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Sea-ice dynamics strongly promote Snowball Earth initiation and destabilize tropical sea-ice margins

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Figure

Fig. 1. Initiation of a Marinoan Snowball Earth in ECHAM5/MPI-OM with the model’s standard highbare sea-ice albedo (Voigt et al., 2011)
Fig. 2.Albedo of snow on sea ice (dashed) and bare sea ice (solid) of the standard setup ofECHAM5/MPI-OM used in Voigt et al
Fig. 5. sea-ice cover.CO COmean thickness of snow on sea ice. Bottom: zonal-mean annual-mean thickness tendencies for snow on sea ice: local melting andsnow/sea-ice conversion (red), sea-ice dynamics (blue), and snow-2, which results in 70 % sea-ice cover
Fig. 6. Simulation with low bare-sea ice albedo and 209 ppm CO2, which results in 70Annual cycle of zonal-mean sea-ice fraction
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