Reconstructing volcanic radiative forcing since 1990, using a comprehensive emission inventory and spatially resolved sulfur injections from satellite data in a chemistry-climate model
Abstract 2) and aerosol extinction, we characterized the chemical and radiative influence of volcanic aerosols for the period between 1990 and 2019. 2 emission inventory that includes more than 500 explosive volcanic eruptions reaching the upper troposphere and the stratosphere. Each perturbation identified was derived from the satellite data and incorporated as a three-dimensional SO2 plume into a chemistry-climate model without the need for additional assumptions about altitude distribution and eruption duration as needed for a “point source” approach. 2 and aerosol extinction by up to four satellite instruments enabled a reliable conversion of extinction measurements into injected SO2. In the chemistry-climate model, the SO2 from each individual plume was converted into aerosol particles and their optical properties were determined. Furthermore, the aerosol optical depth (AOD) and the instantaneous radiative forcing on climate were calculated online. Combined with model improvements, the results of the simulations are consistent with the observations of the various satellites. kt SO2 directly into the upper troposphere/lower stratosphere (UTLS) region or the sulfur species are transported via convection and advection. Our results confirm that these relatively minor eruptions, which occur quite frequently, can nevertheless contribute to the stratospheric aerosol layer and are relevant for the Earth's radiation budget. These minor eruptions cause a total global instantaneous radiative forcing of the order of - 0.1 W m - 2 at the top of the atmosphere (TOA) compared to a background stratospheric aerosol forcing of about - 0.04 W m - 2. Medium-strength eruptions injecting about 400 kt SO2 into the stratosphere or accumulation of consecutive smaller eruptions can lead to a total instantaneous forcing of about - 0.3 W m - 2. We show that it is critical to include the contribution of the extratropical lowermost stratospheric aerosol in the forcing calculations.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Reconstructing volcanic radiative forcing since 1990, using a comprehensive emission inventory and spatially resolved sulfur injections from satellite data in a chemistry-climate model ; volume:23 ; number:2 ; year:2023 ; pages:1169-1207 ; extent:39
Atmospheric chemistry and physics ; 23, Heft 2 (2023), 1169-1207 (gesamt 39)
- Creator
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Schallock, Jennifer
Brühl, Christoph
Bingen, Christine
Höpfner, Michael
Rieger, Landon
Lelieveld, Jos
- DOI
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10.5194/acp-23-1169-2023
- URN
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urn:nbn:de:101:1-2023033008151944052719
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:47 AM CEST
Data provider
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Schallock, Jennifer
- Brühl, Christoph
- Bingen, Christine
- Höpfner, Michael
- Rieger, Landon
- Lelieveld, Jos