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DOI10.1038/s41467-021-23534-w
Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica
Minowa M.; Sugiyama S.; Ito M.; Yamane S.; Aoki S.
发表日期2021
ISSN2041-1723
卷号12期号:1
英文摘要Basal melting of ice shelves is considered to be the principal driver of recent ice mass loss in Antarctica. Nevertheless, in-situ oceanic data covering the extensive areas of a subshelf cavity are sparse. Here we show comprehensive structures of temperature, salinity and current measured in January 2018 through four boreholes drilled at a ~3-km-long ice shelf of Langhovde Glacier in East Antarctica. The measurements were performed in 302–12 m-thick ocean cavity beneath 234–412 m-thick ice shelf. The data indicate that Modified Warm Deep Water is transported into the grounding zone beneath a stratified buoyant plume. Water at the ice-ocean interface was warmer than the in-situ freezing point by 0.65–0.95°C, leading to a mean basal melt rate estimate of 1.42 m a−1. Our measurements indicate the existence of a density-driven water circulation in the cavity beneath the ice shelf of Langhovde Glacier, similar to that proposed for warm-ocean cavities of larger Antarctic ice shelves. © 2021, The Author(s).
语种英语
scopus关键词basal melting; data set; freezing; ice shelf; salinity; thermohaline circulation; Antarctica; East Antarctica
来源期刊Nature Communications
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/251392
作者单位Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan; Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
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Minowa M.,Sugiyama S.,Ito M.,et al. Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica[J],2021,12(1).
APA Minowa M.,Sugiyama S.,Ito M.,Yamane S.,&Aoki S..(2021).Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica.Nature Communications,12(1).
MLA Minowa M.,et al."Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica".Nature Communications 12.1(2021).
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