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Details of Award

NERC Reference : NER/G/S/2002/00192

Glacial-interglacial changes in the lost drainage basin on the West Antarctic ice sheet.

Grant Award

Principal Investigator:
Dr RD Larter, University of Cambridge, Scott Polar Research Institute
Co-Investigator:
Professor JA Dowdeswell, University of Cambridge, Scott Polar Research Institute
Co-Investigator:
Dr C Pudsey, NERC British Antarctic Survey, NERC BAS - Cambridge
Science Area:
Marine
Earth
Overall Classification:
Earth
ENRIs:
Global Change
Environmental Risks and Hazards
Science Topics:
Sediment/Sedimentary Processes
Quaternary Science
Glacial & Cryospheric Systems
Geohazards
Abstract:
Sparse existing data suggest that a very dynamic glacial system has deposited vast quantities of sediment in the Bellingshausen Sea. From approximately 84-88 degrees W the continental slope comprises a trough-mouth fan (TMF) with a gradient of approximately 1.5 degrees, in sharp contrast to the slope farther NE which is much steeper (greater than 10 degrees). A 150 km-wide trough on the outer shelf suggests that the TMF was fed by a major, previously unrecognised ice stream, that may have drained greater than 300,000 km2 of the West Antarctic Ice Sheet (WAIS). We will use swath bathymetry and acoustic profiles to track the course of this ice stream back towards its source, inferring subglacial processes from shelf morphology. Sediment cores on the shelf and slope will reveal the nature of glacial and post-glacial deposition, and the timing of ice retreat. Palaeo-ice stream dimensions will be used to constrain thermo-mechanical models of the WAIS.
Period of Award:
1 May 2004 - 30 Apr 2007
Value:
£81,271 Split Award
Authorised funds only
NERC Reference:
NER/G/S/2002/00192
Grant Stage:
Completed
Scheme:
AFI Pre FEC
Grant Status:
Closed
Programme:
AFI

This grant award has a total value of £81,271  

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FDAB - Financial Details (Award breakdown by headings)

Total - StaffTotal - T&STotal - Other CostsTotal - Indirect Costs
£53,066£2,745£1,049£24,410

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