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| Titel |
Advancing catchment hydrology to deal with predictions under change |
| VerfasserIn |
U. Ehret, H. V. Gupta, M. Sivapalan  , S. V. Weijs, S. J. Schymanski, G. Blöschl, A. N. Gelfan, C. Harman, A. Kleidon, T. A. Bogaard, D. Wang, T. Wagener, U. Scherer, E. Zehe, M. F. P. Bierkens, G. Di Baldassarre, J. Parajka, L. P. H. Van Beek, A. Van Griensven, M. C. Westhoff, H. C. Winsemius |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1027-5606
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| Digitales Dokument |
URL |
| Erschienen |
In: Hydrology and Earth System Sciences ; 18, no. 2 ; Nr. 18, no. 2 (2014-02-19), S.649-671 |
| Datensatznummer |
250120283
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| Publikation (Nr.) |
 copernicus.org/hess-18-649-2014.pdf |
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| Zusammenfassung |
| Throughout its historical development, hydrology as an earth science, but
especially as a problem-centred engineering discipline has largely relied
(quite successfully) on the assumption of stationarity. This includes
assuming time invariance of boundary conditions such as climate, system
configurations such as land use, topography and morphology, and dynamics
such as flow regimes and flood recurrence at different spatio-temporal
aggregation scales. The justification for this assumption was often that
when compared with the temporal, spatial, or topical extent of the questions
posed to hydrology, such conditions could indeed be considered stationary,
and therefore the neglect of certain long-term non-stationarities or
feedback effects (even if they were known) would not introduce a large error. |
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