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dc.contributor.authorMueller, D.
dc.contributor.authorMattis, I.
dc.contributor.authorAnsmann, A.
dc.contributor.authorWandinger, U.
dc.contributor.authorRitter, C.
dc.contributor.authorKaiser, D.
dc.date.accessioned2013-08-01T10:33:06Z
dc.date.available2013-08-01T10:33:06Z
dc.date.issued2007-03-02
dc.identifier.citationMueller , D , Mattis , I , Ansmann , A , Wandinger , U , Ritter , C & Kaiser , D 2007 , ' Multiwavelength Raman lidar observations of particle growth during long-range transport of forest-fire smoke in the free troposphere ' , Geophysical Research Letters , vol. 34 , no. 5 , L05803 . https://doi.org/10.1029/2006GL027936
dc.identifier.issn0094-8276
dc.identifier.otherPURE: 1980903
dc.identifier.otherPURE UUID: df04eec3-7029-4fd0-af01-6b6e8f374bd9
dc.identifier.otherWOS: 000244707200003
dc.identifier.otherScopus: 34249890524
dc.identifier.otherORCID: /0000-0002-0203-7654/work/68611677
dc.identifier.urihttp://hdl.handle.net/2299/11271
dc.description.abstractWe present particle effective radii and Angstrom exponents of aged free-tropospheric forest-fire smoke. The particle plumes were observed with different multiwavelength Raman lidars downwind of the fires that burned in boreal areas of the northern hemisphere. We find an increase of particle size, respectively decrease of the Angstrom exponent with transport time which was more than two weeks in some of the investigated cases. Mean effective radii were as large as 0.4 mu m. Mean Angstrom exponents were as low as 0.04 for the wavelength pair at 355/532 nm. A fit curve that describes particle growth with time is derived. Particle growth levels off after approximately ten days of transport time.en
dc.format.extent4
dc.language.isoeng
dc.relation.ispartofGeophysical Research Letters
dc.subjectOPTICAL-PROPERTIES
dc.subjectPOLLUTION
dc.subjectAEROSOL
dc.subjectPARAMETERS
dc.subjectDISPERSION
dc.titleMultiwavelength Raman lidar observations of particle growth during long-range transport of forest-fire smoke in the free troposphereen
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.versionofrecordhttps://doi.org/10.1029/2006GL027936
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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