Atmospheric Observations Research Group, The University of Queensland, Brisbane, Australia.
School of Agriculture and Environment, The University of Western Australia, Perth, Australia.
Sci Rep. 2020 Oct 22;10(1):18000. doi: 10.1038/s41598-020-75071-z.
Understanding past climate variability is critical to informing debate of likely impacts of global warming on weather and climate, and water resources. Here we present a near annual resolution reconstruction of climate developed from a speleothem that spans the Eemian [Marine Isotope Stage 5e (MIS 5e)] from 117,500 to 123,500 years BP-the most recent period in the Earth's history when temperatures were similar to those of today. Using Mg, Sr, and Ba as proxies, we show the first indication of solar and teleconnection cyclic forcing of Eemian climate in southeast Australia, a region at present often affected by severe drought and bushfires. We find evidence for multi-centennial dry periods interpreted as mega-droughts, and highlight the importance of understanding the causes of these in the context of a rapidly warming world, where temperatures are now, or projected to exceed those of the Eemian.
了解过去的气候变异性对于了解全球变暖对天气和气候以及水资源可能产生的影响至关重要。在这里,我们展示了一项由洞穴石笋发展而来的近乎年度分辨率的气候重建,该石笋记录了全新世[海洋同位素阶段 5e(MIS 5e)]的时间范围为 117500 至 123500 年前——这是地球历史上最近一次温度与今天相似的时期。我们使用 Mg、Sr 和 Ba 作为示踪剂,首次表明了东南澳大利亚全新世气候受太阳和远距离联系循环驱动的迹象,该地区目前经常受到严重干旱和丛林大火的影响。我们发现了证据表明存在多百年的干旱期,可解释为特大干旱,并强调了在全球迅速变暖的背景下理解这些干旱成因的重要性,因为目前或预计全球气温将超过全新世时期的气温。