NSFGEO-NERC: Investigating the Direct Influence of Meltwater on Antarctic Ice Sheet Dynamics

NSFGEO-NERC：研究融水对南极冰盖动力学的直接影响

• 批准号: 2053169
• 负责人: Jonathan Kingslake
• 金额: $ 89.99万
• 依托单位: Columbia University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2023
• 资助国家: 美国
• 起止时间: 2023-08-15 至 2026-07-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2053169&HistoricalAwards=false
• 关键词: NSFGEO; NERC; Investigating; Direct; Influence

When ice sheets and glaciers lose ice faster than it accumulates from snowfall, they shrink and contribute to sea-level rise. This has consequences for coastal communities around the globe by, for example, increasing the frequency of damaging storm surges. Sea-level rise is already underway and a major challenge for the geoscience community is improving predictions of how this will evolve. The Antarctic Ice Sheet is the largest potential contributor to sea-level rise and its future is highly uncertain. It loses ice through two main mechanisms: the formation of icebergs and melting at the base of floating ice shelves on its periphery. Ice flows under gravity towards the ocean and the rate of ice flow controls how fast ice sheets and glaciers shrink. In Greenland and Antarctica, ice flow is focused into outlet glaciers and ice streams, which flow much faster than surrounding areas. Moreover, parts of the Greenland Ice Sheet speed up and slow down substantially on hourly to seasonal time scales, particularly where meltwater from the surface reaches the base of the ice. Meltwater reaching the base changes ice flow by altering basal water pressure and consequently the friction exerted on the ice by the rock and sediment beneath. This phenomenon has been observed frequently in Greenland but not in Antarctica. Recent satellite observations suggest this phenomenon also occurs on outlet glaciers in the Antarctic Peninsula. Meltwater reaching the base of the Antarctic Ice Sheet is likely to become more common as air temperature and surface melting are predicted to increase around Antarctica this century. This project aims to confirm the recent satellite observations, establish a baseline against which to compare future changes, and improve understanding of the direct influence of meltwater on Antarctic Ice Sheet dynamics. This is a project jointly funded by the National Science Foundation’s Directorate for Geosciences (NSF/GEO) and the National Environment Research Council (NERC) of the United Kingdom (UK) via the NSF/GEO-NERC Lead Agency Agreement. This Agreement allows a single joint US/UK proposal to be submitted and peer-reviewed by the Agency whose investigator has the largest proportion of the budget. Upon successful joint determination of an award recommendation, each Agency funds the proportion of the budget that supports scientists at institutions in their respective countries.This project will include a field campaign on Flask Glacier, an Antarctic Peninsula outlet glacier, and a continent-wide remote sensing survey. These activities will allow the team to test three hypotheses related to the Antarctic Ice Sheet’s dynamic response to surface meltwater: (1) short-term changes in ice velocity indicated by satellite data result from surface meltwater reaching the bed, (2) this is widespread in Antarctica today, and (3) this results in a measurable increase in mean annual ice discharge. The project is a collaboration between US- and UK-based researchers and will be supported logistically by the British Antarctic Survey. The project aims to provide insights into both the drivers and implications of short-term changes in ice flow velocity caused by surface melting. For example, showing conclusively that meltwater directly influences Antarctic ice dynamics would have significant implications for understanding the response of Antarctica to atmospheric warming, as it did in Greenland when the phenomenon was first detected there twenty years ago. This work will also potentially influence other fields, as surface meltwater reaching the bed of the Antarctic Ice Sheet may affect ice rheology, subglacial hydrology, submarine melting, calving, ocean circulation, and ocean biogeochemistry. The project aims to have broader impacts on science and society by supporting early-career scientists, UK-US collaboration, education and outreach, and adoption of open data science approaches within the glaciological community.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.

当冰盖和冰川失去冰的速度快于降雪积聚的速度时，它们就会收缩并导致海平面上升，这会对全球沿海社区产生影响，例如增加破坏性风暴潮的频率。南极冰盖是海平面上升的最大潜在贡献者，其未来高度不确定，它通过两种主要机制失去冰。的形成冰山及其外围漂浮冰架底部的融化，冰在重力作用下流向海洋，冰流的速度控制着格陵兰岛和南极洲冰盖和冰川收缩的速度。此外，格陵兰冰盖的部分地区在每小时和季节时间尺度上的流速都显着加快和减慢，尤其是在地表融水到达融水底部的地方。到达底部会改变基础水压，从而改变下方岩石和沉积物对冰的摩擦力，这种现象在格陵兰岛经常被观察到，但最近的卫星观测表明，这种现象也发生在出口冰川上。随着本世纪南极洲周围气温和地表融化的增加，融水到达南极冰盖底部的情况可能会变得更加普遍。该项目旨在证实最近的卫星观测结果。这是一个由美国国家科学基金会地球科学理事会 (NSF/GEO) 和国家环境研究委员会 (NSF/GEO) 共同资助的项目。英国 (UK) 的 NERC）通过 NSF/GEO-NERC 牵头机构协议，该协议允许美国/英国联合提案由其研究人员拥有最大预算比例的机构提交并进行同行评审。之上在成功联合确定一项奖励建议后，每个机构都会资助各自国家机构科学家的预算比例。该项目将包括对弗拉斯克冰川、南极半岛出口冰川和全大陆遥感的实地活动这些活动将使研究小组能够测试与南极冰盖对地表融水的动态响应有关的三个假设：（1）卫星数据显示的冰速度的短期变化是地表融水到达冰床的结果。很普遍(3) 这导致每年平均冰排放量显着增加。该项目是美国和英国研究人员之间的合作，并将得到英国南极调查局的后勤支持。该项目旨在提供见解。例如，确定地表融化引起的冰流速短期变化的驱动因素和影响，最终表明融水直接影响南极冰动态，对于理解南极洲对大气变暖的反应具有重要意义。二十年前在格陵兰岛首次发现这种现象时，这项工作也可能会影响其他领域，因为到达南极冰盖床的地表融水可能会影响冰流变学、冰下水文学、海底融化、崩解、海洋环流，该项目旨在通过支持早期职业科学家、英美合作、教育和推广以及在冰川学界采用开放数据科学方法，对科学和社会产生更广泛的影响。该奖项反映了通过使用基金会的智力价值和更广泛的影响审查标准进行评估，NSF 的法定使命被认为值得支持。