Collaborative Research: Arctic Observing Network For Observing Transformation of the Greenland Ice Sheet Firn Layer

合作研究：观测格陵兰冰盖冰层变化的北极观测网络

• 批准号: 2113391
• 负责人: Joel Harper
• 金额: $ 119.91万
• 依托单位: University of Montana
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-11-01 至 2026-10-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2113391&HistoricalAwards=false
• 关键词: Collaborative; Research; Arctic; Observing; Network

This award is funded in whole or in part under the American Rescue Plan Act of 2021 (Public Law 117-2)As the Arctic warms two-to-three times faster than the global average, the duration and intensity of melting is generally increasing on the surface of the Greenland ice sheet. About 90% of ice sheet is covered by compacted snow that is slowly transitioning into glacier ice. This aged and dense snow is called ‘firn’ and forms a porous layer that is many tens of meters thick. Much of the meltwater generated from the surface of the firn layer infiltrates into the underlying open pore space of the firn and refreezes. However, as this porous layer absorbs more melt it becomes warmer, denser, and filled with ice layers, which reduces its ability to absorb additional melt. Therefore, the thermal and structural transformation that Greenland's firn layer is presently undergoing has important implications for the ice sheet's capacity to retain future melt. This project is directly observing firn evolution with a network of instruments installed within the firn layer and with ice cores sampling the firn. The observational data collected by this project provides on-the-ground documentation of firn conditions needed to develop and test models and remote sensing tools for large-scale investigations of changes to the Greenland ice sheet. Future transformation of the firn layer will govern how much surface melt is retained locally on the ice sheet and how much runs off, thereby impacting hydrologic conditions of the ice sheet and surrounding regions, ocean salinity, and sea level rise.The researchers will install and maintain an observation network along a transect of the Greenland ice sheet to directly measure the state and transformation of firn properties. Repeat sampling of firn cores and instrumentation extending from the surface to 25 meters depth will yield the observational datasets needed by multiple scientific communities: firn temperature, density and ice content, densification rate, surface boundary processes (radiation, snow accumulation, temperature), and ice velocity. The network will yield 4-5 full-year records in this five-year Arctic Observing Network project. The project will provide comprehensive datasets for process-level investigations, testing climate model simulations of firn processes, and interpreting satellite-based measurement of surface elevation change. The project will engage and support a relatively large number of undergraduate and graduate students at R2 institutions with field research experiences and real-world classroom learning. Outreach activities will target three groups poorly represented in cryospheric science: 1) local and Indigenous residents of Greenland; 2) American Indian undergraduate students; and 3) economically disadvantaged school children.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.

该奖项的全部或部分资金来自2021年美国救援计划法案（公法117 - 2）由于北极变暖的速度比全球平均速度快两到三倍，格陵兰冰盖表面融化的持续时间和强度普遍增加。大约90%的冰盖被压实的雪覆盖，这些雪正在慢慢转变为冰川冰。这种古老而致密的雪被称为“积雪”，形成了几十米厚的多孔层。许多融水产生的表面的积雪层渗透到下面的开放的孔隙空间的积雪和refreezes。然而，随着多孔层吸收更多的融化，它变得更温暖，更密集，并充满了冰层，这降低了它吸收额外融化的能力。因此，格陵兰的积雪层目前正在经历的热量和结构转变对冰盖保持未来融化的能力具有重要意义。该项目利用在积雪层内安装的仪器网络和对积雪取样的冰芯直接观测积雪的演变。该项目收集的观测数据提供了实地记录积雪状况的资料，这些资料是为大规模调查格陵兰冰盖变化而开发和测试模型和遥感工具所必需的。未来的雪层变化将决定有多少表层融化物保留在冰盖上，有多少融化物流失，从而影响冰盖和周围地区的水文条件、海洋盐度和海平面上升。研究人员将沿着格陵兰冰盖的一个横断面沿着安装并维护一个观测网络，以直接测量雪属性的状态和变化。对从地表延伸至25米深处的积雪芯和仪器进行重复采样，将产生多个科学界所需的观测数据集：积雪温度、密度和冰含量、致密化率、地表边界过程（辐射、积雪、温度）和冰速度。在这个为期五年的北极观测网络项目中，该网络将产生4 - 5个全年记录。该项目将为过程级调查提供全面的数据集，测试气候模型对积雪过程的模拟，并解释基于卫星的地表高程变化测量结果。该项目将吸引和支持R2机构中相对大量的本科生和研究生，他们具有实地研究经验和现实世界的课堂学习。外展活动将针对在冰冻圈科学中代表性不足的三个群体：1）格陵兰岛的当地和土著居民; 2）美国印第安人本科生; 3）经济困难的学校儿童。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。