197 citations as recorded by crossref.

1. Stopping the flood: could we use targeted geoengineering to mitigate sea level rise? M. Wolovick & J. Moore 10.5194/tc-12-2955-2018
2. History of Anvers-Hugo Trough, western Antarctic Peninsula shelf, since the Last Glacial Maximum. Part I: Deglacial history based on new sedimentological and chronological data Z. Roseby et al. 10.1016/j.quascirev.2022.107590
3. Towards modelling of corrugation ridges at ice-sheet grounding lines K. Hogan et al. 10.5194/tc-17-2645-2023
4. Topographic control on the post-LGM grounding zone locations of the West Antarctic Ice Sheet in the Whales Deep Basin, Eastern Ross Sea M. Danielson & P. Bart 10.1016/j.margeo.2018.11.001
5. Modeling the instantaneous response of glaciers after the collapse of the Larsen B Ice Shelf J. De Rydt et al. 10.1002/2015GL064355
6. Glacier-specific factors drive differing seasonal and interannual dynamics of Nunatakassaap Sermia and Illullip Sermia, Greenland J. Carr et al. 10.1080/15230430.2023.2186456
7. Geothermal Heat Flow and Thermal Structure of the Antarctic Lithosphere C. Haeger et al. 10.1029/2022GC010501
8. Mechanisms and Impacts of Earth System Tipping Elements S. Wang et al. 10.1029/2021RG000757
9. Velocity response of Petermann Glacier, northwest Greenland, to past and future calving events E. Hill et al. 10.5194/tc-12-3907-2018
10. Coupling framework (1.0) for the Úa (2023b) ice sheet model and the FESOM-1.4 z-coordinate ocean model in an Antarctic domain O. Richter et al. 10.5194/gmd-18-2945-2025
11. Linear sea-level response to abrupt ocean warming of major West Antarctic ice basin M. Mengel et al. 10.1038/nclimate2808
12. Steep Glacier Bed Knickpoints Mitigate Inland Thinning in Greenland D. Felikson et al. 10.1029/2020GL090112
13. Atmosphere‐ocean‐ice interactions in the Amundsen Sea Embayment, West Antarctica J. Turner et al. 10.1002/2016RG000532
14. Retreat of Pine Island Glacier controlled by marine ice-sheet instability L. Favier et al. 10.1038/nclimate2094
15. Melt sensitivity of irreversible retreat of Pine Island Glacier B. Reed et al. 10.5194/tc-18-4567-2024
16. Submarine landforms reveal varying rates and styles of deglaciation in North-West Greenland fjords C. Batchelor et al. 10.1016/j.margeo.2017.08.003
17. Calibrated sea level contribution from the Amundsen Sea sector, West Antarctica, under RCP8.5 and Paris 2C scenarios S. Rosier et al. 10.5194/tc-19-2527-2025
18. Palaeo-ice stream pathways and retreat style in the easternmost Amundsen Sea Embayment, West Antarctica, revealed by combined multibeam bathymetric and seismic data J. Klages et al. 10.1016/j.geomorph.2015.05.020
19. Subglacial topography and ice flux along the English Coast of Palmer Land, Antarctic Peninsula K. Winter et al. 10.5194/essd-12-3453-2020
20. Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets M. Haseloff & O. Sergienko 10.1017/jog.2022.29
21. Collapse of the Icelandic ice sheet controlled by sea-level rise? H. Norðdahl & Ó. Ingólfsson 10.1007/s41063-015-0020-x
22. The instantaneous impact of calving and thinning on the Larsen C Ice Shelf T. Mitcham et al. 10.5194/tc-16-883-2022
23. The hysteresis of the Antarctic Ice Sheet J. Garbe et al. 10.1038/s41586-020-2727-5
24. Ocean‐Forcing and Glacier‐Specific Factors Drive Differing Glacier Response Across the 69°N Boundary, East Greenland S. Brough et al. 10.1029/2022JF006857
25. Ice front change of marine-terminating outlet glaciers in northwest and southeast Greenland during the 21st century C. BUNCE et al. 10.1017/jog.2018.44
26. A thicker Antarctic ice stream during the mid-Pliocene warm period M. Mas e Braga et al. 10.1038/s43247-023-00983-3
27. 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) F. Pattyn 10.5194/tc-11-1851-2017
