Award Abstract # 0902240
Collaborative Research: P2C2--Ice Core Paleoclimate Records from Combatant Col, British Columbia, Canada

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: UNIVERSITY OF WASHINGTON
Initial Amendment Date: June 4, 2009
Latest Amendment Date: June 4, 2009
Award Number: 0902240
Award Instrument: Standard Grant
Program Manager: David Verardo
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: September 1, 2009
End Date: August 31, 2012 (Estimated)
Total Intended Award Amount: $217,297.00
Total Awarded Amount to Date: $217,297.00
Funds Obligated to Date: FY 2009 = $217,297.00
ARRA Amount: $217,297.00
History of Investigator:
  • Eric Steig (Principal Investigator)
    steig@uw.edu
Recipient Sponsored Research Office: University of Washington
4333 BROOKLYN AVE NE
SEATTLE
WA  US  98195-1016
(206)543-4043
Sponsor Congressional District: 07
Primary Place of Performance: University of Washington
4333 BROOKLYN AVE NE
SEATTLE
WA  US  98195-1016
Primary Place of Performance
Congressional District:
07
Unique Entity Identifier (UEI): HD1WMN6945W6
Parent UEI:
NSF Program(s): Paleoclimate
Primary Program Source: 01R00910DB RRA RECOVERY ACT
Program Reference Code(s): 1304, 6890, EGCH
Program Element Code(s): 153000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Funding is provided to obtain new ice core accumulation records from Combatant Col, Mt. Waddington, in southwestern British Columbia (BC), Canada. Combatant Col is located significantly farther south than other existing ice core sites along the west coast of North America and variations in precipitation tend to be out of phase with those in Alaska and the Yukon.

Combatant Col sits at 3000 meters and contains more than 200 meters of ice. The net annual snow accumulation is ~2.5 meters/year and the mean annual temperature -5°C. A 65-meter core from the site shows that clear annual layering is preserved in the geochemistry and in dust and black carbon. The age of the ice near bedrock is estimated to be between 200 years and 1000 years old. It is anticipated that an annually-resolved record of layer thickness will be recovered at the site to allow for a record of snow accumulation covering the last 200-1000 years.

The Combatant Col record, in combination with other existing records of precipitation variability along the western margin of North America, will be used to develop an updated and improved reconstruction of precipitation variability in this region over the last 200-1000 years to address fundamental questions about Pacific decadal scale variability.

The broader impacts involve supporting an early career female investigator and strengthening international collaborations with researchers from institutions in Canada.

This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5).

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Neff P; Steig EJ; Clark DH; Pettit E; McConnell JR, Menounos B "An ice core record of net snow accumulation and seasonal snow chemistry at Mt. Waddington, southwest British Columbia, Canada" EOS Transactions American Geophysical Union , 2011

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