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  1. 学術雑誌掲載済論文
  2. 洋雑誌

Shallow firn cores 1989–2019 in southwest Greenland's percolation zone reveal decreasing density and ice layer thickness after 2012

https://kitami-it.repo.nii.ac.jp/records/2000423
https://kitami-it.repo.nii.ac.jp/records/2000423
93801cc1-bff3-4cbb-ae78-a8b4d52f67ab
名前 / ファイル ライセンス アクション
shallow-firn-cores-1989-2019-in-southwest-greenlands-percolation-zone-reveal-decreasing-density-and-ice-layer-thickness-after-2012(1).pdf shallow-firn-cores-1989-2019-in-southwest-greenlands-percolation-zone-reveal-decreasing-density-and-ice-layer-thickness-after-2012(1).pdf (3.4 MB)
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Item type 学術雑誌論文 / Journal Article(1)
公開日 2023-04-20
タイトル
言語 en
タイトル Shallow firn cores 1989–2019 in southwest Greenland's percolation zone reveal decreasing density and ice layer thickness after 2012
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
著者 Åsa K. Rennermalm

× Åsa K. Rennermalm

en Åsa K. Rennermalm

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Regine Hock

× Regine Hock

en Regine Hock

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Federico Covi

× Federico Covi

en Federico Covi

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Jing Xiao

× Jing Xiao

en Jing Xiao

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Giovanni Corti

× Giovanni Corti

en Giovanni Corti

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Jonathan Kingslake

× Jonathan Kingslake

en Jonathan Kingslake

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Sasha Z. Leidman

× Sasha Z. Leidman

en Sasha Z. Leidman

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Clément Miège

× Clément Miège

en Clément Miège

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Michael Macferrin

× Michael Macferrin

en Michael Macferrin

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Horst Machguth

× Horst Machguth

en Horst Machguth

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抄録
内容記述タイプ Abstract
内容記述 Refreezing of meltwater in firn is a major component of Greenland ice-sheet's mass budget, but in situ observations are rare. Here, we compare the firn density and total ice layer thickness in the upper 15 m of 19 new and 27 previously published firn cores drilled at 15 locations in southwest Greenland (1850–2360 m a.s.l.) between 1989 and 2019. At all sites, ice layer thickness covaries with density over time and space. At the two sites with the earliest observations (1989 and 1998), bulk density increased by 15–18%, in the top 15 m over 28 and 21 years, respectively. However, following the extreme melt in 2012, elevation-detrended density using 30 cores from all sites decreased by 15 kg m−3 a−1 in the top 3.75 m between 2013 and 2019. In contrast, the lowest elevation site's density shows no trend. Thus, temporary build-up in firn pore space and meltwater infiltration capacity is possible despite the long-term increase in Greenland ice-sheet melting.
言語 en
書誌情報 en : Journal of Glaciology

巻 68, 号 269, p. 431-442, 発行日 2022-06
DOI
識別子タイプ DOI
関連識別子 https://doi.org/10.1017/jog.2021.102
権利
言語 en
権利情報 © The Author(s), 2021
出版者
言語 en
出版者 Cambridge University Press
著者版フラグ
言語 en
値 publisher
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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