A Method for Retrieving Stratospheric Aerosol Extinction and Particle Size from Ground-Based Rayleigh-Mie-Raman Lidar Observations

dc.bibliographicCitation.firstPage773eng
dc.bibliographicCitation.issue8eng
dc.bibliographicCitation.journalTitleAtmosphereeng
dc.bibliographicCitation.volume11eng
dc.contributor.authorZalach, Jacob
dc.contributor.authorvon Savigny, Christian
dc.contributor.authorLangenbach, Arvid
dc.contributor.authorBaumgarten, Gerd
dc.contributor.authorLübken, Franz-Josef
dc.contributor.authorBourassa, Adam
dc.date.accessioned2021-08-19T09:34:04Z
dc.date.available2021-08-19T09:34:04Z
dc.date.issued2020
dc.description.abstractWe report on the retrieval of stratospheric aerosol particle size and extinction coefficient profiles from multi-color backscatter measurements with the Rayleigh-Mie-Raman lidar operated at the Arctic Lidar Observatory for Middle Atmosphere Research (ALOMAR) in northern Norway. The retrievals are based on a two-step approach. In a first step, the median radius of an assumed monomodal log-normal particle size distribution with fixed width is retrieved based on a color index formed from the measured backscatter ratios at the wavelengths of 1064nm and 532 nm. An intrinsic ambiguity of the retrieved aerosol size information is discussed. In a second step, this particle size information is used to convert the measured lidar backscatter ratio to aerosol extinction coefficients. The retrieval is currently based on monthly-averaged lidar measurements and the results for March 2013 are discussed. A sensitivity study is presented that allows for establishing an error budget for the aerosol retrievals. Assuming a monomodal log-normal aerosol particle size distribution with a geometric width of S = 1.5, median radii on the order of below 100 nm are retrieved. The median radii are found to generally decrease with increasing altitude. The retrieved aerosol extinction profiles are compared to observations with the OSIRIS (Optical Spectrograph and InfraRed Imager System) and the OMPS-LP (Ozone Mapping Profiling Suite Limb Profiler) satellite instruments in the 60° N to 80° N latitude band. The extinction profiles that were retrieved from the lidar measurements show good agreement with the observations of the two satellite instruments when taking the different wavelengths of the instruments into account. © 2020 by the authors.eng
dc.description.fondsLeibniz_Fonds
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6523
dc.identifier.urihttps://doi.org/10.34657/5570
dc.language.isoengeng
dc.publisherBasel, Switzerland : MDPI AGeng
dc.relation.doihttps://doi.org/10.3390/ATMOS11080773
dc.relation.essn2073-4433
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.otherHigh latitude stratosphereeng
dc.subject.otherMulti-wavelength lidar measurementseng
dc.subject.otherStratospheric aerosolseng
dc.titleA Method for Retrieving Stratospheric Aerosol Extinction and Particle Size from Ground-Based Rayleigh-Mie-Raman Lidar Observationseng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorIAPeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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