Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG

Grandey, Benjamin S.; Rothenberg, Daniel; Avramov, Alexander; Jin, Qinjian; Lee, Hsiang-He; Liu, Xiaohong; Lu, Zheng; Albani, Samuel; Wang, Chien

doi:https://doi.org/10.5194/acp-18-15783-2018

Articles | Volume 18, issue 21

https://doi.org/10.5194/acp-18-15783-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-18-15783-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 18, issue 21

Research article

|

02 Nov 2018

Research article |

| 02 Nov 2018

Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG

Benjamin S. Grandey, Daniel Rothenberg, Alexander Avramov, Qinjian Jin, Hsiang-He Lee, Xiaohong Liu, Zheng Lu, Samuel Albani, and Chien Wang

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Final revised paper (published on 02 Nov 2018)
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Preprint (discussion started on 02 May 2018)
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Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Review', Anonymous Referee #1, 28 May 2018
RC2: 'Review of Grandey et al.', Anonymous Referee #2, 30 May 2018
AC1: 'Response to referee comments', Benjamin Grandey, 29 Aug 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Benjamin Grandey on behalf of the Authors (29 Aug 2018) Author's response Manuscript

ED: Referee Nomination & Report Request started (10 Sep 2018) by Kostas Tsigaridis

RR by Anonymous Referee #2 (05 Oct 2018)

ED: Publish subject to minor revisions (review by editor) (13 Oct 2018) by Kostas Tsigaridis

AR by Benjamin Grandey on behalf of the Authors (19 Oct 2018) Author's response Manuscript

ED: Publish as is (21 Oct 2018) by Kostas Tsigaridis

AR by Benjamin Grandey on behalf of the Authors (22 Oct 2018)

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Short summary

Anthropogenic emissions of aerosol particles likely cool the climate system. We investigate the uncertainty in the strength of the cooling effect by exploring the representation of aerosols in a global climate model. We conclude that the specific representation of aerosols in global climate models has important implications for climate modelling. Important factors include the representation of aerosol mixing state, size distribution, and optical properties.