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High-resolution 900 year volcanic and climatic record from the Vostok area, East Antarctica

机译:来自南极东部沃斯托克地区的900年高分辨率火山和气候记录

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Ion chromatography measurements of 1730 snow and firn samples obtained from three short cores and one pit in the Vostok station area, East Antarctica, allowed for the production of the combined volcanic record of the last 900 years (AD 1093a??2010). The resolution of the record is 2a??3 samples per accumulation year. In total, 24 volcanic events have been identified, including seven well-known low-latitude eruptions (Pinatubo 1991, Agung 1963, Krakatoa 1883, Tambora 1815, Huanaputina 1600, Kuwae 1452, El Chichon 1259) found in most of the polar ice cores. In comparison with three other East Antarctic volcanic records (South Pole, Plateau Remote and Dome C), the Vostok record contains more events within the last 900 years. The differences between the records may be explained by local glaciological conditions, volcanic detection methodology, and, probably, differences in atmospheric circulation patterns. The strongest volcanic signal (both in sulfate concentration and flux) was attributed to the AD 1452 Kuwae eruption, similar to the Plateau Remote and Talos Dome records. The average snow accumulation rate calculated between volcanic stratigraphic horizons for the period AD 1260a??2010 is 20.9 mm Hsub2/subO. Positive (+13%) anomalies of snow accumulation were found for AD 1661a??1815 and AD 1992a??2010, and negative (a??12%) for AD 1260a??1601. We hypothesized that the changes in snow accumulation are associated with regional peculiarities in atmospheric transport.
机译:离子色谱法测量了从南极东部沃斯托克站区的三个短岩心和一个坑中获得的1730个雪和烧成的样品,这产生了过去900年(AD 1093a,2010)的合并火山记录。记录的分辨率是每个累积年2a-3个样本。总共发现了24个火山事件,包括在大多数极地冰芯中发现的7个著名的低纬度火山爆发(皮纳图博1991年,阿贡1963年,克拉卡托亚1883年,坦博拉1815年,瓦纳普蒂纳1600年,库瓦伊1452年,埃尔奇琴1259年) 。与其他三个东极南极火山记录(南极,高原偏远和圆顶C)相比,沃斯托克记录包含过去900年中的更多事件。记录之间的差异可以用当地的冰川条件,火山探测方法以及大气环流模式的差异来解释。最强的火山信号(硫酸盐浓度和通量)均归因于AD 1452 Kuwae喷发,类似于高原遥测和Talos Dome记录。计算出的公元1260a ?? 2010年火山地层之间的平均积雪率为20.9 mm H 2 O。 AD 1661a,1815和AD 1992a,2010年积雪的正向(+ 13%)异常,AD 1260a,1601年和2010年的负向(a-12%)。我们假设积雪的变化与大气传输中的区域特征有关。

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