Articles | Volume 15, issue 4
https://doi.org/10.5194/cp-15-1375-2019
https://doi.org/10.5194/cp-15-1375-2019
Research article
 | 
22 Jul 2019
Research article |  | 22 Jul 2019

The relevance of mid-Holocene Arctic warming to the future

Masakazu Yoshimori and Marina Suzuki

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Cited articles

Abe, M., Nozawa, T., Ogura, T., and Takata, K.: Effect of retreating sea ice on Arctic cloud cover in simulated recent global warming, Atmos. Chem. Phys., 16, 14343–14356, https://doi.org/10.5194/acp-16-14343-2016, 2016. 
Abe-Ouchi, A., Saito, F., Kawamura, K., Raymo, M. E., Okuno, J., Takahashi, K., and Blatter, H.: Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume, Nature, 500, 190–193, https://doi.org/10.1038/nature12374, 2013. 
Armour, K. C., Marshall, J., Scott, J. R., Donohoe, A., and Newsom, E. R.: Southern Ocean warming delayed by circumpolar upwelling and equatorward transport, Nat. Geosci., 9, 549–554, https://doi.org/10.1038/ngeo2731, 2016. 
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Short summary
A relation between mid-Holocene (MH) and future Arctic warming mechanisms is investigated with emphasis on the similarities and differences of physical processes. Simulations from 10 atmosphere–ocean general circulation models are analyzed. The several key processes are identified which are linked to multi-model mean response and multi-model variation of the response. This study suggests that knowledge of the MH Arctic climate has a potential to constrain future Arctic climate projections.