论火山作用在Dansgaard-Oeschger旋回中的作用

J. Lohmann, A. Svensson
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引用次数: 0

摘要

摘要以前已经提出了大型火山爆发对制度转变和长期气候变率的重大影响。但是,由于大型火山爆发与过去气候变化的不准确同步,对这一现象的统计评估受到了阻碍。在这里,这是通过结合来自格陵兰和南极冰芯的双极火山活动的新记录和来自相同冰芯的气候突变记录来实现的。在> 99%的可信度下,我们发现在末次冰期最显著的大规模气候突变——Dansgaard-Oeschger事件发生之前,双极火山爆发比预期的偶然性更频繁。在12-60 ka期间的20次气候变化事件中,有5(7)次发生在两极火山爆发后的20(50)年内。因此,如此大规模的喷发可能是大规模气候突变的短期触发因素,并可能部分解释Dansgaard-Oeschger循环的可变性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On the Role of Volcanism in Dansgaard-Oeschger Cycles
Abstract. A significant influence of major volcanic eruptions on regime shifts and long-term climate variability has been suggested previously. But a statistical assessment of this has been hampered by inaccurate synchronization of large volcanic eruptions to changes in past climate. Here, this is achieved by combining a new record of bipolar volcanism from Greenland and Antarctic ice cores with records of abrupt climate change derived from the same ice cores. We show that at > 99 % confidence bipolar volcanic eruptions occurred more frequently than expected by chance just before the onset of Dansgaard-Oeschger events, the most prominent large-scale abrupt climate changes of the last glacial period. Out of 20 climate change events in the 12–60 ka period, 5 (7) occur within 20 (50) years after a bipolar eruption. Thus, such large eruptions may act as short-term triggers for large-scale abrupt climate change, and may explain part of the variability of Dansgaard-Oeschger cycles.
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