Simulation of the cold climate event 8200 years ago by meltwater outburst from Lake Agassiz
Simulation of the cold climate event 8200 years ago by meltwater outburst from Lake Agassiz
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阿加西湖融水爆发模拟 8200 年前的寒冷气候事件
DOI:
10.1029/2004pa001030
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发表时间:
2004
期刊:
影响因子:
--
通讯作者:
M. Montoya
中科院分区:
文献类型:
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作者:
E. Bauer;A. Ganopolski;M. Montoya
meltwater pulse is assumed to have a volume of 1.6 10 14 m 3 and a period of discharge of 2 years on the basis of glaciological modeling of the decay of the Laurentide Ice Sheet (LIS). We present a possible mechanism which can explain the centennial duration of the 8.2 ka cold event. The mechanism is related to the existence of an additional equilibrium climate state with reduced North Atlantic Deep Water (NADW) formation and a southward shift of the NADW formation area. Hints at the additional climate state were obtained from the largely varying duration of the pulse-induced cold episode in response to overlaid random freshwater fluctuations in Monte Carlo simulations. The model equilibrium state was attained by releasing a weak multicentury freshwater flux through the St. Lawrence pathway completed by the meltwater pulse. The existence of such a climate mode appears essential for reproducing climate anomalies in close agreement with paleoclimatic reconstructions of the 8.2 ka event. The results furthermore suggest that the temporal evolution of the cold event was partly a matter of chance. INDEX TERMS: 3344 Meteorology and Atmospheric Dynamics: Paleoclimatology; 4255 Oceanography: General: Numerical modeling; 4532 Oceanography: Physical: General circulation; 4215 Oceanography: General: Climate and interannual variability (3309); 9325 Information Related to Geographic Region: Atlantic Ocean;