Award Abstract # 0732625
Collaborative Research in IPY: Abrupt Environmental Change in the Larsen Ice Shelf System, a Multidisciplinary Approach - Marine and Quaternary Geosciences

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: COLGATE UNIVERSITY
Initial Amendment Date: September 18, 2007
Latest Amendment Date: August 26, 2010
Award Number: 0732625
Award Instrument: Continuing Grant
Program Manager: Lisa Clough
lclough@nsf.gov
 (703)292-4746
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: October 1, 2007
End Date: September 30, 2013 (Estimated)
Total Intended Award Amount: $162,707.00
Total Awarded Amount to Date: $162,707.00
Funds Obligated to Date: FY 2007 = $12,503.00
FY 2008 = $37,620.00

FY 2009 = $39,140.00

FY 2010 = $73,444.00
History of Investigator:
  • Amy Leventer (Principal Investigator)
    aleventer@colgate.edu
Recipient Sponsored Research Office: Colgate University
13 OAK DR
HAMILTON
NY  US  13346-1386
(315)228-7457
Sponsor Congressional District: 22
Primary Place of Performance: Colgate University
13 OAK DR
HAMILTON
NY  US  13346-1386
Primary Place of Performance
Congressional District:
22
Unique Entity Identifier (UEI): D4P7H8NWZER7
Parent UEI:
NSF Program(s): ANT Integrated System Science
Primary Program Source: 0100XXXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 5292, 5295, 5382, OTHR
Program Element Code(s): 529200
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT


Abstract
This award supports a research cruise to perform geologic studies in the area under and surrounding the former Larsen B ice shelf, on the Antarctic Peninsula. The ice shelf's disintegration in 2002 coupled with the unique marine geology of the area make it possible to understand the conditions leading to ice shelf collapse. Bellwethers of climate change that reflect both oceanographic and atmospheric conditions, ice shelves also hold back glacial flow in key areas of the polar regions. Their collapse results in glacial surging and could cause rapid rise in global sea levels. This project characterizes the Larsen ice shelf's history and conditions leading to its collapse by determining: 1) the size of the Larsen B during warmer climates and higher sea levels back to the Eemian interglacial, 125,000 years ago; 2) the configuration of the Antarctic Peninsula ice sheet during the LGM and its subsequent retreat; 3) the causes of the Larsen B's stability through the Holocene, during which other shelves have come and gone; 4) the controls on the dynamics of ice shelf margins, especially the roles of surface melting and oceanic processes, and 5) the changes in sediment flux, both biogenic and lithogenic, after large ice shelf breakup.



The broader impacts include graduate and undergraduate education through research projects and workshops; outreach to the general public through a television documentary and websites, and international collaboration with scientists from Belgium, Spain, Argentina, Canada, Germany and the UK. The work also has important societal relevance. Improving our understanding of how ice shelves behave in a warming world will improve models of sea level rise.



The project is supported under NSF's International Polar Year (IPY) research emphasis area on "Understanding Environmental Change in Polar Regions".




PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Balco, G., Schaefer, J.M., and LARISSA group (Balco, G., Brachfeld, S., deBatist, M., Domack, E., Gordon, A., Haran, T., Henriet, J.-P., Huber, B., Ishman, S., Jeong, S., King, M., Lavoie, C., van Dover, C., Leventer, A., McCormick, M., Pettit, E., Scambo "Terrestrial exposure-age record of Holocene ice sheet and ice shelf change in the northeast Antarctic Peninsula" Quaternary Science Reviews , v.59 , 2013 , p.101

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

DCSIMG