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2016
DOI: 10.5194/acp-2016-183
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Porous aerosol in degassing plumes of Mt. Etna and Mt. Stromboli

Abstract: Aerosols of the volcanic degassing plumes from Mt. Etna and Mt. Stromboli were probed with in situ instruments on board the Deutsches Zentrum fur Luft- und Raumfahrt research aircraft Falcon during the contrail, volcano, and cirrus experiment CONCERT in September 2011. Aerosol properties were analyzed using angular-scattering intensities and particle size distributions measured simultaneously with the Polar Nephelometer and the Forward Scattering Spectrometer probes (FSSP series 100 and 300), respectively. Aer… Show more

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“…To prevent the first few principal component loadings from being dominated by the large absolute variations in forward scattering intensity the analysis was performed on the natural logarithm of theF 11 values. This transformation produces a set of principal 20 components where the first component, for example, explains the largest possible relative variance in data (Shcherbakov et al, 2016). No transformation was applied to the −F 12 /F 11 measurements.…”
Section: Pca Analysismentioning
confidence: 99%
“…To prevent the first few principal component loadings from being dominated by the large absolute variations in forward scattering intensity the analysis was performed on the natural logarithm of theF 11 values. This transformation produces a set of principal 20 components where the first component, for example, explains the largest possible relative variance in data (Shcherbakov et al, 2016). No transformation was applied to the −F 12 /F 11 measurements.…”
Section: Pca Analysismentioning
confidence: 99%