000032823 001__ 32823
000032823 005__ 20180210133602.0
000032823 0247_ $$2DOI$$a10.1016/S1474-7065(03)00033-0
000032823 0247_ $$2WOS$$aWOS:000183436100003
000032823 037__ $$aPreJuSER-32823
000032823 041__ $$aeng
000032823 082__ $$a550
000032823 084__ $$2WoS$$aGeosciences, Multidisciplinary
000032823 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000032823 084__ $$2WoS$$aWater Resources
000032823 1001_ $$0P:(DE-Juel1)129469$$aHerbst, M.$$b0$$uFZJ
000032823 245__ $$aModelling the spatial variability of soil moisture in a micro-scale catchment and comparison with field data using geostatistics
000032823 260__ $$aAmsterdam [u.a.]$$bElsevier Science$$c2003
000032823 300__ $$a239 - 245
000032823 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000032823 3367_ $$2DataCite$$aOutput Types/Journal article
000032823 3367_ $$00$$2EndNote$$aJournal Article
000032823 3367_ $$2BibTeX$$aARTICLE
000032823 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000032823 3367_ $$2DRIVER$$aarticle
000032823 440_0 $$09941$$aPhysics and Chemistry of the Earth$$v28$$x0079-1946
000032823 500__ $$aRecord converted from VDB: 12.11.2012
000032823 520__ $$aThe temporal and spatial variability of soil moisture in the micro-scale Berrensiefen catchment is simulated with SWMS_3D (three-dimensional variably saturated flow based on finite elements) and a loosely coupled model for the atmospheric boundary conditions. An additional model component for macropore and surface runoff and their concentration time is introduced. Time step of precipitation, atmospheric parameters and the simulated hydrologic processes is one hour. Soil parameters are discretized with a horizontal resolution of 10 m and five nodal layers in the vertical direction. A high resolution digital elevation model is used to reconstruct catchment surface morphology.For a nearly 2-month period hydrologic processes are simulated. The process model results are compared with measurements and the influence of the topography, the distributed soil and land use parameters on the soil water fluxes is examined.The spatial structure of soil moisture during a drying period is analysed using geostatistics. The application of standard geostatistical techniques (variogram modelling) captures the main features of spatial variability of the modelled soil moisture distributions. The integral scale or correlation length of soil moisture is constant while the semivariance shows clear correlation with soil moisture status during that period.A geostatistical comparison of the modelled soil moisture patterns of the whole catchment with a measured data set of a single hillslope of the catchment addresses the problem of differing scales of modelling and measurements. It is shown that due to the different spatial scales the results of point measurements of soil moisture can hardly be used to validate the modelled spatial structure of soil moisture. (C) 2003 Elsevier Science Ltd. All rights reserved.
000032823 536__ $$0G:(DE-Juel1)FUEK257$$2G:(DE-HGF)$$aChemie und Dynamik der Geo-Biosphäre$$cU01$$x0
000032823 588__ $$aDataset connected to Web of Science
000032823 650_7 $$2WoSType$$aJ
000032823 65320 $$2Author$$aspatial variability
000032823 65320 $$2Author$$ageostatistics
000032823 65320 $$2Author$$asoil moisture
000032823 65320 $$2Author$$arunoff generation
000032823 65320 $$2Author$$aSWMS_3d
000032823 65320 $$2Author$$ascale
000032823 7001_ $$0P:(DE-HGF)0$$aDiekkrüger, B.$$b1
000032823 773__ $$0PERI:(DE-600)1500664-5$$a10.1016/S1474-7065(03)00033-0$$gVol. 28, p. 239 - 245$$p239 - 245$$q28<239 - 245$$tPhysics and chemistry of the earth$$v28$$x0079-1946$$y2003
000032823 8567_ $$uhttp://dx.doi.org/10.1016/S1474-7065(03)00033-0
000032823 909CO $$ooai:juser.fz-juelich.de:32823$$pVDB
000032823 9131_ $$0G:(DE-Juel1)FUEK257$$bEnvironment (Umwelt)$$kU01$$lChemie und Dynamik der Geo-Biosphäre$$vChemie und Dynamik der Geo-Biosphäre$$x0
000032823 9141_ $$y2003
000032823 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000032823 9201_ $$0I:(DE-Juel1)VDB50$$d31.12.2006$$gICG$$kICG-IV$$lAgrosphäre$$x0
000032823 970__ $$aVDB:(DE-Juel1)36471
000032823 980__ $$aVDB
000032823 980__ $$aConvertedRecord
000032823 980__ $$ajournal
000032823 980__ $$aI:(DE-Juel1)IBG-3-20101118
000032823 980__ $$aUNRESTRICTED
000032823 981__ $$aI:(DE-Juel1)IBG-3-20101118