Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1029/2020GL090978 |
Basal crevasse formation on Byrd Glacier, East Antarctica, as proxy for past subglacial flooding events | |
Sarah F. Child; Leigh A. Stearns; C. J. vander Veen; Pedro Eló; segui | |
2021-07-21 | |
发表期刊 | Geophysical Research Letters
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出版年 | 2021 |
英文摘要 | Linear elastic fracture mechanics (LEFM) suggests that short-lived flow accelerations, such as the one initiated by a flooding event beneath Byrd Glacier in 2006, can form abnormally large basal crevasses at the grounding line. Airborne radar measurements acquired in 2011 reveal hundreds of basal crevasses ranging in height from |
领域 | 气候变化 |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/334125 |
专题 | 气候变化 |
推荐引用方式 GB/T 7714 | Sarah F. Child,Leigh A. Stearns,C. J. vander Veen,et al. Basal crevasse formation on Byrd Glacier, East Antarctica, as proxy for past subglacial flooding events[J]. Geophysical Research Letters,2021. |
APA | Sarah F. Child,Leigh A. Stearns,C. J. vander Veen,Pedro Eló,&segui.(2021).Basal crevasse formation on Byrd Glacier, East Antarctica, as proxy for past subglacial flooding events.Geophysical Research Letters. |
MLA | Sarah F. Child,et al."Basal crevasse formation on Byrd Glacier, East Antarctica, as proxy for past subglacial flooding events".Geophysical Research Letters (2021). |
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