首页> 外文期刊>Annals of Glaciology >A 275 year ice-core record from Akaciemil Nauk Ice cap, Severnaya ZemSya, Russian Arctic
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A 275 year ice-core record from Akaciemil Nauk Ice cap, Severnaya ZemSya, Russian Arctic

机译:来自俄罗斯北极地区Severnaya ZemSya的Akaciemil Nauk冰盖的275年冰芯记录

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摘要

Between 1999 and 2001, a 724 m long ice core was drilled on Akademii Nauk, the largest glacier on Severnaya Zemlya, Russian Arctic. The drilling site is located near the summit. The core is characterized by high melt-layer content. The melt layers are caused by melting and even by rain during the summer. We present high-resolution data of density, electrical conductivity (dielectrical profiling), stable water isotopes and melt-layer content for the upper 136 m (120 m w.e.) of the ice core. The dating by isotopic cycles and electrical conductivity peak identification suggests that this core section covers approximately the past 275 years. Singularities of volcanogenic and anthropogenic origin provide well-defined additional time markers. Long-term temperatures inferred from 12 year running mean averages of 51(IO reach their lowest level in the entire record around 1790. Thereafter the 818O values indicate a continuously increasing mean temperature on the Akademii Nauk ice cap until 1935, interrupted only by minor cooling episodes. The 20th century is found to be the warmest period in this record.
机译:在1999年至2001年之间,在俄罗斯北极Severnaya Zemlya上最大的冰川Akademii Nauk上钻了724 m长的冰芯。钻井地点位于山顶附近。芯的特征在于高熔体层含量。夏季,融化层是由融化甚至降雨引起的。我们提供了冰芯上层136 m(120 m w.e.)的密度,电导率(介电谱),稳定的水同位素和熔融层含量的高分辨率数据。通过同位素循环和电导率峰值鉴定的年代表明,该核心部分大约涵盖了过去的275年。火山成因和人为起源的奇异性提供了明确的附加时间标记。从12年的平均运行平均值推算得出的长期温度(IO达到1790年左右的整个记录​​的最低水平。此后818O值表明Akademii Nauk冰帽的平均温度持续升高,直到1935年,仅因略微冷却而中断记录中发现20世纪是最温暖的时期。

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