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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 1 | Copyright

Special issue: The SPARC Reanalysis Intercomparison Project (S-RIP) (ACP/ESSD...

Atmos. Chem. Phys., 17, 485-499, 2017
https://doi.org/10.5194/acp-17-485-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 11 Jan 2017

Research article | 11 Jan 2017

Revisiting the observed surface climate response to large volcanic eruptions

Fabian Wunderlich and Daniel M. Mitchell
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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
ED: Publish subject to technical corrections (14 Aug 2016) by Peter Haynes
ED: Referee Nomination & Report Request started (15 Aug 2016) by Peter Haynes
RR by Anonymous Referee #1 (01 Sep 2016)
RR by Anonymous Referee #2 (05 Sep 2016)
ED: Reconsider after minor revisions (Editor review) (13 Sep 2016) by Peter Haynes
ED: Reconsider after minor revisions (Editor review) (10 Oct 2016) by Peter Haynes
ED: Publish as is (25 Oct 2016) by Peter Haynes
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Large volcanic eruptions can eject aerosols into the stratosphere and prevent UV radiation reaching the surface, resulting in surface cooling. A secondary, non-linear effect occurs at high latitudes. While the surface cooling is robust in observations, we show that the non-linear, high-latitude effect is less robust. Climate models have failures at reproducing both aspects, probably because of aliasing with other climate modes and overrepresentation of stratospheric aerosol.
Large volcanic eruptions can eject aerosols into the stratosphere and prevent UV radiation...
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