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Mechanisms causing reduced Arctic sea ice loss in a coupled climate model

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Figure

Fig. 1. (a) Arctic September mean sea ice extent in the HadGEM1historical forcing runs and (b) 15-yr running gradient of extent.
Fig. 2. (a–c) show linear trend in September ice concentrationice thickness from 1994–2000 in a superposition of satellite andsubmarine observations from that period (described more fully inHadGEM1 ALL and ANT ensembles respectively.(yr−1) from 1979–2011 in the HadISST observations, and in the (d–f) show meanAppendix A), and in the ALL and ANT ensembles respectively.
Fig. 3. (a) shows time series of global and Arctic temperaturebles;September mean ice extent ((mean temperature north of 70◦ N) in the ALL and ANT ensem- (b) shows annual mean global temperature (◦C) plotted against× 106 km2).
Fig. 5. Decadal means of terms in the Arctic heat budget for theeach term, the time mean of the equivalent periods in the controlruns from 1980–2030 has been subtracted
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