000172290 001__ 172290
000172290 005__ 20230310131318.0
000172290 0247_ $$2doi$$a10.1175/JAMC-D-14-0140.1
000172290 0247_ $$2ISSN$$a1558-8424
000172290 0247_ $$2ISSN$$a1558-8432
000172290 0247_ $$2WOS$$aWOS:000347953700013
000172290 0247_ $$2Handle$$a2128/20367
000172290 0247_ $$2altmetric$$aaltmetric:12269539
000172290 037__ $$aFZJ-2014-05773
000172290 082__ $$a550
000172290 1001_ $$0P:(DE-HGF)0$$aEder, Fabian$$b0$$eCorresponding Author
000172290 245__ $$aMeso-scale eddies affect near-surface turbulent exchange: evidence from lidar and tower measurements
000172290 260__ $$aBoston, Mass.$$bAMS$$c2015
000172290 3367_ $$2DRIVER$$aarticle
000172290 3367_ $$2DataCite$$aOutput Types/Journal article
000172290 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1422267057_24685
000172290 3367_ $$2BibTeX$$aARTICLE
000172290 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000172290 3367_ $$00$$2EndNote$$aJournal Article
000172290 520__ $$aThe eddy-covariance technique tends to underestimate turbulent heat fluxes, which results in nonclosure of the surface energy balance. This study shows experimental evidence that mesoscale turbulent organized structures, which are inherently not captured by the standard eddy-covariance technique, can affect near-surface turbulent exchange. By using a combined setup of three Doppler wind lidars above a cropland-dominated area in Germany, low-frequency turbulent structures were detected in the surface layer down to a few meters above ground. In addition, data from two micrometeorological stations in the study area were analyzed with respect to energy balance closure. In accordance with several previous studies, the data confirm a strong friction velocity dependence of the energy balance residual. At both stations, the energy balance residual was found to be positively correlated with the vertical moisture gradient in the lower atmospheric boundary layer, but at only one station was it correlated with the temperature gradient. This result indicates that mesoscale transport probably contributes more to the latent heat flux than to the sensible heat flux, but this conclusion depends largely on the measurement site. Moreover, flow distortion due to tower mountings and measurement devices affects the energy balance closure considerably for certain wind directions.
000172290 536__ $$0G:(DE-HGF)POF3-255$$a255 - Terrestrial Systems: From Observation to Prediction (POF3-255)$$cPOF3-255$$fPOF III$$x0
000172290 536__ $$0G:(DE-HGF)TERENO-2008$$aTERENO - Terrestrial Environmental Observatories (TERENO-2008)$$cTERENO-2008$$fTERENO-2008$$x1
000172290 536__ $$0G:(DE-HGF)POF3-255$$a255 - Terrestrial Systems: From Observation to Prediction (POF3-255)$$cPOF3-255$$fPOF III$$x2
000172290 536__ $$0G:(GEPRIS)15232683$$aDFG project 15232683 - TRR 32: Muster und Strukturen in Boden-Pflanzen-Atmosphären-Systemen: Erfassung, Modellierung und Datenassimilation (15232683)$$c15232683$$x3
000172290 588__ $$aDataset connected to CrossRef, juser.fz-juelich.de
000172290 7001_ $$0P:(DE-Juel1)144420$$aSchmidt, Marius$$b1$$ufzj
000172290 7001_ $$0P:(DE-HGF)0$$aDamian, Thomas$$b2
000172290 7001_ $$0P:(DE-HGF)0$$aTräumner, Katja$$b3
000172290 7001_ $$0P:(DE-HGF)0$$aMauder, Matthias$$b4
000172290 773__ $$0PERI:(DE-600)2227779-1$$a10.1175/JAMC-D-14-0140.1$$gp. 141017114326002 -$$n1$$p189-206$$tJournal of applied meteorology and climatology$$v54$$x1558-8432$$y2015
000172290 8564_ $$uhttps://juser.fz-juelich.de/record/172290/files/jamc-d-14-0140.1.pdf$$yOpenAccess
000172290 909CO $$ooai:juser.fz-juelich.de:172290$$pdnbdelivery$$pVDB$$pVDB:Earth_Environment$$pdriver$$popen_access$$popenaire
000172290 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)144420$$aForschungszentrum Jülich GmbH$$b1$$kFZJ
000172290 9131_ $$0G:(DE-HGF)POF3-255$$1G:(DE-HGF)POF3-250$$2G:(DE-HGF)POF3-200$$aDE-HGF$$bMarine, Küsten- und Polare Systeme$$lTerrestrische Umwelt$$vTerrestrial Systems: From Observation to Prediction$$x0
000172290 9130_ $$0G:(DE-HGF)TERENO-2008$$aDE-HGF$$vTerrestrial Environmental Observatories$$x0
000172290 9130_ $$0G:(DE-HGF)POF2-246$$1G:(DE-HGF)POF2-240$$2G:(DE-HGF)POF2-200$$aDE-HGF$$bErde und Umwelt$$lTerrestrische Umwelt$$vModelling and Monitoring Terrestrial Systems: Methods and Technologies$$x1
000172290 9130_ $$0G:(DE-HGF)POF3-255$$1G:(DE-HGF)POF3-250$$2G:(DE-HGF)POF3-200$$aDE-HGF$$bMarine, Küsten- und Polare Systeme$$lTerrestrische Umwelt$$vTerrestrial Systems: From Observation to Prediction$$x2
000172290 9141_ $$y2015
000172290 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000172290 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000172290 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS
000172290 915__ $$0StatID:(DE-HGF)0110$$2StatID$$aWoS$$bScience Citation Index
000172290 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000172290 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF <  5
000172290 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000172290 915__ $$0StatID:(DE-HGF)1150$$2StatID$$aDBCoverage$$bCurrent Contents - Physical, Chemical and Earth Sciences
000172290 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000172290 920__ $$lyes
000172290 9201_ $$0I:(DE-Juel1)IBG-3-20101118$$kIBG-3$$lAgrosphäre$$x0
000172290 980__ $$ajournal
000172290 980__ $$aVDB
000172290 980__ $$aUNRESTRICTED
000172290 980__ $$aI:(DE-Juel1)IBG-3-20101118
000172290 9801_ $$aFullTexts