Disentangling fast and slow responses of the East Asian summer monsoon to reflecting and absorbing aerosol forcings

Wang, Zhili; Lin, Lei; Yang, Meilin; Xu, Yangyang; Li, Jiangnan

doi:https://doi.org/10.5194/acp-17-11075-2017

Articles | Volume 17, issue 18

https://doi.org/10.5194/acp-17-11075-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-17-11075-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 18

Research article

|

19 Sep 2017

Research article |

| 19 Sep 2017

Disentangling fast and slow responses of the East Asian summer monsoon to reflecting and absorbing aerosol forcings

Zhili Wang, Lei Lin, Meilin Yang, Yangyang Xu, and Jiangnan Li

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Final revised paper (published on 19 Sep 2017)
Supplement to the final revised paper
Preprint (discussion started on 02 Jun 2017)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'comments to authors', Anonymous Referee #2, 23 Jun 2017
- AC1: 'Response to referee 2', Zhili Wang, 31 Jul 2017
RC2: 'Comments on ”Disentangling fast and slow responses of the East Asian summer monsoon to reflecting and absorbing aerosol forcings” by Zhili Wang et al.,', Anonymous Referee #1, 05 Jul 2017
- AC2: 'Response to referee 1', Zhili Wang, 31 Jul 2017

Peer-review completion

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

AR by Zhili Wang on behalf of the Authors (31 Jul 2017) Author's response Manuscript

ED: Referee Nomination & Report Request started (31 Jul 2017) by Rolf Müller

RR by Anonymous Referee #2 (09 Aug 2017)

RR by Anonymous Referee #1 (11 Aug 2017)

ED: Publish as is (24 Aug 2017) by Rolf Müller

AR by Zhili Wang on behalf of the Authors (25 Aug 2017)

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Short summary

There is still debate over whether the total aerosols enhance or weaken the East Asian summer monsoon (EASM). This could be related to both the complicated nature of aerosol chemical compositions and ocean responses to aerosols. Our results show that there is a clear distinction between fast and slow responses of the EASM to scattering and absorbing aerosols, and the slow response due to aerosol-induced change in sea surface temperature plays an important role in driving the change of the EASM.