First exposure ages from the Amundsen Sea Embayment, West Antarctica: The Late Quaternary context for recent thinning of Pine Island, Smith, and Pope Glaciers
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- Type
- article
- Published
- 2008-03-01
- Cited by
- 64
- References
- 19
- Access
- Open access
- OpenAlex
- https://openalex.org/W1964367186
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:62886936
Keywords
Context (archaeology), Glacier, Geological survey, Geology, Physical geography
References
- The weak underbelly of the West Antarctic ice sheet
- Why Is It Hard to Predict the Future of Ice Sheets?
- Warm ocean is eroding West Antarctic Ice Sheet
- Recent dramatic thinning of largest West Antarctic ice stream triggered by oceans
- Measurements of Past Ice Sheet Elevations in Interior West Antarctica.
- Geological and geomorphological insights into Antarctic ice sheet evolution
- Inland thinning of Pine Island Glacier, West Antarctica.
- West Antarctic Ice Sheet change since the last glacial period
- Timing of Recent Accelerations of Pine Island Glacier, Antarctica
- New boundary conditions for the West Antarctic Ice Sheet: Subglacial topography of the Thwaites and Smith glacier catchments
- Acceleration of Pine Island and Thwaites Glaciers, West Antarctica
- Selective glacial erosion and weathering zones in the coastal mountains of Marie Byrd Land, Antarctica
- Holocene Deglaciation of Marie Byrd Land, West Antarctica
- New boundary conditions for the West Antarctic ice sheet: Subglacial topography beneath Pine Island Glacier
- Reconstruction of the West Antarctic ice sheet in Pine Island Bay during the Last Glacial Maximum and its subsequent retreat history
- Mid-Pleistocene cosmogenic minimum-age limits for pre-Wisconsinan glacial surfaces in southwestern Minnesota and southern Baffin Island: a multiple nuclide approach
- Geomorphological evidence and cosmogenic 10Be/26Al exposure ages for the Last Glacial Maximum and deglaciation of the Antarctic Peninsula Ice Sheet
- Snowfall-Driven Growth in East Antarctic Ice Sheet Mitigates Recent Sea-Level Rise
- Modelling Antarctic sea-level data to explore the possibility of a dominant Antarctic contribution to meltwater pulse IA
Cited by
- An improved glacial isostatic adjustment model for the British Isles
- Contributions and unrealized potential contributions of cosmogenic-nuclide exposure dating to glacier chronology, 1990–2010
- Holocene glacial history of Antarctica and the sub-Antarctic islands
- Constraints on Antarctic Ice Sheet configuration during and following the Last Glacial Maximum and its episodic contribution to sea-level rise
- The last deglacial history of Lützow‐Holm Bay, East Antarctica
- Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum
- Identifying the causes of sea-level change
- The Last Glacial Maximum
- Basement control on past ice sheet dynamics in the Amundsen Sea Embayment, West Antarctica
- Holocene deglacial history of the northeast Antarctic Peninsula – A review and new chronological constraints
- A deglacial model for Antarctica: geological constraints and glaciological modelling as a basis for a new model of Antarctic glacial isostatic adjustment
- Psychological science's contributions to a sustainable environment: extending our reach to a grand challenge of society.
- Antarctic Peninsula Ice Sheet evolution during the Cenozoic Era
- Retreat of the East Antarctic ice sheet during the last glacial termination
- Rapid early Holocene retreat of a Laurentide outlet glacier through an Arctic fjord
- Dynamics of the last glacial maximum Antarctic ice-sheet and its response to ocean forcing
- Glacial retreat in the Amundsen Sea sector, West Antarctica – first cosmogenic evidence from central Pine Island Bay and the Kohler Range
- Weak bed control of the eastern shear margin of Thwaites Glacier, West Antarctica
- Rapid Thinning of Pine Island Glacier in the Early Holocene
- History of the Antarctic Peninsula ice sheet since the early Pliocene - evidence from cosmogenic dating of Pliocene lavas on James Ross Island, Antarctica.
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