Understanding the impacts of permafrost thaw on surface water flux and storage

了解永久冻土融化对地表水通量和储存的影响

• 批准号: RGPIN-2020-07229
• 负责人: Quinton, William
• 金额: $ 5.46万
• 依托单位: Wilfrid Laurier University
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2022
• 资助国家: 加拿大
• 起止时间: 2022-01-01 至 2023-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=754917
• 关键词: Understanding; impacts; permafrost; thaw; surface

The subarctic region of north-western Canada is one of the most rapidly warming on Earth. The permafrost of this region is thawing at unprecedented rates causing damage to roads, air strips, ferry crossings, pipelines, and buildings, while transforming land covers and disrupting the water cycle. For example, in the peatland-dominated region of discontinuous permafrost in the southern Northwest Territories, permafrost thaw is transforming large areas of forest into wetland, enabling wetlands to drain, and the flow of streams and rivers to rise. Considering that land cover characteristics strongly affect water flow and storage processes, and that permafrost is the foundation of much of the land cover in this region, the thaw and disappearance of permafrost has profound implications for the region's water cycle. However, regulatory authorities, resource management boards, and communities are ill-equipped to respond effectively to this new and growing challenge, because there is little or no permafrost thaw monitoring, adaptation or predictive capacity in the region, and therefore no appropriate basis for decision support. As a result, there is an urgent need to investigate thaw-induced changes to land and water, develop and mobilise knowledge on these changes, develop predictive modelling tools, and provide interactive training to decision makers and other stakeholders. In direct response, this research programme will co-develop and co-implement (with Indigenous communities and other northern end-users) new knowledge on permafrost distribution, thaw, thaw-induced land cover change, and resulting hydrological impacts; in addition to high-quality public data sets, and customised knowledge-based predictive tools and innovative adaptation and risk management strategies. Each of these will be customised to meet the specialised decision support needs of the study region so that environmental and resource management strategies can be confidently applied. It is expected that the products of this research programme will also have wide applicability throughout the circumpolar subarctic.

加拿大西北部的亚北极地区是地球上变暖最快的地区之一。该地区的永久冻土正在以前所未有的速度融化，对道路、机场跑道、渡口、管道和建筑物造成破坏，同时改变了土地覆盖，破坏了水循环。例如，在西北地区南部以泥炭地为主的不连续永久冻土地区，永久冻土融化正在将大片森林转变为湿地，使湿地排水，溪流和河流的流量上升。考虑到土地覆盖特征强烈影响水流和储存过程，而永久冻土是该地区大部分土地覆盖的基础，永久冻土的融化和消失对该地区的水循环具有深远的影响。然而，监管当局、资源管理委员会和社区缺乏有效应对这一日益严峻的新挑战的能力，因为该地区几乎没有或根本没有永久冻土融化监测、适应或预测能力，因此没有适当的决策支持基础。因此，迫切需要调查融化引起的土地和水的变化，开发和动员有关这些变化的知识，开发预测建模工具，并为决策者和其他利益相关者提供互动培训。作为直接回应，这一研究方案将（与土著社区和其他北方最终用户）共同开发和共同实施关于永久冻土分布、解冻、融化引起的土地覆盖变化以及由此产生的水文影响的新知识；除了高质量的公共数据集、定制的基于知识的预测工具以及创新的适应和风险管理战略之外。每一个都将被定制，以满足研究区域的专门决策支持需求，以便环境和资源管理战略可以自信地应用。预期这一研究方案的产品也将广泛适用于整个环极亚北极地区。