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Grant: Discovery Grants Program - Individual

Wilfrid Laurier University

$75,000.00

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

FY 2022-23

Summary
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.
Program
Discovery Grants Program - Individual
Location
Ontario, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
RGPIN-2020-07229
Name nom
Quinton, William
Department département
Geography and Environmental Studies - Geography and Environmental Studies
Organization id
35
Institution établissement
Wilfrid Laurier University
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2022
Competition year année de concours
2020
Award amount
75000
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
DISCOVERY RESEARCH
Group fr
RECHERCHE AXÉE SUR LA DÉCOUVERTE
Committee code
1506
Committee name en
Geosciences
Committee name fr
Géosciences
Area of application code
400
Area of application group en
Environment
Area of application group fr
Environnement
Area of application en
Environment
Area of application fr
Environnement
Research subject code
4500
Research subject group en
Hydrology
Research subject group fr
Hydrologie
Research subject en
Hydrology
Research subject fr
Hydrologie
Installment
inst:3
Partie
1
Nb partie
5
Application title
Understanding the impacts of permafrost thaw on surface water flux and storage
Application summary
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.