Articles | Volume 11, issue 5
https://doi.org/10.5194/tc-11-2283-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-11-2283-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| Highlight paper
| 
05 Oct 2017
Research article | Highlight paper |
| 05 Oct 2017
Boundary layer models for calving marine outlet glaciers
Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2020–2207 Main Mall, Vancouver, BC, V6T 1Z4, Canada
Andrew D. Davis
Department of Aeronautical Engineering, Massachusetts Institute of Technology,
Cambridge, MA, USA
Tiberiu V. Popa
Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2020–2207 Main Mall, Vancouver, BC, V6T 1Z4, Canada
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Cited
29 citations as recorded by crossref.
- Future Evolution of Greenland's Marine‐Terminating Outlet Glaciers G. Catania et al. 10.1029/2018JF004873
- Ocean‐Forcing and Glacier‐Specific Factors Drive Differing Glacier Response Across the 69°N Boundary, East Greenland S. Brough et al. 10.1029/2022JF006857
- Geometric controls of tidewater glacier dynamics T. Frank et al. 10.5194/tc-16-581-2022
- 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
- Marine outlet glacier dynamics, steady states and steady-state stability O. Sergienko 10.1017/jog.2022.13
- No general stability conditions for marine ice-sheet grounding lines in the presence of feedbacks O. Sergienko 10.1038/s41467-022-29892-3
- Rapid retreat of a Scandinavian marine outlet glacier in response to warming at the last glacial termination H. Åkesson et al. 10.1016/j.quascirev.2020.106645
- 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
- Modeling the response of Greenland outlet glaciers to global warming using a coupled flow line–plume model J. Beckmann et al. 10.5194/tc-13-2281-2019
- Suppression of marine ice sheet instability S. Pegler 10.1017/jfm.2018.742
- The Relative Impacts of Initialization and Climate Forcing in Coupled Ice Sheet‐Ocean Modeling: Application to Pope, Smith, and Kohler Glaciers D. Goldberg & P. Holland 10.1029/2021JF006570
- The effect of hydrology and crevasse wall contact on calving M. Zarrinderakht et al. 10.5194/tc-16-4491-2022
- 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
- Impact of Fjord Geometry on Grounding Line Stability H. Åkesson et al. 10.3389/feart.2018.00071
- Bed topography and marine ice-sheet stability O. Sergienko & D. Wingham 10.1017/jog.2021.79
- Marine ice sheet dynamics: the impacts of ice-shelf buttressing S. Pegler 10.1017/jfm.2018.741
- 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
- Hydraulic suppression of basal glacier melt in sill fjords J. Nilsson et al. 10.5194/tc-17-2455-2023
- The Case for a Sustained Greenland Ice Sheet-Ocean Observing System (GrIOOS) F. Straneo et al. 10.3389/fmars.2019.00138
- Twenty-first century response of Petermann Glacier, northwest Greenland to ice shelf loss E. Hill et al. 10.1017/jog.2020.97
- Velocity response of Petermann Glacier, northwest Greenland, to past and future calving events E. Hill et al. 10.5194/tc-12-3907-2018
- Uncertainty quantification of the multi-centennial response of the Antarctic ice sheet to climate change K. Bulthuis et al. 10.5194/tc-13-1349-2019
- AMOC Stabilization Under the Interaction With Tipping Polar Ice Sheets S. Sinet et al. 10.1029/2022GL100305
- 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
- ‘Stable’ and ‘unstable’ are not useful descriptions of marine ice sheets in the Earth's climate system O. Sergienko & M. Haseloff 10.1017/jog.2023.40
- The role of sliding in ice stream formation C. Schoof & E. Mantelli 10.1098/rspa.2020.0870
- Timescales of outlet-glacier flow with negligible basal friction: theory, observations and modeling J. Feldmann & A. Levermann 10.5194/tc-17-327-2023
- Simulated retreat of Jakobshavn Isbræ since the Little Ice Age controlled by geometry N. Steiger et al. 10.5194/tc-12-2249-2018
- Response of Marine‐Terminating Glaciers to Forcing: Time Scales, Sensitivities, Instabilities, and Stochastic Dynamics A. Robel et al. 10.1029/2018JF004709
28 citations as recorded by crossref.
