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      Channelized Ice Melting in the Ocean Boundary Layer Beneath Pine Island Glacier, Antarctica

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          Ice flow of the Antarctic ice sheet.

          E Rignot, J Mouginot, B Scheuchl (2011)
          We present a reference, comprehensive, high-resolution, digital mosaic of ice motion in Antarctica assembled from multiple satellite interferometric synthetic-aperture radar data acquired during the International Polar Year 2007 to 2009. The data reveal widespread, patterned, enhanced flow with tributary glaciers reaching hundreds to thousands of kilometers inland over the entire continent. This view of ice sheet motion emphasizes the importance of basal-slip-dominated tributary flow over deformation-dominated ice sheet flow, redefines our understanding of ice sheet dynamics, and has far-reaching implications for the reconstruction and prediction of ice sheet evolution.
          Article 0 comments Cited 374 times – based on 0 reviews     Review now
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            Extensive dynamic thinning on the margins of the Greenland and Antarctic ice sheets.

            Hamish Pritchard, Robert J. Arthern, David Vaughan … (2009)
            Many glaciers along the margins of the Greenland and Antarctic ice sheets are accelerating and, for this reason, contribute increasingly to global sea-level rise. Globally, ice losses contribute approximately 1.8 mm yr(-1) (ref. 8), but this could increase if the retreat of ice shelves and tidewater glaciers further enhances the loss of grounded ice or initiates the large-scale collapse of vulnerable parts of the ice sheets. Ice loss as a result of accelerated flow, known as dynamic thinning, is so poorly understood that its potential contribution to sea level over the twenty-first century remains unpredictable. Thinning on the ice-sheet scale has been monitored by using repeat satellite altimetry observations to track small changes in surface elevation, but previous sensors could not resolve most fast-flowing coastal glaciers. Here we report the use of high-resolution ICESat (Ice, Cloud and land Elevation Satellite) laser altimetry to map change along the entire grounded margins of the Greenland and Antarctic ice sheets. To isolate the dynamic signal, we compare rates of elevation change from both fast-flowing and slow-flowing ice with those expected from surface mass-balance fluctuations. We find that dynamic thinning of glaciers now reaches all latitudes in Greenland, has intensified on key Antarctic grounding lines, has endured for decades after ice-shelf collapse, penetrates far into the interior of each ice sheet and is spreading as ice shelves thin by ocean-driven melt. In Greenland, glaciers flowing faster than 100 m yr(-1) thinned at an average rate of 0.84 m yr(-1), and in the Amundsen Sea embayment of Antarctica, thinning exceeded 9.0 m yr(-1) for some glaciers. Our results show that the most profound changes in the ice sheets currently result from glacier dynamics at ocean margins.
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              Recent Antarctic ice mass loss from radar interferometry and regional climate modelling

              Eric Rignot, Jonathan L. Bamber, Michiel R van den Broeke … (2008)
              Article 0 comments Cited 296 times – based on 0 reviews     Review now
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                Author and article information

                Journal
                Title: Science
                Abbreviated Title: Science
                Publisher: American Association for the Advancement of Science (AAAS)
                ISSN (Print): 0036-8075
                ISSN (Electronic): 1095-9203
                Publication date Created: September 12 2013
                Publication date (Print): September 12 2013
                Volume: 341
                Issue: 6151
                Pages: 1236-1239
                Article
                DOI: 10.1126/science.1239373
                PubMed ID: 24031016
                SO-VID: bea106dd-b069-4195-a4ab-8cc2ef4bebf5
                Copyright © © 2013
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