Articles | Volume 21, issue 10
https://doi.org/10.5194/acp-21-7671-2021
https://doi.org/10.5194/acp-21-7671-2021
Research article
 | 
20 May 2021
Research article |  | 20 May 2021

Wintertime direct radiative effects due to black carbon (BC) over the Indo-Gangetic Plain as modelled with new BC emission inventories in CHIMERE

Sanhita Ghosh, Shubha Verma, Jayanarayanan Kuttippurath, and Laurent Menut

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Shubha Verma on behalf of the Authors (08 Feb 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (06 Mar 2021) by Yafang Cheng
AR by Shubha Verma on behalf of the Authors (16 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (20 Mar 2021) by Yafang Cheng
AR by Shubha Verma on behalf of the Authors (30 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (31 Mar 2021) by Yafang Cheng
AR by Shubha Verma on behalf of the Authors (10 Apr 2021)  Manuscript 
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Short summary
Wintertime direct radiative perturbation due to black carbon (BC) aerosols was assessed over the Indo-Gangetic Plain with an efficiently modelled BC distribution. The atmospheric radiative warming due to BC was about 50–70 % larger than surface cooling. Compared to the atmosphere without BC, for which a net cooling at the top of the atmosphere was exhibited, enhanced atmospheric radiative warming by 2–3 times and a reduction in surface cooling by 10–20 % were found due to BC.
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