Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M

<p>Stratospheric aerosol size distribution parameters are derived from the multiple-wavelength aerosol extinction retrievals of the SAGE III/M3M instrument (Stratospheric Aerosol and Gas Experiment III on the Russian satellite Meteor-3M) and analyzed for their evolution between 2002 and 2005....

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Main Authors: F. Wrana, T. Deshler, C. Löns, L. W. Thomason, C. von Savigny
Format: Article
Language:English
Published: Copernicus Publications 2025-03-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/25/3717/2025/acp-25-3717-2025.pdf
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author F. Wrana
T. Deshler
C. Löns
L. W. Thomason
L. W. Thomason
C. von Savigny
author_facet F. Wrana
T. Deshler
C. Löns
L. W. Thomason
L. W. Thomason
C. von Savigny
author_sort F. Wrana
collection DOAJ
description <p>Stratospheric aerosol size distribution parameters are derived from the multiple-wavelength aerosol extinction retrievals of the SAGE III/M3M instrument (Stratospheric Aerosol and Gas Experiment III on the Russian satellite Meteor-3M) and analyzed for their evolution between 2002 and 2005. The broad wavelength spectrum of the measurements enables us to derive all three parameters within an assumed monomodal lognormal size distribution. The 2002–2005 stratospheric aerosol layer was mostly at close to background conditions but included three moderate-magnitude tropical volcanic eruptions (Ruang, Reventador, and Manam). The SAGE III/M3M instrument measured only at middle and high latitudes, but derived particle size distribution (PSD) parameters indicate a reduction in particle size and an increase in particle number concentration after all three eruptions. In addition to this likely volcanic effect on the PSD, an influence of seasonal polar winter condensation events including meteoric smoke particles on the derived aerosol size is possible, especially due to the long-lasting low stratospheric temperatures during the northern winters of 2002/2003 and 2004/2005. During the same winters, polar stratospheric clouds (PSCs) were likely observed by the instrument. A comparison of the derived stratospheric aerosol size dataset with balloon-borne in situ measurements in Kiruna, Sweden, shows generally good agreement, but there are systematic differences below roughly 15 km altitude. Finally, the effect of the necessary assumption of a PSD shape on the aerosol size derivation with remote sensing instruments is shown and discussed.</p>
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spelling doaj-art-5fba1460376d4abebfdafcf12b705fd92025-08-20T01:49:43ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242025-03-01253717373610.5194/acp-25-3717-2025Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3MF. Wrana0T. Deshler1C. Löns2L. W. Thomason3L. W. Thomason4C. von Savigny5Institute of Physics, University of Greifswald, Felix-Hausdorff-Str. 6, 17489 Greifswald, GermanyDepartment of Atmospheric Science, University of Wyoming, Laramie, Wyoming, USAInstitute of Physics, University of Greifswald, Felix-Hausdorff-Str. 6, 17489 Greifswald, Germanyformerly at: NASA Langley Research Center, Hampton, Virginia, USAretiredInstitute of Physics, University of Greifswald, Felix-Hausdorff-Str. 6, 17489 Greifswald, Germany<p>Stratospheric aerosol size distribution parameters are derived from the multiple-wavelength aerosol extinction retrievals of the SAGE III/M3M instrument (Stratospheric Aerosol and Gas Experiment III on the Russian satellite Meteor-3M) and analyzed for their evolution between 2002 and 2005. The broad wavelength spectrum of the measurements enables us to derive all three parameters within an assumed monomodal lognormal size distribution. The 2002–2005 stratospheric aerosol layer was mostly at close to background conditions but included three moderate-magnitude tropical volcanic eruptions (Ruang, Reventador, and Manam). The SAGE III/M3M instrument measured only at middle and high latitudes, but derived particle size distribution (PSD) parameters indicate a reduction in particle size and an increase in particle number concentration after all three eruptions. In addition to this likely volcanic effect on the PSD, an influence of seasonal polar winter condensation events including meteoric smoke particles on the derived aerosol size is possible, especially due to the long-lasting low stratospheric temperatures during the northern winters of 2002/2003 and 2004/2005. During the same winters, polar stratospheric clouds (PSCs) were likely observed by the instrument. A comparison of the derived stratospheric aerosol size dataset with balloon-borne in situ measurements in Kiruna, Sweden, shows generally good agreement, but there are systematic differences below roughly 15 km altitude. Finally, the effect of the necessary assumption of a PSD shape on the aerosol size derivation with remote sensing instruments is shown and discussed.</p>https://acp.copernicus.org/articles/25/3717/2025/acp-25-3717-2025.pdf
spellingShingle F. Wrana
T. Deshler
C. Löns
L. W. Thomason
L. W. Thomason
C. von Savigny
Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M
Atmospheric Chemistry and Physics
title Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M
title_full Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M
title_fullStr Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M
title_full_unstemmed Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M
title_short Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M
title_sort spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with sage iii m3m
url https://acp.copernicus.org/articles/25/3717/2025/acp-25-3717-2025.pdf
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