Publication Abstracts

Kageyama et al. 2021

Kageyama, M., L.C. Sime, M. Sicard, M.-V. Guarino, A. de Vernal, R. Stein, D. Schroeder, I. Malmierca-Vallet, A. Abe-Ouchi, C. Bitz, P. Braconnot, E.C. Brady, J. Cao, M.A. Chamberlain, D. Feltham, C. Guo, A.N. LeGrande, G. Lohmann, K.J. Meissner, L. Menviel, P. Morozova, K.H. Nisancioglu, B.L. Otto-Bliesner, R. O'ishi, S. Ramos Buarque, D. Salas y Melia, S. Sherriff-Tadano, J. Stroeve, X. Shi, B. Sun, R.A. Tomas, E. Volodin, N.K.H. Yeung, Q. Zhang, Z. Zhang, W. Zheng, and T. Ziehn, 2021: A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: Sea ice data compilation and model differences. Clim. Past, 17, no. 1, 37-62, doi:10.5194/cp-17-37-2021.

The Last Interglacial period (LIG) is a period with increased summer insolation at high northern latitudes, which results in strong changes in the terrestrial and marine cryosphere. Understanding the mechanisms for this response via climate modelling and comparing the models' representation of climate reconstructions is one of the objectives set up by the Paleoclimate Modelling Intercomparison Project for its contribution to the sixth phase of the Coupled Model Intercomparison Project. Here we analyse the results from 16 climate models in terms of Arctic sea ice. The multi-model mean reduction in minimum sea ice area from the pre industrial period (PI) to the LIG reaches 50% (multi-model mean LIG area is 3.20×106 km2, compared to 6.46×106 km2 for the PI). On the other hand, there is little change for the maximum sea ice area (which is 15-16×106 km2 for both the PI and the LIG. To evaluate the model results we synthesise LIG sea ice data from marine cores collected in the Arctic Ocean, Nordic Seas and northern North Atlantic. The reconstructions for the northern North Atlantic show year-round ice-free conditions, and most models yield results in agreement with these reconstructions. Model-data disagreement appear for the sites in the Nordic Seas close to Greenland and at the edge of the Arctic Ocean. The northernmost site with good chronology, for which a sea ice concentration larger than 75% is reconstructed even in summer, discriminates those models which simulate too little sea ice. However, the remaining models appear to simulate too much sea ice over the two sites south of the northernmost one, for which the reconstructed sea ice cover is seasonal. Hence models either underestimate or overestimate sea ice cover for the LIG, and their bias does not appear to be related to their bias for the pre-industrial period. Drivers for the inter-model differences are different phasing of the up and down short-wave anomalies over the Arctic Ocean, which are associated with differences in model albedo; possible cloud property differences, in terms of optical depth; and LIG ocean circulation changes which occur for some, but not all, LIG simulations. Finally, we note that inter-comparisons between the LIG simulations and simulations for future climate with moderate (1%/yr) CO2 increase show a relationship between LIG sea ice and sea ice simulated under CO2 increase around the years of doubling CO2. The LIG may therefore yield insight into likely 21st century Arctic sea ice changes using these LIG simulations.

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BibTeX Citation

  author={Kageyama, M. and Sime, L. C. and Sicard, M. and Guarino, M.-V. and de Vernal, A. and Stein, R. and Schroeder, D. and Malmierca-Vallet, I. and Abe-Ouchi, A. and Bitz, C. and Braconnot, P. and Brady, E. C. and Cao, J. and Chamberlain, M. A. and Feltham, D. and Guo, C. and LeGrande, A. N. and Lohmann, G. and Meissner, K. J. and Menviel, L. and Morozova, P. and Nisancioglu, K. H. and Otto-Bliesner, B. L. and O'ishi, R. and Ramos Buarque, S. and Salas y Melia, D. and Sherriff-Tadano, S. and Stroeve, J. and Shi, X. and Sun, B. and Tomas, R. A. and Volodin, E. and Yeung, N. K. H. and Zhang, Q. and Zhang, Z. and Zheng, W. and Ziehn, T.},
  title={A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: Sea ice data compilation and model differences},
  journal={Clim. Past},

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RIS Citation

ID  - ka01400p
AU  - Kageyama, M.
AU  - Sime, L. C.
AU  - Sicard, M.
AU  - Guarino, M.-V.
AU  - de Vernal, A.
AU  - Stein, R.
AU  - Schroeder, D.
AU  - Malmierca-Vallet, I.
AU  - Abe-Ouchi, A.
AU  - Bitz, C.
AU  - Braconnot, P.
AU  - Brady, E. C.
AU  - Cao, J.
AU  - Chamberlain, M. A.
AU  - Feltham, D.
AU  - Guo, C.
AU  - LeGrande, A. N.
AU  - Lohmann, G.
AU  - Meissner, K. J.
AU  - Menviel, L.
AU  - Morozova, P.
AU  - Nisancioglu, K. H.
AU  - Otto-Bliesner, B. L.
AU  - O'ishi, R.
AU  - Ramos Buarque, S.
AU  - Salas y Melia, D.
AU  - Sherriff-Tadano, S.
AU  - Stroeve, J.
AU  - Shi, X.
AU  - Sun, B.
AU  - Tomas, R. A.
AU  - Volodin, E.
AU  - Yeung, N. K. H.
AU  - Zhang, Q.
AU  - Zhang, Z.
AU  - Zheng, W.
AU  - Ziehn, T.
PY  - 2021
TI  - A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: Sea ice data compilation and model differences
JA  - Clim. Past
VL  - 17
IS  - 1
SP  - 37
EP  - 62
DO  - 10.5194/cp-17-37-2021
ER  -

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