Articles | Volume 20, issue 17
https://doi.org/10.5194/acp-20-10545-2020
https://doi.org/10.5194/acp-20-10545-2020
Research article
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10 Sep 2020
Research article | Highlight paper |  | 10 Sep 2020

Vertical profiles of light absorption and scattering associated with black carbon particle fractions in the springtime Arctic above 79° N

W. Richard Leaitch, John K. Kodros, Megan D. Willis, Sarah Hanna, Hannes Schulz, Elisabeth Andrews, Heiko Bozem, Julia Burkart, Peter Hoor, Felicia Kolonjari, John A. Ogren, Sangeeta Sharma, Meng Si, Knut von Salzen, Allan K. Bertram, Andreas Herber, Jonathan P. D. Abbatt, and Jeffrey R. Pierce

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Richard Leaitch on behalf of the Authors (24 Jan 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (29 Jan 2020) by Lynn M. Russell
RR by Anonymous Referee #3 (07 Feb 2020)
RR by Anonymous Referee #1 (23 Feb 2020)
ED: Reconsider after major revisions (23 Feb 2020) by Lynn M. Russell
AR by Richard Leaitch on behalf of the Authors (06 Apr 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (10 Apr 2020) by Lynn M. Russell
RR by Anonymous Referee #1 (22 Apr 2020)
ED: Reconsider after major revisions (24 Apr 2020) by Lynn M. Russell
AR by Richard Leaitch on behalf of the Authors (02 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (01 Jul 2020) by Lynn M. Russell
AR by Richard Leaitch on behalf of the Authors (02 Jul 2020)  Author's response   Manuscript 
ED: Publish as is (09 Jul 2020) by Lynn M. Russell
AR by Richard Leaitch on behalf of the Authors (15 Jul 2020)  Manuscript 
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Short summary
Black carbon is a factor in the warming of the Arctic atmosphere due to its ability to absorb light, but the uncertainty is high and few observations have been made in the high Arctic above 80° N. We combine airborne and ground-based observations in the springtime Arctic, at and above 80° N, with simulations from a global model to show that light absorption by black carbon may be much larger than modelled. However, the uncertainty remains high.
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