5 dossier(s) trouvé(s) portant l’étiquette "permafrost degradation" (les projets pluriannuels sont regroupés): Vous ne trouvez pas les résultats souhaités? Essayez la recherche avancée..
chercheur principal:Lantz, Trevor C. Année(s) de permis:2016201520142013
2012
Résumé:
This project has three main objectives:
Objective 1: To use satellite imagery (Landsat, QuickBird, InSAR, etc.) to document the rate and extent of landscape change (slumps, subsidence, vegetation change, etc.) in the northern Mackenzie Basin.
To quantify landscape disturbances and vegetation regeneration patterns since 1985 Landsat satellite images will be obtained, that will provide refle...
chercheur principal:Kanigan, Julian Année(s) de permis:
2012
2011 Résumé:
In discontinuous permafrost of the southern NWT, cleared transportation corridors, such as seismic lines, have recently been associated with permafrost loss, increased soil moisture and vegetation changes. Permafrost loss can lead to ground subsidence, infrastructure instability and the release of stored carbon into the atmosphere. The research team will test whether seismic lines can be construc...
chercheur principal:Kershaw, G. Peter Année(s) de permis:201820172016201520142012
2010
2009200820072006200520042003 Résumé:
Permafrost landforms are shrinking in response to climate warming. The researchers want to measure the amount of change each year and to measure the temperature of the permafrost year-round. In addition they want to measure the rate of plant recovery on disturbed areas resulting from the CANOL Project (1942-45).
Access during the summer is via the Yukon along the Canol Road through Macmillan ...
chercheur principal:Prowse, Terry D Année(s) de permis:200820072006
2005
Résumé:
The researchers want to develop a model for small Arctic lakes that will help them see how sensitive or vulnerable Arctic lake ecosystems are to various forms of disturbance, such as future climate change or water withdrawal. In order to develop their m...
chercheur principal:Lacelle, Denis Année(s) de permis:
2000
Résumé:
This is a study of retrogressive thaw sumps produced by the exposure and melting of massive ice in continuous permafrost (Richardson Range, NWT). These sumps are recently occurring and presumably a result of global climate change. This research will recognize retrogressive thaw slumps that have massive ice, identify the type of massive ice (glacier buried or segregated) and measure the rate of ...