Articles | Volume 14, issue 3
https://doi.org/10.5194/amt-14-2345-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-14-2345-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Retrieval of stratospheric aerosol size distribution parameters using satellite solar occultation measurements at three wavelengths
Felix Wrana
CORRESPONDING AUTHOR
Institute of Physics, University of Greifswald,
Felix-Hausdorff-Straße 6, 17489 Greifswald, Germany
Christian von Savigny
Institute of Physics, University of Greifswald,
Felix-Hausdorff-Straße 6, 17489 Greifswald, Germany
Jacob Zalach
Institute of Physics, University of Greifswald,
Felix-Hausdorff-Straße 6, 17489 Greifswald, Germany
Larry W. Thomason
NASA Langley Research Center, Hampton, Virginia, USA
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17 citations as recorded by crossref.
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- Sulfate aerosol properties derived from combining coincident ACE-FTS and SAGE III/ISS measurements C. Boone et al. 10.1016/j.jqsrt.2023.108815
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16 citations as recorded by crossref.
- Characterization of stratospheric particle size distribution uncertainties using SAGE II and SAGE III/ISS extinction spectra T. Knepp et al. 10.5194/amt-17-2025-2024
- Growth and Global Persistence of Stratospheric Sulfate Aerosols From the 2022 Hunga Tonga–Hunga Ha'apai Volcanic Eruption M. Boichu et al. 10.1029/2023JD039010
- Stratospheric Aerosol Characteristics from the 2017–2019 Volcanic Eruptions Using the SAGE III/ISS Observations B. Madhavan et al. 10.3390/rs15010029
- Sulfate aerosol properties derived from combining coincident ACE-FTS and SAGE III/ISS measurements C. Boone et al. 10.1016/j.jqsrt.2023.108815
- Stratospheric aerosol size reduction after volcanic eruptions F. Wrana et al. 10.5194/acp-23-9725-2023
- Explaining the green volcanic sunsets after the 1883 eruption of Krakatoa C. von Savigny et al. 10.5194/acp-24-2415-2024
- Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M F. Wrana et al. 10.5194/acp-25-3717-2025
- OMPS-LP aerosol extinction coefficients and their applicability in GloSSAC M. Kovilakam et al. 10.5194/acp-25-535-2025
- An empirical characterization of the aerosol Ångström exponent interpolation bias using SAGE III/ISS data R. Damadeo et al. 10.5194/amt-17-3669-2024
- Observation of the Aerosol Plume From the 2022 Hunga Tonga—Hunga Ha'apai Eruption With SAGE III/ISS C. Duchamp et al. 10.1029/2023GL105076
- Modeling actinic flux and photolysis frequencies in dense biomass burning plumes J. Tirpitz et al. 10.5194/acp-25-1989-2025
- Identification of smoke and sulfuric acid aerosol in SAGE III/ISS extinction spectra T. Knepp et al. 10.5194/amt-15-5235-2022
- Stratospheric Aerosol Composition Observed by the Atmospheric Chemistry Experiment Following the 2019 Raikoke Eruption C. Boone et al. 10.1029/2022JD036600
- The January 2022 Hunga eruption cooled the southern hemisphere in 2022 and 2023 A. Gupta et al. 10.1038/s43247-025-02181-9
- Stratospheric aerosol characteristics from SCIAMACHY limb observations: two-parameter retrieval C. Pohl et al. 10.5194/amt-17-4153-2024
- Version 5 retrievals for ACE-FTS and ACE-imagers C. Boone et al. 10.1016/j.jqsrt.2023.108749
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Short summary
In this paper, we describe a new method for calculating the size of naturally occurring droplets (aerosols) made mostly of sulfuric acid and water that can be found roughly at 20 km altitude in the atmosphere. We use data from the instrument SAGE III/ISS that is mounted on the International Space Station. We show that our method works well, and that the size parameters we calculate are reasonable and can be a valuable addition for a better understanding of aerosols and their effect on climate.
In this paper, we describe a new method for calculating the size of naturally occurring droplets...