Award Abstract # 1142085
Revealing Late Holocence Climate Variability in Antarctica from Borehole Paleothermometry

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: THE PENNSYLVANIA STATE UNIVERSITY
Initial Amendment Date: June 20, 2012
Latest Amendment Date: August 26, 2015
Award Number: 1142085
Award Instrument: Standard Grant
Program Manager: Julie Palais
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: July 1, 2012
End Date: February 29, 2016 (Estimated)
Total Intended Award Amount: $185,149.00
Total Awarded Amount to Date: $185,149.00
Funds Obligated to Date: FY 2013 = $131,963.00
History of Investigator:
  • Atsuhiro Muto (Principal Investigator)
  • Richard Alley (Former Principal Investigator)
  • Atsuhiro Muto (Former Co-Principal Investigator)
Recipient Sponsored Research Office: Pennsylvania State Univ University Park
201 OLD MAIN
UNIVERSITY PARK
PA  US  16802-1503
(814)865-1372
Sponsor Congressional District: 15
Primary Place of Performance: Pennsylvania State Univ University Park
PA  US  16802-7000
Primary Place of Performance
Congressional District:
Unique Entity Identifier (UEI): NPM2J7MSCF61
Parent UEI:
NSF Program(s): ANT Glaciology
Primary Program Source: 0100XXXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 7754
Program Element Code(s): 511600
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

Alley/1142085

This award supports a project to continue the collection and analyses of firn temperature data from three automated firn thermal profiling units deployed in Dronning Maud Land sector of East Antarctica as part of the Norway-US IPY Traverse project between 2007 and 2009. The intellectual merits of this project are as follows: 1) to constrain and improve the parameterization of firn thermal properties (thermal conductivity and specific heat capacity) that are required for the borehole paleothermometry, 2) to study the change in firn temperature since the deployment of thermal profiling units ~5 years ago and derive the surface temperature trend for that time period, and 3) to compare and contrast the surface temperatures and their trends derived from the measured firn temperatures and satellite thermal infrared data for the past three decades. The project also involves acquiring and deploying an automated system to record transient temperatures at multiple depths in the top 16 meters of the shallow borehole at Dome Fuji, to provide useful data and to prepare for the possibility of conducting temperature-logging in the existing deep (3035 m) and shallow (112 m) boreholes at Dome Fuji in the near future. The preparation of the shallow borehole and the installation of the automated system will be carried out by collaborators from the Japanese Antarctic Research Expedition (JARE) in 2012-13 Antarctic field season. The data collected by this automated system will be used to constrain the thermal properties of upper firn layer at Dome Fuji, as well as comparing with data from other sites, increasing the geographic extent of these studies. The broader impacts of the project include presentation of results at scientific conferences and publication of results in peer-reviewed journals. Public outreach will include targeted work with science teachers and middle school students.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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A. Orsi, K. Kawamura, J.M. Fegyveresi, M.A. Headly, R.B. Alley and J.P. Severinghaus "Differentiating bubble-free layers from melt layers in ice cores using noble gases" Journal of Glaciology , v.61 , 2015 , p.585 10.3189/2015JoG14J237

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