Zobrazeno 1 - 10
of 706
pro vyhledávání: '"W, Haeberli"'
Publikováno v:
The Cryosphere, Vol 18, Pp 1669-1683 (2024)
Viscous-flow features in perennially frozen talus/debris called rock glaciers are being systematically inventoried as part of the global climate-related monitoring of mountain permafrost. In order to avoid duplication and confusion, guidelines were d
Externí odkaz:
https://doaj.org/article/7895229722dc44bfa9efaebdcef52e42
Publikováno v:
The Cryosphere, Vol 16, Pp 2083-2101 (2022)
Digitized aerial images were used to monitor the evolution of perennially frozen debris and polythermal glacier ice at the intensely investigated Gruben site in the Swiss Alps over a period of about 50 years. The photogrammetric analysis allowed for
Externí odkaz:
https://doaj.org/article/a5ef138e532d4b1e940a47fd6d9d4632
Publikováno v:
The Cryosphere, Vol 12, Pp 2515-2544 (2018)
At the Last Glacial Maximum (LGM), the Rhine glacier in the Swiss Alps covered an area of about 16 000 km2. As part of an integrative study about the safety of repositories for radioactive waste under ice age conditions in Switzerland, we mode
Externí odkaz:
https://doaj.org/article/0c23616aaf2342eb99da05c0f7315711
Akademický článek
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Publikováno v:
Annals of Glaciology, Vol 57, Pp 119-130 (2016)
Surface digital elevation models (DEMs) and slope-related estimates of glacier thickness enable modelling of glacier-bed topographies over large ice-covered areas. Due to the erosive power of glaciers, such bed topographies can contain numerous overd
Externí odkaz:
https://doaj.org/article/f46a8d83cd5b43b38df87aba5123ff1f
Autor:
W. Haeberli, A. Linsbauer
Publikováno v:
The Cryosphere, Vol 7, Iss 3, Pp 817-821 (2013)
The potential contribution of glaciers and ice caps to sea level rise is usually calculated by comparing the estimated total ice volume with the surface area of the ocean. Part of this total ice volume, however, does not contribute to sea level rise
Externí odkaz:
https://doaj.org/article/f5ecabbbe3a74f66842b534b5d0bdb23
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 12, Iss 1, Pp 241-254 (2012)
The ongoing debate about the effects of changes in the high-mountain cryosphere on rockfalls and rock avalanches suggests a need for more knowledge about characteristics and distribution of recent rock-slope instabilities. This paper investigates 56
Externí odkaz:
https://doaj.org/article/07f1eec06e2d41e3b116f439142e94e9
Publikováno v:
The Cryosphere, Vol 5, Iss 4, Pp 977-988 (2011)
The thermal condition of high-alpine mountain flanks can be an important determinant of climate change impact on slope stability and correspondingly down-slope hazard regimes. In this study we analyze time-series from 17 shallow temperature-depth pro
Externí odkaz:
https://doaj.org/article/a92619423f434423bf0804dba77594ce
Publikováno v:
The Cryosphere, Vol 4, Iss 3, Pp 333-343 (2010)
Storglaciären, located in the Kebnekaise massif in northern Sweden, has a long history of glaciological research. Early photo documentations date back to the late 19th century. Measurements of front position variations and distributed mass balance h
Externí odkaz:
https://doaj.org/article/04f55b09d29e45d4b579c7427d91a7db
Publikováno v:
The Cryosphere, Vol 4, Iss 3, Pp 345-357 (2010)
Seasonal glaciological mass balances have been measured on Storglaciären without interruption since 1945/46. In addition, aerial surveys have been carried out on a decadal basis since the beginning of the observation program. Early studies had used
Externí odkaz:
https://doaj.org/article/d652f58cd8a44279ba09981f7f654f89