Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes
The polarization lidar photometer networking (POLIPHON) method introduced to separate coarse-mode and fine-mode particle properties of Eyjafjallajökull volcanic aerosols in 2010 is extended to cover Saharan dust events as well. Furthermore, new volcanic dust observations performed after the Grimsvöt...
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ftleibnizopen:oai:oai.leibnizopen.de:U_VC-IYBdbrxVwz6dLzH 2023-05-15T16:09:24+02:00 Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes Ansmann, A. Seifert, P. Tesche, M. Wandinger, U. 2012 application/pdf https://doi.org/10.34657/1199 https://oa.tib.eu/renate/handle/123456789/527 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ Atmospheric Chemistry and Physics, Volume 12, Issue 20, Page 9399-9415 aerosol property atmospheric plume biomass burning concentration (composition) dust extinction coefficient mixing particulate matter photometer volcanic aerosol 550 article Text 2012 ftleibnizopen https://doi.org/10.34657/1199 2023-03-20T00:12:40Z The polarization lidar photometer networking (POLIPHON) method introduced to separate coarse-mode and fine-mode particle properties of Eyjafjallajökull volcanic aerosols in 2010 is extended to cover Saharan dust events as well. Furthermore, new volcanic dust observations performed after the Grimsvötn volcanic eruptions in 2011 are presented. The retrieval of particle mass concentrations requires mass-specific extinction coefficients. Therefore, a review of recently published mass-specific extinction coefficients for Saharan dust and volcanic dust is given. Case studies of four different scenarios corroborate the applicability of the profiling technique: (a) Saharan dust outbreak to central Europe, (b) Saharan dust plume mixed with biomass-burning smoke over Cape Verde, and volcanic aerosol layers originating from (c) the Eyjafjallajökull eruptions in 2010 and (d) the Grimsvötn eruptions in 2011. Strong differences in the vertical aerosol layering, aerosol mixing, and optical properties are observed for the different volcanic events. publishedVersion Article in Journal/Newspaper Eyjafjallajökull LeibnizOpen (The Leibniz Association) |
institution |
Open Polar |
collection |
LeibnizOpen (The Leibniz Association) |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
aerosol property atmospheric plume biomass burning concentration (composition) dust extinction coefficient mixing particulate matter photometer volcanic aerosol 550 |
spellingShingle |
aerosol property atmospheric plume biomass burning concentration (composition) dust extinction coefficient mixing particulate matter photometer volcanic aerosol 550 Ansmann, A. Seifert, P. Tesche, M. Wandinger, U. Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes |
topic_facet |
aerosol property atmospheric plume biomass burning concentration (composition) dust extinction coefficient mixing particulate matter photometer volcanic aerosol 550 |
description |
The polarization lidar photometer networking (POLIPHON) method introduced to separate coarse-mode and fine-mode particle properties of Eyjafjallajökull volcanic aerosols in 2010 is extended to cover Saharan dust events as well. Furthermore, new volcanic dust observations performed after the Grimsvötn volcanic eruptions in 2011 are presented. The retrieval of particle mass concentrations requires mass-specific extinction coefficients. Therefore, a review of recently published mass-specific extinction coefficients for Saharan dust and volcanic dust is given. Case studies of four different scenarios corroborate the applicability of the profiling technique: (a) Saharan dust outbreak to central Europe, (b) Saharan dust plume mixed with biomass-burning smoke over Cape Verde, and volcanic aerosol layers originating from (c) the Eyjafjallajökull eruptions in 2010 and (d) the Grimsvötn eruptions in 2011. Strong differences in the vertical aerosol layering, aerosol mixing, and optical properties are observed for the different volcanic events. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Ansmann, A. Seifert, P. Tesche, M. Wandinger, U. |
author_facet |
Ansmann, A. Seifert, P. Tesche, M. Wandinger, U. |
author_sort |
Ansmann, A. |
title |
Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes |
title_short |
Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes |
title_full |
Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes |
title_fullStr |
Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes |
title_full_unstemmed |
Profiling of fine and coarse particle mass: Case studies of Saharan dust and Eyjafjallajökull/Grimsvötn volcanic plumes |
title_sort |
profiling of fine and coarse particle mass: case studies of saharan dust and eyjafjallajökull/grimsvötn volcanic plumes |
publisher |
München : European Geopyhsical Union |
publishDate |
2012 |
url |
https://doi.org/10.34657/1199 https://oa.tib.eu/renate/handle/123456789/527 |
genre |
Eyjafjallajökull |
genre_facet |
Eyjafjallajökull |
op_source |
Atmospheric Chemistry and Physics, Volume 12, Issue 20, Page 9399-9415 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.34657/1199 |
_version_ |
1766405301627518976 |