Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day

[1]  C. Stewart,et al.  Crevasse refreezing and signatures of retreat observed at Kamb Ice Stream grounding zone , 2023, Nature Geoscience.

[2]  F. Straneo,et al.  Submarine melting of glaciers in Greenland amplified by atmospheric warming , 2022, Nature Geoscience.

[3]  John B. Anderson,et al.  Rapid retreat of Thwaites Glacier in the pre-satellite era , 2022, Nature Geoscience.

[4]  J. Dowdeswell,et al.  Geomorphic signature of the presence and breakup of large ice-sheet derived multi-keeled tabular icebergs , 2022, Marine Geology.

[5]  J. Dowdeswell,et al.  Distinctive iceberg ploughmarks on the mid-Norwegian margin: Tidally influenced chains of pits with implications for iceberg drift , 2022, Arctic, Antarctic, and Alpine Research.

[6]  J. Dowdeswell,et al.  Glacial landforms reveal dynamic ice-sheet behaviour along the mid-Norwegian margin during the last glacial-deglacial cycle , 2022, Quaternary Science Reviews.

[7]  T. L. Rasmussen,et al.  The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet , 2022, Communications Earth & Environment.

[8]  D. Roberts,et al.  The Ocean and Cryosphere in a Changing Climate , 2022 .

[9]  L. Dini,et al.  Rapid glacier retreat rates observed in West Antarctica , 2022, Nature Geoscience.

[10]  Stergios D. Zarkogiannis Disruption of the Atlantic Meridional Circulation during Deglacial Climates Inferred from Planktonic Foraminiferal Shell Weights , 2021, Journal of Marine Science and Engineering.

[11]  C. Clark,et al.  Timing and pace of ice‐sheet withdrawal across the marine–terrestrial transition west of Ireland during the last glaciation , 2021, Journal of Quaternary Science.

[12]  M. Winsborrow,et al.  Exceptions to bed-controlled ice sheet flow and retreat from glaciated continental margins worldwide , 2021, Science Advances.

[13]  J. Paden,et al.  New gravity-derived bathymetry for the Thwaites, Crosson, and Dotson ice shelves revealing two ice shelf populations , 2020 .

[14]  J. Dowdeswell,et al.  New insights into the formation of submarine glacial landforms from high-resolution Autonomous Underwater Vehicle data , 2020 .

[15]  H. Fricker,et al.  Interannual variations in meltwater input to the Southern Ocean from Antarctic ice shelves , 2020, Nature Geoscience.

[16]  J. Dowdeswell,et al.  Delicate seafloor landforms reveal past Antarctic grounding-line retreat of kilometers per year , 2020, Science.

[17]  M. Petrini,et al.  Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions , 2020, Quaternary Science Reviews.

[18]  M. Braun,et al.  Remote sensing of glacier and ice sheet grounding lines: A review , 2020 .

[19]  Eric Rignot,et al.  Mass balance of the Greenland Ice Sheet from 1992 to 2018 , 2019, Nature.

[20]  James A. Smith,et al.  The marine geological imprint of Antarctic ice shelves , 2019, Nature Communications.

[21]  B. Smith,et al.  Ice shelf basal melt rates from a high-resolution digital elevation model (DEM) record for Pine Island Glacier, Antarctica , 2019, The Cryosphere.

[22]  Won Sang Lee,et al.  Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet , 2019, The Cryosphere.

[23]  C. Kienholz,et al.  Direct observations of submarine melt and subsurface geometry at a tidewater glacier , 2019, Science.

[24]  M. Montoya,et al.  Ocean-driven millennial-scale variability of the Eurasian ice sheet during the last glacial period simulated with a hybrid ice-sheet–shelf model , 2019, Climate of the Past.

[25]  Eric Rignot,et al.  Forty-six years of Greenland Ice Sheet mass balance from 1972 to 2018 , 2019, Proceedings of the National Academy of Sciences.

[26]  B. Scheuchl,et al.  Heterogeneous retreat and ice melt of Thwaites Glacier, West Antarctica , 2019, Science Advances.

[27]  G. Madec,et al.  Simulating or prescribing the influence of tides on the Amundsen Sea ice shelves , 2019, Ocean Modelling.

[28]  R. Bell,et al.  Antarctic surface hydrology and impacts on ice-sheet mass balance , 2018, Nature Climate Change.

[29]  Myoung-Jong Noh,et al.  The Reference Elevation Model of Antarctica , 2018, The Cryosphere.

[30]  M. Morlighem,et al.  Hard rock landforms generate 130 km ice shelf channels through water focusing in basal corrugations , 2018, Nature Communications.

[31]  Eric Rignot,et al.  Mass balance of the Antarctic Ice Sheet from 1992 to 2017 , 2018, Nature.

[32]  A. Shepherd,et al.  Net retreat of Antarctic glacier grounding lines , 2018, Nature Geoscience.

