C018
Holocene to Historical Context of Recent Ice Loss in the Amundsen Sea Embayment and along the West Antarctic Coast
Holocene to Historical Context of Recent Ice Loss in the Amundsen Sea Embayment and along the West Antarctic Coast
Session ID#: 160759
Session Description:
Sedimentary and geomorphological evidence show that the ice grounding line had already retreated to within 100 km of its present position by the early Holocene in most areas around the Amundsen Sea Embayment. Surface exposure ages from sites around Pine Island Bay record a period of rapid ice surface lowering in the mid Holocene, but little is known about subsequent ice sheet change prior to the initiation of contemporary rapid ice loss in the mid 20th century. Was Holocene retreat gradual or pulsed? Did the ice sheet retreat and thin beyond its current limits and then re-advance, as has been proposed for other sectors? We welcome presentations of results from all types of onshore and offshore studies and models that provide insight on West Antarctic Ice Sheet change through the Holocene and the initiation of contemporary rapid ice loss.
Index Terms:
0726 Ice sheets [CRYOSPHERE]
0730 Ice streams [CRYOSPHERE]
1621 Cryospheric change [GLOBAL CHANGE]
4926 Glacial [PALEOCEANOGRAPHY]
Primary Liaison: Kelly Hogan, British Antarctic Survey, Cambridge, United Kingdom
Primary Convener: Kelly Hogan, British Antarctic Survey, Cambridge, United Kingdom
Conveners: Asmara Lehrmann1, Joanne Johnson2 and Robert D Larter2, (1)University of Alabama, Geological Sciences, Tuscaloosa, United States(2)British Antarctic Survey, Cambridge, United Kingdom
Student/Early Career Convener: Asmara Lehrmann, University of Alabama, Geological Sciences, Tuscaloosa, United States
See more of: Cryosphere
