McClymont, E.L. and Ford, H. and Ho, S.-L. and Tindall, J. and Haywood, A.M. and Alonso-Garcia, M. and Bailey, I. and Berke, M. A. and Littler, K. and Patterson, M. and Petrick, B. and Peterse, F. and Ravelo, A. C. and Risebrobakken, B. and Schepper, S. De and Swann, G. E. A. and Thirumalai, K. and Tierney, J. E. and Weijst, C. van der and White, S. and Abe-Ouchi, A. and Baatsen, M.L.J. and Brady, E.C. and Chan, W.-L. and Chandan, D. and Feng, R. and Guo, C. and von der Heydt, A.S. and Hunter, S. and Li, X. and Lohmann, G. and Nisancioglu, K.H. and Otto-Bliesner, B.L. and Peltier, W.R. and Stepanek, C. and Zhang, Z. (2020) 'Lessons from a high CO2 world : an ocean view from ~ 3 million years ago.', Climate of the past., 16 (4). pp. 1599-1615.
A range of future climate scenarios are projected for high atmospheric CO2 concentrations, given uncertainties over future human actions as well as potential environmental and climatic feedbacks. The geological record offers an opportunity to understand climate system response to a range of forcings and feedbacks which operate over multiple temporal and spatial scales. Here, we examine a single interglacial during the late Pliocene (KM5c, ca. 3.205 ± 0.01 Ma) when atmospheric CO2 concentrations were higher than pre-industrial, but similar to today and to the lowest emission scenarios for this century. As orbital forcing and continental configurations were almost identical to today, we are able to focus on equilibrium climate system response to modern and near-future CO2. Using proxy data from 32 sites, we demonstrate that global mean sea-surface temperatures were warmer than pre-industrial, by ~ 2.3 ºC for the combined proxy data (foraminifera Mg/Ca and alkenones), or by ~ 3.2 ºC (alkenones only). Compared to the pre-industrial, reduced meridional gradients and enhanced warming in the North Atlantic are consistently reconstructed. There is broad agreement between data and models at the global scale, with regional differences reflecting ocean circulation and/or proxy signals. An uneven distribution of proxy data in time and space does, however, add uncertainty to our anomaly calculations. The reconstructed global mean sea-surface temperature anomaly for KM5c is warmer than all but three of the PlioMIP2 model outputs, and the reconstructed North Atlantic data tend to align with the warmest KM5c model values. Our results demonstrate that even under low CO2 emission scenarios, surface ocean warming may be expected to exceed model projections, and will be accentuated in the higher latitudes.
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|Publisher Web site:||https://doi.org/10.5194/cp-16-1599-2020|
|Publisher statement:||© Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.|
|Date accepted:||02 July 2020|
|Date deposited:||27 August 2020|
|Date of first online publication:||27 August 2020|
|Date first made open access:||27 August 2020|
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