Articles | Volume 11, issue 1
https://doi.org/10.5194/tc-11-541-2017
© 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-11-541-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Models for polythermal ice sheets and glaciers
University of Oxford, Oxford, UK
Christian Schoof
University of British Columbia, BC, Canada
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Cited
21 citations as recorded by crossref.
- A continuum model for meltwater flow through compacting snow C. Meyer & I. Hewitt 10.5194/tc-11-2799-2017
- A permeameter for temperate ice: first results on permeability sensitivity to grain size J. Fowler & N. Iverson 10.1017/jog.2021.136
- Numerical simulation of basal crevasses of the tidewater glacier with Galerkin least-squares finite element method H. Lee et al. 10.1007/s10665-024-10356-0
- Lubricated viscous gravity currents of power-law fluids. Part 2. Stability analysis L. Leung & K. Kowal 10.1017/jfm.2022.263
- 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
- Landslide Accumulation Ice‐Snow Melting for Thermo‐Hydromechanical Coupling and Numerical Simulation T. Xiong et al. 10.1155/2021/6664213
- Complex motion of Greenland Ice Sheet outlet glaciers with basal temperate ice R. Law et al. 10.1126/sciadv.abq5180
- The role of sliding in ice stream formation C. Schoof & E. Mantelli 10.1098/rspa.2020.0870
- 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
- A model for French-press experiments of dry snow compaction C. Meyer et al. 10.5194/tc-14-1449-2020
- The role of subtemperate slip in thermally driven ice stream margin migration M. Haseloff et al. 10.5194/tc-12-2545-2018
- Meltwater generation in ice stream shear margins: case study in Antarctic ice streams M. Ranganathan et al. 10.1098/rspa.2022.0473
- Extended enthalpy formulations in the Ice-sheet and Sea-level System Model (ISSM) version 4.17: discontinuous conductivity and anisotropic streamline upwind Petrov–Galerkin (SUPG) method M. Rückamp et al. 10.5194/gmd-13-4491-2020
- Complementary Approaches Towards a Universal Model of Glacier Surges Y. Terleth et al. 10.3389/feart.2021.732962
- Distribution of cold and temperate ice and water in glaciers at Nordenskiöld Land, Svalbard, according to data on ground-based radio-echo sounding Y. Macheret et al. 10.2478/bgeo-2019-0016
- A two-dimensional, higher-order, enthalpy-based thermomechanical ice flow model for mountain glaciers and its benchmark experiments Y. Wang et al. 10.1016/j.cageo.2020.104526
- Propagation of Vertical Fractures through Planetary Ice Shells: The Role of Basal Fractures at the Ice–Ocean Interface and Proximal Cracks C. Walker et al. 10.3847/PSJ/ac01ee
- FROSch Preconditioners for Land Ice Simulations of Greenland and Antarctica A. Heinlein et al. 10.1137/21M1395260
- Processes controlling the downstream evolution of ice rheology in glacier shear margins: case study on Rutford Ice Stream, West Antarctica B. MINCHEW et al. 10.1017/jog.2018.47
- Englacial Pore Water Localizes Shear in Temperate Ice Stream Margins M. Haseloff et al. 10.1029/2019JF005399
- Distribution of cold and temperate ice in glaciers on the Nordenskiold Land, Spitsbergen, from ground-based radio-echo sounding Y. Macheret et al. 10.15356/20766734-2019-2-430
20 citations as recorded by crossref.
- A continuum model for meltwater flow through compacting snow C. Meyer & I. Hewitt 10.5194/tc-11-2799-2017
- A permeameter for temperate ice: first results on permeability sensitivity to grain size J. Fowler & N. Iverson 10.1017/jog.2021.136
- Numerical simulation of basal crevasses of the tidewater glacier with Galerkin least-squares finite element method H. Lee et al. 10.1007/s10665-024-10356-0
- Lubricated viscous gravity currents of power-law fluids. Part 2. Stability analysis L. Leung & K. Kowal 10.1017/jfm.2022.263
- 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
- Landslide Accumulation Ice‐Snow Melting for Thermo‐Hydromechanical Coupling and Numerical Simulation T. Xiong et al. 10.1155/2021/6664213
- Complex motion of Greenland Ice Sheet outlet glaciers with basal temperate ice R. Law et al. 10.1126/sciadv.abq5180
- The role of sliding in ice stream formation C. Schoof & E. Mantelli 10.1098/rspa.2020.0870
- 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
- A model for French-press experiments of dry snow compaction C. Meyer et al. 10.5194/tc-14-1449-2020
- The role of subtemperate slip in thermally driven ice stream margin migration M. Haseloff et al. 10.5194/tc-12-2545-2018
- Meltwater generation in ice stream shear margins: case study in Antarctic ice streams M. Ranganathan et al. 10.1098/rspa.2022.0473
- Extended enthalpy formulations in the Ice-sheet and Sea-level System Model (ISSM) version 4.17: discontinuous conductivity and anisotropic streamline upwind Petrov–Galerkin (SUPG) method M. Rückamp et al. 10.5194/gmd-13-4491-2020
- Complementary Approaches Towards a Universal Model of Glacier Surges Y. Terleth et al. 10.3389/feart.2021.732962
- Distribution of cold and temperate ice and water in glaciers at Nordenskiöld Land, Svalbard, according to data on ground-based radio-echo sounding Y. Macheret et al. 10.2478/bgeo-2019-0016
- A two-dimensional, higher-order, enthalpy-based thermomechanical ice flow model for mountain glaciers and its benchmark experiments Y. Wang et al. 10.1016/j.cageo.2020.104526
- Propagation of Vertical Fractures through Planetary Ice Shells: The Role of Basal Fractures at the Ice–Ocean Interface and Proximal Cracks C. Walker et al. 10.3847/PSJ/ac01ee
- FROSch Preconditioners for Land Ice Simulations of Greenland and Antarctica A. Heinlein et al. 10.1137/21M1395260
- Processes controlling the downstream evolution of ice rheology in glacier shear margins: case study on Rutford Ice Stream, West Antarctica B. MINCHEW et al. 10.1017/jog.2018.47
- Englacial Pore Water Localizes Shear in Temperate Ice Stream Margins M. Haseloff et al. 10.1029/2019JF005399
Latest update: 23 Nov 2024
Short summary
Many glaciers contain ice both below and at the melting temperature. Predicting the evolution of temperature and water content in such ice masses is important because they exert a strong control on the flow of the ice. We present two new models to calculate these quantities, demonstrate a number of example numerical calculations, and compare the results with existing methods. The novelty of the new methods is the inclusion of gravity-driven water transport within the ice.
Many glaciers contain ice both below and at the melting temperature. Predicting the evolution...