Articles | Volume 12, issue 11
https://doi.org/10.5194/tc-12-3635-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-12-3635-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Marine ice sheet instability and ice shelf buttressing of the Minch Ice Stream, northwest Scotland
School of Earth and Environment, University of Leeds, Leeds, LS2
9JT, UK
Lauren J. Gregoire
School of Earth and Environment, University of Leeds, Leeds, LS2
9JT, UK
Jeremy C. Ely
Department of Geography, University of Sheffield, Sheffield, S10
2TN, UK
Christopher D. Clark
Department of Geography, University of Sheffield, Sheffield, S10
2TN, UK
David M. Hodgson
School of Earth and Environment, University of Leeds, Leeds, LS2
9JT, UK
Victoria Lee
School of Geographical Sciences, University of Bristol, Bristol,
BS8 1SS, UK
Tom Bradwell
Biological and Environmental Sciences, University of Stirling,
Stirling, FK9 4LA, UK
Ruza F. Ivanovic
School of Earth and Environment, University of Leeds, Leeds, LS2
9JT, UK
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24 citations as recorded by crossref.
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- Proglacial Lakes Control Glacier Geometry and Behavior During Recession J. Sutherland et al. 10.1029/2020GL088865
- Surface mass balance and climate of the Last Glacial Maximum Northern Hemisphere ice sheets: simulations with CESM2.1 S. Bradley et al. 10.5194/cp-20-211-2024
- Nonlinear climate dynamics: From deterministic behaviour to stochastic excitability and chaos D. Alexandrov et al. 10.1016/j.physrep.2020.11.002
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- A litho-tectonic event stratigraphy from dynamic Late Devensian ice flow of the North Sea Lobe, Tunstall, east Yorkshire, UK J. Sutherland et al. 10.1016/j.pgeola.2020.03.001
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- Simulating the Early Holocene demise of the Laurentide Ice Sheet with BISICLES (public trunk revision 3298) I. Matero et al. 10.5194/gmd-13-4555-2020
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- Interaction of multiple ice streams on the Malin Shelf during deglaciation of the last British–Irish Ice Sheet K. Craven et al. 10.1002/jqs.3266
- Pattern, style and timing of British–Irish Ice Sheet advance and retreat over the last 45 000 years: evidence from NW Scotland and the adjacent continental shelf T. Bradwell et al. 10.1002/jqs.3296
- Complexities in interpreting chironomid-based temperature reconstructions over the Holocene from a lake in Western Ireland M. McKeown et al. 10.1016/j.quascirev.2019.105908
- Relative importance of the mechanisms triggering the Eurasian ice sheet deglaciation in the GRISLI2.0 ice sheet model V. van Aalderen et al. 10.5194/cp-20-187-2024
- Exploring the ingredients required to successfully model the placement, generation, and evolution of ice streams in the British-Irish Ice Sheet N. Gandy et al. 10.1016/j.quascirev.2019.105915
- Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet J. Ely et al. 10.1002/jqs.3098
- Timing, pace and controls on ice sheet retreat: an introduction to the BRITICE‐CHRONO transect reconstructions of the British–Irish Ice Sheet C. Clark et al. 10.1002/jqs.3326
- Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction C. Clark et al. 10.1111/bor.12594
- Large-ensemble simulations of the North American and Greenland ice sheets at the Last Glacial Maximum with a coupled atmospheric general circulation–ice sheet model S. Sherriff-Tadano et al. 10.5194/cp-20-1489-2024
- Left High and Dry: Deglaciation of Dogger Bank, North Sea, Recorded in Proglacial Lake Evolution A. Emery et al. 10.3389/feart.2019.00234
- De‐Tuning Albedo Parameters in a Coupled Climate Ice Sheet Model to Simulate the North American Ice Sheet at the Last Glacial Maximum N. Gandy et al. 10.1029/2023JF007250
22 citations as recorded by crossref.
