Title | Using remote sensing-based spatial modelling to assess the changes of permafrost in Wapusk National Park
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Author | Zhang, Y ; Li, J;
Wang, X; Chen, W ; Sladen, W; Dyke, L; Dredge, L; Poitevin, J;
McLennan, D; Stewart, H; Kowalchuk, S; Wu, W; Kershaw, G P; Brook, R K |
Source | Proceeding of GEO2010, the 63rd Canadian Geotechnical Conference and the 6th Canadian Permafrost Conference; 2010 p. 1291-1297 |
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Year | 2010 |
Alt Series | Earth Sciences Sector, Contribution Series 20100085 |
Meeting | GEO2010, the 63rd Canadian Geotechnical Conference and the 6th Canadian Permafrost Conference; Calgary; CA; September 12-15, 2010 |
Document | book |
Lang. | English |
Media | paper; digital |
Province | Manitoba |
NTS | 54F; 54K |
Area | Wapusk National Park |
Lat/Long WENS | -94.0000 -92.5000 59.0000 57.0000 |
Subjects | environmental geology; Nature and Environment; permafrost; freezing ground; ground ice; ground temperatures; climate; climate, arctic; remote sensing; Climate change |
Illustrations | satellite images; histograms; plots |
Program | Climate Change Geoscience |
Released | 2010 01 01 |
Abstract | Each Canadian national park is required to monitor and report on the state of the park. Permafrost is an integral part of the northern landscapes and ecosystems. Observations show that permafrost is
thawing in response to climate change. Northern national parks are large and expensive to access and monitor in the field. This study reports on the application of remote sensing-based spatial modelling to assess the changes of permafrost in Wapusk
National Park located in the northwest of the Hudson Bay Lowlands. Permafrost was mapped at an unprecedented high resolution of 30 m by 30 m using a process-based model. Spatial input datasets were developed based on remote sensing data and site
observations. The results show that the active-layer had a deepening trend throughout most of the park and that permafrost was degrading in areas in recent decades, especially in treed areas in southern regions. |
GEOSCAN ID | 285590 |
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