Articles | Volume 21, issue 1
Atmos. Chem. Phys., 21, 535–560, 2021
https://doi.org/10.5194/acp-21-535-2021

Special issue: Satellite observations, in situ measurements and model simulations...

Atmos. Chem. Phys., 21, 535–560, 2021
https://doi.org/10.5194/acp-21-535-2021

Research article 15 Jan 2021

Research article | 15 Jan 2021

Stratospheric aerosol layer perturbation caused by the 2019 Raikoke and Ulawun eruptions and their radiative forcing

Corinna Kloss et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Corinna Kloss on behalf of the Authors (04 Nov 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (17 Nov 2020) by Peter Haynes
RR by J.M. Haywood (18 Nov 2020)
RR by Anonymous Referee #1 (19 Nov 2020)
ED: Publish subject to technical corrections (24 Nov 2020) by Peter Haynes
AR by Corinna Kloss on behalf of the Authors (28 Nov 2020)  Author's response    Manuscript
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Short summary
The year 2019 was particularly rich for the stratospheric aerosol layer due to two volcanic eruptions (at Raikoke and Ulawun) and wildfire events. With satellite observations and models, we describe the exceptionally complex situation following the Raikoke eruption. The respective plume overwhelmed the Northern Hemisphere stratosphere in terms of aerosol load and resulted in the highest climate impact throughout the past decade.
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