Collaborative Research: RUI: Zero-order to first-order: Hydrologic drivers of surface-subsurface storage dynamics in thawing permafrost landscapes

合作研究：RUI：零阶到一阶：解冻永久冻土景观中地表-地下储存动态的水文驱动因素

• 批准号: 2102338
• 负责人: Sarah Evans
• 金额: $ 27.64万
• 依托单位: Appalachian State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-01-01 至 2024-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2102338&HistoricalAwards=false
• 关键词: Collaborative; Research; RUI; Zero; order

This award is funded in whole or in part under the American Rescue Plan Act of 2021 (Public Law 117-2).Liquid water in the Arctic flows at or near the surface above frozen ground known as permafrost. As permafrost thaws, water flows along new paths, mobilizing previously frozen carbon. If permafrost soils thaw and dry, carbon is released three times more readily than if permafrost soils thaw and remain saturated, implying that water patterns partially control carbon release. Yet, the patterns or drivers of permafrost saturation and how they vary with climate remain poorly understood. This research will use field measurements, remote sensing, and modeling to investigate the dynamics, drivers, and sensitivity of hillslope saturation patterns on the North Slope of Alaska. Results will help to create an ‘H2cOld: Water in the Arctic’ traveling outreach activity for rural K-12 students and communities throughout the southern Appalachians and Idaho. The project will also train four undergraduate students and a graduate student for science careers.The hydrology of Arctic hillslopes underlain by continuous permafrost is largely controlled by water tracks, seasonally saturated zero-order features draining a third of the upland Arctic. Water tracks can rapidly degrade into thermoerosional gullies, the most common Arctic thermoerosional feature, altering seasonal saturation and fluxes of water, nutrients, and sediments. Although water tracks and thermoerosional gullies are the largest and most variable aquatic sources of permafrost carbon release, their saturation dynamics and how these dynamics change as permafrost thaws remain poorly understood. These two features are hypothesized to represent endmembers of the surface network extent of Arctic hillslope hydrology with distinct saturation patterns that are diverging as the climate warms. This research project will test this hypothesis in paired water tracks and thermoerosional gullies in northern Alaska via remote sensing and field campaigns to calibrate a water-energy transport model with variable saturation and freeze-thaw capabilities. Collectively, this work will improve predictions of saturation-controlled carbon release from the Arctic.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.

该奖项全部或部分由2021年美国救援计划法案（公法117-2）资助。北极的液态水在被称为永久冻土的冻土表面或附近流动。随着永冻层的融化，水沿着沿着新的路径流动，调动了以前冻结的碳。如果永久冻土融化和干燥，碳的释放比永久冻土融化和保持饱和的情况容易三倍，这意味着水的模式部分控制碳的释放。然而，永冻层饱和度的模式或驱动因素以及它们如何随气候变化仍然知之甚少。本研究将使用实地测量，遥感和建模，以调查阿拉斯加北坡的山坡饱和模式的动态，驱动程序和敏感性。研究结果将有助于为整个阿巴拉契亚山脉南部和爱达荷州的农村K-12学生和社区创建一个“H2 cold：北极地区的水”旅游推广活动。该项目还将培养四名本科生和一名研究生从事科学事业。连续多年冻土层下的北极山坡的水文主要受水迹控制，季节性饱和的零阶特征排水了三分之一的高地北极。水迹可以迅速退化成热侵蚀沟，这是北极最常见的热侵蚀特征，改变了水、营养物和沉积物的季节性饱和度和通量。尽管水迹和热侵蚀沟是冻土碳释放的最大和最可变的水生来源，但它们的饱和动态以及这些动态如何随着冻土融化而变化仍然知之甚少。这两个功能被假设为代表北极山坡水文的表面网络范围的端元，具有不同的饱和度模式，随着气候变暖而发散。本研究项目将通过遥感和实地活动在阿拉斯加北方成对的水迹和热侵蚀沟中测试这一假设，以校准具有可变饱和度和冻融能力的水能传输模型。总的来说，这项工作将改善对北极饱和控制碳释放的预测。该奖项反映了NSF的法定使命，并被认为值得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来支持。