Professor Dave Roberts d.h.roberts@durham.ac.uk
Professor
New constraints on Greenland ice sheet dynamics during the last glacial cycle: evidence from the Uummannaq ice stream system
Roberts, D.H.; Rea, B.; Lane, T.; Schnabel, C.; Rodés, A.
Authors
B. Rea
T. Lane
C. Schnabel
A. Rodés
Abstract
This paper presents the first assessment of the Uummannaq ice stream system (UISS) in West Greenland. The UISS drained ~6% of the Greenland ice sheet (GrIS) at the Last Glacial Maximum (LGM). The onset of the UISS is a function of a convergent network of fjords which feed a geologically controlled trough system running offshore to the shelf break. Mapping, cosmogenic radiogenic nuclide (CRN) dating, and model output reveal that glacially scoured surfaces up to 1266 m above sea level (asl) in fjord-head areas were produced by warm-based ice moving offshore during the LGM, with the elevation of warm-based ice dropping westwards to ~700 m asl as the ice stream trunk zone developed. Marginal plateaux with allochthonous blockfields suggest that warm-based ice produced till and erratics up to ~1200 m asl, but CRN ages and weathering pits suggest this was pre-LGM, with only cold-based ice operating during the LGM. Deglaciation began on the outer shelf at ~14.8 cal. kyrs B.P., with Ubekendt Ejland becoming ice free at ~12.4 ka. The UISS then collapsed with over 100 km of retreat by ~11.4 ka–10.8 cal. kyrs B.P., a rapid and complex response to bathymetric deepening, trough widening, and sea-level rise coinciding with rapidly increasing air temperatures and solar radiation, but which occurred prior to ocean warming at ~8.4 cal. kyrs B.P. Local fjord constriction temporarily stabilized the unzipped UISS margins at the start of the Holocene before ice retreat inland of the current margin at ~8.7 ka.
Citation
Roberts, D., Rea, B., Lane, T., Schnabel, C., & Rodés, A. (2013). New constraints on Greenland ice sheet dynamics during the last glacial cycle: evidence from the Uummannaq ice stream system. Journal of Geophysical Research: Earth Surface, 118(2), 519-541. https://doi.org/10.1002/jgrf.20032
Journal Article Type | Article |
---|---|
Acceptance Date | Jul 11, 2013 |
Publication Date | Jun 1, 2013 |
Deposit Date | Feb 26, 2013 |
Publicly Available Date | Mar 7, 2016 |
Journal | Journal of Geophysical Research: Earth Surface |
Print ISSN | 2169-9011 |
Electronic ISSN | 2169-9011 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 118 |
Issue | 2 |
Pages | 519-541 |
DOI | https://doi.org/10.1002/jgrf.20032 |
Public URL | https://durham-repository.worktribe.com/output/1488933 |
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Copyright Statement
Roberts, D. H., B. R. Rea, T. P. Lane, C. Schnabel, and A. Rodés (2013), New constraints on Greenland ice sheet dynamics during the last glacial cycle: Evidence from the Uummannaq ice stream system, Journal of Geophysical Research: Earth Surface, 118, 519-541, 10.1002/jgrf.20032 (DOI). To view the published open abstract, go to http://dx.doi.org and enter the DOI.
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