Rapid landscape evolution at the permafrost-glacier interface

永久冻土-冰川界面的快速景观演化

• 批准号: RGPIN-2017-04135
• 负责人: Moorman, Brian
• 金额: $ 1.6万
• 依托单位: University of Calgary
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2017
• 资助国家: 加拿大
• 起止时间: 2017-01-01 至 2018-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=633945
• 关键词: Rapid; landscape; evolution; permafrost; glacier

Permafrost underlies a large portion of Canada's landscape and in some locations, massive amounts of ice have been preserved for thousands of years. However, much of the permafrost in Canada is thawing, resulting in the melt-out of ground ice and dramatic alterations to the landscape and overall terrestrial environment. This is resulting in a step change (a tipping point) in the rate and character of landscape evolution - something seldom taken into account in the climate change impact predictions due to its complexity. It is most obvious in the Arctic where glaciers are rapidly retreating, producing large volumes of melt water impacting the frozen ground and massive buried ice surrounding the glaciers. The result is an environment which is changing in ways we have not witnessed before. Four interrelated projects designed to better understand the changes occurring are:

多年冻土是加拿大景观中很大一部分的基础，在某些地方，已经保存了数千年的冰。但是，加拿大多年冻土的大部分是融化，导致地面冰的融化以及对景观和整体陆地环境的巨大改变。这导致了景观演化的速率和特征的阶跃变化（临界点） - 由于其复杂性而导致的气候变化影响预测很少考虑到这一点。在北极最明显的地方，冰川正在迅速退缩，产生大量的熔融水，影响冰冻的冰冻地面和冰川周围的大量埋水。结果是一个我们以前从未见过的方式发生了变化。旨在更好地了解发生的变化的四个相互关联的项目是：