Investigating the potential contribution of the East Antarctic Ice Sheet to future sea level change.

调查东南极冰盖对未来海平面变化的潜在贡献。

• 批准号: NE/G012733/1
• 负责人: Anne Le Brocq
• 金额: $ 26.03万
• 依托单位: Durham University
• 依托单位国家: 英国
• 项目类别: Fellowship
• 财政年份: 2010
• 资助国家: 英国
• 起止时间: 2010 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=NE%2FG012733%2F1
• 关键词: Investigating; potential; contribution; East; Antarctic

There is currently major uncertainty about the potential contribution of the Antarctic Ice Sheet (AIS) to global sea level change in the immediate and long term future. Part of the AIS rests on land that is below sea level and, hence, has a very different flow regime to other parts which rest on land above sea level. It is, therefore, susceptible to changes in ocean circulation as well as atmospheric change. A small change in ocean temperatures can have a large impact on ice flow, whereas a large change is required in atmospheric temperatures (which are in general tens of degrees below freezing over the AIS). A hypothesis exists that suggests marine based ice sheets (those that rest on bed below sea level) which also have a bed which deepens inland, are inherently unstable due to their configuration. A small thinning/retreat in the grounding line (the location where the ice sheet changes from being grounded on its bed to floating) makes the ice thinner inland where the bed is deeper, the ice is no longer able to ground and hence flows faster due to increased basal resistance. This leads to a feedback mechanism that could, in the worst case, lead to the breakup of large parts of the ice sheet. The smaller West AIS (WAIS) has so far been the region of greatest concern, with most of the ice sheet resting on bed below sea level and a strong thinning signal observed in one of the drainage sectors (Amundsen Sea sector). The larger East AIS (EAIS) has previously been considered to be stable, as the majority of the ice sheet rests on land above sea level. However, there are some large basins known to be below sea level (Wilkes and Aurora subglacial basins), though there is currently sparse data coverage from these basins. The ice in these regions is also currently exhibiting a surface thinning signal near the coastal regions that cannot be explained by changes in the snowfall pattern and hence must have a dynamic origin. Part of the uncertainty over ice sheet stability and future sea level change comes from the inadequacy of numerical models in reproducing the processes which occur at the grounding line, and hence in representing change in its location. Recent model developments are improving the representation of grounding line processes and a major data collection mission will in the near future provide detailed information about the nature of the bedrock in the two EAIS marine basins. These two advances will allow a better understanding of the nature of EAIS stability to be derived though numerical ice sheet modelling. This research, therefore, proposes to use an advanced numerical ice sheet model to investigate the changing dynamics of the marine sectors of the EAIS, in order to investigate the future stability of the ice sheet and its potential contribution to future global sea level change in both the immediate future, and on a decadal and millennial scale. The work will be carried out at the University of Durham, in association with other researchers at the forefront of Antarctic research at the Universities of Edinburgh and Bristol, and the British Antarctic Survey. Understanding and quantifying ice sheet stability and future change in global sea level is highly relevant to current concerns about global environmental change and its impact on millions of people living in low lying regions. The research is therefore timely and relevant to current research priorities.

目前，南极冰盖（AIS）在近期和长期对全球海平面变化的潜在贡献存在很大的不确定性。AIS的一部分位于海平面以下的陆地上，因此与位于海平面以上的陆地上的其他部分具有非常不同的流态。因此，它容易受到海洋环流和大气变化的影响。海洋温度的微小变化可以对冰流产生很大的影响，而大气温度的变化则需要很大的变化（在AIS上通常低于冰点几十度）。有一种假说认为，基于海洋的冰盖（那些在海平面以下的床上休息的冰盖）也有一个深入内陆的床，由于它们的结构，它们本质上是不稳定的。接地线（冰盖从接地到漂浮的位置）中的小变薄/后退使冰在床较深的内陆变薄，冰不再能够接地，因此由于增加的基底阻力而流动得更快。这导致了一种反馈机制，在最坏的情况下，可能导致大部分冰盖的破裂。到目前为止，规模较小的西AIS（WAIS）是最令人担忧的区域，大部分冰盖位于海平面以下的河床上，在一个排水部门（阿蒙森海部门）观察到强烈的变薄信号。较大的东AIS（EAIS）以前被认为是稳定的，因为大部分冰盖位于海平面以上的陆地上。然而，也有一些已知的大盆地低于海平面（威尔克斯和奥罗拉冰下盆地），虽然目前有稀疏的数据覆盖这些盆地。这些地区的冰目前在沿海地区附近也显示出表面变薄的信号，这不能用降雪模式的变化来解释，因此必须有一个动态的起源。冰盖稳定性和未来海平面变化的不确定性部分来自于数值模型在再现接地线处发生的过程方面的不足，因此在表示其位置的变化方面。最近的模型开发正在改善接地线过程的代表性，在不久的将来，一项主要的数据收集使命将提供有关两个EAIS海洋盆地基岩性质的详细信息。这两个进步将允许更好地理解EAIS的稳定性的性质，通过数值冰盖建模。因此，本研究建议使用先进的数值冰盖模型来研究EAIS海洋部门的变化动态，以研究冰盖的未来稳定性及其对未来全球海平面变化的潜在贡献。这项工作将在达勒姆大学进行，与爱丁堡大学和布里斯托大学南极研究前沿的其他研究人员以及英国南极调查局合作。了解和量化冰盖稳定性和全球海平面的未来变化与当前对全球环境变化及其对生活在低洼地区的数百万人的影响的担忧高度相关。因此，这项研究是及时的，与当前的研究重点有关。