期刊
GEOPHYSICAL RESEARCH LETTERS
卷 33, 期 15, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2006GL026705
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The last deglaciation was interrupted by three major cooling events, the Younger Dryas, the Preboreal Oscillation and the 8.2-ka cold event. As the Laurentide Ice Sheet retreated, different outlets from Lake Agassiz became available causing the proglacial lake to drain to a new level in a rather short timescale ( flood) and divert continental runoff over hundreds of years ( routing). Here we use an Earth System Model to investigate the impact of floods ( short term, high amplitude) versus routing events ( long term, low amplitude) on the thermohaline circulation and the resulting climate change. We show that the initial outbursts of freshwater are not strong enough to influence large-scale climate and can therefore not be the cause of millennial-scale climate variability. However, routing events have the potential of weakening the thermohaline circulation and therefore causing a cool event in the Northern Hemisphere.
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