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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 18, issue 16
Atmos. Chem. Phys., 18, 12345–12361, 2018
https://doi.org/10.5194/acp-18-12345-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 18, 12345–12361, 2018
https://doi.org/10.5194/acp-18-12345-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 27 Aug 2018

Research article | 27 Aug 2018

Historical black carbon deposition in the Canadian High Arctic: a >250-year long ice-core record from Devon Island

Christian M. Zdanowicz et al.

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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
AR by Christian Zdanowicz on behalf of the Authors (18 Feb 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Feb 2018) by Ari Laaksonen
RR by Anonymous Referee #1 (16 Mar 2018)
RR by Anonymous Referee #3 (05 Apr 2018)
ED: Reconsider after major revisions (05 Apr 2018) by Ari Laaksonen
AR by Christian Zdanowicz on behalf of the Authors (18 May 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 May 2018) by Ari Laaksonen
RR by Anonymous Referee #3 (09 Jul 2018)
ED: Publish subject to minor revisions (review by editor) (09 Jul 2018) by Ari Laaksonen
AR by Christian Zdanowicz on behalf of the Authors (26 Jul 2018)  Author's response    Manuscript
ED: Publish as is (09 Aug 2018) by Ari Laaksonen
Publications Copernicus
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Short summary
Black carbon (BC) particles emitted by natural and anthropogenic sources (e.g., wildfires, coal burning) can amplify climate warming by increasing sunlight energy absorption on snow-covered surfaces. This paper presents a new ice-core record of historical (1810–1990) BC deposition in the Canadian Arctic. The Devon ice cap record differs from Greenland ice cores, implying large variations in BC deposition across the Arctic that must be accounted for to better quantity their future climate impact.
Black carbon (BC) particles emitted by natural and anthropogenic sources (e.g., wildfires, coal...
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