Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Robert Kenner"'
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Rising air temperatures and increasingly intense precipitation are being observed in the Swiss Alps. These changes strongly affect the evolution of the temperature regime and the dynamics of mountain permafrost. Changes occur at different rates depen
Externí odkaz:
https://doaj.org/article/57440bdc8ba643de946e2a8b02dd6c18
Autor:
Jacopo Boaga, Marcia Phillips, Jeannette Noetzli, Anna Haberkorn, Robert Kenner, Alexander Bast
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Alpine permafrost is currently warming, leading to changes such as active layer deepening and talik formation. Frequency domain electro-magnetometry (FDEM) measurements were tested as a simple and efficient method to investigate ground characteristic
Externí odkaz:
https://doaj.org/article/3d4ad0ed95c64f77aec6973de913b2e5
Autor:
Robert Kenner, Valentin Gischig, Zan Gojcic, Yvain Quéau, Christian Kienholz, Daniel Figi, Reto Thöny, Yves Bonanomi
Publikováno v:
Landslides, 19 (6)
Lidar measurements and UAV photogrammetry provide high-resolution point clouds well suited for the investigation of slope deformations. Today, however, the information contained in these point clouds is rarely fully exploited. This study shows three
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::da5c3879a4d0c5988495b16766250ed4
https://hdl.handle.net/20.500.11850/540017
https://hdl.handle.net/20.500.11850/540017
Publikováno v:
Reference module in earth systems and environmental sciences
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b255a7bb1ec4a2d804d0138f94dc21b4
https://doi.org/10.1016/b978-0-12-818234-5.00112-7
https://doi.org/10.1016/b978-0-12-818234-5.00112-7
Autor:
Robert Kenner
Publikováno v:
Land Degradation & Development. 31:451-462
An alpine permafrost talus slope at Fluelapass (Eastern Swiss Alps) was observed using annual terrestrial laser scanning measurements between 2009 and 2018. The high‐resolution digital elevation models derived from these measurements enabled the de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e7e1d0f95dc50e29c31f71df545f7142
https://doi.org/10.1002/ldr.3462
https://doi.org/10.1002/ldr.3462
Publikováno v:
Permafrost and Periglacial Processes. 31:3-14
An increasing number of studies highlight the controlling influence of water on rock glacier deformation velocities. The link between the concept of water‐driven shearing processes and numerous observations of correlating mean annual air or ground
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d60f237ec33489e793f99f595f8db3f2
https://doi.org/10.1002/ppp.2023
https://doi.org/10.1002/ppp.2023
Publikováno v:
The Cryosphere, Vol 13, Pp 1925-1941 (2019)
Mountain permafrost is invisible, and mapping it is still a challenge. Available permafrost distribution maps often overestimate the permafrost extent and include large permafrost-free areas in their permafrost zonation. In addition, the representati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7441c61aa5dd9ac6866bd6b490abba14
https://www.the-cryosphere.net/13/1925/2019/tc-13-1925-2019.pdf
https://www.the-cryosphere.net/13/1925/2019/tc-13-1925-2019.pdf
Autor:
Robert Kenner
Publikováno v:
Land Degradation & Development. 30:580-591
The interaction of glaciers and rock glaciers and the associated development and degradation of permafrost landforms are intensely discussed fields of periglacial geomorphology. This study presents examples of glacier–rock glacier interactions sinc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1a5d15c1c40ae7b4950804f4a9f945c
https://doi.org/10.1002/ldr.3238
https://doi.org/10.1002/ldr.3238
Autor:
Robert Kenner, Marcia Phillips
Publikováno v:
World Geomorphological Landscapes ISBN: 9783030432010
Landscapes and landforms of Switzerland
Landscapes and landforms of Switzerland
The landscape above Pontresina in the Eastern Swiss Alps is characterized by mountain peaks reaching around 3,000 m a.s.l, steep rock walls, ice-bearing scree slopes and dynamic rock glaciers in a corrie—all located above a precipitous gully leadin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::777d15e544f32a9371858893dd62e878
https://doi.org/10.1007/978-3-030-43203-4_28
https://doi.org/10.1007/978-3-030-43203-4_28