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A continuous 250-year record of volcanic activity from Princess Elizabeth Land, East Antarctica

机译:来自南极东部伊丽莎白公主地的火山活动连续250年记录

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A 51.85 m ice core collected from site LGB65 (accumulation rate 127 kg m?2 a?1, mean annual temperature ?33.1°C) in Princess Elizabeth Land, East Antarctica, during the 1996–97 Chinese First Antarctic Inland Expedition has been analysed for chemical composition and oxygen isotope ratio. Based on the high definition of seasonal variations of major ions, the ice core was dated with errors within ± 3 years. The continuous sulphate analysis of the ice core provides an annually resolved proxy history of southern hemisphere volcanism in the past 250 years. High nssSO42?, concentrations seem to be well correlated to some explosive volcanic eruptions, such as Tambora (AD 1815), Coseguina (AD 1835), Krakatoa (AD 1883) and Tarawera (AD 1886). In comparison with other volcanic records, it seems that nssSO42? concentration data provide a better proxy for detecting volcanic activity than nssSO42? fluxes in low and intermediate accumulation regions, however, in high accumulation regions, small and moderate events may be more identifiable using of nssSO42? flux data.
机译:分析了1996-97年中国第一次南极内陆探险期间从南极东部伊丽莎白公主地LGB65站点收集的51.85 m冰芯(累积速率为127 kg m?2 a?1,年平均气温为33.1°C)。用于化学成分和氧同位素比。根据主要离子的季节性变化的高清晰度,冰芯的日期误差在±3年以内。对冰芯的连续硫酸盐分析提供了过去250年中南半球火山活动的年度解析代理历史。高nssSO42?浓度似乎与一些爆炸性火山喷发有很好的相关性,例如Tambora(AD 1815),Coseguina(AD 1835),Krakatoa(AD 1883)和Tarawera(AD 1886)。与其他火山记录相比,似乎是nssSO42?浓度数据比nssSO42提供更好的代理来检测火山活动?低和中等积累区的通量,但是,在高积累区,使用nssSO42可以更容易识别小事件和中等事件。通量数据。

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