Collaborative Research: Building Geologically Informed Bed Classes to Improve Projections of Ice Sheet Change

合作研究：建立地质信息床类以改进冰盖变化的预测

• 批准号: 2001714
• 负责人: Atsuhiro Muto
• 金额: $ 17.42万
• 依托单位: Temple University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2020
• 资助国家: 美国
• 起止时间: 2020-08-15 至 2024-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2001714&HistoricalAwards=false
• 关键词: Collaborative; Research; Building; Geologically; Informed

Predictions of future changes of the Antarctic ice sheet are essential for understanding changes in the global sea level expected for the coming centuries. These predictions rely on models of ice-sheet flow that in turn rely on knowledge of the physical conditions of the Antarctic continent beneath the ice. Exploration of Antarctica by land, sea, and air has advanced our understanding of the geological material under the Antarctic ice sheet, but this information has not yet been fully integrated into ice-sheet models. This project will take advantage of existing data from decades of US and international investment in geophysical surveys to create a new understanding of the geology underlying the Amundsen Sea and the adjacent areas of the West Antarctic Ice Sheet—a portion of Antarctica that is considered particularly vulnerable to collapse. A series of new datasets called “Bed Classes” will be developed that will translate the geological properties of the Antarctic continent in ways that can be incorporated into ice-sheet models. This project will develop a new regional geologic/tectonic framework for the Amundsen Sea Embayment and its ice catchments using extensive marine and airborne geophysical data together with ground-based onshore geophysical and geological constraints to delineate sedimentary basins, bedrock ridges, faults, and volcanic structures. Using this new geologic interpretation of the region, several key issues regarding the geologic influence on ice-sheet stability will be addressed: whether the regional heat flow is dominated by localization along the faults or lithology; the role of geology on the sources, sinks, and flow-paths of subglacial water; the distribution of sediments that determine bed-character variability; and the extent of geologic control on the current Thwaites Glacier grounding line. The impact of improved geological knowledge on ice-sheet models will be tested with the development of a set of “Bed Class” grids to capture these new insights for use in the models. Bed Classes will be tested within the Parallel Ice Sheet Model framework with initial experiments to identify the sensitivity of model simulations to geological parameterizations. Through a series of workshops with ice-sheet modelers, the Bed Classes will be refined and made accessible to the broader modelling community. This work aims to ensure that the Bed-Class concept can be applied more broadly to ice-sheet models working in different geographic areas and on different timescales.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

预测南极冰盖的未来变化对于了解未来几个世纪全球海平面的变化至关重要。 这些预测依赖于冰盖流动模型，而冰盖流动模型又依赖于对冰下南极大陆物理条件的了解。 通过陆地、海洋和空中对南极洲的探索，增进了我们对南极冰盖下地质物质的了解，但这些信息尚未完全融入冰盖模型。 该项目将利用美国和国际几十年来在地球物理调查方面的投资所获得的现有数据，对阿蒙森海和南极西部冰盖的邻近地区的地质情况有一个新的认识，南极洲的一部分被认为特别容易崩溃。 将开发一系列新的数据集，称为“床类”，将以可纳入冰盖模型的方式转换南极大陆的地质特性。 该项目将利用广泛的海洋和航空地球物理数据以及陆基陆上地球物理和地质制约因素，为阿蒙森海湾及其冰集区制定新的区域地质/构造框架，以描绘沉积盆地、基岩脊、断层和火山结构。利用这一新的地质解释的地区，几个关键问题的地质影响冰盖的稳定性将得到解决：是否区域热流是由局部控制沿着断层或岩性;地质作用的源，汇，和流动路径的冰下水;分布的沉积物，决定床的性质变化;以及目前思韦茨冰川接地线的地质控制程度。改进的地质知识对冰盖模型的影响将通过开发一套“床类”网格来测试，以捕捉这些新的见解用于模型。 将在平行冰盖模型框架内测试河床类别，并进行初步实验，以确定模型模拟对地质参数化的敏感性。 通过一系列与冰盖建模者的研讨会，将完善床类，并使更广泛的建模社区。 这项工作旨在确保床级概念可以更广泛地应用于在不同地理区域和不同时间尺度上工作的冰盖模型。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。