Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Johanna Nemec"'
Autor:
Elena Stoll, Florian Hanzer, Felix Oesterle, Johanna Nemec, Johannes Schöber, Matthias Huttenlau, Kristian Förster
Publikováno v:
Atmosphere, Vol 11, Iss 9, p 981 (2020)
Glacio-hydrological models combine both glacier and catchment hydrology modeling and are used to assess the hydrological response of high-mountain glacierized catchments to climate change. To capture the uncertainties from these model combinations, i
Externí odkaz:
https://doaj.org/article/7b16dc43676d43209c884382ab7228fe
Autor:
Antoine Rabatel, Raymond Le Bris, Roberto Sergio Azzoni, Davide Fugazza, Frank Paul, Johanna Nemec, Guglielmina Diolaiuti, Gabriele Schwaizer, Claudio Smiraglia, Philipp Rastner, Mélanie Ramusovic
Publikováno v:
Earth System Science Data, Vol 12, Pp 1805-1821 (2020)
The ongoing glacier shrinkage in the Alps requires frequent updates of glacier outlines to provide an accurate database for monitoring, modelling purposes (e.g. determination of run-off, mass balance, or future glacier extent), and other applications
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9edba78a5d40bfe3b3f8ffe45ce755d
https://essd.copernicus.org/articles/12/1805/2020/essd-12-1805-2020.pdf
https://essd.copernicus.org/articles/12/1805/2020/essd-12-1805-2020.pdf
Publikováno v:
International Journal of Climatology. 38:3106-3122
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::056e7706733b0bdd97be3f94f35d50e6
https://doi.org/10.1002/joc.5488
https://doi.org/10.1002/joc.5488
Autor:
Frank Paul, Philipp Rastner, Roberto Sergio Azzoni, Guglielmina Diolaiuti, Davide Fugazza, Raymond Le Bris, Johanna Nemec, Antoine Rabatel, Mélanie Ramusovic, Gabriele Schwaizer, Claudio Smiraglia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1255a2329cc2902e9d690b588666fbb0
https://doi.org/10.5194/essd-2019-213-supplement
https://doi.org/10.5194/essd-2019-213-supplement
Publikováno v:
Hydrology and Earth System Sciences, Vol 22, Pp 1593-1614 (2018)
A physically based hydroclimatological model (AMUNDSEN) is used to assess future climate change impacts on the cryosphere and hydrology of the Ötztal Alps (Austria) until 2100. The model is run in 100 m spatial and 3 h temporal resolution using
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1dfa3d883d01347c32cae0989546c689
https://www.hydrol-earth-syst-sci.net/22/1593/2018/
https://www.hydrol-earth-syst-sci.net/22/1593/2018/
Publikováno v:
Hydrology and Earth System Sciences 22 (2018), Nr. 2
A physically based hydroclimatological model (AMUNDSEN) is used to assess future climate change impacts on the cryosphere and hydrology of the Ötztal Alps (Austria) until 2100. The model is run in 100 m spatial and 3 h temporal resolution using in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85271a1615dc6b808d05f6cf573f2126
https://doi.org/10.5194/hess-2017-309
https://doi.org/10.5194/hess-2017-309
Publikováno v:
International Journal of Climatology. 33:1538-1550
Instrumental time series are often affected by inhomogeneities which can mask or amplify climate change signals. Various procedures for the detection and adjustment of breaks exist for monthly and annual time series. Homogenization methods on a daily
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::970e6b18df72f5bca31adf02b68089da
https://doi.org/10.1002/joc.3532
https://doi.org/10.1002/joc.3532
Publikováno v:
Geoscientific Model Development, 5 (3
Geoscientific Model Development, Vol 5, Iss 3, Pp 599-609 (2012)
Geoscientific Model Development, Vol 5, Iss 3, Pp 599-609 (2012)
We describe and evaluate a dynamical continental runoff routing model for the Northern Hemisphere that calculates the runoff pathways in response to topographic modifications due to changes in ice thickness and isostatic adjustment. The algorithm is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c72d84741697d46dcf1cd2ebbb75e816
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/305507
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/305507
Publikováno v:
Vrije Universiteit Brussel
EPIC3Annals of Glaciology, 50, pp. 126-134
EPIC3Annals of Glaciology, 50, pp. 126-134
We have reconstructed the annual balance of Vadret da Morteratsch, Engadine, Switzerland, with a two-dimensional energy-balance model for the period 1865–2005. The model takes into account a parameterization of the surface energy fluxes, an albedo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c7f0e4de79ce8510fef04bbb4c2de627
https://researchportal.vub.be/en/publications/e3c41c1e-7236-429d-a676-0ff5d6cb78d6
https://researchportal.vub.be/en/publications/e3c41c1e-7236-429d-a676-0ff5d6cb78d6