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Grant: Discovery Grants Program - Northern Research Supplement

University of Northern British Columbia

$15,000.00

Holocene glacier fluctuations in the Keele Peak region, Yukon, Canada

EF 2013-14

Résumé
A recent review of the evidence for Holocene glacier fluctuations in western Canada recommends that future efforts should focus on documenting glacier fluctuations in eastern Yukon and the ranges in the Northwest Territories since little work has been completed in this region to date. One promising region is centered around the Keele Peak region (N 63 deg 26', W 130 deg 19') in the Hess Mountains, Yukon. Based on an analysis of pollen records, substantial climate change affected the adjacent Mackenzie Mountains during the Holocene. Given the location of the study area at high latitude in the Northern Hemisphere, it is believed that orbital forcing caused glaciers to expand from minimal extents in the early Holocene to maximum downvalley positions during the Little Ice Age. I aim to test the role that orbital forcing played on glacier activity at high latitudes by completing work in the Keele Peak area and at sites in southern Patagonia (proposed in my Discovery Grant). If orbital forcing is a primary factor that explains long-term behavior of glaciers during the Holocene, then the records of glacier activity in the northern and southern Hemispheres should diverge. The development of continuous glacier proxies from the Hess mountains should also provide insight into the timing, amplitude, and duration of Holocene climate change that affected this portion of the Canadian Cordillera.The research that I propose directly benefits Canadians by helping to understand the behavior of the climate system. A careful study of past glacier fluctuations can help assess the magnitude, rapidity, and duration of past climatic events. These events provide valuable scenarios for calibrating and verifying general and regional circulation models. This research will provide undergraduate and graduate students with appropriate training in northern environments to minimize the projected Canadian deficit of highly qualified personnel (HQP) in the next decade. In addition to HQP training and publication of research findings, I plan to deliver several public talks about the research completed in the Keele Peak region to the communities of Ross River and Whitehorse.
Programme
Discovery Grants Program - Northern Research Supplement
Emplacement
British Columbia, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data

Tel que publié

Application id
305522-2009
Name nom
Menounos, Brian
Department département
Geography
Organization id
3
Institution établissement
University of Northern British Columbia
Province en
British Columbia
Province fr
Colombie-Britannique
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2013
Competition year année de concours
2009
Award amount
15000
Program id
RGPNS
Program name en
Discovery Grants Program - Northern Research Supplement
Program name fr
Porgramme de subventions à la découverte - supplément en recherche nordique
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
1025
Committee name en
Northern Research Supplement Program
Committee name fr
Programme de suppléments en recherche nordique
Area of application code
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4013
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Earth-systems science
Research subject fr
Sciences des systèmes terrestres
Partie
5
Nb partie
5
Application title
Holocene glacier fluctuations in the Keele Peak region, Yukon, Canada
Keyword
NSERC
Application summary
A recent review of the evidence for Holocene glacier fluctuations in western Canada recommends that future efforts should focus on documenting glacier fluctuations in eastern Yukon and the ranges in the Northwest Territories since little work has been completed in this region to date. One promising region is centered around the Keele Peak region (N 63 deg 26', W 130 deg 19') in the Hess Mountains, Yukon. Based on an analysis of pollen records, substantial climate change affected the adjacent Mackenzie Mountains during the Holocene. Given the location of the study area at high latitude in the Northern Hemisphere, it is believed that orbital forcing caused glaciers to expand from minimal extents in the early Holocene to maximum downvalley positions during the Little Ice Age. I aim to test the role that orbital forcing played on glacier activity at high latitudes by completing work in the Keele Peak area and at sites in southern Patagonia (proposed in my Discovery Grant). If orbital forcing is a primary factor that explains long-term behavior of glaciers during the Holocene, then the records of glacier activity in the northern and southern Hemispheres should diverge. The development of continuous glacier proxies from the Hess mountains should also provide insight into the timing, amplitude, and duration of Holocene climate change that affected this portion of the Canadian Cordillera.The research that I propose directly benefits Canadians by helping to understand the behavior of the climate system. A careful study of past glacier fluctuations can help assess the magnitude, rapidity, and duration of past climatic events. These events provide valuable scenarios for calibrating and verifying general and regional circulation models. This research will provide undergraduate and graduate students with appropriate training in northern environments to minimize the projected Canadian deficit of highly qualified personnel (HQP) in the next decade. In addition to HQP training and publication of research findings, I plan to deliver several public talks about the research completed in the Keele Peak region to the communities of Ross River and Whitehorse.