Articles | Volume 20, issue 14
Atmos. Chem. Phys., 20, 9067–9085, 2020
https://doi.org/10.5194/acp-20-9067-2020
Atmos. Chem. Phys., 20, 9067–9085, 2020
https://doi.org/10.5194/acp-20-9067-2020

Research article 30 Jul 2020

Research article | 30 Jul 2020

Source attribution of Arctic black carbon and sulfate aerosols and associated Arctic surface warming during 1980–2018

Lili Ren et al.

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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 Lili Ren on behalf of the Authors (26 May 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (07 Jun 2020) by Toshihiko Takemura
RR by Anonymous Referee #2 (13 Jun 2020)
RR by Anonymous Referee #3 (17 Jun 2020)
RR by Anonymous Referee #1 (28 Jun 2020)
ED: Publish as is (29 Jun 2020) by Toshihiko Takemura
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Short summary
Observations show that the concentrations of Arctic aerosols have declined since the early 1980s, which potentially contributed to the recent, rapid Arctic warming. We found that changes in sulfate and black carbon aerosols over the midlatitudes of the Northern Hemisphere had a larger impact on Arctic temperature than other regions and that the aerosol-induced temperature change explained approximately 20 % of the observed Arctic warming during 1980–2018.
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