Ceilometer lidar comparison: Backscatter coefficient retrieval and signal-to-noise ratio determination

dc.bibliographicCitation.firstPage1763eng
dc.bibliographicCitation.issue6eng
dc.bibliographicCitation.lastPage1770eng
dc.bibliographicCitation.volume3
dc.contributor.authorHeese, B.
dc.contributor.authorFlentje, H.
dc.contributor.authorAlthausen, D.
dc.contributor.authorAnsmann, A.
dc.contributor.authorFrey, S.
dc.date.accessioned2018-01-09T11:15:47Z
dc.date.available2019-06-26T17:20:55Z
dc.date.issued2010
dc.description.abstractThe potential of a new generation of ceilometer instruments for aerosol monitoring has been studied in the Ceilometer Lidar Comparison (CLIC) study. The used ceilometer was developed by Jenoptik, Germany, and is designed to find both thin cirrus clouds at tropopause level and aerosol layers at close ranges during day and night-time. The comparison study was performed to determine up to which altitude the ceilometers are capable to deliver particle backscatter coefficient profiles. For this, the derived ceilometer profiles are compared to simultaneously measured lidar profiles at the same wavelength. The lidar used for the comparison was the multi-wavelengths Raman lidar PollyXT. To demonstrate the capabilities and limits of ceilometers for the derivation of particle backscatter coefficient profiles from their measurements two examples of the comparison results are shown. Two cases, a daytime case with high background noise and a less noisy night-time case, are chosen. In both cases the ceilometer profiles compare well with the lidar profiles in atmospheric structures like aerosol layers or the boundary layer top height. However, the determination of the correct magnitude of the particle backscatter coefficient needs a calibration of the ceilometer data with an independent measurement of the aerosol optical depth by a sun photometer. To characterizes the ceilometers signal performance with increasing altitude a comprehensive signal-to-noise ratio study was performed. During daytime the signal-to-noise ratio is higher than 1 up to 4–5 km depending on the aerosol content. In our night-time case the SNR is higher than 1 even up to 8.5 km, so that also aerosol layers in the upper troposphere had been detected by the ceilometer.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/810
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/814
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/amt-3-1763-2010
dc.relation.ispartofseriesAtmospheric Measurement Techniques, Volume 3, Issue 6, Page 1763-1770eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectbackscattereng
dc.subjectcomparative studyeng
dc.subjectlidareng
dc.subjectoptical deptheng
dc.subjectRaman spectroscopyeng
dc.subjectsignal-to-noise ratioeng
dc.subjecttroposphereeng
dc.subjectwavelengtheng
dc.subject.ddc550eng
dc.titleCeilometer lidar comparison: Backscatter coefficient retrieval and signal-to-noise ratio determinationeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Measurement Techniqueseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
Files
Original bundle
Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
amt-3-1763-2010.pdf
Size:
833.68 KB
Format:
Adobe Portable Document Format
Description: