Award Abstract # 0520375
Fracture of Sea Ice Under Low Confinement: The Transition from Splitting to Shear Faulting

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: TRUSTEES OF DARTMOUTH COLLEGE
Initial Amendment Date: August 26, 2005
Latest Amendment Date: August 26, 2005
Award Number: 0520375
Award Instrument: Standard Grant
Program Manager: William J. Wiseman, Jr.
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: September 1, 2005
End Date: August 31, 2008 (Estimated)
Total Intended Award Amount: $255,878.00
Total Awarded Amount to Date: $255,878.00
Funds Obligated to Date: FY 2005 = $255,878.00
History of Investigator:
  • Carl Renshaw (Principal Investigator)
    Carl.E.Renshaw@Dartmouth.EDU
  • Erland Schulson (Co-Principal Investigator)
Recipient Sponsored Research Office: Dartmouth College
7 LEBANON ST
HANOVER
NH  US  03755-2170
(603)646-3007
Sponsor Congressional District: 02
Primary Place of Performance: Dartmouth College
7 LEBANON ST
HANOVER
NH  US  03755-2170
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): EB8ASJBCFER9
Parent UEI: T4MWFG59C6R3
NSF Program(s): ANS-Arctic Natural Sciences
Primary Program Source: 0100CYXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 1079, 9150, OTHR
Program Element Code(s): 528000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

Splits and shear faults that form within the sea ice cover of the Arctic Ocean during winter result in reductions in the sea ice's integrity, albedo and effectiveness as a thermal barrier to the transfer of heat from the ocean to the atmosphere. Funds are provided to perform new experiments and modeling aimed at elucidating the fundamental physical processes that underlie these types of fractures within the winter sea ice cover. The focus of this proposal is the set of conditions under which each type of fracture forms, the underlying physical mechanisms, and how confinement governs the transition from splitting to faulting. To examine these issues, the principal investigators propose a series of systematic experiments on salt-water ice (and on fresh-water ice for comparison) with a long-term goal of better understanding the physics of sea ice failure. In addition, they propose to develop quantitative models of these physics, using as inputs direct observations of the physical processes.

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Wachter, L.M.; Renshaw, C.E.; Schulson, E.M. "Transition in brittle failure mode under low confinement" Eos Trans. AGU Fall Meet. Suppl. , v.87(52) , 2006 , p.T11C-0447

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