Ablation of sloping ice faces into polar seawater
The effects of the slope of an ice–seawater interface on the mechanisms and rate of ablation of the ice by natural convection are examined using turbulence-resolving simulations. Solutions are obtained for ice slopes ???? , at a fixed ambient salinity and temperature, chosen to represent common Anta...
Published in: | Journal of Fluid Mechanics |
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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/196871 2024-01-14T10:02:04+01:00 Ablation of sloping ice faces into polar seawater Mondal, Mainak Gayen, Bishakhdatta Griffiths, Ross Kerr, Ross application/pdf http://hdl.handle.net/1885/196871 https://doi.org/10.1017/jfm.2018.970 https://openresearch-repository.anu.edu.au/bitstream/1885/196871/6/ablation_sloping_iceface_mainak.pdf.jpg en_AU eng Cambridge University Press http://purl.org/au-research/grants/arc/DP120102772 http://purl.org/au-research/grants/arc/DP120102744 http://purl.org/au-research/grants/arc/DE140100089 0022-1120 http://hdl.handle.net/1885/196871 doi:10.1017/jfm.2018.970 https://openresearch-repository.anu.edu.au/bitstream/1885/196871/6/ablation_sloping_iceface_mainak.pdf.jpg © 2019 Cambridge University Press Journal of Fluid Mechanics buoyant boundary layers ice sheets turbulent convection Journal article ftanucanberra https://doi.org/10.1017/jfm.2018.970 2023-12-15T09:38:47Z The effects of the slope of an ice–seawater interface on the mechanisms and rate of ablation of the ice by natural convection are examined using turbulence-resolving simulations. Solutions are obtained for ice slopes ???? , at a fixed ambient salinity and temperature, chosen to represent common Antarctic ocean conditions. For laminar boundary layers the ablation rate decreases with height, whereas in the turbulent regime the ablation rate is found to be height independent. The simulated laminar ablation rates scale with ???? , whereas in the turbulent regime it follows a ???? scaling, both consistent with the theoretical predictions developed here. The reduction in the ablation rate with shallower slopes arises as a result of the development of stable density stratification beneath the ice face, which reduces turbulent buoyancy fluxes to the ice. The turbulent kinetic energy budget of the flow shows that, for very steep slopes, both buoyancy and shear production are drivers of turbulence, whereas for shallower slopes shear production becomes the dominant mechanism for sustaining turbulence in the convective boundary layer. Computations were carried out using the Australian National Computational Infrastructure, through the National Computational Merit Allocation Scheme supported Ablation of a sloping ice face 569 by the Australian Government. This work was supported by Australian Research Council grants DP120102772 and DP120102744. B.G. was supported by ARC DECRA Fellowship DE140100089 and an Australian Antarctic Division RJL Hawk Fellowship to B.G. Article in Journal/Newspaper Antarc* Antarctic Antarctic Ocean Australian Antarctic Division Australian National University: ANU Digital Collections Antarctic Antarctic Ocean Journal of Fluid Mechanics 863 545 571 |
institution |
Open Polar |
collection |
Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
English |
topic |
buoyant boundary layers ice sheets turbulent convection |
spellingShingle |
buoyant boundary layers ice sheets turbulent convection Mondal, Mainak Gayen, Bishakhdatta Griffiths, Ross Kerr, Ross Ablation of sloping ice faces into polar seawater |
topic_facet |
buoyant boundary layers ice sheets turbulent convection |
description |
The effects of the slope of an ice–seawater interface on the mechanisms and rate of ablation of the ice by natural convection are examined using turbulence-resolving simulations. Solutions are obtained for ice slopes ???? , at a fixed ambient salinity and temperature, chosen to represent common Antarctic ocean conditions. For laminar boundary layers the ablation rate decreases with height, whereas in the turbulent regime the ablation rate is found to be height independent. The simulated laminar ablation rates scale with ???? , whereas in the turbulent regime it follows a ???? scaling, both consistent with the theoretical predictions developed here. The reduction in the ablation rate with shallower slopes arises as a result of the development of stable density stratification beneath the ice face, which reduces turbulent buoyancy fluxes to the ice. The turbulent kinetic energy budget of the flow shows that, for very steep slopes, both buoyancy and shear production are drivers of turbulence, whereas for shallower slopes shear production becomes the dominant mechanism for sustaining turbulence in the convective boundary layer. Computations were carried out using the Australian National Computational Infrastructure, through the National Computational Merit Allocation Scheme supported Ablation of a sloping ice face 569 by the Australian Government. This work was supported by Australian Research Council grants DP120102772 and DP120102744. B.G. was supported by ARC DECRA Fellowship DE140100089 and an Australian Antarctic Division RJL Hawk Fellowship to B.G. |
format |
Article in Journal/Newspaper |
author |
Mondal, Mainak Gayen, Bishakhdatta Griffiths, Ross Kerr, Ross |
author_facet |
Mondal, Mainak Gayen, Bishakhdatta Griffiths, Ross Kerr, Ross |
author_sort |
Mondal, Mainak |
title |
Ablation of sloping ice faces into polar seawater |
title_short |
Ablation of sloping ice faces into polar seawater |
title_full |
Ablation of sloping ice faces into polar seawater |
title_fullStr |
Ablation of sloping ice faces into polar seawater |
title_full_unstemmed |
Ablation of sloping ice faces into polar seawater |
title_sort |
ablation of sloping ice faces into polar seawater |
publisher |
Cambridge University Press |
url |
http://hdl.handle.net/1885/196871 https://doi.org/10.1017/jfm.2018.970 https://openresearch-repository.anu.edu.au/bitstream/1885/196871/6/ablation_sloping_iceface_mainak.pdf.jpg |
geographic |
Antarctic Antarctic Ocean |
geographic_facet |
Antarctic Antarctic Ocean |
genre |
Antarc* Antarctic Antarctic Ocean Australian Antarctic Division |
genre_facet |
Antarc* Antarctic Antarctic Ocean Australian Antarctic Division |
op_source |
Journal of Fluid Mechanics |
op_relation |
http://purl.org/au-research/grants/arc/DP120102772 http://purl.org/au-research/grants/arc/DP120102744 http://purl.org/au-research/grants/arc/DE140100089 0022-1120 http://hdl.handle.net/1885/196871 doi:10.1017/jfm.2018.970 https://openresearch-repository.anu.edu.au/bitstream/1885/196871/6/ablation_sloping_iceface_mainak.pdf.jpg |
op_rights |
© 2019 Cambridge University Press |
op_doi |
https://doi.org/10.1017/jfm.2018.970 |
container_title |
Journal of Fluid Mechanics |
container_volume |
863 |
container_start_page |
545 |
op_container_end_page |
571 |
_version_ |
1788056914843664384 |