Superelevation and overspill control secondary flow dynamics in submarine channels
Superelevation and overspill control secondary flow dynamics in submarine channels
In subaerial and submarine meander bends, fluid flow travels downstream in a helical spiral, the structure of which is determined by centrifugal, hydrostatic, baroclinic, and Coriolis forces that together balance frictional stresses generated by the flow. The sense of rotation of this helical flow, and in particular, whether the near bed flow is directed toward the inner bank, e.g., “river-normal,” or outer bank, e.g., “river-reversed,” is crucial to the morphodynamic evolution of the channel. However, in recent years, there has been a debate over the river-normal or river-reversed nature of submarine flows. Herein, we develop a novel three-dimensional closure of secondary flow dynamics, incorporating downstream convective material transport, to cast new light on this debate. Specifically, we show that the presence of net radial material transport, arising from flow superelevation and overspill, exerts a key control on the near bed orientation of secondary flow in submarine meanders. Our analysis implies that river-reversed flows are likely to be much more prevalent throughout submarine-canyon fan systems than prior studies have indicated.
density current, meander, secondary flow
3895-3915
Dorrell, R.D.
be6b2a8f-f768-40a9-8bcd-63f39fc5bca7
Darby, S.E.
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Peakall, J.
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Sumner, E.J.
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Parsons, D.R.
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Wynn, R.B.
72ccd765-9240-45f8-9951-4552b497475a
13 August 2013
Dorrell, R.D.
be6b2a8f-f768-40a9-8bcd-63f39fc5bca7
Darby, S.E.
4c3e1c76-d404-4ff3-86f8-84e42fbb7970
Peakall, J.
2351dbf6-2c4f-4250-bacf-fe1b69870f26
Sumner, E.J.
dbba4b92-89cc-45d9-888e-d0e87e5c10ac
Parsons, D.R.
8bc551f4-ae49-48cd-8533-82a34e749d74
Wynn, R.B.
72ccd765-9240-45f8-9951-4552b497475a
Dorrell, R.D., Darby, S.E., Peakall, J., Sumner, E.J., Parsons, D.R. and Wynn, R.B.
(2013)
Superelevation and overspill control secondary flow dynamics in submarine channels.
Journal of Geophysical Research, 118 (8), .
(doi:10.1002/jgrc.20277).
Abstract
In subaerial and submarine meander bends, fluid flow travels downstream in a helical spiral, the structure of which is determined by centrifugal, hydrostatic, baroclinic, and Coriolis forces that together balance frictional stresses generated by the flow. The sense of rotation of this helical flow, and in particular, whether the near bed flow is directed toward the inner bank, e.g., “river-normal,” or outer bank, e.g., “river-reversed,” is crucial to the morphodynamic evolution of the channel. However, in recent years, there has been a debate over the river-normal or river-reversed nature of submarine flows. Herein, we develop a novel three-dimensional closure of secondary flow dynamics, incorporating downstream convective material transport, to cast new light on this debate. Specifically, we show that the presence of net radial material transport, arising from flow superelevation and overspill, exerts a key control on the near bed orientation of secondary flow in submarine meanders. Our analysis implies that river-reversed flows are likely to be much more prevalent throughout submarine-canyon fan systems than prior studies have indicated.
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Dorrell et al 2013_reversals.pdf
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Published date: 13 August 2013
Keywords:
density current, meander, secondary flow
Organisations:
Geology & Geophysics, Marine Geoscience, Earth Surface Dynamics
Identifiers
Local EPrints ID: 360036
URI: http://eprints.soton.ac.uk/id/eprint/360036
ISSN: 0148-0227
PURE UUID: 36386f5c-fb55-4357-88cc-bff80548a1d4
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Date deposited: 16 Dec 2013 10:02
Last modified: 15 Mar 2024 02:58
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Contributors
Author:
R.D. Dorrell
Author:
J. Peakall
Author:
D.R. Parsons
Author:
R.B. Wynn
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