Holocene history of the west Greenland Ice Sheet and the GH-8 . 2 event
@inproceedings{Longa2006HoloceneHO, title={Holocene history of the west Greenland Ice Sheet and the GH-8 . 2 event}, author={Anna Longa and D RobertsA and Susan Dawsonb}, year={2006}, url={https://api.semanticscholar.org/CorpusID:27805577} }
The margin of the Greenland Ice Sheet retreated rapidly during the first few thousand years of the Holocene. During this period of relative warmth, known as the Holocene thermal maximum, ice core records identify a significant short-lived cooling event at approximately 8.4–8.0 ka cal. yr BP (the ‘GH-8.2 event’) associated with a 5–7 1C fall in mean annual air temperature over the centre of the ice sheet. In this paper we constrain the history of the ice sheet margin in Disko Bugt (west…
2 Citations
Response of a land-terminating sector of the western Greenland Ice Sheet to early Holocene climate change: Evidence from 10 Be dating in the Søndre Isortoq region
- 2018
Environmental Science, Geology
retreat using Osmium isotopes: Insights from the Greenland
- 2017
Environmental Science, Geology
20 High-resolution Os isotope stratigraphy can aid in reconstructing Pleistocene ice sheet 21 fluctuation and elucidating the role of local and regional weathering fluxes on the marine 22 Os…
54 References
The Greenland ice sheet-a model for its culmination and decay during and after the last glacial maximum
- 2008
Environmental Science, Geology
Ice margin reconstructions of the Greenland ice sheet during LGM (c. 21-16 ka) and 10 ka are based on published onshore field evidence supplemented with recent studies on the East Greenland shelf and…
Late Wisconsinan and Holocene History of the Laurentide Ice Sheet
- 2008
Geology, Environmental Science
Eleven paleogeographic maps and a summary ice retreat map outline the history of advance, retreat, and readvances of the Laurentide Ice Sheet along with associated changes in proglacial drainage and…
Topographic controls on post-Oligocene changes in ice-sheet dynamics, Prydz Bay region, East Antarctica
- 2004
Geology, Environmental Science
Within the general trend of post-Eocene cooling, the largest and oldest outlet of the East Antarctic Ice Sheet underwent a change from ice-cliff to ice-stream and/or ice-shelf dynamics, with an…
A revised chronology for the ‘Fjord Stade’ moraine in Disko Bugt, west Greenland
- 2002
Geology, Environmental Science
This paper re‐evaluates the age of the ‘Fjord Stade’ moraine in Disko Bugt, a large marine embayment in west Greenland. Previous work suggests that this moraine is part of a widespread moraine…
Holocene Climatic Variations—Their Pattern and Possible Cause
- 1973
Environmental Science, Geology
Holocene Relative Sea Level Changes in Disko Bugt, West Greenland
- 2000
Environmental Science, Geology
An investigation of Holocene relative sea level (RSL) changes in Disko Bugt has been carried out with the purpose of reconstructing, with a good resolution in time and space, the Holocene RSL changes…
Isolation basin stratigraphy and Holocene relative sea-level change on Arveprinsen Ejland, Disko Bugt, West Greenland
- 1999
Geology, Environmental Science
This paper presents the results of an investigation into Holocene relative sea-level (RSL) change, isostatic rebound and ice sheet dynamics in Disko Bugt, West Greenland. Data collected from nine…
Early Holocene glacier advance, southern Coast Mountains, British Columbia, Canada
- 2004
Geology, Environmental Science
Holocene climatic instability: A prominent, widespread event 8200 yr ago
- 1997
Environmental Science, Geology
The most prominent Holocene climatic event in Greenland ice-core proxies, with approximately half the amplitude of the Younger Dryas, occurred ∼8000 to 8400 yr ago. This Holocene event affected…