001     51898
005     20180211163407.0
024 7 _ |2 DOI
|a 10.1016/j.jhydrol.2005.10.036
024 7 _ |2 WOS
|a WOS:000238776800003
037 _ _ |a PreJuSER-51898
041 _ _ |a eng
082 _ _ |a 690
084 _ _ |2 WoS
|a Engineering, Civil
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Water Resources
100 1 _ |a Herbst, M.
|b 0
|u FZJ
|0 P:(DE-Juel1)129469
245 _ _ |a Numerical experiments on the sensitivity of runoff generation to the spatial variation of soil hydraulic properties
260 _ _ |a Amsterdam [u.a.]
|b Elsevier
|c 2006
300 _ _ |a 43 - 58
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
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336 7 _ |a Output Types/Journal article
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336 7 _ |a Journal Article
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336 7 _ |a ARTICLE
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336 7 _ |a JOURNAL_ARTICLE
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336 7 _ |a article
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440 _ 0 |a Journal of Hydrology
|x 0022-1694
|0 3413
|v 326
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Spatially distributed soil hydraulic properties are required for distributed hydrological modelling. These soil hydraulic properties are known to vary significantly in space, and considering the non-linearity of runoff generation, the question arises how the spatial variation of soil hydraulic parameters affects the continuous runoff modelling for a micro-scale catchment. This was analysed by applying a three-dimensional hydrological model to the 28.6 ha 'Berrensiefen' catchment, Germany, for a simulation period of one year. The model was based on an observed distribution of soil hydraulic properties, which were assumed to be layered in vertical and to vary continuously in horizontal direction, and validated for total runoff. Numerical experiments with five spatial distributions of soil hydraulic parameters derived from the observed spatial distribution, which was supposed to be the 'true' underlying spatial variation, were carried out. These five spatial concepts were: choropleth map, spatially homogeneous case, random distribution, stochastic simulation and conditional stochastic simulation. The comparative modelling revealed a significant sensitivity of runoff generation towards the spatial variation of soil hydraulic properties. The comparison of the hydrograph of surface and macropore runoff to the initial model runs exhibited the highest root mean square error with 1.3 mm h(-1) for the homogeneous case. Further we detected, that the frequency distribution of soil hydraulic properties played an important role for the reproduction of runoff amounts. But also the spatial topology (deterministic spatial variation) was relevant for an adequate description of runoff generation. Conditional stochastic simulation is seen as a promising approach, because it preserved both, the frequency distribution and the deterministic variation. (c) 2005 Elsevier B.V. All rights reserved.
536 _ _ |a Terrestrische Umwelt
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588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
|2 WoSType
653 2 0 |2 Author
|a conditional stochasic simulation
653 2 0 |2 Author
|a soil mapping
653 2 0 |2 Author
|a macropore runoff
653 2 0 |2 Author
|a soil hydraulic properties
653 2 0 |2 Author
|a spatial variation
653 2 0 |2 Author
|a soil heterogeneity
700 1 _ |a Diekkrüger, B.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Vanderborght, J.
|b 2
|u FZJ
|0 P:(DE-Juel1)129548
773 _ _ |a 10.1016/j.jhydrol.2005.10.036
|g Vol. 326, p. 43 - 58
|p 43 - 58
|q 326<43 - 58
|0 PERI:(DE-600)1473173-3
|t Journal of hydrology
|v 326
|y 2006
|x 0022-1694
856 7 _ |u http://dx.doi.org/10.1016/j.jhydrol.2005.10.036
909 C O |o oai:juser.fz-juelich.de:51898
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913 1 _ |k P24
|v Terrestrische Umwelt
|l Terrestrische Umwelt
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914 1 _ |y 2006
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-IV
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|d 31.12.2006
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970 _ _ |a VDB:(DE-Juel1)81500
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980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)IBG-3-20101118


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