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1.000 1.050 1.100

Insolation (cal. cnv2d"1)

FIGURE 6.53 Schematic diagram showing the relationship between SSTs in the southeastern Norwegian Sea and Sl80 in the ice core from Dye-3, meltwater discharge from continental ice sheets (Fairbanks, 1989), insolation at 60° N and 5 ' 3C in the Southern Ocean. A series of oscillations in temperature, related to meltwater events, preceded the cold conditions of the Younger Dryas. Deepwater production (registered as a rise in 8I3C) appears to have increased around the time of mwp-IA, and continued through the Younger Dryas chronozone (Koç Karpuz and Jansen, 1992).

1.000 1.050 1.100

Insolation (cal. cnv2d"1)

FIGURE 6.53 Schematic diagram showing the relationship between SSTs in the southeastern Norwegian Sea and Sl80 in the ice core from Dye-3, meltwater discharge from continental ice sheets (Fairbanks, 1989), insolation at 60° N and 5 ' 3C in the Southern Ocean. A series of oscillations in temperature, related to meltwater events, preceded the cold conditions of the Younger Dryas. Deepwater production (registered as a rise in 8I3C) appears to have increased around the time of mwp-IA, and continued through the Younger Dryas chronozone (Koç Karpuz and Jansen, 1992).

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