NSF-NERC: Melting at Thwaites Grounding Zone and its Control on Sea Level (THWAITES-MELT)

NSF-NERC：思韦茨接地区的融化及其对海平面的控制（THWAITES-MELT）

• 批准号: 1739003
• 负责人: David Holland
• 金额: $ 216.5万
• 依托单位: New York University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2018
• 资助国家: 美国
• 起止时间: 2018-04-01 至 2024-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1739003&HistoricalAwards=false
• 关键词: NSF; NERC; Melting; Thwaites; Grounding

This project contributes to the joint initiative launched by the U.S. National Science Foundation (NSF) and the U.K. Natural Environment Research Council (NERC) to substantially improve decadal and longer-term projections of ice loss and sea-level rise originating from Thwaites Glacier in West Antarctica. The fate of the West Antarctic Ice Sheet (WAIS) is one of the largest uncertainties in projections of sea-level change. Thwaites Glacier (TG) is a primary contributor to sea-level rise and its flow is accelerating. This faster flow is a response to reduced buttressing from its thinning, floating ice shelf, and is ultimately caused by ocean-driven melting. The degree to which costly and geopolitically-challenging sea-level rise will occur therefore hangs to a large extent on ice-ocean interactions beneath such Antarctic ice shelves. However, the Thwaites system is not sufficiently well understood, exposing a significant gap in our understanding of WAIS retreat, its ocean-driven forcing, and the consequences for sea level. The chief regulators of TG's retreat are ice and ocean processes in its grounding zone, the location where the ice flowing from inland goes afloat. Ice and ocean processes at this precise locale are central to our understanding of sea-level rise, yet key variables have not been constrained by observation. Model projections of TG's future display extreme sensitivity to melting in the grounding zone and how that melting is applied. Equally-credible melt rates and grounding-zone glaciological treatments yield divergent trajectories for the future of West Antarctica, ranging from little change to large-scale ice sheet collapse with a half a meter or more of sea-level rise. The enormous uncertainty in outcome stems from the lack of observations in this critical grounding zone region. The enhanced understanding of melting of TG's ice shelf that will come from this project's focused observational program will be built into state-of-the-art coupled ice-sheet and ocean models. These physics-rich, high-resolution models will allow the potential sea-level contribution of TG to be bounded to an unprecedented degree.This project will enable global and regional climate modelers to make a substantial improvement to projections of future ocean conditions over the continental shelf by providing physics-based projections of TG's sea-level contribution. The team proposes a suite of integrated activities: (1) multi-year oceanographic time series from beneath TG's ice shelf to quantify melting processes that need inclusion in ocean models, with a strong focus on the grounding zone, (2) analogous measurements on the glacier to validate processes governing grounding-line retreat, (3) coupling of these in situ measurements with novel, high-resolution space-borne observations, (4) building this new understanding into state-of-the-art ocean (MIT General Circulation Model and Imperial College Ocean Model) and ice sheet (WAVI) models to correctly simulate the TG system, (5) coupling the models and running with realistic present-day ocean forcing to project the state of TG basin over the next hundred years. The international team will use a range of techniques, from the well-established, such as using a hot-water drill to instrument the ice column and water column in the grounding zone, through to the cutting-edge, such as deploying a borehole deployable remotely operated vehicle to survey the grounding zone, and using phase-coherent radar to monitor ice strain and basal melt rates. The outcome of the project will be a more complete understanding of the TG system in the critical zone extending from a few kilometers inland of the grounding line, through the grounding zone, and out under the ice shelf.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.

该项目为美国国家科学基金会 (NSF) 和英国自然环境研究委员会 (NERC) 发起的联合倡议做出了贡献，该倡议旨在大幅改进对源自西部思韦茨冰川的冰损失和海平面上升的十年和长期预测南极洲。南极西部冰盖（WAIS）的命运是海平面变化预测中最大的不确定因素之一。思韦茨冰川 (TG) 是海平面上升的主要原因，而且其流量正在加速。这种更快的流动是对其变薄的浮动冰架支撑减少的反应，最终是由海洋驱动的融化造成的。因此，代价高昂且具有地缘政治挑战性的海平面上升的程度在很大程度上取决于南极冰架下冰海的相互作用。然而，人们对思韦茨系统的了解还不够充分，这暴露了我们对 WAIS 撤退、其海洋驱动力以及对海平面影响的理解存在重大差距。 TG 撤退的主要调节者是其接地区的冰和海洋过程，即从内陆流出的冰漂浮的位置。这一精确地点的冰和海洋过程是我们了解海平面上升的核心，但关键变量并未受到观测的限制。 TG 未来的模型预测显示出对接地区域熔化以及熔化的应用方式极其敏感。同样可信的融化速度和接地区冰川处理为西南极洲的未来带来了不同的轨迹，从微小变化到大规模冰盖崩塌，海平面上升半米或更多。结果的巨大不确定性源于对这个关键接地区域缺乏观测。 该项目的重点观测计划将加深对 TG 冰架融化的理解，并将其纳入最先进的冰盖和海洋耦合模型中。这些物理丰富的高分辨率模型将使 TG 对海平面的潜在贡献限制在前所未有的程度。该项目将使全球和区域气候建模者能够大幅改进对大陆未来海洋状况的预测通过提供 TG 对海平面贡献的基于物理的预测。该团队提出了一系列综合活动：(1) TG 冰架下方的多年海洋学时间序列，以量化需要纳入海洋模型的融化过程，重点关注接地区，(2) 对冰川来验证控制接地线撤退的过程，（3）将这些现场测量与新颖的高分辨率星载观测相结合，（4）将这种新的理解融入最先进的海洋（麻省理工学院大气环流）模型和帝国理工学院海洋模型）和冰盖（WAVI）模型，以正确模拟 TG 系统，（5）耦合模型并与现实的当前海洋强迫一起运行，以预测未来一百年 TG 盆地的状态。国际团队将使用一系列技术，从成熟的技术（例如使用热水钻来测量接地区域的冰柱和水柱）到尖端技术（例如部署可部署的钻孔）远程操作车辆调查接地区域，并使用相位相干雷达监测冰应变和基底融化速率。该项目的成果将是对关键区域内 TG 系统的更全面的了解，该系统从接地线内陆几公里处延伸，穿过接地区域，一直到冰架下。该奖项反映了 NSF 的法定使命，并具有通过使用基金会的智力优点和更广泛的影响审查标准进行评估，被认为值得支持。

项目成果

The Southern Ocean and its interaction with the Antarctic Ice Sheet

• DOI: 10.1126/science.aaz5491
• 发表时间: 2020-03-20
• 期刊: SCIENCE
• 影响因子: 56.9
• 作者: Holland, David M.;Nicholls, Keith W.;Basinski, Aurora
• 通讯作者: Basinski, Aurora

Rapid glacier retreat rates observed in West Antarctica

• DOI: 10.1038/s41561-021-00877-z
• 发表时间: 2022-01
• 期刊: Nature Geoscience
• 影响因子: 18.3
• 作者: P. Milillo;E. Rignot;P. Rizzoli;B. Scheuchl;J. Mouginot;J. Bueso-Bello;P. Prats-Iraola;L. Dini