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Fig. 4 Results of MIROC freshwater hosing simulations (0

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1 Fig. 4 Results of MIROC freshwater hosing simulations (0
Fig. 4 Results of MIROC freshwater hosing simulations (0.05 sverdrup) for temperature and precipitation. Results of MIROC freshwater hosing simulations (0.05 sverdrup) for temperature and precipitation. (A) Map of atmospheric temperature difference and (B) precipitation difference between hosing and control experiments for interglacial climate (mean for 400 to 500 model years after onset of hosing, which is the last 100 years of the “hosing” period). As in (A) and (B), but for (C and D) midglacial climate and (E and F) full-glacial climate. As in (A) and (B), but for sensitivity experiment of (G and H) midglacial climate “without” ice sheet and for (I and J) interglacial climate “with” ice sheet. In the left panels, solid line (dashed line) contours are drawn for every degree Celsius of temperature increase (decrease). The right panels show the same climatological pattern (preindustrial, contour lines) and anomaly in % (colors) caused by freshwater hosing (mean for 400 to 500 model years) for each climate state. Dome Fuji Ice Core Project Members: et al. Sci Adv 2017;3:e Copyright © 2017, The Authors

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