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Arctic sea ice simulation in the PlioMIP ensemble

  • Fergus W. Howell
  • , Alan M. Haywood
  • , Bette L. Otto-Bliesner
  • , Fran Bragg
  • , Wing Le Chan
  • , Mark A. Chandler
  • , Camille Contoux
  • , Youichi Kamae
  • , Ayako Abe-Ouchi
  • , Nan A. Rosenbloom
  • , Christian Stepanek
  • , Zhongshi Zhang
  • University of Leeds
  • National Center for Atmospheric Research
  • University of Bristol
  • The University of Tokyo
  • Columbia University
  • Aix-Marseille Université
  • University of Tsukuba
  • Japan Agency for Marine-Earth Science and Technology
  • Alfred Wegener Institute - Helmholtz Centre for Polar and Marine Research
  • Bjerknes Centre for Climate Research

Research output: Contribution to journalArticlepeer-review

15 Scopus citations

Abstract

Eight general circulation models have simulated the mid-Pliocene warm period (mid-Pliocene, 3.264 to 3.025Ma) as part of the Pliocene Modelling Intercomparison Project (PlioMIP). Here, we analyse and compare their simulation of Arctic sea ice for both the pre-industrial period and the mid-Pliocene. Mid-Pliocene sea ice thickness and extent is reduced, and the model spread of extent is more than twice the pre-industrial spread in some summer months. Half of the PlioMIP models simulate ice-free conditions in the mid-Pliocene. This spread amongst the ensemble is in line with the uncertainties amongst proxy reconstructions for mid-Pliocene sea ice extent. Correlations between mid-Pliocene Arctic temperatures and sea ice extents are almost twice as strong as the equivalent correlations for the pre-industrial simulations. The need for more comprehensive sea ice proxy data is highlighted, in order to better compare model performances.

Original languageEnglish
Pages (from-to)749-767
Number of pages19
JournalClimate of the Past
Volume12
Issue number3
DOIs
StatePublished - Mar 23 2016

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