28. Damage accelerates ice shelf instability and mass loss in Amundsen Sea Embayment S. Lhermitte et al. 10.1073/pnas.1912890117
29. Trickle and Treat? The Critical Role of Marine‐Terminating Glaciers as Icy Macronutrient Pumps in Polar Regions J. Hawkings 10.1029/2021JG006598
30. Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration B. Miles et al. 10.5194/tc-15-663-2021
31. Out of the Ice Age: Megatides of the Arctic Ocean and the Bølling‐Ållerød, Younger Dryas Transition J. Velay-Vitow & W. Richard Peltier 10.1029/2020GL089870
32. Diagnosing the sensitivity of grounding-line flux to changes in sub-ice-shelf melting T. Zhang et al. 10.5194/tc-14-3407-2020
33. Weak bed control of the eastern shear margin of Thwaites Glacier, West Antarctica J. MacGregor et al. 10.3189/2013JoG13J050
34. Ice dynamics will remain a primary driver of Greenland ice sheet mass loss over the next century Y. Choi et al. 10.1038/s43247-021-00092-z
35. Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum R. Larter et al. 10.1016/j.quascirev.2013.10.016
36. Basal friction of Fleming Glacier, Antarctica – Part 2: Evolution from 2008 to 2015 C. Zhao et al. 10.5194/tc-12-2653-2018
37. Assessment of numerical schemes for transient, finite-element ice flow models using ISSM v4.18 T. dos Santos et al. 10.5194/gmd-14-2545-2021
38. Ice shelf fracture parameterization in an ice sheet model S. Sun et al. 10.5194/tc-11-2543-2017
39. Scaling of instability timescales of Antarctic outlet glaciers based on one-dimensional similitude analysis A. Levermann & J. Feldmann 10.5194/tc-13-1621-2019
40. Sensitivity of the Weddell Sea sector ice streams to sub-shelf melting and surface accumulation A. Wright et al. 10.5194/tc-8-2119-2014
41. Calculations of extreme sea level rise scenarios are strongly dependent on ice sheet model resolution C. Williams et al. 10.1038/s43247-025-02010-z
42. Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica G. GUDMUNDSSON et al. 10.1017/jog.2016.132
43. Timescales of outlet-glacier flow with negligible basal friction: theory, observations and modeling J. Feldmann & A. Levermann 10.5194/tc-17-327-2023
44. The long-term sea-level commitment from Antarctica A. Klose et al. 10.5194/tc-18-4463-2024
45. An improved model for tidally modulated grounding-line migration V. Tsai & G. Gudmundsson 10.3189/2015JoG14J152
46. Stochastic modeling of subglacial topography exposes uncertainty in water routing at Jakobshavn Glacier E. MacKie et al. 10.1017/jog.2020.84
47. The sensitivity of West Antarctica to the submarine melting feedback R. Arthern & C. Williams 10.1002/2017GL072514
48. Slowdown in Antarctic mass loss from solid Earth and sea-level feedbacks E. Larour et al. 10.1126/science.aav7908
49. Predicting ocean-induced ice-shelf melt rates using deep learning S. Rosier et al. 10.5194/tc-17-499-2023
50. Future sea-level rise due to projected ocean warming beneath the Filchner Ronne Ice Shelf: A coupled model study M. Thoma et al. 10.1016/j.epsl.2015.09.013
51. Controls on the early Holocene collapse of the Bothnian Sea Ice Stream C. Clason et al. 10.1002/2016JF004050
52. Dynamic influence of pinning points on marine ice-sheet stability: a numerical study in Dronning Maud Land, East Antarctica L. Favier et al. 10.5194/tc-10-2623-2016
53. Exceptional Retreat of Kangerlussuaq Glacier, East Greenland, Between 2016 and 2018 S. Brough et al. 10.3389/feart.2019.00123
54. Interaction of marine ice-sheet instabilities in two drainage basins: simple scaling of geometry and transition time J. Feldmann & A. Levermann 10.5194/tc-9-631-2015
55. Marine ice-sheet profiles and stability under Coulomb basal conditions V. Tsai et al. 10.3189/2015JoG14J221
56. Hysteretic evolution of ice rises and ice rumples in response to variations in sea level A. Henry et al. 10.5194/tc-16-3889-2022
