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[PDF] Top 20 Dynamic response of Antarctic ice shelves to bedrock uncertainty

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Dynamic response of Antarctic ice shelves to bedrock uncertainty

Dynamic response of Antarctic ice shelves to bedrock uncertainty

... by ice flow from the continent (Rignot et al., 2008, 2013). Ice shelves play an important role in the mass balance of the Antarctic ice sheet through their buttressing effect on the ... See full document

16

Glacier dynamics, ice mass unloading and bedrock response in the southern Antarctic Peninsula

Glacier dynamics, ice mass unloading and bedrock response in the southern Antarctic Peninsula

... embayment-wide ice shelf in 1966 to smaller individual remnant ice shelves in 1997 ...an ice tongue in 1997 (Cook and Vaughan 2010), and as such would likely have imposed much lower backstress ... See full document

130

Uncertainty quantification of the multi-centennial response  of the Antarctic ice sheet to climate change

Uncertainty quantification of the multi-centennial response of the Antarctic ice sheet to climate change

... of ice-sheet geometry by Pollard and DeConto ...present-day ice-sheet con- figuration while assuming that the present-day configuration is in steady ...in ice streams with a slid- ing multiplier ... See full document

32

Surface undulations of Antarctic ice streams tightly controlled by bedrock topography

Surface undulations of Antarctic ice streams tightly controlled by bedrock topography

... flowing ice streams transmit information about their bedrock topography most efficiently to the surface for basal undula- tions with length scales between 1 and 20 times the mean ice ...current-day ... See full document

11

Reducing uncertainties in projections of Antarctic ice mass loss

Reducing uncertainties in projections of Antarctic ice mass loss

... whole Antarctic ice sheet, a number of studies have simulated the effect of ice shelf melting at the basin ...the response of PIG is mainly driven by the bedrock topography rather than ... See full document

13

A high-resolution bedrock map for the Antarctic Peninsula

A high-resolution bedrock map for the Antarctic Peninsula

... the dynamic response of glaciers on the Antarctic Peninsula to changed atmospheric and oceanic forcing requires high-resolution ice thickness data as an essential geometric constraint for ... See full document

13

Changes in flow of Crosson and Dotson ice shelves, West Antarctica, in response to elevated melt

Changes in flow of Crosson and Dotson ice shelves, West Antarctica, in response to elevated melt

... of ice-shelf–ice-stream sys- tems are also strongly controlled by grounding-line posi- ...of ice flux across the grounding line on ice thickness there, which is termed the marine ... See full document

17

Sea-level response to melting of Antarctic ice shelves on multi-centennial timescales with the fast Elementary Thermomechanical Ice Sheet model (f.ETISh v1.0)

Sea-level response to melting of Antarctic ice shelves on multi-centennial timescales with the fast Elementary Thermomechanical Ice Sheet model (f.ETISh v1.0)

... marine ice sheet instability (MISI) for ice sheets where the bedrock dips deeper inland from the grounding line (retrograde bed slopes) so that increased (atmospheric–oceanic) melting leads to re- ... See full document

28

The Antarctic Ice Sheet response to glacial millennial-scale  variability

The Antarctic Ice Sheet response to glacial millennial-scale variability

... thermomechanical ice-sheet model GRISLI-UCM based on the GRISLI model developed by Ritz et ...whole Antarctic domain. Initial topographic condi- tions (ice thickness, surface, and bedrock ... See full document

13

Antarctic bedrock topography uncertainty and ice sheet stability

Antarctic bedrock topography uncertainty and ice sheet stability

... Another ice sheet instability mechanism recently suggested by Bassis and Walker [2011] and explored in an ice sheet modeling study by Pollard et ...in bedrock eleva- ...information) ice ... See full document

6

Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves

Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves

... floating ice in addition to the freely evolving calv- ing front forcing (Experiment ...respective ice shelf (Paolo et ...is ice-shelf break-up in combination with the calving crite- ria that ... See full document

20

Can SMOS Ocean Salinity Data Detect a Link Between Increasing Antarctic Sea Ice Extent and Freshwater Flux from Basal Melting of Antarctic ice shelves?

Can SMOS Ocean Salinity Data Detect a Link Between Increasing Antarctic Sea Ice Extent and Freshwater Flux from Basal Melting of Antarctic ice shelves?

... sea ice in the Southern Ocean has revealed several ...sea ice extent (Turner et ...sea ice extent (Bitz & Polvani, 2012; Sigmond & Fyfe, ...the Antarctic region (Holland & Kwok, ... See full document

28

Recent ice dynamic and surface mass balance of Union Glacier in the West Antarctic Ice Sheet

Recent ice dynamic and surface mass balance of Union Glacier in the West Antarctic Ice Sheet

... West Antarctic Ice Sheet (WAIS), a major outlet glacier within the Ellsworth ...Ronne Ice Shelf, where recent mod- els have indicated the potential for significant grounding line zone (GLZ) ... See full document

12

Antarctic ice-sheet response to atmospheric CO

Antarctic ice-sheet response to atmospheric CO

... high-latitude, Antarctic box is subdivided into smaller grid cells with a resolution of ...underlying bedrock (F s ). In all boxes ice flow veloc- ities and ice height are computed, depending ... See full document

14

Surface energy budget on Larsen and Wilkins ice shelves in the Antarctic Peninsula: results based on reanalyses in 1989–2010

Surface energy budget on Larsen and Wilkins ice shelves in the Antarctic Peninsula: results based on reanalyses in 1989–2010

... tic ice shelves, on inter-annual variations in the budget terms, and on the weather conditions associated with high and low net heat flux to the ice ...Larsen ice shelves and WIS are ... See full document

20

Responses of basal melting of Antarctic ice shelves to the climatic forcing of the last glacial maximum and CO2 doubling

Responses of basal melting of Antarctic ice shelves to the climatic forcing of the last glacial maximum and CO2 doubling

... used Antarctic subsurface ocean temperatures (Beckmann and Goosse 2003) derived from an AOGCM to parameterize the basal mass balance beneath the ice shelves in their ice sheet models (de Boer ... See full document

25

The Response of Antarctic Sea Ice Algae to Changes in
pH and CO2

The Response of Antarctic Sea Ice Algae to Changes in pH and CO2

... the ice or those in brine channels, cells grow despite exposure to extremes of temperature and salinity, while those on the underside of the ice remain at close to freezing ... See full document

6

Past, Present and Future Climate of Antarctica

Past, Present and Future Climate of Antarctica

... Some recommendations for future studies are as fol- lows: 1) Observational program for Antarctica should be taken on a larger scale. A high accurate meteorological, glaciological and environmental chemistry data are ... See full document

19

Dynamic Antarctic ice sheet during the early to mid-Miocene.

Dynamic Antarctic ice sheet during the early to mid-Miocene.

... the Antarctic ice sheet had stabilized by 14 Ma [ 35], implying that the majority of glacial erosion had already occurred by this time [ 64] and that the bedrock topography may have been similar to ... See full document

7

Calving glaciers and ice shelves

Calving glaciers and ice shelves

... Totten ice shelf in eastern Antarctica ...the ice-base mainly over re-grounding ...by ice flow, and widen and grow by melt and stretching until they reach the terminus region where they precondition ... See full document

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