Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks
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Martin Jakobsson | Julian A. Dowdeswell | J. Dowdeswell | M. Jakobsson | R. Larter | Matthew G. Wise | Robert D. Larter | M. Wise
[1] C. C. Walker,et al. Upper and lower limits on the stability of calving glaciers from the yield strength envelope of ice , 2012, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[2] John B. Anderson,et al. Ice sheet retreat dynamics inferred from glacial morphology of the central Pine Island Bay Trough, West Antarctica , 2012 .
[3] J. Dowdeswell,et al. Geomorphic signature of Antarctic submarine gullies: Implications for continental slope processes , 2013 .
[4] John B. Anderson,et al. Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum , 2014 .
[5] John B. Anderson,et al. Paleo ice flow and subglacial meltwater dynamics in Pine Island Bay, West Antarctica , 2012 .
[6] A. Jenkins,et al. Submarine glacial-landform distribution across the West Antarctic margin, from grounding line to slope: the Pine Island–Thwaites ice-stream system , 2016, memoirs.
[7] B. Scheuchl,et al. Widespread, rapid grounding line retreat of Pine Island, Thwaites, Smith, and Kohler glaciers, West Antarctica, from 1992 to 2011 , 2014 .
[8] C. Ó. Cofaigh,et al. Mechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula region , 2009 .
[9] Frank Pattyn,et al. Power law or power flaw , 1998 .
[10] Eric Rignot,et al. Basal terraces on melting ice shelves , 2014 .
[11] Bo Sun,et al. Bedmap2: improved ice bed, surface and thickness datasets for Antarctica , 2012 .
[12] D. Macayeal,et al. Breakup of the Larsen B Ice Shelf triggered by chain reaction drainage of supraglacial lakes , 2013 .
[13] Fernando S. Paolo,et al. Volume loss from Antarctic ice shelves is accelerating , 2015, Science.
[14] John B. Anderson,et al. Geological record of ice shelf break-up and grounding line retreat, Pine Island Bay, West Antarctica , 2011 .
[15] R. DeConto,et al. Contribution of Antarctica to past and future sea-level rise , 2016, Nature.
[16] D. Vaughan,et al. Sub-ice-shelf sediments record history of twentieth-century retreat of Pine Island Glacier , 2016, Nature.
[17] J. Dowdeswell,et al. Possible iceberg-produced submarine terraces in Hambergbukta, Spitsbergen , 2016, memoirs.
[18] Joseph A. MacGregor,et al. Widespread rifting and retreat of ice-shelf margins in the eastern Amundsen Sea Embayment between 1972 and 2011 , 2012, Journal of Glaciology.
[19] D. Abbot,et al. Laboratory investigations of iceberg capsize dynamics, energy dissipation and tsunamigenesis , 2012 .
[20] Eric Rignot,et al. Ice-shelf changes in Pine Island Bay, Antarctica, 1947-2000 , 2002, Journal of Glaciology.
[21] James A. Smith,et al. West Antarctic Ice Sheet retreat driven by Holocene warm water incursions , 2017, Nature.
[22] Richard B. Alley,et al. Potential Antarctic Ice Sheet retreat driven by hydrofracturing and ice cliff failure , 2015 .
[23] J. Dowdeswell,et al. A subglacial landform assemblage on the outer shelf of M'Clure Strait, Canadian Arctic, ploughed by iceberg keels , 2016, memoirs.
[24] Eric Rignot,et al. Changes in West Antarctic ice stream dynamics observed with ALOS PALSAR data , 2008 .
[25] J. Goff,et al. Seismic and bathymetric evidence for four different episodes of iceberg scouring on the New Jersey outer shelf: Possible correlation to Heinrich events , 2008 .
[26] T. Hughes,et al. On the Disintegration of Ice Shelves: The Role of Fracture , 1983, Journal of Glaciology.
[27] J. Dowdeswell,et al. Relict sea-floor ploughmarks record deep-keeled Antarctic icebergs to 45°S on the Argentine margin , 2011 .
[28] L. M. Cathles,et al. The role of cooperative iceberg capsize in ice-shelf disintegration , 2013, Annals of Glaciology.
[29] D. Benn,et al. Calving processes and the dynamics of calving glaciers , 2007 .
[30] B. Smith,et al. Has a marine ice sheet collapse begun in the Thwaites Glacier basin, West Antarctica? , 2014 .
[31] R. Finkel,et al. Rapid Thinning of Pine Island Glacier in the Early Holocene , 2014, Science.
[32] W. T. Pfeffer,et al. Kinematic Constraints on Glacier Contributions to 21st-Century Sea-Level Rise , 2008, Science.
[33] O. Gagliardini,et al. The stability of grounding lines on retrograde slopes , 2012 .
[34] A. Payne,et al. Retreat of Pine Island Glacier controlled by marine ice-sheet instability , 2014 .
[35] Matt A. King,et al. A new glacial isostatic adjustment model for Antarctica: calibrated and tested using observations of relative sea‐level change and present‐day uplift rates , 2012 .
[36] T. Hughes. West Antarctic Ice Streams , 1977 .
[37] Y. Kristoffersen,et al. Seabed erosion on the Lomonosov Ridge, central Arctic Ocean: A tale of deep draft icebergs in the Eurasia Basin and the influence of Atlantic water inflow on iceberg motion? , 2004 .
[38] Projecting Antarctic ice discharge using response functions from SeaRISE ice-sheet models , 2013 .
[39] J. Barrie,et al. The physical processes of seabed disturbance during iceberg grounding and scouring , 1991 .
[40] Jonathan L. Bamber,et al. Keel depths of modern Antarctic icebergs and implications for sea-floor scouring in the geological record , 2007 .
[41] J. Goff,et al. Relict iceberg keel marks on the New Jersey outer shelf, southern Hudson apron , 2001 .
[42] B. Todd,et al. Comparison of trends of iceberg scour marks with iceberg trajectories and evidence of paleocurrent trends on Saglek Bank, northern Labrador Shelf , 1988 .