57. Impact of Fjord Geometry on Grounding Line Stability H. Åkesson et al. 10.3389/feart.2018.00071
58. The stability of present-day Antarctic grounding lines – Part 2: Onset of irreversible retreat of Amundsen Sea glaciers under current climate on centennial timescales cannot be excluded R. Reese et al. 10.5194/tc-17-3761-2023
59. Potential sea-level rise from Antarctic ice-sheet instability constrained by observations C. Ritz et al. 10.1038/nature16147
60. Geometric amplification and suppression of ice-shelf basal melt in West Antarctica J. De Rydt & K. Naughten 10.5194/tc-18-1863-2024
61. Thermal structure and basal sliding parametrisation at Pine Island Glacier – a 3-D full-Stokes model study N. Wilkens et al. 10.5194/tc-9-675-2015
62. Rate of Mass Loss Across the Instability Threshold for Thwaites Glacier Determines Rate of Mass Loss for Entire Basin M. Waibel et al. 10.1002/2017GL076470
63. ATAT 1.1, the Automated Timing Accordance Tool for comparing ice-sheet model output with geochronological data J. Ely et al. 10.5194/gmd-12-933-2019
64. Basal topographic controls on rapid retreat of Humboldt Glacier, northern Greenland J. Carr et al. 10.3189/2015JoG14J128
65. Antarctic sub-shelf melt rates via PICO R. Reese et al. 10.5194/tc-12-1969-2018
66. Improving Bed Topography Mapping of Greenland Glaciers Using NASA’s Oceans Melting Greenland (OMG) Data M. Morlighem et al. 10.5670/oceanog.2016.99
67. Glacial to postglacial submarine landform assemblages in fiords of northeastern Baffin Island E. Brouard & P. Lajeunesse 10.1016/j.geomorph.2019.01.007
68. Ambiguous stability of glaciers at bed peaks A. Robel et al. 10.1017/jog.2022.31
69. Geophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciation H. Patton et al. 10.1002/2015RG000495
70. Glacial landforms reveal dynamic ice-sheet behaviour along the mid-Norwegian margin during the last glacial-deglacial cycle D. Ottesen et al. 10.1016/j.quascirev.2022.107462
71. Exploring mechanisms responsible for tidal modulation in flow of the Filchner–Ronne Ice Shelf S. Rosier & G. Gudmundsson 10.5194/tc-14-17-2020
72. Ice viscosity is more sensitive to stress than commonly assumed J. Millstein et al. 10.1038/s43247-022-00385-x
73. Exceptions to bed-controlled ice sheet flow and retreat from glaciated continental margins worldwide S. Greenwood et al. 10.1126/sciadv.abb6291
74. Changes in ice-shelf buttressing following the collapse of Larsen A Ice Shelf, Antarctica, and the resulting impact on tributaries S. ROYSTON & G. GUDMUNDSSON 10.1017/jog.2016.77
75. Framework for High‐End Estimates of Sea Level Rise for Stakeholder Applications D. Stammer et al. 10.1029/2019EF001163
76. Current state and future perspectives on coupled ice-sheet – sea-level modelling B. de Boer et al. 10.1016/j.quascirev.2017.05.013
77. Boundary layer models for calving marine outlet glaciers C. Schoof et al. 10.5194/tc-11-2283-2017
78. The sensitivity of Cook Glacier, East Antarctica, to changes in ice-shelf extent and grounding-line position J. Jordan et al. 10.1017/jog.2021.106
79. Simulated Twentieth‐Century Ocean Warming in the Amundsen Sea, West Antarctica K. Naughten et al. 10.1029/2021GL094566
80. Ice-sheet mass balance and climate change E. Hanna et al. 10.1038/nature12238
81. Atmosphere-driven ice sheet mass loss paced by topography: Insights from modelling the south-western Scandinavian Ice Sheet H. Åkesson et al. 10.1016/j.quascirev.2018.07.004
82. Bathymetric Control on Borchgrevink and Roi Baudouin Ice Shelves in East Antarctica H. Eisermann et al. 10.1029/2021JF006342
83. Drivers of Change of Thwaites Glacier, West Antarctica, Between 1995 and 2015 T. dos Santos et al. 10.1029/2021GL093102
84. Gapless-REMA100: A gapless 100-m reference elevation model of Antarctica with voids filled by multi-source DEMs Y. Dong et al. 10.1016/j.isprsjprs.2022.01.024
