Climate Change Data Portal
DOI | 10.1073/pnas.1516130113 |
Dynamic Antarctic ice sheet during the early to mid-Miocene | |
Gasson E.; DeConto R.M.; Pollard D.; Levy R.H. | |
发表日期 | 2016 |
ISSN | 0027-8424 |
起始页码 | 3459 |
结束页码 | 3464 |
卷号 | 113期号:13 |
英文摘要 | Geological data indicate that there were major variations in Antarctic ice sheet volume and extent during the early to mid-Miocene. Simulating such large-scale changes is problematic because of a strong hysteresis effect, which results in stability once the ice sheets have reached continental size. A relatively narrow range of atmospheric CO2 concentrations indicated by proxy records exacerbates this problem. Here, we are able to simulate large-scale variability of the early to mid-Miocene Antarctic ice sheet because of three developments in our modeling approach. (i) We use a climate-ice sheet coupling method utilizing a high-resolution atmospheric component to account for ice sheet-climate feedbacks. (ii) The ice sheet model includes recently proposed mechanisms for retreat into deep subglacial basins caused by ice-cliff failure and ice-shelf hydrofracture. (iii)We account for changes in the oxygen isotopic composition of the ice sheet by using isotope-enabled climate and ice sheet models. We compare our modeling results with ice-proximal records emerging from a sedimentological drill core from the Ross Sea (Andrill-2A) that is presented in a companion article. The variability in Antarctic ice volume that we simulate is equivalent to a seawater oxygen isotope signal of 0.52-0.66‰, or a sea level equivalent change of 30-36 m, for a range of atmospheric CO2 between 280 and 500 ppm and a changing astronomical configuration. This result represents a substantial advance in resolving the long-standing model data conflict of Miocene Antarctic ice sheet and sea level variability. |
英文关键词 | Antarctic ice sheet; Miocene; Oxygen isotopes; Sea level |
语种 | 英语 |
scopus关键词 | carbon dioxide; oxygen; sea water; Antarctica; Article; astronomy; climate; continental shelf; glaciation; ice sheet; ice shelf; Lower Miocene; Middle Miocene; priority journal; sea level; vegetation |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/158905 |
作者单位 | Gasson, E., Climate System Research Center, University of Massachusetts, Amherst, MA 01003, United States; DeConto, R.M., Climate System Research Center, University of Massachusetts, Amherst, MA 01003, United States; Pollard, D., Earth and Environmental Systems Institute, Pennsylvania State University, State College, PA 16802, United States; Levy, R.H., GNS Science, Avalon, Lower Hutt, 5011, New Zealand |
推荐引用方式 GB/T 7714 | Gasson E.,DeConto R.M.,Pollard D.,et al. Dynamic Antarctic ice sheet during the early to mid-Miocene[J],2016,113(13). |
APA | Gasson E.,DeConto R.M.,Pollard D.,&Levy R.H..(2016).Dynamic Antarctic ice sheet during the early to mid-Miocene.Proceedings of the National Academy of Sciences of the United States of America,113(13). |
MLA | Gasson E.,et al."Dynamic Antarctic ice sheet during the early to mid-Miocene".Proceedings of the National Academy of Sciences of the United States of America 113.13(2016). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。