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DOI | 10.1126/science.aao1447 |
Observed rapid bedrock uplift in amundsen sea embayment promotes ice-sheet stability | |
Barletta V.R.; Bevis M.; Smith B.E.; Wilson T.; Brown A.; Bordoni A.; Willis M.; Khan S.A.; Rovira-Navarro M.; Dalziel I.; Smalley R.; Kendrick E.; Konfal S.; Caccamise D.J.; Aster R.C.; Nyblade A.; Wiens D.A. | |
发表日期 | 2018 |
ISSN | 0036-8075 |
起始页码 | 1335 |
结束页码 | 1339 |
卷号 | 360期号:6395 |
英文摘要 | The marine portion of the West Antarctic Ice Sheet (WAIS) in the Amundsen Sea Embayment (ASE) accounts for one-fourth of the cryospheric contribution to global sea-level rise and is vulnerable to catastrophic collapse. The bedrock response to ice mass loss, glacial isostatic adjustment (GIA), was thought to occur on a time scale of 10,000 years. We used new GPS measurements, which show a rapid (41 millimeters per year) uplift of the ASE, to estimate the viscosity of the mantle underneath. We found a much lower viscosity (4 × 1018 pascal-second) than global average, and this shortens the GIA response time scale to decades up to a century. Our finding requires an upward revision of ice mass loss from gravity data of 10% and increases the potential stability of the WAIS against catastrophic collapse. © 2017 The Authors. |
英文关键词 | ice; bedrock; catastrophic event; collapse; cryosphere; glacioisostasy; GPS; mantle; sea level change; uplift; viscosity; vulnerability; Antarctica; Article; bedrock; Cretaceous; cryosphere; geological time; glacial isostatic adjustment; glaciation; gravity; ice sheet stability; lithosphere; negative feedback; Paleozoic; physical parameters; prediction; priority journal; rock; sea level; signal noise ratio; viscoelasticity; viscosity; Amundsen Sea; Antarctic Ice Sheet; Antarctica; Southern Ocean; West Antarctic Ice Sheet; West Antarctica |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/242957 |
作者单位 | DTU Space, National Space Institute, Geodynamics Department, Technical University of Denmark, Kgs. Lyngby, Denmark; School of Earth Science, Ohio State University, Columbus, OH, United States; University of Washington, Seattle, WA, United States; DTU Compute, Technical University of Denmark, Kgs. Lyngby, Denmark; University of Colorado Boulder, Boulder, CO, United States; TU Delft, Delft, Netherlands; Institute for Geophysics, University of Texas, Austin, TX, United States; Center for Earthquake Research and Information, University of Memphis, Memphis, TN, United States; Colorado State University, Fort Collins, CO, United States; Penn State University, State CollegePA, United States; Washington University in St. Louis, St. Louis, MO, United States |
推荐引用方式 GB/T 7714 | Barletta V.R.,Bevis M.,Smith B.E.,et al. Observed rapid bedrock uplift in amundsen sea embayment promotes ice-sheet stability[J],2018,360(6395). |
APA | Barletta V.R..,Bevis M..,Smith B.E..,Wilson T..,Brown A..,...&Wiens D.A..(2018).Observed rapid bedrock uplift in amundsen sea embayment promotes ice-sheet stability.Science,360(6395). |
MLA | Barletta V.R.,et al."Observed rapid bedrock uplift in amundsen sea embayment promotes ice-sheet stability".Science 360.6395(2018). |
条目包含的文件 | 条目无相关文件。 |
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