85. Implementation and performance of adaptive mesh refinement in the Ice Sheet System Model (ISSM v4.14) T. dos Santos et al. 10.5194/gmd-12-215-2019
86. Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions M. Petrini et al. 10.1016/j.quascirev.2020.106314
87. A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets B. Bonan et al. 10.5194/tc-10-1-2016
88. Evidence for variable grounding-zone and shear-margin basal conditions across Thwaites Glacier, West Antarctica D. Schroeder et al. 10.1190/geo2015-0122.1
89. Similitude of ice dynamics against scaling of geometry and physical parameters J. Feldmann & A. Levermann 10.5194/tc-10-1753-2016
90. Two-timescale response of a large Antarctic ice shelf to climate change K. Naughten et al. 10.1038/s41467-021-22259-0
91. Exploring grid sensitivity in an ice sheet model: A case study of the Amery Ice Shelf Q. Wang et al. 10.1016/j.accre.2024.12.001
92. Recent progress in understanding climate thresholds P. Good et al. 10.1177/0309133317751843
93. Calving cycle of the Brunt Ice Shelf, Antarctica, driven by changes in ice shelf geometry J. De Rydt et al. 10.5194/tc-13-2771-2019
94. Coupled ice shelf‐ocean modeling and complex grounding line retreat from a seabed ridge J. De Rydt & G. Gudmundsson 10.1002/2015JF003791
95. Twenty-first century response of Petermann Glacier, northwest Greenland to ice shelf loss E. Hill et al. 10.1017/jog.2020.97
96. A watery ice sheet demise: Formation and drainage of ice-dammed lakes in southern Norway during the Early Holocene F. Høgaas et al. 10.1016/j.quascirev.2025.109250
97. Active ice sheet conservation cannot stop the retreat of Sermeq Kujalleq glacier, Greenland L. Zhao et al. 10.1038/s43247-025-02120-8
98. Viscoelastic mechanics of tidally induced lake drainage in the grounding zone H. Zhang et al. 10.5194/tc-19-2087-2025
99. Simulated retreat of Jakobshavn Isbræ since the Little Ice Age controlled by geometry N. Steiger et al. 10.5194/tc-12-2249-2018
100. The far reach of ice-shelf thinning in Antarctica R. Reese et al. 10.1038/s41558-017-0020-x
101. The dynamics of confined extensional flows S. Pegler 10.1017/jfm.2016.516
102. Marine ice sheet dynamics: the impacts of ice-shelf buttressing S. Pegler 10.1017/jfm.2018.741
103. Variational formulation of marine ice-sheet and subglacial-lake grounding-line dynamics A. Stubblefield et al. 10.1017/jfm.2021.394
104. The sensitivity of flowline models of tidewater glaciers to parameter uncertainty E. Enderlin et al. 10.5194/tc-7-1579-2013
105. Anisotropic metric-based mesh adaptation for ice flow modelling in Firedrake D. Dundovic et al. 10.5194/gmd-18-4023-2025
106. Selective erosion beneath the Antarctic Peninsula Ice Sheet during LGM retreat N. Golledge 10.1017/S0954102014000340
107. A Full‐Stokes 3‐D Calving Model Applied to a Large Greenlandic Glacier J. Todd et al. 10.1002/2017JF004349
108. Sensitivity of grounding line dynamics to the choice of the friction law J. BRONDEX et al. 10.1017/jog.2017.51
109. High spatial and temporal variability in Antarctic ice discharge linked to ice shelf buttressing and bed geometry B. Miles et al. 10.1038/s41598-022-13517-2
110. Suppression of marine ice sheet instability S. Pegler 10.1017/jfm.2018.742
111. Eddy and tidal driven basal melting of the Totten and Moscow University ice shelves Y. Xia et al. 10.3389/fmars.2023.1159353
112. Persistence and variability of ice-stream grounding lines on retrograde bed slopes A. Robel et al. 10.5194/tc-10-1883-2016
113. Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations D. Docquier et al. 10.3189/2014JoG13J117
114. Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica B. MINCHEW et al. 10.1017/jog.2018.24
115. Inequality-constrained free-surface evolution in a full Stokes ice flow model (evolve_glacier v1.1) A. Wirbel & A. Jarosch 10.5194/gmd-13-6425-2020
