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An ice-core record of Antarctic sea-ice extent in the southern Indian Ocean for the past 300 years

机译:过去300年南印度洋南极海冰范围的冰芯记录

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摘要

The differing response of ice extent in the Arctic and Antarctic to global average temperature change, over approximately the last three decades, highlights the importance of reconstructing long-term sea-ice history. Here, using high-resolution ice-core records of methanesulfonate (MS-) from the East Antarctic ice sheet in Princess Elizabeth Land, we reconstruct southern Indian Ocean sea-ice extent (SIE) for the sector 62-92 degrees E for the period AD 1708-2000. Annual MS concentration positively correlates in this sector with satellite-derived SIE for the period 1979-2000 (r(2) = 0.25, P<0.02). The 293 year MS- record of proxy SIE shows multi-decadal variations, with large decreases occurring in two warm intervals during the Little Ice Age, and during the 1940s. It is very likely that the global temperature is the controlling factor of Antarctic sea-ice variation at the centennial scale, although there has been a change in phase between them in recent decades.
机译:在大约过去的三十年中,北极和南极的冰范围对全球平均温度变化的不同响应,凸显了重建长期海冰历史的重要性。在这里,利用伊丽莎白公主乐园东极南极冰盖的甲烷磺酸盐(MS-)高分辨率冰芯记录,我们重建了该时期东段62-92度的印度洋南部海冰范围(SIE)公元1708-2000年。 1979-2000年期间,该领域的年度MS浓度与卫星衍生的SIE正相关(r(2)= 0.25,P <0.02)。代理SIE的293年MS记录显示了十年的变化,在小冰期和1940年代的两个暖期中出现了较大的下降。尽管近几十年来两者之间的相位发生了变化,但全球温度很可能是百年尺度南极海冰变化的控制因素。

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