Articles | Volume 13, issue 8
Clim. Past, 13, 1037–1048, 2017
https://doi.org/10.5194/cp-13-1037-2017
Clim. Past, 13, 1037–1048, 2017
https://doi.org/10.5194/cp-13-1037-2017

Research article 18 Aug 2017

Research article | 18 Aug 2017

Atmospheric circulation and hydroclimate impacts of alternative warming scenarios for the Eocene

Henrik Carlson and Rodrigo Caballero

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Interactive discussion

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
ED: Reconsider after major revisions (05 May 2017) by Arne Winguth
AR by Henrik Carlson on behalf of the Authors (22 Jun 2017)  Author's response    Manuscript
ED: Publish as is (12 Jul 2017) by Arne Winguth
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Short summary
Climate models are able to simulate the surface temperature of the early Eocene as reconstructed from paleoclimatology data, but only by using extremely high CO2 concentrations or clouds that are more transparent to solar radiation. We explore the potential for distinguishing among these two forcing agents via their impact on regional climate. Better constraining the radiative forcing that led to Eocene warmth has important implications for understanding Earth's climate sensitivity.