Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes
The hydrodynamic and sedimentary processes that operate on submerged passive continental margins are often difficult to study due to their remoteness and the sparse data coverage associated with these regions. Numerical simulations provide a powerful experimental framework to investigate such physic...
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ftunivsydney:oai:ses.library.usyd.edu.au:2123/22836 2023-05-15T18:18:43+02:00 Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes Thran, Amanda Chayce 2020 application/pdf https://hdl.handle.net/2123/22836 en eng University of Sydney The University of Sydney Faculty of Science, School of Geosciences https://hdl.handle.net/2123/22836 The author retains copyright of this thesis. It may only be used for the purposes of research and study. It must not be used for any other purposes and may not be transmitted or shared with others without prior permission. numerical modelling sedimentology coastal contourite tsunami surface processes Thesis Doctor of Philosophy 2020 ftunivsydney 2022-05-30T13:46:37Z The hydrodynamic and sedimentary processes that operate on submerged passive continental margins are often difficult to study due to their remoteness and the sparse data coverage associated with these regions. Numerical simulations provide a powerful experimental framework to investigate such physical processes. In this thesis, a variety of numerical models are used to provide process-based insights into the regional-scale hydrodynamic and sedimentary consequences of margin flows. Margin geometry plays a critical role in preconditioning and modifying three types of flows: along-slope flows, down-shelf and down-slope flows, and cross-shelf flows. In a study of along-slope flows, ocean sea-ice model results indicate that contourite drifts, which are anomalously high accumulations of deep-sea sediments, form in areas that exhibit vigorous bottom current activity. Simulations show that bottom current speeds fluctuate more over contourites, suggesting that contourite formation can be attributed to repeated acute, high-energy bottom current events rather than continuous accumulation under ambient background flow. In a study of down-shelf and down-slope flows, surface and marine process-based simulations indicate that carbonate platforms play a fundamental role in the regional geomorphological development of the mixed carbonate-siliciclastic Great Barrier Reef margin. Finally, in a study of cross-shelf flows, tsunami propagation simulations show that coral reef ecosystems offer varying degrees of protection to the coastline. Various factors related to bathymetry dictate the degree of wave energy attenuation by coral cover. These findings highlight the importance of site-specific seafloor geometry in modulating hydrodynamic and sedimentary processes in margin settings. Additionally, they also provide new mechanistic insights into the hydrodynamic and sedimentary consequences of topographically-mediated margin flows. Thesis Sea ice The University of Sydney: Sydney eScholarship Repository |
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The University of Sydney: Sydney eScholarship Repository |
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ftunivsydney |
language |
English |
topic |
numerical modelling sedimentology coastal contourite tsunami surface processes |
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numerical modelling sedimentology coastal contourite tsunami surface processes Thran, Amanda Chayce Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes |
topic_facet |
numerical modelling sedimentology coastal contourite tsunami surface processes |
description |
The hydrodynamic and sedimentary processes that operate on submerged passive continental margins are often difficult to study due to their remoteness and the sparse data coverage associated with these regions. Numerical simulations provide a powerful experimental framework to investigate such physical processes. In this thesis, a variety of numerical models are used to provide process-based insights into the regional-scale hydrodynamic and sedimentary consequences of margin flows. Margin geometry plays a critical role in preconditioning and modifying three types of flows: along-slope flows, down-shelf and down-slope flows, and cross-shelf flows. In a study of along-slope flows, ocean sea-ice model results indicate that contourite drifts, which are anomalously high accumulations of deep-sea sediments, form in areas that exhibit vigorous bottom current activity. Simulations show that bottom current speeds fluctuate more over contourites, suggesting that contourite formation can be attributed to repeated acute, high-energy bottom current events rather than continuous accumulation under ambient background flow. In a study of down-shelf and down-slope flows, surface and marine process-based simulations indicate that carbonate platforms play a fundamental role in the regional geomorphological development of the mixed carbonate-siliciclastic Great Barrier Reef margin. Finally, in a study of cross-shelf flows, tsunami propagation simulations show that coral reef ecosystems offer varying degrees of protection to the coastline. Various factors related to bathymetry dictate the degree of wave energy attenuation by coral cover. These findings highlight the importance of site-specific seafloor geometry in modulating hydrodynamic and sedimentary processes in margin settings. Additionally, they also provide new mechanistic insights into the hydrodynamic and sedimentary consequences of topographically-mediated margin flows. |
format |
Thesis |
author |
Thran, Amanda Chayce |
author_facet |
Thran, Amanda Chayce |
author_sort |
Thran, Amanda Chayce |
title |
Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes |
title_short |
Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes |
title_full |
Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes |
title_fullStr |
Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes |
title_full_unstemmed |
Understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes |
title_sort |
understanding the influence of passive continental margin geometry on shallow and deep hydrodynamic and sedimentary processes |
publisher |
University of Sydney |
publishDate |
2020 |
url |
https://hdl.handle.net/2123/22836 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
https://hdl.handle.net/2123/22836 |
op_rights |
The author retains copyright of this thesis. It may only be used for the purposes of research and study. It must not be used for any other purposes and may not be transmitted or shared with others without prior permission. |
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