116. From cyclic ice streaming to Heinrich-like events: the grow-and-surge instability in the Parallel Ice Sheet Model J. Feldmann & A. Levermann 10.5194/tc-11-1913-2017
117. Basal conditions of two Transantarctic Mountains outlet glaciers from observation-constrained diagnostic modelling N. Golledge et al. 10.3189/2014JoG13J131
118. Experimental design for three interrelated marine ice sheet and ocean model intercomparison projects: MISMIP v. 3 (MISMIP +), ISOMIP v. 2 (ISOMIP +) and MISOMIP v. 1 (MISOMIP1) X. Asay-Davis et al. 10.5194/gmd-9-2471-2016
119. Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks M. Wise et al. 10.1038/nature24458
120. Present day Jakobshavn Isbræ (West Greenland) close to the Holocene minimum extent K. Kajanto et al. 10.1016/j.quascirev.2020.106492
121. Assessment of sub-shelf melting parameterisations using the ocean–ice-sheet coupled model NEMO(v3.6)–Elmer/Ice(v8.3) L. Favier et al. 10.5194/gmd-12-2255-2019
122. Inferred basal friction and mass flux affected by crystal-orientation fabrics N. Rathmann & D. Lilien 10.1017/jog.2021.88
123. Monitoring the Multiple Stages of Climate Tipping Systems from Space: Do the GCOS Essential Climate Variables Meet the Needs? S. Loriani et al. 10.1007/s10712-024-09866-4
124. Geometric controls of tidewater glacier dynamics T. Frank et al. 10.5194/tc-16-581-2022
125. Early Warning from Space for a Few Key Tipping Points in Physical, Biological, and Social-Ecological Systems D. Swingedouw et al. 10.1007/s10712-020-09604-6
126. Temperate ice in the shear margins of the Antarctic Ice Sheet: Controlling processes and preliminary locations C. Meyer & B. Minchew 10.1016/j.epsl.2018.06.028
127. Retreat of Thwaites Glacier, West Antarctica, over the next 100 years using various ice flow models, ice shelf melt scenarios and basal friction laws H. Yu et al. 10.5194/tc-12-3861-2018
128. Rapid Thinning of Pine Island Glacier in the Early Holocene J. Johnson et al. 10.1126/science.1247385
129. Pervasive glacier retreats across Svalbard from 1985 to 2023 T. Li et al. 10.1038/s41467-025-55948-1
130. Diverse behaviors of marine ice sheets in response to temporal variability of the atmospheric and basal conditions O. Sergienko & D. Wingham 10.1017/jog.2024.43
131. Seven decades of uninterrupted advance of Good Friday Glacier, Axel Heiberg Island, Arctic Canada D. MEDRZYCKA et al. 10.1017/jog.2019.21
132. High sensitivity of tidewater outlet glacier dynamics to shape E. Enderlin et al. 10.5194/tc-7-1007-2013
133. Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years J. Jordan et al. 10.1038/s41467-023-37553-2
134. Present-day mass loss rates are a precursor for West Antarctic Ice Sheet collapse T. van den Akker et al. 10.5194/tc-19-283-2025
135. Modelling calving front dynamics using a level-set method: application to Jakobshavn Isbræ, West Greenland J. Bondzio et al. 10.5194/tc-10-497-2016
136. Sill-Influenced Exchange Flows in Ice Shelf Cavities K. Zhao et al. 10.1175/JPO-D-18-0076.1
137. Sea-Level Rise: From Global Perspectives to Local Services G. Durand et al. 10.3389/fmars.2021.709595
138. Thwaites Glacier thins and retreats fastest where ice-shelf channels intersect its grounding zone A. Chartrand et al. 10.5194/tc-18-4971-2024
139. Emulating Present and Future Simulations of Melt Rates at the Base of Antarctic Ice Shelves With Neural Networks C. Burgard et al. 10.1029/2023MS003829
140. Evidence for multiple Quaternary ice advances and fan development from the Amundsen Gulf cross-shelf trough and slope, Canadian Beaufort Sea margin C. Batchelor et al. 10.1016/j.marpetgeo.2013.11.005
141. Interplay of grounding-line dynamics and sub-shelf melting during retreat of the Bjørnøyrenna Ice Stream M. Petrini et al. 10.1038/s41598-018-25664-6
