Articles | Volume 15, issue 2
https://doi.org/10.5194/gmd-15-617-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-15-617-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The Whole Antarctic Ocean Model (WAOM v1.0): development and evaluation
Institute for Marine and Antarctic Studies, University of Tasmania, Private Bag 129, Hobart, TAS, 7001, Australia
Geography and Spatial Sciences, School of Technology, Environments and Design, University of Tasmania, Hobart, TAS, 7001, Australia
now at: Alfred Wegener Institute, PO Box 120161, 27515 Bremerhaven, Germany
David E. Gwyther
Institute for Marine and Antarctic Studies, University of Tasmania, Private Bag 129, Hobart, TAS, 7001, Australia
Coastal and Regional Oceanography Laboratory, School of Mathematics and Statistics, University of New South Wales, Sydney, NSW, 2052, Australia
Benjamin K. Galton-Fenzi
Australian Antarctic Division, Kingston, TAS, 7050, Australia
Australian Antarctic Program Partnership, Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia
The Australian Centre for Excellence in Antarctic Science, University of Tasmania, Hobart, Australia
Kaitlin A. Naughten
British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, United Kingdom
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Cited
20 citations as recorded by crossref.
- Initial transformation and export of dense shelf water from the Prydz Bay and Cape Darnley regions: A Lagrangian perspective using clustered drifters M. Murakami et al.
- The glacial systems model (GSM) Version 25G L. Tarasov et al.
- Sensitivity of Totten Glacier dynamics to sliding parameterizations and ice shelf basal melt rates Y. Ma et al.
- Seasonal variability in Antarctic ice shelf velocities forced by sea surface height variations C. Mosbeux et al.
- Sensitivity of simulated water mass transformation on the Antarctic shelf to tides, topography and model resolution F. Boeira Dias et al.
- The Antarctic coastal ocean heat budget is dominated by heat loss to land ice melt R. Moorman et al.
- Lagrangian pathways under the Filchner-Ronne Ice Shelf and in the Weddell Sea V. Maderich et al.
- Results of the second Ice Shelf–Ocean Model Intercomparison Project (ISOMIP+) C. Yung et al.
- Multi-model estimate of Antarctic ice-shelf basal mass budget and ocean drivers B. Galton-Fenzi et al.
- The coupled Southern Ocean–Sea ice–Ice shelf Model (SOSIM v1.0): configuration and evaluation C. Liu et al.
- The case for a Framework for UnderStanding Ice-Ocean iNteractions (FUSION) in the Antarctic-Southern Ocean system F. McCormack et al.
- Modelling Antarctic ice shelf basal melt patterns using the one-layer Antarctic model for dynamical downscaling of ice–ocean exchanges (LADDIE v1.0) E. Lambert et al.
- Stratified suppression of turbulence in an ice shelf basal melt parameterisation C. Yung et al.
- Similarities and differences in circulation beneath the Filchner- Ronne and Ross Ice Shelves: A Lagrangian point of view V. Maderich et al.
- How Does the Ocean Melt Antarctic Ice Shelves? M. Rosevear et al.
- Conservation of heat and mass in P-SKRIPS version 1: the coupled atmosphere–ice–ocean model of the Ross Sea A. Malyarenko et al.
- Data initiatives for ocean-driven melt of Antarctic ice shelves S. Cook et al.
- The impact of tides on Antarctic ice shelf melting O. Richter et al.
- Seasonal variability of ocean heat transport and ice-shelf basal melt around Antarctica F. Boeira Dias et al.
- Evaluating an accelerated forcing approach for improving computational efficiency in coupled ice sheet–ocean modelling Q. Zhou et al.
20 citations as recorded by crossref.
- Initial transformation and export of dense shelf water from the Prydz Bay and Cape Darnley regions: A Lagrangian perspective using clustered drifters M. Murakami et al.
- The glacial systems model (GSM) Version 25G L. Tarasov et al.
- Sensitivity of Totten Glacier dynamics to sliding parameterizations and ice shelf basal melt rates Y. Ma et al.
- Seasonal variability in Antarctic ice shelf velocities forced by sea surface height variations C. Mosbeux et al.
- Sensitivity of simulated water mass transformation on the Antarctic shelf to tides, topography and model resolution F. Boeira Dias et al.
- The Antarctic coastal ocean heat budget is dominated by heat loss to land ice melt R. Moorman et al.
- Lagrangian pathways under the Filchner-Ronne Ice Shelf and in the Weddell Sea V. Maderich et al.
- Results of the second Ice Shelf–Ocean Model Intercomparison Project (ISOMIP+) C. Yung et al.
- Multi-model estimate of Antarctic ice-shelf basal mass budget and ocean drivers B. Galton-Fenzi et al.
- The coupled Southern Ocean–Sea ice–Ice shelf Model (SOSIM v1.0): configuration and evaluation C. Liu et al.
- The case for a Framework for UnderStanding Ice-Ocean iNteractions (FUSION) in the Antarctic-Southern Ocean system F. McCormack et al.
- Modelling Antarctic ice shelf basal melt patterns using the one-layer Antarctic model for dynamical downscaling of ice–ocean exchanges (LADDIE v1.0) E. Lambert et al.
- Stratified suppression of turbulence in an ice shelf basal melt parameterisation C. Yung et al.
- Similarities and differences in circulation beneath the Filchner- Ronne and Ross Ice Shelves: A Lagrangian point of view V. Maderich et al.
- How Does the Ocean Melt Antarctic Ice Shelves? M. Rosevear et al.
- Conservation of heat and mass in P-SKRIPS version 1: the coupled atmosphere–ice–ocean model of the Ross Sea A. Malyarenko et al.
- Data initiatives for ocean-driven melt of Antarctic ice shelves S. Cook et al.
- The impact of tides on Antarctic ice shelf melting O. Richter et al.
- Seasonal variability of ocean heat transport and ice-shelf basal melt around Antarctica F. Boeira Dias et al.
- Evaluating an accelerated forcing approach for improving computational efficiency in coupled ice sheet–ocean modelling Q. Zhou et al.
Saved (final revised paper)
Latest update: 30 Apr 2026
Short summary
Here we present an improved model of the Antarctic continental shelf ocean and demonstrate that it is capable of reproducing present-day conditions. The improvements are fundamental and regard the inclusion of tides and ocean eddies. We conclude that the model is well suited to gain new insights into processes that are important for Antarctic ice sheet retreat and global ocean changes. Hence, the model will ultimately help to improve projections of sea level rise and climate change.
Here we present an improved model of the Antarctic continental shelf ocean and demonstrate that...