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Impact of Iceberg Calving on the Retreat of Thwaites Glacier, West Antarctica Over the Next Century With Different Calving Laws and Ocean Thermal Forcing 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2019
作者:  Yu, Hongju;  Rignot, Eric;  Seroussi, Helene;  Morlighem, Mathieu;  Choi, Youngmin
收藏  |  浏览/下载：8/0  |  提交时间：2020/02/17
Thwaites Glacier  Calving  Fracture  Mass balance  Southern Ocean  Sea level rise  
Ice sheet melting: Estimates still uncertain, experts warn 新闻
来源平台：EurekAlert! - Earth Science. 发布日期：2019
作者:  admin
收藏  |  浏览/下载：6/0  |  提交时间：2020/01/16
Ice Sheet Melting: Estimates Still Uncertain 新闻
来源平台：Science Daily. 发布日期：2019
作者:  admin
收藏  |  浏览/下载：8/0  |  提交时间：2020/01/20
Shrinking of Greenland's Glaciers Began Accelerating in 2000, Research Finds 新闻
来源平台：Science Daily. 发布日期：2019
作者:  admin
收藏  |  浏览/下载：1/0  |  提交时间：2020/01/20
Shrinking of Greenland's glaciers began accelerating in 2000, research finds 新闻
来源平台：EurekAlert!. 发布日期：2019
作者:  admin
收藏  |  浏览/下载：7/0  |  提交时间：2020/01/16
The Possible Transition From Glacial Surge to Ice Stream on Vavilov Ice Cap 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2019, 46 (23) : 13892-13902
作者:  Zheng, Whyjay;  Pritchard, Matthew E.;  Willis, Michael J.;  Stearns, Leigh A.
收藏  |  浏览/下载：8/0  |  提交时间：2020/02/17
glacial surge  ice stream  Vavilov Ice Cap  shear margins  Peclet number  summer speedup  
Development of the Patagonian Ice Fields reveals the enormous complexity of physical interactions 新闻
来源平台：German Aerosapce Center. 发布日期：2019
作者:  admin
收藏  |  浏览/下载：3/0  |  提交时间：2020/01/16
Greenland ice loss much faster than expected 新闻
来源平台：European Space Agency. 发布日期：2019
作者:  admin
收藏  |  浏览/下载：4/0  |  提交时间：2020/01/16
Greenland Ice Losses Rising Faster Than Expected 新闻
来源平台：Science Daily. 发布日期：2019
作者:  admin
收藏  |  浏览/下载：6/0  |  提交时间：2020/01/20
Mass balance of the Greenland Ice Sheet from 1992 to 2018 期刊论文
NATURE, 2020, 579 (7798) : 233-+
作者:  Scudellari, Megan
收藏  |  浏览/下载：11/0  |  提交时间：2020/04/16

The Greenland Ice Sheet has been a major contributor to global sea-level rise in recent decades(1,2), and it is expected to continue to be so(3). Although increases in glacier flow(4-6) and surface melting(7-9) have been driven by oceanic(10-12) and atmospheric(13,14) warming, the magnitude and trajectory of the ice sheet'  s mass imbalance remain uncertain. Here we compare and combine 26 individual satellite measurements of changes in the ice sheet'  s volume, flow and gravitational potential to produce a reconciled estimate of its mass balance. The ice sheet was close to a state of balance in the 1990s, but annual losses have risen since then, peaking at 345 +/- 66 billion tonnes per year in 2011. In all, Greenland lost 3,902 +/- 342 billion tonnes of ice between 1992 and 2018, causing the mean sea level to rise by 10.8 +/- 0.9 millimetres. Using three regional climate models, we show that the reduced surface mass balance has driven 1,964 +/- 565 billion tonnes (50.3 per cent) of the ice loss owing to increased meltwater runoff. The remaining 1,938 +/- 541 billion tonnes (49.7 per cent) of ice loss was due to increased glacier dynamical imbalance, which rose from 46 +/- 37 billion tonnes per year in the 1990s to 87 +/- 25 billion tonnes per year since then. The total rate of ice loss slowed to 222 +/- 30 billion tonnes per year between 2013 and 2017, on average, as atmospheric circulation favoured cooler conditions(15) and ocean temperatures fell at the terminus of Jakobshavn Isbr AE(16). Cumulative ice losses from Greenland as a whole have been close to the rates predicted by the Intergovernmental Panel on Climate Change for their high-end climate warming scenario(17), which forecast an additional 70 to 130 millimetres of global sea-level rise by 2100 compared with their central estimate.