dc.contributor.author | Tesche, Matthias | |
dc.contributor.author | Ansmann, Albert | |
dc.contributor.author | Mueller, D. | |
dc.contributor.author | Althausen, Dietrich | |
dc.contributor.author | Engelmann, Ronny | |
dc.contributor.author | Hu, Min | |
dc.contributor.author | Zhang, Yuanghang | |
dc.date.accessioned | 2013-08-01T10:18:06Z | |
dc.date.available | 2013-08-01T10:18:06Z | |
dc.date.issued | 2007-09-01 | |
dc.identifier.citation | Tesche , M , Ansmann , A , Mueller , D , Althausen , D , Engelmann , R , Hu , M & Zhang , Y 2007 , ' Particle backscatter, extinction, and lidar ratio profiling with Raman lidar in south and north China ' , Applied Optics , vol. 46 , no. 25 , pp. 6302-6308 . | |
dc.identifier.issn | 0003-6935 | |
dc.identifier.other | ORCID: /0000-0002-0203-7654/work/68611619 | |
dc.identifier.uri | http://hdl.handle.net/2299/11269 | |
dc.description.abstract | Aerosol Raman lidar observations of profiles of the particle extinction and backscatter coefficients and the respective extinction-to-backscatter ratio (lidar ratio) were performed under highly polluted conditions in the Pearl River Delta (PRD) in southern China in October 2004 and at Beijing during a clear period with moderately polluted to background aerosol conditions in January 2005. The anthropogenic haze in the PRD is characterized by volume light-extinction coefficients of particles ranging from approximately 200 to 800 Mm(-1) and lidar ratios mostly between 40 and 55 sr (average of 47 +/- 6 sr). Almost clean air masses were observed throughout the measurements of the Beijing campaign. These air masses originated from and desert-steppe-like regions (greater Gobi area). Extinction values usually varied between 100 and 300 Mm(-1), and the lidar ratios were considerably lower (compared with PRD values) with values mostly from 30 to 45 sr (average of 38 +/- 7 sr). Gobi dust partly influenced the observations. Unexpectedly low lidar ratios of approximately 25 sr were found for a case of background aerosol with a low optical depth of 0.05. The low lidar ratios are consistent with Mie-scattering calculations applied to ground-based observations of particle size distributions. (c) 2007 Optical Society of America. | en |
dc.format.extent | 7 | |
dc.language.iso | eng | |
dc.relation.ispartof | Applied Optics | |
dc.subject | ASIAN DUST EVENTS | |
dc.subject | AEROSOL EXTINCTION | |
dc.subject | CLOUDS | |
dc.title | Particle backscatter, extinction, and lidar ratio profiling with Raman lidar in south and north China | en |
dc.contributor.institution | School of Physics, Astronomy and Mathematics | |
dc.contributor.institution | Centre for Atmospheric and Climate Physics Research | |
dc.contributor.institution | School of Physics, Engineering & Computer Science | |
dc.contributor.institution | Department of Physics, Astronomy and Mathematics | |
dc.description.status | Peer reviewed | |
rioxxterms.type | Journal Article/Review | |
herts.preservation.rarelyaccessed | true | |