Umfang:
1 Online-Ressource (XVIII, 138 Seiten, Seite XIX-XLIV, 13767 KB)
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Illustrationen, Diagramme
Inhalt:
Assessing the impact of global change on hydrological systems is one of the greatest hydrological challenges of our time. Changes in land cover, land use, and climate have an impact on water quantity, quality, and temporal availability. There is a widespread consensus that, given the far-reaching effects of global change, hydrological systems can no longer be viewed as static in their structure; instead, they must be regarded as entire ecosystems, wherein hydrological processes interact and coevolve with biological, geomorphological, and pedological processes. To accurately predict the hydrological response under the impact of global change, it is essential to understand this complex coevolution. The knowledge of how hydrological processes, in particular the formation of subsurface (preferential) flow paths, evolve within this coevolution and how they feed back to the other processes is still very limited due to a lack of observational data. At the hillslope scale, this intertwined system of interactions is known as the hillslope ...
Anmerkung:
kumulative Dissertation
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Dissertation Universität Potsdam 2024
Weitere Ausg.:
Erscheint auch als Druck-Ausgabe Hartmann, Anne Tracing the evolution of hillslope structure and hillslope hydrological response over ten millennia in two glacial forefields of different geology Potsdam, 2024
Sprache:
Englisch
Schlagwort(e):
Hochschulschrift
DOI:
10.25932/publishup-62862
URN:
urn:nbn:de:kobv:517-opus4-628629
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