Zobrazeno 1 - 10
of 1 004
pro vyhledávání: '"M, Huß"'
Autor:
L. Piermattei, M. Zemp, C. Sommer, F. Brun, M. H. Braun, L. M. Andreassen, J. M. C. Belart, E. Berthier, A. Bhattacharya, L. Boehm Vock, T. Bolch, A. Dehecq, I. Dussaillant, D. Falaschi, C. Florentine, D. Floricioiu, C. Ginzler, G. Guillet, R. Hugonnet, M. Huss, A. Kääb, O. King, C. Klug, F. Knuth, L. Krieger, J. La Frenierre, R. McNabb, C. McNeil, R. Prinz, L. Sass, T. Seehaus, D. Shean, D. Treichler, A. Wendt, R. Yang
Publikováno v:
The Cryosphere, Vol 18, Pp 3195-3230 (2024)
Observations of glacier mass changes are key to understanding the response of glaciers to climate change and related impacts, such as regional runoff, ecosystem changes, and global sea level rise. Spaceborne optical and radar sensors make it possible
Externí odkaz:
https://doaj.org/article/3d24e47842a943a1bec0821da8ba2b07
Publikováno v:
Climate of the Past, Vol 20, Pp 1251-1267 (2024)
Glacier mass balance reconstructions provide a means of placing relatively short observational records into a longer-term context. Here, we use multiple proxies from Pinus cembra trees from God da Tamangur, combining tree ring anatomy and stable isot
Externí odkaz:
https://doaj.org/article/101901dee4ad48f09b8f09b93af8d46d
Publikováno v:
The Cryosphere, Vol 17, Pp 2285-2303 (2023)
In order to assess future glacier evolution and meltwater runoff, accurate knowledge on the volume and the ice thickness distribution of glaciers is crucial. However, in situ observations of glacier thickness are sparse in many regions worldwide due
Externí odkaz:
https://doaj.org/article/ca53a49f126b492fbeb2eb4ff5621525
Publikováno v:
The Cryosphere, Vol 17, Pp 1895-1912 (2023)
Accelerating glacier melt rates were observed during the last decades. Substantial ice loss occurs particularly during heat waves that are expected to intensify in the future. Because measuring and modelling glacier mass balance on a daily scale rema
Externí odkaz:
https://doaj.org/article/8cbf4a22b9374331980669fa16ec42ef
Publikováno v:
The Cryosphere, Vol 17, Pp 977-1002 (2023)
Spatio-temporal reconstruction of winter glacier mass balance is important for assessing long-term impacts of climate change. However, high-altitude regions significantly lack reliable observations, which is limiting the calibration of glaciological
Externí odkaz:
https://doaj.org/article/235f30d14d1f4b8c9a9d65276ee7a35c
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
More than 13% of the area of the Caucasus glaciers is covered by debris affecting glacier mass balance. Using the Caucasus as example, we introduce a new model configuration that incorporates a physically-based subroutine for the evolution of supragl
Externí odkaz:
https://doaj.org/article/0a6a71bea4b741bf964d05c9b48aa0a3
Autor:
P. Wiersma, J. Aerts, H. Zekollari, M. Hrachowitz, N. Drost, M. Huss, E. H. Sutanudjaja, R. Hut
Publikováno v:
Hydrology and Earth System Sciences, Vol 26, Pp 5971-5986 (2022)
Global hydrological models have become a valuable tool for a range of global impact studies related to water resources. However, glacier parameterization is often simplistic or non-existent in global hydrological models. By contrast, global glacier m
Externí odkaz:
https://doaj.org/article/10645fdece6b44a6899896c00b5ea269
Publikováno v:
The Cryosphere, Vol 16, Pp 3249-3268 (2022)
The monitoring of glaciers in Switzerland has a long tradition, yet glacier changes during the 20th century are only known through sparse observations. Here, we estimate a halving of Swiss glacier volumes between 1931 and 2016 by mapping historical g
Externí odkaz:
https://doaj.org/article/d9ce4f5f51ee482db978aeceb3cfc5db
Publikováno v:
Earth System Science Data, Vol 14, Pp 3293-3312 (2022)
Glacier monitoring in Switzerland has resulted in some of the longest and most complete data series globally. Mass balance observations at individual locations, starting in the 19th century, are the backbone of the monitoring as they represent the ra
Externí odkaz:
https://doaj.org/article/8048f58eccf54c17a7435836cec9ad67
Publikováno v:
Earth Surface Dynamics, Vol 10, Pp 723-741 (2022)
Ongoing climate change and associated glacier retreat is causing rapid environmental change, including shifts in high-alpine landscapes. Glacier lakes, which can form in topographical depressions left behind by glacier retreat, are prominent features
Externí odkaz:
https://doaj.org/article/5d81abe7bb164424bb181acce1466104