001     19607
005     20200702121613.0
024 7 _ |2 DOI
|a 10.5194/hessd-8-6031-2011
024 7 _ |2 WOS
|a WOS:000296745600007
037 _ _ |a PreJuSER-19607
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Water Resources
100 1 _ |0 P:(DE-HGF)0
|a Vernieuwe, H.
|b 0
245 _ _ |a Integrating coarse-scale uncertain soil moisture data into a fine-scale hydrological modelling scenario
260 _ _ |a Katlenburg-Lindau
|b EGU
|c 2011
300 _ _ |a 3101 - 3114
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
336 7 _ |a Output Types/Journal article
|2 DataCite
336 7 _ |a Journal Article
|0 0
|2 EndNote
336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |0 22262
|a Hydrology and Earth System Sciences
|v 15
|x 1027-5606
|y 10
500 _ _ |3 POF3_Assignment on 2016-02-29
500 _ _ |a This work has been performed in the framework of the STEREO-project SR/00/100, financed by the Belgian Science Policy and project G.0837.10 granted by the Research Foundation Flanders. Computational resources and services used in this work were provided by Ghent University.
520 _ _ |a In a hydrological modelling scenario, often the modeller is confronted with external data, such as remotely-sensed soil moisture observations, that become available to update the model output. However, the scale triplet ( spacing, extent and support) of these data is often inconsistent with that of the model. Furthermore, the external data can be cursed with epistemic uncertainty. Hence, a method is needed that not only integrates the external data into the model, but that also takes into account the difference in scale and the uncertainty of the observations. In this paper, a synthetic hydrological modelling scenario is set up in which a high-resolution distributed hydrological model is run over an agricultural field. At regular time steps, coarse-scale field-averaged soil moisture data, described by means of possibility distributions ( epistemic uncertainty), are retrieved by synthetic aperture radar and assimilated into the model. A method is presented that allows to integrate the coarse-scale possibility distribution of soil moisture content data with the fine-scale model-based soil moisture data. The method is subdivided in two steps. The first step, the disaggregation step, employs a scaling relationship between field-averaged soil moisture content data and its corresponding standard deviation. In the second step, the soil moisture content values are updated using two alternative methods.
536 _ _ |0 G:(DE-Juel1)FUEK407
|2 G:(DE-HGF)
|a Terrestrische Umwelt
|c P24
|x 0
588 _ _ |a Dataset connected to Web of Science
650 _ 7 |2 WoSType
|a J
700 1 _ |0 P:(DE-HGF)0
|a De Baets, B.
|b 1
700 1 _ |0 P:(DE-HGF)0
|a Minet, J.
|b 2
700 1 _ |0 P:(DE-HGF)0
|a Pauwels, V.R.N.
|b 3
700 1 _ |0 P:(DE-Juel1)VDB54976
|a Lambot, S.
|b 4
|u FZJ
700 1 _ |0 P:(DE-HGF)0
|a Vanclooster, M.
|b 5
700 1 _ |0 P:(DE-HGF)0
|a Verhoest, N.E.C.
|b 6
773 _ _ |0 PERI:(DE-600)2100610-6
|a 10.5194/hessd-8-6031-2011
|g Vol. 8, p. 3101 - 3114
|p 3101 - 3114
|q 8<3101 - 3114
|t Hydrology and earth system sciences
|v 8
|x 1027-5606
|y 2011
856 7 _ |u http://dx.doi.org/10.5194/hessd-8-6031-2011
909 C O |o oai:juser.fz-juelich.de:19607
|p VDB
|p VDB:Earth_Environment
913 1 _ |0 G:(DE-Juel1)FUEK407
|a DE-HGF
|b Erde und Umwelt
|k P24
|l Terrestrische Umwelt
|v Terrestrische Umwelt
|x 0
913 2 _ |a DE-HGF
|b Marine, Küsten- und Polare Systeme
|l Terrestrische Umwelt
|1 G:(DE-HGF)POF3-250
|0 G:(DE-HGF)POF3-259H
|2 G:(DE-HGF)POF3-200
|v Addenda
|x 0
914 1 _ |y 2011
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |0 I:(DE-Juel1)IBG-3-20101118
|g IBG
|k IBG-3
|l Agrosphäre
|x 0
970 _ _ |a VDB:(DE-Juel1)134473
980 _ _ |a VDB
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)IBG-3-20101118
980 _ _ |a UNRESTRICTED


LibraryCollectionCLSMajorCLSMinorLanguageAuthor
Marc 21