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The potential for sea ice-albedo feedback to give rise to nonlinear climate change in the Arctic Ocean region -defined as a nonlinear relationship between polar and global temperature change or, equivalently, a time-varying polar amplification -is explored in IPCC climate models. Five models supplying SRES A1B ensembles for the 21 st century are examined and very linear relationships are found between polar and global temperatures (indicating linear polar region climate change), and betweendoi:10.1016/b978-0-12-382100-3.10013-7 fatcat:fb2n3h4lcnbxpli5hdcoa54s3i