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ACP | Articles | Volume 18, issue 11
Atmos. Chem. Phys., 18, 7827–7840, 2018
https://doi.org/10.5194/acp-18-7827-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 18, 7827–7840, 2018
https://doi.org/10.5194/acp-18-7827-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 04 Jun 2018

Research article | 04 Jun 2018

Aerosol–fog interaction and the transition to well-mixed radiation fog

Ian Boutle 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 Ian Boutle on behalf of the Authors (29 Jan 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (18 Mar 2018) by Yafang Cheng
RR by Anonymous Referee #2 (28 Mar 2018)
RR by Anonymous Referee #1 (29 Mar 2018)
ED: Reconsider after major revisions (24 Apr 2018) by Yafang Cheng
AR by Ian Boutle on behalf of the Authors (04 May 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 May 2018) by Yafang Cheng
RR by Thierry Bergot (17 May 2018)
ED: Publish as is (17 May 2018) by Yafang Cheng
Publications Copernicus
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Short summary
Aerosol processes are a key mechanism in the development of fog. Poor representation of aerosol–fog interaction can result in large biases in fog forecasts, such as surface temperatures which are too high and fog which is too deep and long lived. A relatively simple representation of aerosol–fog interaction can actually lead to significant improvements in forecasting. Aerosol–fog interaction can have a large effect on the climate system but is poorly represented in climate models.
Aerosol processes are a key mechanism in the development of fog. Poor representation of...
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