Current and future roles of meltwater–groundwater dynamics in a proglacial Alpine outwash plain
<p>Glacierized alpine catchments are rapidly evolving due to glacier retreat and consequent geomorphological and ecological changes. As more terrain becomes ice-free, reworking of exposed terrain by the river as well as thawing of the top layer may lead to an increase in surface and subsurface...
Principais autores: | T. Müller, M. Roncoroni, D. Mancini, S. N. Lane, B. Schaefli |
---|---|
Formato: | Artigo |
Idioma: | English |
Publicado em: |
Copernicus Publications
2024-02-01
|
coleção: | Hydrology and Earth System Sciences |
Acesso em linha: | https://hess.copernicus.org/articles/28/735/2024/hess-28-735-2024.pdf |
Registros relacionados
-
Separating snow and ice melt using water stable isotopes and glacio-hydrological modelling: towards improving the application of isotope analyses in highly glacierized catchments
por: T. Müller, et al.
Publicado em: (2025-01-01) -
Proglacial methane emissions driven by meltwater and groundwater flushing in a high-Arctic glacial catchment
por: G. E. Kleber, et al.
Publicado em: (2025-02-01) -
Filtering of the Signal of Sediment Export From a Glacier by Its Proglacial Forefield
por: D. Mancini, et al.
Publicado em: (2023-11-01) -
Proglacial river sediments are a substantial sink of perfluoroalkyl substances released by glacial meltwater
por: Yunqiao Zhou, et al.
Publicado em: (2024-02-01) -
Aeolian processes on the outwash plain in the Oświęcim Basin, southern Poland
por: Dulias Renata
Publicado em: (2023-03-01)