Modelling ice-ocean interactions in and around ice shelves

Physical processes in Antarctica and the Southern Ocean are of great importance to the global climate system. This thesis considers two such processes, namely ice- ocean interaction in ice shelf basal crevasses and the conditional instability of frazil ice growth. It has been suggested that freezing...

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Main Author: Jordan, James
Other Authors: Piggott, Matthew, Natural Environment Research Council (Great Britain)
Format: Doctoral or Postdoctoral Thesis
Language:unknown
Published: Imperial College London 2015
Subjects:
Online Access:http://hdl.handle.net/10044/1/28616
https://doi.org/10.25560/28616
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spelling ftimperialcol:oai:spiral.imperial.ac.uk:10044/1/28616 2023-05-15T14:01:35+02:00 Modelling ice-ocean interactions in and around ice shelves Jordan, James Piggott, Matthew Natural Environment Research Council (Great Britain) 2015-11 http://hdl.handle.net/10044/1/28616 https://doi.org/10.25560/28616 unknown Imperial College London Earth Science & Engineering Thesis or dissertation Doctoral Doctor of Philosophy (PhD) 2015 ftimperialcol https://doi.org/10.25560/28616 2019-11-14T23:38:41Z Physical processes in Antarctica and the Southern Ocean are of great importance to the global climate system. This thesis considers two such processes, namely ice- ocean interaction in ice shelf basal crevasses and the conditional instability of frazil ice growth. It has been suggested that freezing within basal crevasses can act as a stabilising in uence on ice shelves, preventing their break up. Using Fluidity, a nite element ocean model, it is found that ocean circulation within a crevasse is highly dependent upon the amount of freezing in the crevasse. It is also found that frazil ice formation is responsible for the vast majority of freezing within a crevasse, and that there is a non linear relationship between the amount of supercooling in a crevasse and its freeze rate. The conditional instability of frazil ice growth is a little investigated mechanism of ice growth. Any frazil forming in the water column reduces the bulk density of a parcel of frazil-seawater mixture, causing it to rise. Due to the pressure-decrease in the freezing point, this causes more frazil to form, causing the parcel to accelerate, and so on. Numerical modelling nds that the instability does not operate in the presence of strong strati cation, high thermal driving (warm water), a small initial perturbation, high `background' mixing or the prevalence of large frazil ice crystals. Given a large enough initial perturbation this instability could allow signi cant rates of ice growth even in water that is above the freezing point. The research presented in this thesis forms the material for two peer-reviewed publi- cations; `Modelling ice ocean interactions in ice shelf basal crevasses' (Jordan et al., 2014) and `On the conditional frazil ice instability in seawater' (Jordan et al., 2015) Open Access Doctoral or Postdoctoral Thesis Antarc* Antarctica Ice Shelf Ice Shelves Southern Ocean Imperial College London: Spiral Southern Ocean
institution Open Polar
collection Imperial College London: Spiral
op_collection_id ftimperialcol
language unknown
description Physical processes in Antarctica and the Southern Ocean are of great importance to the global climate system. This thesis considers two such processes, namely ice- ocean interaction in ice shelf basal crevasses and the conditional instability of frazil ice growth. It has been suggested that freezing within basal crevasses can act as a stabilising in uence on ice shelves, preventing their break up. Using Fluidity, a nite element ocean model, it is found that ocean circulation within a crevasse is highly dependent upon the amount of freezing in the crevasse. It is also found that frazil ice formation is responsible for the vast majority of freezing within a crevasse, and that there is a non linear relationship between the amount of supercooling in a crevasse and its freeze rate. The conditional instability of frazil ice growth is a little investigated mechanism of ice growth. Any frazil forming in the water column reduces the bulk density of a parcel of frazil-seawater mixture, causing it to rise. Due to the pressure-decrease in the freezing point, this causes more frazil to form, causing the parcel to accelerate, and so on. Numerical modelling nds that the instability does not operate in the presence of strong strati cation, high thermal driving (warm water), a small initial perturbation, high `background' mixing or the prevalence of large frazil ice crystals. Given a large enough initial perturbation this instability could allow signi cant rates of ice growth even in water that is above the freezing point. The research presented in this thesis forms the material for two peer-reviewed publi- cations; `Modelling ice ocean interactions in ice shelf basal crevasses' (Jordan et al., 2014) and `On the conditional frazil ice instability in seawater' (Jordan et al., 2015) Open Access
author2 Piggott, Matthew
Natural Environment Research Council (Great Britain)
format Doctoral or Postdoctoral Thesis
author Jordan, James
spellingShingle Jordan, James
Modelling ice-ocean interactions in and around ice shelves
author_facet Jordan, James
author_sort Jordan, James
title Modelling ice-ocean interactions in and around ice shelves
title_short Modelling ice-ocean interactions in and around ice shelves
title_full Modelling ice-ocean interactions in and around ice shelves
title_fullStr Modelling ice-ocean interactions in and around ice shelves
title_full_unstemmed Modelling ice-ocean interactions in and around ice shelves
title_sort modelling ice-ocean interactions in and around ice shelves
publisher Imperial College London
publishDate 2015
url http://hdl.handle.net/10044/1/28616
https://doi.org/10.25560/28616
geographic Southern Ocean
geographic_facet Southern Ocean
genre Antarc*
Antarctica
Ice Shelf
Ice Shelves
Southern Ocean
genre_facet Antarc*
Antarctica
Ice Shelf
Ice Shelves
Southern Ocean
op_doi https://doi.org/10.25560/28616
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