Collaborative Research: Watershed-scale Geomorphic Response to Climate Change in the Aklavik Range, NWT (Canada)

合作研究：西北地区阿克拉维克山脉流域规模地貌对气候变化的响应（加拿大）

• 批准号: 2116571
• 负责人: Jill Marshall
• 金额: $ 25.65万
• 依托单位: University of Arkansas
• 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=2116571&HistoricalAwards=false
• 关键词: Collaborative; Research; Watershed; scale; Geomorphic

Arctic landscape response to rapid anthropogenic climate change has the potential to fundamentally alter both human and natural systems. This includes increased hazards to Arctic communities from permafrost thaw and associated slope instability and the destruction of river and coastal habitats from higher sediment and nutrient yields in Arctic rivers. While it is clear that Arctic landscapes are sensitive to climate change, a gap exists in our knowledge about how changes in temperature will affect the ways in which sediment is transported across a watershed. In order to address this knowledge gap, the investigators will be conducting a field- and remote sensing-based study of Arctic watersheds in the Aklavik Range of the Northwest Territories (NWT), Canada, where numerous First Nations communities are situated. The research team will test the specific hypothesis that climate change in the Arctic is leading to faster production of sediment within mountainous regions and causing subsequent increases in sediment delivery to hillslopes and rivers. This is an interdisciplinary project that involves three Early Career tenure-track faculty, multiple local collaborators, as well as the Ehdiitat Gwich’in. The investigators will study two small bedrock watersheds (where sediment is produced) and their associated fan deposits (where sediment is stored) along a north-south climate gradient. Prior geomorphic work on these fan deposits was conducted in the 1960s to 1980s, making them an ideal location to quantitively assess change over time. The major objectives are to: (1) conduct fieldwork to understand how sediment is produced and the processes by which it moves across this landscape; (2) perform laboratory analyses on samples collected in the field to quantify rates of sediment production and transport over decadal to millennial scales; (3) use remote sensing techniques to extend local findings to the broader region over the last several decades; and (4) to use these data to calibrate sediment production and transport models so that we can predict future Arctic landscape response to anthropogenic warming scenarios. Many of the dating and remote sensing techniques have greatly advanced in the last several decades, but have not been applied to an integrated Arctic study spanning an entire watershed. Once proven in this study, this combination of methods could be used in other landscapes (both in the Arctic and at low latitudes) to better quantify how changes in rates of one geomorphic process (e.g., breakdown of bedrock) affects changes in rates of another (e.g., rates of sediment delivery to a river). In addition, the data collected during this project will calibrate state-of-the-science models allowing scientists to better inform local communities of potential hazards due to future warming.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.

北极景观对快速的人为气候变化的反应有可能从根本上改变人类和自然系统。这包括永久冻土融化和相关斜坡不稳定对北极社区的危害增加，以及北极河流沉积物和养分产量增加对河流和沿海栖息地的破坏。虽然北极地貌显然对气候变化很敏感，但我们对于温度变化将如何影响沉积物跨流域运输的方式的了解存在差距。为了弥补这一知识差距，研究人员将对加拿大西北地区（NWT）阿克拉维克山脉的北极流域进行实地和遥感研究，那里有许多原住民社区。研究小组将测试一个具体的假设，即北极的气候变化导致山区沉积物的产生速度加快，并导致随后向山坡和河流的沉积物输送量增加。这是一个跨学科项目，涉及三名早期职业终身教授、多名当地合作者以及 Ehdiitat Gwich’in。研究人员将沿着南北气候梯度研究两个小型基岩流域（产生沉积物的地方）及其相关扇沉积物（沉积物储存的地方）。先前对这些扇沉积物的地貌研究是在 20 世纪 60 年代至 1980 年代进行的，使它们成为定量评估随时间变化的理想地点。主要目标是：（1）进行实地考察，了解沉积物是如何产生的以及沉积物在该景观中移动的过程； (2) 对现场收集的样品进行实验室分析，以量化十年至千年尺度的沉积物产生和运输速率； （3）利用遥感技术将过去几十年的本地发现扩展到更广泛的区域； （4）利用这些数据来校准沉积物产生和运输模型，以便我们可以预测未来北极景观对人为变暖情景的反应。许多测年和遥感技术在过去几十年中取得了巨大进步，但尚未应用于跨越整个流域的综合北极研究。一旦在本研究中得到证实，这种方法组合可以用于其他景观（北极和低纬度地区），以更好地量化一种地貌过程的速率变化（例如，基岩的破裂）如何影响另一种地貌过程的速率变化（例如，沉积物输送到河流的速率）。此外，该项目期间收集的数据将校准最先进的科学模型，使科学家能够更好地向当地社区通报未来变暖带来的潜在危害。该奖项反映了 NSF 的法定使命，并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，被认为值得支持。