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DOI | 10.1038/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 |
ISSN | 2041-1723 |
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
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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 |
推荐引用方式 GB/T 7714 | 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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