9 record(s) found in the location "Inuvialuit Settlement Region" (multi-year projects are grouped): Not seeing the results you want? Tryadvanced search.
Principal Investigator:Langer, Moritz Licensed Year(s):20242023
2022
Summary:
This licence has been issued for the scientific research application No.5218.
The aim of the citizen science project UndercoverEisAgenten is to study permafrost changes in the Arctic to raise awareness of these environmental changes and strengthen the data basis for science. Students from Moose Kerr School in Aklavik will design their own permafrost change related research questions and work wi...
Principal Investigator:Pisaric, Michael FJ Licensed Year(s):
2018
201720162015201420132012201120102009 Summary:
This research will continue the long term objective of documenting and understanding the impacts of recent climate change on northern terrestrial and aquatic ecosystems. The short term objectives of my research for 2018 are: 1) to investigate the impacts of permafrost degradation and subsequent thaw slumping on freshwater ecosystems; 2) to examine the limnological implications of drained lakes on ...
Principal Investigator:Wrona, Frederick J Licensed Year(s):
2010
Summary:
The overall objective of the Lake 5A mesocosm study is to better understand the impact of permafrost thaw shoreline slumping (an analogue for a warming climate) on the bottom components of the aquatic food-web in small Arctic tundra lakes in order to better predict the effects of a warming climate on food-web structure, function and productivity.
To assess the direct and indirect effects of per...
Principal Investigator:Eglinton, Timothy I Licensed Year(s):2011
2009
2007 Summary:
This licence is being issued for the scientific research application no. 955.
The objective of this research is to collect sediment cores from the Mackenzie River Delta in order to study how the river has behaved in the past, and see if the researchers can detect recent changes due to thawing permafrost. More specifically, the goal is to determine whether the researchers can reconstruct past c...
Principal Investigator:Zhou, Fuqun Licensed Year(s):
2004
Summary:
Structural infrastructure in northern communities is dependent on the permafrost layer for stability. The thawing and disappearance of the permafrost layer has accelerated in recent decades, damaging buildings and other infrastructure, and causing public...
Principal Investigator:Kokelj, Steven V Licensed Year(s):
2004
200320022001200020001999 Summary:
This research will investigate: A) the physical and chemical characteristics of permafrost in the Mackenzie Delta region to identify areas of ice-rich permafrost or thaw sensitive terrain. Second; B) the effect of permafrost degradation on water quality...
Principal Investigator:Lacelle, Denis Licensed Year(s):
2000
Summary:
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 ...
Principal Investigator:Dyke, Larry Licensed Year(s):
1999
Summary:
The goal of this research is to examine landslides on the slopes along the Mackenzie Valley, so that researchers can better understand their causes and the effect climate change will have on the landscape. Field work will be carried out between Wrigley and Inuvik along the Mackenzie River, with some access along the Dempster Highway. Tree increment cores will be used to determine tree age and dat...
Principal Investigator:Marsh, Philip Licensed Year(s):2005200420032002200120001999
1998
1997199619951994199319921990 Summary:
The Trail Valley Creek site will be accessed by Twin Otter, helicopter and snowmobile, while the Havikpak Creek site will be accessed by foot and snowmobile. We plan to have a small field crew at each site to measure the amount of snow on the ground in the middle of April, and to again return to measure snowmelt and the streamflow in mid to late May. Actual timing of the spring melt trip will depe...