris on glaciers is sourced by the erosion of the surrounding ice-free rockwalls. Where the supply of debris relative to that of snow is high, glaciers tend to develop a significant debris cover, which influences their surface mass balance. Therefo
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::173a104cd8900e3d7c6337b9b0e09592
Akademický článek
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This data publication is supplementary to the study on headwall erosion rates at Glacier d'Otemma in Switzerland, by Wetterauer et al. (in press). Debris on glacier surfaces stems from steep bedrock hillslopes that tower above the ice, so-called head
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______156::417b38dceb5209348c9146df90c6415c
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011811
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011811
Autor:
Dennis, D., Scherler, D.
The stochastic erosion in-situ cosmogenic nuclide model is a 1D numerical model that simulates the evolution of the concentrations of in situ-produced Be-10, C-14, and He-3 alongside the bedrock thermal field in the shallow Earth surface. It is usefu
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https://explore.openaire.eu/search/publication?articleId=od_______156::aed2e31128b89a9f826b8cf392ad0582
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011812
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011812
The DFG Priority Program 1803 “EarthShape” (www.earthshape.net) investigates Earth surface shaping by biota. As part of this project, we present Light Detection and Ranging (LiDAR) data of land surface areas for the four core research sites of th
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https://explore.openaire.eu/search/publication?articleId=od_______156::32d6d4d07f86eeb6741a707bbd55cd0b
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011871
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011871
These datasets were used to evaluate the main controls on last ~6 million years erosion rate variability of the northwestern Himalaya. The Earth’s climate has been cooling during the last ~15 million years and started fluctuating between cold and w
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https://explore.openaire.eu/search/publication?articleId=od_______156::7f2e3beea08b3d2ba67b8eb70c4820b9
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5007635
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5007635
Autor:
Scherler, D., Egholm, D. L.
Publikováno v:
Journal of Geophysical Research: Earth Surface
Scherler, D & Egholm, D L 2020, ' Production and Transport of Supraglacial Debris : Insights From Cosmogenic 10 Be and Numerical Modeling, Chhota Shigri Glacier, Indian Himalaya ', Journal of Geophysical Research: Earth Surface, vol. 125, no. 10, e2020JF005586 . https://doi.org/10.1029/2020JF005586
Scherler, D & Egholm, D L 2020, ' Production and Transport of Supraglacial Debris : Insights From Cosmogenic 10 Be and Numerical Modeling, Chhota Shigri Glacier, Indian Himalaya ', Journal of Geophysical Research: Earth Surface, vol. 125, no. 10, e2020JF005586 . https://doi.org/10.1029/2020JF005586
Plain Language Summary High and steep mountain ranges are currently undergoing changes due to increasing temperatures. These changes include rapidly shrinking glaciers as well as thawing permafrost, which together destabilize rock walls that surround
Autor:
Scherler, D., Schwanghart, W.
Publikováno v:
Earth Surface Dynamics
Drainage divides are organized into tree-like networks that may record information about drainage divide mobility. However, views diverge about how to best assess divide mobility. Here, we apply a new approach of automatically extracting and ordering
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::81154fd886fc1f5331586142c5ef24b7
https://www.earth-surf-dynam.net/8/261/2020/
https://www.earth-surf-dynam.net/8/261/2020/
Autor:
Scherler, D., Egholm, D.
The files in this dataset are supplementary to the article of Scherler and Egholm (2020), in which experiments with the ice flow and landscape evolution model iSOSIA (Egholm et al., 2011) have been conducted to analyze the production and transport of
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https://explore.openaire.eu/search/publication?articleId=od_______156::df8b9fa0d81da942e7d4b9865f45729b
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5002546
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5002546