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低估了北太平洋弧形火山带复发远程火山灰扩散的风险。

Underestimated risks of recurrent long-range ash dispersal from northern Pacific Arc volcanoes.

机构信息

Department of Geography, College of Science, Swansea University, Swansea, UK.

Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Denmark.

出版信息

Sci Rep. 2016 Jul 21;6:29837. doi: 10.1038/srep29837.

DOI:10.1038/srep29837
PMID:27445233
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC4956762/
Abstract

Widespread ash dispersal poses a significant natural hazard to society, particularly in relation to disruption to aviation. Assessing the extent of the threat of far-travelled ash clouds on flight paths is substantially hindered by an incomplete volcanic history and an underestimation of the potential reach of distant eruptive centres. The risk of extensive ash clouds to aviation is thus poorly quantified. New evidence is presented of explosive Late Pleistocene eruptions in the Pacific Arc, currently undocumented in the proximal geological record, which dispersed ash up to 8000 km from source. Twelve microscopic ash deposits or cryptotephra, invisible to the naked eye, discovered within Greenland ice-cores, and ranging in age between 11.1 and 83.7 ka b2k, are compositionally matched to northern Pacific Arc sources including Japan, Kamchatka, Cascades and Alaska. Only two cryptotephra deposits are correlated to known high-magnitude eruptions (Towada-H, Japan, ca 15 ka BP and Mount St Helens Set M, ca 28 ka BP). For the remaining 10 deposits, there is no evidence of age- and compositionally-equivalent eruptive events in regional volcanic stratigraphies. This highlights the inherent problem of under-reporting eruptions and the dangers of underestimating the long-term risk of widespread ash dispersal for trans-Pacific and trans-Atlantic flight routes.

摘要

广泛分布的火山灰对社会构成重大的自然危害,尤其是对航空运输造成严重干扰。评估远距离火山灰云对飞行航线的威胁程度,受到火山活动历史记录不完全和对远距离喷发中心潜在影响范围的低估的严重阻碍。因此,火山灰对航空业的广泛风险难以准确量化。本文提出了新的证据,表明在太平洋火环地区曾发生过末次冰期晚期的猛烈喷发,但目前在近地表地质记录中尚未记录到这些喷发,喷发物最远扩散至 8000 公里之外。在格陵兰冰芯中发现了 12 个肉眼不可见的微小火山灰沉积物或隐火山灰,其年龄在 11.1 至 83.7 ka b2k 之间,与包括日本、堪察加半岛、喀斯喀特山脉和阿拉斯加在内的北太平洋火环源区的成分相匹配。只有两个隐火山灰沉积物与已知的高幅度喷发(日本的十和田火山喷发,约 15 ka BP 和美国的圣海伦斯山 Set M 喷发,约 28 ka BP)相关。对于其余 10 个沉积物,在区域火山地层学中没有发现与它们年龄和成分相当的喷发事件的证据。这突显了火山喷发报告不足的固有问题,以及低估跨太平洋和跨大西洋飞行航线广泛火山灰扩散的长期风险的危险。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bd03/4956762/f05d3adc9688/srep29837-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bd03/4956762/fe336058e7e5/srep29837-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bd03/4956762/659f6e90e106/srep29837-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bd03/4956762/f05d3adc9688/srep29837-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bd03/4956762/fe336058e7e5/srep29837-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bd03/4956762/659f6e90e106/srep29837-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bd03/4956762/f05d3adc9688/srep29837-f3.jpg

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Proc Natl Acad Sci U S A. 2013 May 14;110(20):8025-9. doi: 10.1073/pnas.1301474110. Epub 2013 Apr 29.
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