000015494 001__ 15494
000015494 005__ 20200702121555.0
000015494 0247_ $$2DOI$$a10.1016/j.jhydrol.2011.01.037
000015494 0247_ $$2WOS$$aWOS:000289325100021
000015494 037__ $$aPreJuSER-15494
000015494 041__ $$aeng
000015494 082__ $$a690
000015494 084__ $$2WoS$$aEngineering, Civil
000015494 084__ $$2WoS$$aGeosciences, Multidisciplinary
000015494 084__ $$2WoS$$aWater Resources
000015494 1001_ $$0P:(DE-Juel1)VDB98986$$aAndre, F.$$b0$$uFZJ
000015494 245__ $$aSpatial and temporal patterns of throughfall volume in a deciduous mixed-species stand
000015494 260__ $$aAmsterdam [u.a.]$$bElsevier$$c2011
000015494 300__ $$a
000015494 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000015494 3367_ $$2DataCite$$aOutput Types/Journal article
000015494 3367_ $$00$$2EndNote$$aJournal Article
000015494 3367_ $$2BibTeX$$aARTICLE
000015494 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000015494 3367_ $$2DRIVER$$aarticle
000015494 440_0 $$03413$$aJournal of Hydrology$$v400$$x0022-1694$$y1
000015494 500__ $$3POF3_Assignment on 2016-02-29
000015494 500__ $$aThis research was co-funded by a FRIA (Fonds pour la Recherche dans l'Industrie et l'Agriculture) grant and the "Accord cadre - Recherche et Vulgarisation forestieres" project. We wish to thank Ir. A. Barjasse and the local forester A. Laboureix for giving us access to the site. We are grateful to E. Dambrine for his advices as well as to C. Nys and his technical team and to J. Morren for technical and material assistance. Field measurements and maintenance were carried out by C. Tilquin, M. Pierard, F. Plume, and F. Hardy. We also gratefully thank the two anonymous reviewers for their constructive comments and suggestions on an earlier version of the manuscript.
000015494 520__ $$aThe effects of canopy structure on the spatial and temporal patterns of throughfall (TF) in deciduous mixed-species stands remains poorly documented. TF was collected on a rain event basis in an oak-beech stand, within 12 structural units of contrasting densities (low, LD; high, HD) and species composition (beech, oak, mixture) delimited by three neighbouring trees. A roof was installed at the centre of each unit, and gutters were placed at the periphery of the LD units. Based on selected rain events, a simplified mass balance approach was used to describe water fluxes reaching and leaving the canopy. During the leafed season, the proportions of incident rainfall (RF) collected as TF on the roofs steadily increased with increasing RF up to a RF volume of about 5 mm; for larger RF volumes, IF proportions stabilised around 55% under pure (LD, HD) beech and HD mixture, and around 65% under pure (LD, HD) oak and LD mixture. During the leafless period, TF proportions (on average 60%) were independent of RF but were still affected by local stand characteristics (HD mixture < HD beech < HD oak < LD beech and mixture < LD oak). At canopy saturation, lateral transfers as branch flow (BF) were substantial (35 <= (BF/RF)% <= 46) in all plots, and were significantly higher in the HD units compared to the LD plots in the leafless period; part of BF falled down as indirect TF before reaching the trunks, except in the HD units during the leafless season where stemflow and BF were similar. A mechanistic numerical model using rainfall partitioning parameters determined in this study allowed to successfully describe real-time throughfall measurements. (C) 2011 Elsevier B.V. All rights reserved.
000015494 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000015494 588__ $$aDataset connected to Web of Science
000015494 650_7 $$2WoSType$$aJ
000015494 65320 $$2Author$$aThroughfall
000015494 65320 $$2Author$$aRainfall partitioning
000015494 65320 $$2Author$$aQuercus petraea
000015494 65320 $$2Author$$aFagus sylvatica
000015494 65320 $$2Author$$aMixed-species stand
000015494 7001_ $$0P:(DE-HGF)0$$aJonard, M.$$b1
000015494 7001_ $$0P:(DE-Juel1)VDB95614$$aJonard, F.$$b2$$uFZJ
000015494 7001_ $$0P:(DE-HGF)0$$aPonette, Q.$$b3
000015494 773__ $$0PERI:(DE-600)1473173-3$$a10.1016/j.jhydrol.2011.01.037$$gVol. 400$$q400$$tJournal of hydrology$$v400$$x0022-1694$$y2011
000015494 8567_ $$uhttp://dx.doi.org/10.1016/j.jhydrol.2011.01.037
000015494 909CO $$ooai:juser.fz-juelich.de:15494$$pVDB$$pVDB:Earth_Environment
000015494 9131_ $$0G:(DE-Juel1)FUEK407$$bErde und Umwelt$$kP24$$lTerrestrische Umwelt$$vTerrestrische Umwelt$$x0
000015494 9132_ $$0G:(DE-HGF)POF3-259H$$1G:(DE-HGF)POF3-250$$2G:(DE-HGF)POF3-200$$aDE-HGF$$bMarine, Küsten- und Polare Systeme$$lTerrestrische Umwelt$$vAddenda$$x0
000015494 9141_ $$y2011
000015494 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000015494 9201_ $$0I:(DE-Juel1)IBG-3-20101118$$gIBG$$kIBG-3$$lAgrosphäre$$x0
000015494 970__ $$aVDB:(DE-Juel1)128461
000015494 980__ $$aVDB
000015494 980__ $$aConvertedRecord
000015494 980__ $$ajournal
000015494 980__ $$aI:(DE-Juel1)IBG-3-20101118
000015494 980__ $$aUNRESTRICTED