142. Basal Melting, Roughness and Structural Integrity of Ice Shelves R. Larter 10.1029/2021GL097421
143. Weak relationship between remotely detected crevasses and inferred ice rheological parameters on Antarctic ice shelves C. Gerli et al. 10.5194/tc-18-2677-2024
144. Flow dynamics of Byrd Glacier, East Antarctica C. Van Der Veen et al. 10.3189/2014JoG14J052
145. Reducing uncertainties in projections of Antarctic ice mass loss G. Durand & F. Pattyn 10.5194/tc-9-2043-2015
146. Internal dynamics condition centennial-scale oscillations in marine-based ice-stream retreat R. Smedley et al. 10.1130/G38991.1
147. Activation of Existing Surface Crevasses Has Limited Impact on Grounding Line Flux of Antarctic Ice Streams C. Gerli et al. 10.1029/2022GL101687
148. Antarctic ice rise formation, evolution, and stability L. Favier & F. Pattyn 10.1002/2015GL064195
149. Shear-margin melting causes stronger transient ice discharge than ice-stream melting in idealized simulations J. Feldmann et al. 10.5194/tc-16-1927-2022
150. Projecting Antarctica's contribution to future sea level rise from basal ice shelf melt using linear response functions of 16 ice sheet models (LARMIP-2) A. Levermann et al. 10.5194/esd-11-35-2020
151. Brief communication: Impact of mesh resolution for MISMIP and MISMIP3d experiments using Elmer/Ice O. Gagliardini et al. 10.5194/tc-10-307-2016
152. Intermittent structural weakening and acceleration of the Thwaites Glacier Tongue between 2000 and 2018 B. Miles et al. 10.1017/jog.2020.20
153. On the reconstruction of palaeo-ice sheets: Recent advances and future challenges C. Stokes et al. 10.1016/j.quascirev.2015.07.016
154. Grounding-line migration in plan-view marine ice-sheet models: results of the ice2sea MISMIP3d intercomparison F. Pattyn et al. 10.3189/2013JoG12J129
155. The Bothnian Sea ice stream: early Holocene retreat dynamics of the south‐central Fennoscandian Ice Sheet S. Greenwood et al. 10.1111/bor.12217
156. FastIsostasy v1.0 – a regional, accelerated 2D glacial isostatic adjustment (GIA) model accounting for the lateral variability of the solid Earth J. Swierczek-Jereczek et al. 10.5194/gmd-17-5263-2024
157. Detecting high spatial variability of ice shelf basal mass balance, Roi Baudouin Ice Shelf, Antarctica S. Berger et al. 10.5194/tc-11-2675-2017
158. Physical processes and feedbacks obscuring the future of the Antarctic Ice Sheet D. Li 10.1016/j.geogeo.2022.100084
159. Progress in Numerical Modeling of Antarctic Ice-Sheet Dynamics F. Pattyn et al. 10.1007/s40641-017-0069-7
160. Marine outlet glacier dynamics, steady states and steady-state stability O. Sergienko 10.1017/jog.2022.13
161. Sensitivity to forecast surface mass balance outweighs sensitivity to basal sliding descriptions for 21st century mass loss from three major Greenland outlet glaciers J. Carr et al. 10.5194/tc-18-2719-2024
162. An Overview of Interactions and Feedbacks Between Ice Sheets and the Earth System J. Fyke et al. 10.1029/2018RG000600
163. Dynamic response of Antarctic ice shelves to bedrock uncertainty S. Sun et al. 10.5194/tc-8-1561-2014
164. Strong Sensitivity of Pine Island Ice-Shelf Melting to Climatic Variability P. Dutrieux et al. 10.1126/science.1244341
165. Helheim Glacier Poised for Dramatic Retreat J. Williams et al. 10.1029/2021GL094546
166. Neutral equilibrium and forcing feedbacks in marine ice sheet modelling R. Gladstone et al. 10.5194/tc-12-3605-2018
167. Grounding-line flux conditions for marine ice-sheet systems under effective-pressure- dependent and hybrid friction laws T. Gregov et al. 10.1017/jfm.2023.760
168. Sensitivity of centennial mass loss projections of the Amundsen basin to the friction law J. Brondex et al. 10.5194/tc-13-177-2019