- Investigating the roles of relative sea-level change and glacio-isostatic adjustment on the retreat of a marine based ice stream in NW Scotland A. Simms et al. 10.1016/j.quascirev.2021.107366
- Quantifying the uncertainty in the Eurasian ice-sheet geometry at the Penultimate Glacial Maximum (Marine Isotope Stage 6) O. Pollard et al. 10.5194/tc-17-4751-2023
- Ice-stream demise dynamically conditioned by trough shape and bed strength T. Bradwell et al. 10.1126/sciadv.aau1380
- Proglacial Lakes Control Glacier Geometry and Behavior During Recession J. Sutherland et al. 10.1029/2020GL088865
- Surface mass balance and climate of the Last Glacial Maximum Northern Hemisphere ice sheets: simulations with CESM2.1 S. Bradley et al. 10.5194/cp-20-211-2024
- Nonlinear climate dynamics: From deterministic behaviour to stochastic excitability and chaos D. Alexandrov et al. 10.1016/j.physrep.2020.11.002
- Exploring the extent to which fluctuations in ice‐rafted debris reflect mass changes in the source ice sheet: a model–observation comparison using the last British–Irish Ice Sheet D. Wilton et al. 10.1002/jqs.3273
- Collapse of the Last Eurasian Ice Sheet in the North Sea Modulated by Combined Processes of Ice Flow, Surface Melt, and Marine Ice Sheet Instabilities N. Gandy et al. 10.1029/2020JF005755
- A litho-tectonic event stratigraphy from dynamic Late Devensian ice flow of the North Sea Lobe, Tunstall, east Yorkshire, UK J. Sutherland et al. 10.1016/j.pgeola.2020.03.001
- Behavioural tendencies of the last British–Irish Ice Sheet revealed by data–model comparison J. Ely et al. 10.1002/jqs.3628
- Simulating the Early Holocene demise of the Laurentide Ice Sheet with BISICLES (public trunk revision 3298) I. Matero et al. 10.5194/gmd-13-4555-2020
- Using bed-roughness signatures to characterise glacial landform assemblages beneath palaeo-ice sheets F. Falcini et al. 10.1017/jog.2021.122
- Cordilleran Ice Sheet Stability During the Last Deglaciation C. Darvill et al. 10.1029/2021GL097191
- Interaction of multiple ice streams on the Malin Shelf during deglaciation of the last British–Irish Ice Sheet K. Craven et al. 10.1002/jqs.3266
- Pattern, style and timing of British–Irish Ice Sheet advance and retreat over the last 45 000 years: evidence from NW Scotland and the adjacent continental shelf T. Bradwell et al. 10.1002/jqs.3296
- Complexities in interpreting chironomid-based temperature reconstructions over the Holocene from a lake in Western Ireland M. McKeown et al. 10.1016/j.quascirev.2019.105908
- Relative importance of the mechanisms triggering the Eurasian ice sheet deglaciation in the GRISLI2.0 ice sheet model V. van Aalderen et al. 10.5194/cp-20-187-2024
- Exploring the ingredients required to successfully model the placement, generation, and evolution of ice streams in the British-Irish Ice Sheet N. Gandy et al. 10.1016/j.quascirev.2019.105915
- Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet J. Ely et al. 10.1002/jqs.3098
- Timing, pace and controls on ice sheet retreat: an introduction to the BRITICE‐CHRONO transect reconstructions of the British–Irish Ice Sheet C. Clark et al. 10.1002/jqs.3326
- Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction C. Clark et al. 10.1111/bor.12594
- Large-ensemble simulations of the North American and Greenland ice sheets at the Last Glacial Maximum with a coupled atmospheric general circulation–ice sheet model S. Sherriff-Tadano et al. 10.5194/cp-20-1489-2024
2 citations as recorded by crossref.
- Left High and Dry: Deglaciation of Dogger Bank, North Sea, Recorded in Proglacial Lake Evolution A. Emery et al. 10.3389/feart.2019.00234
- De‐Tuning Albedo Parameters in a Coupled Climate Ice Sheet Model to Simulate the North American Ice Sheet at the Last Glacial Maximum N. Gandy et al. 10.1029/2023JF007250
Latest update: 14 Nov 2024
Short summary
We use the deglaciation of the last British–Irish Ice Sheet as a valuable case to examine the processes of contemporary ice sheet change, using an ice sheet model to simulate the Minch Ice Stream. We find that ice shelves were a control on retreat and that the Minch Ice Stream was vulnerable to the same marine mechanisms which threaten the future of the West Antarctic Ice Sheet. This demonstrates the importance of marine processes when projecting the future of our contemporary ice sheets.
We use the deglaciation of the last British–Irish Ice Sheet as a valuable case to examine the...