- Future Evolution of Greenland's Marine‐Terminating Outlet Glaciers G. Catania et al. 10.1029/2018JF004873
- Ocean‐Forcing and Glacier‐Specific Factors Drive Differing Glacier Response Across the 69°N Boundary, East Greenland S. Brough et al. 10.1029/2022JF006857
- Geometric controls of tidewater glacier dynamics T. Frank et al. 10.5194/tc-16-581-2022
- 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
- Marine outlet glacier dynamics, steady states and steady-state stability O. Sergienko 10.1017/jog.2022.13
- No general stability conditions for marine ice-sheet grounding lines in the presence of feedbacks O. Sergienko 10.1038/s41467-022-29892-3
- Rapid retreat of a Scandinavian marine outlet glacier in response to warming at the last glacial termination H. Åkesson et al. 10.1016/j.quascirev.2020.106645
- 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
- Modeling the response of Greenland outlet glaciers to global warming using a coupled flow line–plume model J. Beckmann et al. 10.5194/tc-13-2281-2019
- Suppression of marine ice sheet instability S. Pegler 10.1017/jfm.2018.742
- The Relative Impacts of Initialization and Climate Forcing in Coupled Ice Sheet‐Ocean Modeling: Application to Pope, Smith, and Kohler Glaciers D. Goldberg & P. Holland 10.1029/2021JF006570
- The effect of hydrology and crevasse wall contact on calving M. Zarrinderakht et al. 10.5194/tc-16-4491-2022
- 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
- Impact of Fjord Geometry on Grounding Line Stability H. Åkesson et al. 10.3389/feart.2018.00071
- Bed topography and marine ice-sheet stability O. Sergienko & D. Wingham 10.1017/jog.2021.79
- Marine ice sheet dynamics: the impacts of ice-shelf buttressing S. Pegler 10.1017/jfm.2018.741
- 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
- Hydraulic suppression of basal glacier melt in sill fjords J. Nilsson et al. 10.5194/tc-17-2455-2023
- The Case for a Sustained Greenland Ice Sheet-Ocean Observing System (GrIOOS) F. Straneo et al. 10.3389/fmars.2019.00138
- Twenty-first century response of Petermann Glacier, northwest Greenland to ice shelf loss E. Hill et al. 10.1017/jog.2020.97
- Velocity response of Petermann Glacier, northwest Greenland, to past and future calving events E. Hill et al. 10.5194/tc-12-3907-2018
- Uncertainty quantification of the multi-centennial response of the Antarctic ice sheet to climate change K. Bulthuis et al. 10.5194/tc-13-1349-2019
- AMOC Stabilization Under the Interaction With Tipping Polar Ice Sheets S. Sinet et al. 10.1029/2022GL100305
- 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
- ‘Stable’ and ‘unstable’ are not useful descriptions of marine ice sheets in the Earth's climate system O. Sergienko & M. Haseloff 10.1017/jog.2023.40
- The role of sliding in ice stream formation C. Schoof & E. Mantelli 10.1098/rspa.2020.0870
- Timescales of outlet-glacier flow with negligible basal friction: theory, observations and modeling J. Feldmann & A. Levermann 10.5194/tc-17-327-2023
- Simulated retreat of Jakobshavn Isbræ since the Little Ice Age controlled by geometry N. Steiger et al. 10.5194/tc-12-2249-2018
Saved (final revised paper)
Latest update: 19 Apr 2024
Short summary
We show mathematically and computationally how discharge of ice from ocean-terminating glaciers is controlled by a combination of different forces acting on ice near the grounding line of a glacier and how that combination of forces is affected by the process of iceberg formation, which limits the length of floating ice tongues extending in front of the glacier. We show that a deeper fjord may lead to a longer ice tongue providing greater drag on the glacier, slowing the rate of ice discharge.
We show mathematically and computationally how discharge of ice from ocean-terminating glaciers...
