Simulation of observed climate changes in 1850–2014 with climate model INM-CM5

Volodin, Evgeny; Gritsun, Andrey

doi:https://doi.org/10.5194/esd-9-1235-2018

Articles | Volume 9, issue 4

https://doi.org/10.5194/esd-9-1235-2018

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

https://doi.org/10.5194/esd-9-1235-2018

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

Articles | Volume 9, issue 4

Research article

|

25 Oct 2018

Research article |

| 25 Oct 2018

Simulation of observed climate changes in 1850–2014 with climate model INM-CM5

Evgeny Volodin and Andrey Gritsun

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Final revised paper (published on 25 Oct 2018)
Preprint (discussion started on 08 May 2018)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'referee comment on MS No esd-2018-21', Anonymous Referee #1, 15 Jul 2018
- AC1: 'response to comment of referee 1', Evgeny Volodin, 27 Jul 2018
RC2: 'Minor technical corrections', Anonymous Referee #2, 22 Jul 2018
- AC2: 'response to comment of referee 2', Evgeny Volodin, 27 Jul 2018

Peer-review completion

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

ED: Reconsider after major revisions (17 Sep 2018) by Christian Franzke

AR by Evgeny Volodin on behalf of the Authors (04 Oct 2018)

ED: Publish as is (08 Oct 2018) by Christian Franzke

AR by Evgeny Volodin on behalf of the Authors (09 Oct 2018)

Short summary

Climate changes of 1850–2014 are modeled with the climate model INM-CM5. Periods of fast warming in 1920–1940 and 1980–2000 as well as its slowdown in 1950–1975 and 2000–2014 are correctly reproduced by the model. The notable improvement with respect to the previous model version is the correct reproduction of slowdowns in global warming that we attribute to a new aerosol block in the model and a more accurate description of the solar constant in the new (CMIP6) IPCC protocol.