169. Grounding line retreat of Pope, Smith, and Kohler Glaciers, West Antarctica, measured with Sentinel‐1a radar interferometry data B. Scheuchl et al. 10.1002/2016GL069287
170. Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) S. Cornford et al. 10.5194/tc-14-2283-2020
171. An assessment of basal melt parameterisations for Antarctic ice shelves C. Burgard et al. 10.5194/tc-16-4931-2022
172. The tipping points and early warning indicators for Pine Island Glacier, West Antarctica S. Rosier et al. 10.5194/tc-15-1501-2021
173. Hysteresis of idealized, instability-prone outlet glaciers in response to pinning-point buttressing variation J. Feldmann et al. 10.5194/tc-18-4011-2024
174. The long future of Antarctic melting A. Robel 10.1038/526327a
175. A new approach to inferring basal drag and ice rheology in ice streams, with applications to West Antarctic Ice Streams M. Ranganathan et al. 10.1017/jog.2020.95
176. The effect of buttressing on grounding line dynamics M. HASELOFF & O. SERGIENKO 10.1017/jog.2018.30
177. Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves C. Schannwell et al. 10.5194/tc-12-2307-2018
178. Ice-stream demise dynamically conditioned by trough shape and bed strength T. Bradwell et al. 10.1126/sciadv.aau1380
179. Simulated dynamic regrounding during marine ice sheet retreat L. Jong et al. 10.5194/tc-12-2425-2018
180. Quantifying the potential future contribution to global mean sea level from the Filchner–Ronne basin, Antarctica E. Hill et al. 10.5194/tc-15-4675-2021
181. Understanding controls on rapid ice‐stream retreat during the last deglaciation of Marguerite Bay, Antarctica, using a numerical model S. Jamieson et al. 10.1002/2013JF002934
182. Grounding-line flux formula applied as a flux condition in numerical simulations fails for buttressed Antarctic ice streams R. Reese et al. 10.5194/tc-12-3229-2018
183. Recent irreversible retreat phase of Pine Island Glacier B. Reed et al. 10.1038/s41558-023-01887-y
184. Nunataks as barriers to ice flow: implications for palaeo ice sheet reconstructions M. Mas e Braga et al. 10.5194/tc-15-4929-2021
185. Tidally induced variations in vertical and horizontal motion on Rutford Ice Stream, West Antarctica, inferred from remotely sensed observations B. Minchew et al. 10.1002/2016JF003971
186. Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica J. De Rydt et al. 10.5194/tc-12-505-2018
187. Representation of basal melting at the grounding line in ice flow models H. Seroussi & M. Morlighem 10.5194/tc-12-3085-2018
188. The stability of present-day Antarctic grounding lines – Part 1: No indication of marine ice sheet instability in the current geometry E. Hill et al. 10.5194/tc-17-3739-2023
189. Drivers of Pine Island Glacier speed-up between 1996 and 2016 J. De Rydt et al. 10.5194/tc-15-113-2021
190. A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats J. Christian et al. 10.5194/tc-16-2725-2022
191. A High‐End Estimate of Sea Level Rise for Practitioners R. van de Wal et al. 10.1029/2022EF002751
192. Response of Marine‐Terminating Glaciers to Forcing: Time Scales, Sensitivities, Instabilities, and Stochastic Dynamics A. Robel et al. 10.1029/2018JF004709
193. A 3-D coupled ice sheet – sea level model applied to Antarctica through the last 40 ky N. Gomez et al. 10.1016/j.epsl.2013.09.042
194. Recent progress in understanding marine-terminating Arctic outlet glacier response to climatic and oceanic forcing J. Carr et al. 10.1177/0309133313483163
195. Ice-shelf buttressing and the stability of marine ice sheets G. Gudmundsson 10.5194/tc-7-647-2013
196. Ice-sheet grounding-zone wedges (GZWs) on high-latitude continental margins C. Batchelor & J. Dowdeswell 10.1016/j.margeo.2015.02.001
197. Description of a hybrid ice sheet-shelf model, and application to Antarctica D. Pollard & R. DeConto 10.5194/gmd-5-1273-2012