Grant: Discovery Grants Program - Individual
University of Northern British Columbia
$30,000.00
The relation between climate, glaciers, and lacustrine sedimentation in the american cordillera
FY 2010-11
Summary
Mountain glaciers are sensitive indicators of climate change. Moraines, trimlines, and forests overrun by glaciers during an advance provide opportunities to reconstruct past glacier activity. Proglacial lake sediments represent another valuable proxy of glacier fluctuations because more extensive ice cover should increase the proportion of substrate subject to glacier erosion. An advantage that lake sediments afford over terrestrial glacier proxies is the continuity that they can provide. In addition to long-term changes in ice cover, glacigenic sediments can also be used to infer hydro-climatic conditions that favor episodic delivery of clastic sediments to the lake basin. Progress in the use of these unique sedimentary records to reconstruct glacier activity and events such as floods requires an appreciation of the role that changes in sediment storage and availability play in controlling clastic sedimentation rates. Over the next five years I plan to advance our understanding of the relation between climate, glaciers, and downvalley sedimentation in western North America and Patagonia. My proposed research has two objectives: 1) to asses the relation between climate, glacier fluctuations and proglacial sedimentation at time scales of years to decades; and 2) to document the controls of clastic sedimentation at time scales of centuries to millennia. The research that I propose will help assess the relation between sediment export and glacier dynamics. Given the strong interplay between climate, glacier nourishment, and sediment yield, this work will provide insight into long-term changes in glacier extent and the external factors that drive these changes at high latitudes. The Holocene Epoch includes numerous climate events that provide important analogues for potential future behavior. These events also provide valuable scenarios for calibrating and verifying general and regional circulation models. Finally, undergraduate and graduate students are integral to successfully undertake the proposed research. Their involvement should help minimize the projected Canadian deficit of highly qualified personnel in the next decade.
Program
Discovery Grants Program - Individual
Location
British Columbia, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data
As published
Application id
261619-2009
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
2010
Competition year année de concours
2009
Award amount
30000
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
9
Committee name en
Environmental Earth Sciences
Committee name fr
Sc. de la Terre : environ.
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
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
2
Nb partie
5
Application title
The relation between climate, glaciers, and lacustrine sedimentation in the american cordillera
Keyword
NSERC
Application summary
Mountain glaciers are sensitive indicators of climate change. Moraines, trimlines, and forests overrun by glaciers during an advance provide opportunities to reconstruct past glacier activity. Proglacial lake sediments represent another valuable proxy of glacier fluctuations because more extensive ice cover should increase the proportion of substrate subject to glacier erosion. An advantage that lake sediments afford over terrestrial glacier proxies is the continuity that they can provide. In addition to long-term changes in ice cover, glacigenic sediments can also be used to infer hydro-climatic conditions that favor episodic delivery of clastic sediments to the lake basin. Progress in the use of these unique sedimentary records to reconstruct glacier activity and events such as floods requires an appreciation of the role that changes in sediment storage and availability play in controlling clastic sedimentation rates. Over the next five years I plan to advance our understanding of the relation between climate, glaciers, and downvalley sedimentation in western North America and Patagonia. My proposed research has two objectives: 1) to asses the relation between climate, glacier fluctuations and proglacial sedimentation at time scales of years to decades; and 2) to document the controls of clastic sedimentation at time scales of centuries to millennia. The research that I propose will help assess the relation between sediment export and glacier dynamics. Given the strong interplay between climate, glacier nourishment, and sediment yield, this work will provide insight into long-term changes in glacier extent and the external factors that drive these changes at high latitudes. The Holocene Epoch includes numerous climate events that provide important analogues for potential future behavior. These events also provide valuable scenarios for calibrating and verifying general and regional circulation models. Finally, undergraduate and graduate students are integral to successfully undertake the proposed research. Their involvement should help minimize the projected Canadian deficit of highly qualified personnel in the next decade.