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[PDF] Top 20 Mapping Ice Sheet Grounding Lines With CryoSat-2

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Mapping Ice Sheet Grounding Lines With CryoSat-2

Mapping Ice Sheet Grounding Lines With CryoSat-2

... continuous ice sheet grounding ...of ice sheet observations acquired by any instrument to ...grounded ice boundary from the break in surface slope, although the earlier satellite ... See full document

12

An improved CryoSat-2 sea ice freeboard retrieval algorithm through the use of waveform fitting

An improved CryoSat-2 sea ice freeboard retrieval algorithm through the use of waveform fitting

... mean CryoSat-2 data for three campaign periods spanning March 2011 to March ...sea ice freeboard, snow depth, and thickness products (Kurtz et ...Digital Mapping System camera (Dominguez, ... See full document

21

Ice streams in the Laurentide Ice Sheet: a new mapping inventory

Ice streams in the Laurentide Ice Sheet: a new mapping inventory

... (Figures 2–5 and 7), topographic con- straints (Figures 4, 6, and 7) and major sedimentary depo-centres (Figure 6; Batchelor and Dowdes- well, ...or ice rafted debris traced to its sediment sources. ... See full document

17

Diagnosing ice sheet grounding line stability from landform morphology

Diagnosing ice sheet grounding line stability from landform morphology

... of ice to grounding lines is highly spatially vari- able, determined by the overall flow structure of the ice sheet (Bamber et ...of ice shelf buttressing (Rignot et ...the ... See full document

20

Glacier change along West Antarctica's Marie Byrd Land Sector and links to inter-decadal atmosphere–ocean variability

Glacier change along West Antarctica's Marie Byrd Land Sector and links to inter-decadal atmosphere–ocean variability

... Antarctic Ice Sheet into the ocean, particularly across the Amundsen Sea ...Ross Ice Shelf, glaciological change has been only sparsely ...track grounding-line migration along the Marie Byrd ... See full document

19

Persistence and variability of ice-stream grounding lines on retrograde bed slopes

Persistence and variability of ice-stream grounding lines on retrograde bed slopes

... of grounding-line migra- tion, a critical question is whether retreat on a retrograde slope necessarily implies continued irreversible retreat in the future due to the marine ice-sheet ...internal ... See full document

14

The stability of grounding lines on retrograde slopes

The stability of grounding lines on retrograde slopes

... of ice sheets to external forcing is of key ...of grounding-line position to changes in basal melt rates depends on bed ...the grounding-line po- sition is independent of any forcing to which an ... See full document

9

Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes

Three-dimensional mapping by CryoSat-2 of subglacial lake volume changes

... upon ice dynamics of variable rates of water delivery into the subglacial system ...estimate ice sheet mass balance over timescales longer than the periodicity of lake evolution and suggests that ... See full document

8

Hydrostatic grounding line parameterization in ice sheet models

Hydrostatic grounding line parameterization in ice sheet models

... of grounding lines, where ice detaches from the un- derlying bedrock and becomes afloat in the ocean, is possi- ble using satellite remote sensing with either visible imagery (Bohlander and Scambos, ... See full document

13

Parameterization of basal friction near grounding lines in a one-dimensional ice sheet model

Parameterization of basal friction near grounding lines in a one-dimensional ice sheet model

... accurate grounding- line migration only with a resolution of 200 m or less (Corn- ford et ...marine ice sheets at much lower computational expense than would be required with traditional friction ...whole ... See full document

21

Improved retrieval of land ice topography from CryoSat-2 data and its impact for volume-change estimation of the Greenland Ice Sheet

Improved retrieval of land ice topography from CryoSat-2 data and its impact for volume-change estimation of the Greenland Ice Sheet

... the ice-front position of the Zacahariæ Isstrøm beginning in ...the ice-front position, while a large positive signal is observed roughly 100 km upstream of the ...velocity mapping. Rates of ... See full document

17

Heterogeneous and rapid ice loss over the Patagonian Ice Fields revealed by CryoSat-2 swath radar altimetry

Heterogeneous and rapid ice loss over the Patagonian Ice Fields revealed by CryoSat-2 swath radar altimetry

... south and Lake Greve to the north. From 1945 to present, the tidewater terminus advanced ~13 km and is currently at its Neoglacial maximum (Wilson et al., 2016; Fig. 9 and Fig. E1). Looped supraglacial moraines were used ... See full document

15

Near-real-time Arctic sea ice thickness and volume from CryoSat-2

Near-real-time Arctic sea ice thickness and volume from CryoSat-2

... sea ice edge, which can im- prove the safety and efficiency of their operational missions (Posey et ...sea ice concentration data, it has been suggested that forecast model skill could be further im- proved ... See full document

10

Future sea level change from Antarctica's Lambert Amery glacial system

Future sea level change from Antarctica's Lambert Amery glacial system

... the ice shelf, the calving front is still north of the MISW and Clemence Massif (Figure ...the grounding line and the MISW can be seen in the profile of the ice shelf (ice shelf left of ... See full document

9

Sensitivity of CryoSat-2 Arctic sea-ice freeboard and thickness on radar-waveform interpretation

Sensitivity of CryoSat-2 Arctic sea-ice freeboard and thickness on radar-waveform interpretation

... The range to the main scattering horizon is estimated at the leading edge of the radar echo waveforms (Tonboe et al., 2006). In synthetic aperture radar (SAR) altimetry, the wave- form consists of a stack of collocated ... See full document

16

Retrieval of snow freeboard of Antarctic sea ice using waveform fitting of CryoSat-2 returns

Retrieval of snow freeboard of Antarctic sea ice using waveform fitting of CryoSat-2 returns

... sea ice. First, CryoSat-2 data are processed 1 month at a time and the outlying data points are filtered out to reduce the inherent noise of the ...the CryoSat-2 orbit and subtracting ... See full document

18

Grounding-line flux formula applied as a flux condition in numerical simulations fails for buttressed Antarctic ice streams

Grounding-line flux formula applied as a flux condition in numerical simulations fails for buttressed Antarctic ice streams

... calculated ice fluxes for steady-state condi- ...calculated ice fluxes for but- tressed ...predicts grounding-line ice fluxes for realistic geometries such as that of the present-day ... See full document

14

An ice sheet model validation framework for the Greenland ice sheet

An ice sheet model validation framework for the Greenland ice sheet

... the ice sheet in its initial configuration ...the ice sheet margin to retreat but not advance; at each time step, we apply a mask to simply remove any ice that has advanced beyond the ... See full document

16

Impact of assimilating a merged sea-ice thickness from CryoSat-2 and SMOS in the Arctic reanalysis

Impact of assimilating a merged sea-ice thickness from CryoSat-2 and SMOS in the Arctic reanalysis

... winter ice, as previously noted with the assimila- tion work of ICESat SIT data in Mathiot et ...and 2 November 2014, followed by a large decrease in the subsequent ...the 2 November reveals that the ... See full document

21

Climatic Conditions for modelling the Northern Hemisphere ice sheets throughout the ice age cycle

Climatic Conditions for modelling the Northern Hemisphere ice sheets throughout the ice age cycle

... The ice to- pography effect can have a “local” effect and “non-local” ...“local” ice topography effect is the so-called “lapse rate effect”, which causes cooling over the ice sheet just ... See full document

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