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dc.contributor.authorHeinold, Bernd
dc.contributor.authorTegen, Ina
dc.contributor.authorSchepanski, Kerstin
dc.contributor.authorTesche, Matthias
dc.contributor.authorEsselborn, Michael
dc.contributor.authorFreudenthaler, Volker
dc.contributor.authorGross, Silke
dc.contributor.authorKandler, Konrad
dc.contributor.authorKnippertz, Peter
dc.contributor.authorMueller, D.
dc.contributor.authorSchladitz, Alexander
dc.contributor.authorToledano, Carlos
dc.contributor.authorWeinzierl, Bernadett
dc.contributor.authorAnsmann, Albert
dc.contributor.authorAlthausen, Dietrich
dc.contributor.authorMüller, Thomas
dc.contributor.authorPetzold, Andreas
dc.contributor.authorWiedensohler, Alfred
dc.date.accessioned2013-08-01T08:48:06Z
dc.date.available2013-08-01T08:48:06Z
dc.date.issued2011-09
dc.identifier.citationHeinold , B , Tegen , I , Schepanski , K , Tesche , M , Esselborn , M , Freudenthaler , V , Gross , S , Kandler , K , Knippertz , P , Mueller , D , Schladitz , A , Toledano , C , Weinzierl , B , Ansmann , A , Althausen , D , Müller , T , Petzold , A & Wiedensohler , A 2011 , ' Regional modelling of Saharan dust and biomass-burning smoke. Part 1 : Model description and evaluation ' , Tellus Series B-Chemical and Physical Meteorology , vol. 63 , no. 4 , pp. 781-799 . https://doi.org/10.1111/j.1600-0889.2011.00570.x
dc.identifier.issn0280-6509
dc.identifier.otherORCID: /0000-0002-0203-7654/work/68611711
dc.identifier.urihttp://hdl.handle.net/2299/11250
dc.descriptionPublished under the terms of the Creative Commons Attribution-Noncommercial 3.0 Unported License
dc.description.abstractThe spatio-temporal evolution of the Saharan dust and biomass-burning plume during the SAMUM-2 field campaign in January and February 2008 is simulated at 28 km horizontal resolution with the regional model-system COSMO-MUSCAT. The model performance is thoroughly tested using routine ground-based and space-borne remote sensing and local field measurements. Good agreement with the observations is found in many cases regarding transport patterns, aerosol optical thicknesses and the ratio of dust to smoke aerosol. The model also captures major features of the complex aerosol layering. Nevertheless, discrepancies in the modelled aerosol distribution occur, which are analysed in detail. The dry synoptic dynamics controlling dust uplift and transport during the dry season are well described by the model, but surface wind peaks associated with the breakdown of nocturnal low-level jets are not always reproduced. Thus, a strong dust outbreak is underestimated. While dust emission modelling is a priori more challenging, since strength and placement of dust sources depend on on-line computed winds, considerable inaccuracies also arise in observation-based estimates of biomass-burning emissions. They are caused by cloud and spatial errors of satellite fire products and uncertainties in fire emission parameters, and can lead to unrealistic model results of smoke transport. © 2011 The Authors Tellus B © 2011 John Wiley & Sons A/S.en
dc.format.extent19
dc.format.extent2023717
dc.language.isoeng
dc.relation.ispartofTellus Series B-Chemical and Physical Meteorology
dc.subjectSCHEME
dc.subjectFIRE
dc.subjectEMISSIONS
dc.subjectTRANSPORT
dc.subjectOPTICAL-PROPERTIES
dc.subjectAEROSOL
dc.subjectPARTICLES
dc.subjectRUNGE-KUTTA METHODS
dc.subjectSAMUM 2006
dc.subjectMODIS
dc.subjectAtmospheric Science
dc.titleRegional modelling of Saharan dust and biomass-burning smoke. Part 1 : Model description and evaluationen
dc.contributor.institutionSchool of Physics, Astronomy and Mathematics
dc.contributor.institutionCentre for Atmospheric and Climate Physics Research
dc.contributor.institutionSchool of Physics, Engineering & Computer Science
dc.contributor.institutionDepartment of Physics, Astronomy and Mathematics
dc.description.statusPeer reviewed
rioxxterms.versionofrecord10.1111/j.1600-0889.2011.00570.x
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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