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Collapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulation

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Figure

Figure 1. (a) Northern Hemisphere ice sheet mass balance 14.5–14.3 ka and its influence on mean annual sea surface salinity 14.4 ka (100 year mean; SC_south minusNoSC_south); the thick black lines delimit major drainage basins at 14.5 ka, the colored circle
Figure 2. Evolution of (a) mean Arctic Ocean and Greenland-Iceland-Norwegian sea surface salinity; (b) maximum Atlantic Meridional Overturning Circulation(AMOC) stream function; (c) surface air temperature over central Greenland (“Summit” region; 35–45°W,
Figure 3. (a) Central Greenland surface air temperature [Laurentide-Cordilleran ice saddle collapse delimited with colored boxes

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