Zobrazeno 1 - 10
of 83
pro vyhledávání: '"THOMAS V. SCHULER"'
Publikováno v:
Journal of Glaciology, Vol 67, Pp 485-499 (2021)
Projected climate warming and wettening will have a major impact on the state of glaciers and seasonal snow in High Arctic regions. Following up on a historical simulation (1957–2018) for Svalbard, we make future projections of glacier climatic mas
Externí odkaz:
https://doaj.org/article/fd150d17c711430184621f8cfb9fafd7
Publikováno v:
Polar Research, Vol 38, Iss 0, Pp 1-13 (2019)
We evaluate how precipitation forcing data used in glacier mass balance models characterize snow accumulation events on synoptic timescales for two glaciers in north-western Svalbard (Kongsvegen and Holtedahlfonna). Using sonic ranger (snow depth) an
Externí odkaz:
https://doaj.org/article/cee88bb4b14d47e7878a569dd2691264
Publikováno v:
Journal of Glaciology, Vol 64, Pp 943-956 (2018)
The Kongsfjord basin in northwest Svalbard is the site of a number of interdisciplinary studies concerned with the effect of fresh water from seasonal snow and glacier melt on the physical and biological environment. We use an energy-balance model co
Externí odkaz:
https://doaj.org/article/661eef4d0753407e89c791c46d39d498
Autor:
Thomas V. Schuler, Jack Kohler, Nelly Elagina, Jon Ove M. Hagen, Andrew J. Hodson, Jacek A. Jania, Andreas M. Kääb, Bartłomiej Luks, Jakub Małecki, Geir Moholdt, Veijo A. Pohjola, Ireneusz Sobota, Ward J. J. Van Pelt
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Since the first estimates of Svalbard-wide glacier mass balance were made in the early 2000s, there has been great progress in remote sensing and modeling of mass balance, existing field records have been extended, field records at new locations have
Externí odkaz:
https://doaj.org/article/d6211ecef511455c98e50ccc3a871583
Publikováno v:
Frontiers in Earth Science, Vol 6 (2018)
Assessing and modeling precipitation in mountainous areas remains a major challenge in glacier mass balance modeling. Observations are typically scarce and reanalysis data and similar climate products are too coarse to accurately capture orographic e
Externí odkaz:
https://doaj.org/article/9e1675926fb74635963b05ac708c155e
Publikováno v:
Remote Sensing, Vol 11, Iss 1, p 28 (2018)
Remote sensing fractional snow cover area (fSCA) has been increasingly used to get an improved estimate of the spatiotemporal distribution of snow water equivalent (SWE) through reanalysis using different data assimilation (DA) schemes. Although the
Externí odkaz:
https://doaj.org/article/e9becf589fb546bd92c98c16a237a8a3
Publikováno v:
Journal of Glaciology, Pp 1-20
Empirical glacier mass-balance models are commonly used in assessments of glacier and runoff evolution. Recent satellite-borne geodetic mass-balance observations of global coverage facilitate large-scale model calibration that previously relied on sp
Externí odkaz:
https://doaj.org/article/3af8c5509b4d4e4ba471c57362a3c6a2
We have identified large spatiotemporal variability in the extent of supraglacial lakes on ice shelves in Dronning Maud Land, East Antarctica. While large lakes were found over Nivlisen and Roi Baudouin ice shelf areas, only small lakes were mapped o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e677cfd254f77c4878e7ddd087ee2565
https://doi.org/10.5194/egusphere-egu23-12647
https://doi.org/10.5194/egusphere-egu23-12647
Autor:
Coline Bouchayer, Ugo Nanni, Pierre-Marie Lefeuvre, John Hulth, Louise Steffensen Schmidt, Jack Kohler, François Renard, Thomas V. Schuler
Publikováno v:
eISSN
Fast glacier flow and dynamic instabilities, such as surges, are primarily caused by changes at the ice-bed interface, where basal slip and sediment deformation drive basal glacier motion. Determining subglacial conditions and their responses to hydr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1d282f791b75a12f3ddebf1f7d1722d6
https://doi.org/10.5194/egusphere-2023-618
https://doi.org/10.5194/egusphere-2023-618