Aerosol measurements with a shipborne Sun-sky-lunar photometer and collocated multiwavelength Raman polarization lidar over the Atlantic Ocean
dc.bibliographicCitation.firstPage | 5685 | eng |
dc.bibliographicCitation.issue | 10 | eng |
dc.bibliographicCitation.volume | 12 | eng |
dc.contributor.author | Yin, Z. | |
dc.contributor.author | Ansmann, A. | |
dc.contributor.author | Baars, H. | |
dc.contributor.author | Seifert, P. | |
dc.contributor.author | Engelmann, R. | |
dc.contributor.author | Radenz, M. | |
dc.contributor.author | Jimenez, C. | |
dc.contributor.author | Herzog, A. | |
dc.contributor.author | Ohneiser, K. | |
dc.contributor.author | Hanbuch, K. | |
dc.contributor.author | Blarel, L. | |
dc.contributor.author | Goloub, P. | |
dc.contributor.author | Victori, S. | |
dc.contributor.author | Maupin, F. | |
dc.date.accessioned | 2020-07-13T11:01:23Z | |
dc.date.available | 2020-07-13T11:01:23Z | |
dc.date.issued | 2019 | |
dc.description.abstract | A shipborne Sun-sky-lunar photometer of type CE318-T was tested during two trans-Atlantic cruises aboard the German research vessel <i>Polarstern</i> from 54<span classCombining double low line"inline-formula">ĝ</span> N to 54<span classCombining double low line"inline-formula">ĝ</span> S in May/June and December 2018. The continuous observations of the motion-stabilized shipborne CE318-T enabled the first-time observation of a full diurnal cycle of aerosol optical depth (AOD) and column-mean Ångström coefficient of a mixed dust-smoke episode. The latitudinal distribution of the AOD from the shipborne CE318-T, Raman lidar and MICROTOPS II shows the same trend with highest values in the dust belt from 0 to 20<span classCombining double low line"inline-formula">ĝ</span> N and overall low values in the Southern Hemisphere. The linear-regression coefficients of determination between MICROTOPS II and the CE318-T were 0.988, 0.987, 0.994 and 0.994 for AODs at 380, 440, 500 and 870 nm and 0.896 for the Ångström exponent at 440-870 nm. The root-mean-squared differences of AOD at 380, 440, 500 and 870 nm were 0.015, 0.013, 0.010 and 0.009, respectively. | eng |
dc.description.sponsorship | Leibniz_Fonds | eng |
dc.description.version | publishedVersion | eng |
dc.identifier.uri | https://oa.tib.eu/renate/handle/123456789/4924 | |
dc.identifier.uri | https://doi.org/10.34657/3553 | |
dc.language.iso | eng | eng |
dc.publisher | Göttingen : Copernicus GmbH | eng |
dc.relation.doi | https://doi.org/10.5194/amt-12-5685-2019 | |
dc.relation.ispartofseries | Atmospheric Measurement Techniques 12 (2019), 10 | eng |
dc.relation.issn | 1867-1381 | |
dc.rights.license | CC BY 4.0 Unported | eng |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | eng |
dc.subject | aerosol | eng |
dc.subject | Doppler lidar | eng |
dc.subject | lidar | eng |
dc.subject | optical depth | eng |
dc.subject | photometer | eng |
dc.subject | research vessel | eng |
dc.subject | Southern Hemisphere | eng |
dc.subject | spectrophotometry | eng |
dc.subject | African Margin [Atlantic Ocean] | eng |
dc.subject | Atlantic Ocean | eng |
dc.subject.ddc | 550 | eng |
dc.title | Aerosol measurements with a shipborne Sun-sky-lunar photometer and collocated multiwavelength Raman polarization lidar over the Atlantic Ocean | eng |
dc.type | article | eng |
dc.type | Text | eng |
dcterms.bibliographicCitation.journalTitle | Atmospheric Measurement Techniques | eng |
tib.accessRights | openAccess | eng |
wgl.contributor | TROPOS | eng |
wgl.subject | Umweltwissenschaften | eng |
wgl.type | Zeitschriftenartikel | eng |
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