[33]  M. Winsborrow,et al.  Retreat patterns and dynamics of the Sentralbankrenna glacial system, central Barents Sea , 2017 .

[34]  P. Whitehouse,et al.  Deglaciation of the Eurasian ice sheet complex , 2017 .

[35]  John B. Anderson,et al.  Past ice-sheet behaviour: retreat scenarios and changing controls in the Ross Sea, Antarctica , 2016 .

[36]  J. Mangerud,et al.  The last Eurasian ice sheets – a chronological database and time‐slice reconstruction, DATED‐1 , 2016 .

[37]  F. Nitsche,et al.  Palaeo-ice stream pathways and retreat style in the easternmost Amundsen Sea Embayment, West Antarctica, revealed by combined multibeam bathymetric and seismic data , 2015 .

[38]  Haibo Hu,et al.  On the stability of the Atlantic meridional overturning circulation during the last deglaciation , 2015, Climate Dynamics.

[39]  Helmut Rott,et al.  Evolution of surface velocities and ice discharge of Larsen B outlet glaciers from 1995 to 2013 , 2014 .

[40]  E. Berthier,et al.  Detailed ice loss pattern in the northern Antarctic Peninsula: widespread decline driven by ice front retreats , 2014 .

[41]  K. Lambeck,et al.  Sea level and global ice volumes from the Last Glacial Maximum to the Holocene , 2014, Proceedings of the National Academy of Sciences.

[42]  B. Smith,et al.  Marine Ice Sheet Collapse Potentially Under Way for the Thwaites Glacier Basin, West Antarctica , 2014, Science.

[43]  M. Winsborrow,et al.  Ice stream retreat dynamics inferred from an assemblage of landforms in the northern Barents Sea , 2014 .

[44]  Julian A. Dowdeswell,et al.  Ice-sheet grounding-zone wedges (GZWs) on high-latitude continental margins , 2014 .

[45]  D. Menemenlis,et al.  Subaqueous melting of Store Glacier, west Greenland from three‐dimensional, high‐resolution numerical modeling and ocean observations , 2013, Geophysical Research Letters.

[46]  Adrian Jenkins,et al.  Seabed corrugations beneath an Antarctic ice shelf revealed by autonomous underwater vehicle survey: Origin and implications for the history of Pine Island Glacier , 2013 .

[47]  Duncan J. Wingham,et al.  Sustained retreat of the Pine Island Glacier , 2013 .

[48]  Sridhar Anandakrishnan,et al.  Ice-Shelf Tidal Flexure and Subglacial Pressure Variations , 2013 .

[49]  Stewart S. R. Jamieson,et al.  Ice-stream stability on a reverse bed slope , 2012 .

[50]  D. Vaughan,et al.  Antarctic ice-sheet loss driven by basal melting of ice shelves , 2012, Nature.

[51]  C. Schoof Marine ice sheet stability , 2012, Journal of Fluid Mechanics.

[52]  C. Ritz,et al.  Heinrich event 1: an example of dynamical ice-sheet reaction to oceanic changes , 2011 .

[53]  Kelly M. Brunt,et al.  Analysis of ice plains of the Filchner–Ronne Ice Shelf, Antarctica, using ICESat laser altimetry , 2011, Journal of Glaciology.

[54]  P. Clark,et al.  Ice-shelf collapse from subsurface warming as a trigger for Heinrich events , 2011, Proceedings of the National Academy of Sciences.

[55]  Kelly M. Brunt,et al.  Getting around Antarctica: new high-resolution mappings of the grounded and freely-floating boundaries of the Antarctic ice sheet created for the International Polar Year , 2011 .

[56]  Z. Liu,et al.  Transient Simulation of Last Deglaciation with a New Mechanism for Bølling-Allerød Warming , 2009, Science.

[57]  J. Matthiessen,et al.  Re-advance of the Fennoscandian Ice Sheet during Heinrich Event 1 , 2007 .

[58]  Jacques Laskar,et al.  A long-term numerical solution for the insolation quantities of the Earth , 2004 .

[59]  S. Tulaczyk,et al.  A groove-ploughing theory for the production of mega-scale glacial lineations, and implications for ice-stream mechanics , 2003 .

[60]  Eric Rignot,et al.  Ice-shelf changes in Pine Island Bay, Antarctica, 1947-2000 , 2002, Journal of Glaciology.

[61]  Richard Coleman,et al.  A new tide model for the Antarctic ice shelves and seas , 2002, Annals of Glaciology.

[62]  E. Rignot,et al.  Fast recession of a west antarctic glacier , 1998, Science.

[63]  Anders Solheim,et al.  Iceberg scouring and sea bed morphology on the eastern Weddell Sea shelf, Antarctica* , 1989 .

[64]  C. Bentley,et al.  A Model for Holocene Retreat of the West Antarctic Ice Sheet , 1978, Quaternary Research.