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Modeling the Tilt of Bend-Traversing Turbidity Currents: Implications for Sinuous Submarine Channel Development

Crisóstomo-Figueroa, Adriana; Dorrell, Robert M.; Amy, Lawrence; McArthur, Adam D.; McCaffrey, William D.

Authors

Adriana Crisóstomo-Figueroa

Robert M. Dorrell

Lawrence Amy

Adam D. McArthur

William D. McCaffrey



Abstract

The controls on the development of submarine channel sinuosity are contested: slope gradient and Coriolis forcing have both been recognized as key governing factors: gradient via an inverse relationship (low sinuosity at high slope and vice versa), and Coriolis forcing through its effect on sedimentation patterns (reducing lateral bend migration, and hence sinuosity development, at high latitudes and/or in large channels). Using theoretical models to calculate the bulk properties of channelized turbidity currents, this study investigates the joint role of the Coriolis force and parameters including channel size, downchannel slope and turbidity current properties in the development of submarine channel sinuosity. Model validation is undertaken through the comparison of the calculated turbidity current tilting against the measured tilting of channel levees in the Northwest Atlantic Mid-Ocean Channel; this approach is then used to evaluate the controls on channel sinuosity in nine other modern seafloor channels. The results indicate that the Coriolis force only becomes significant when the size of the channel, the slope gradient and flow conditions are within appropriate ranges instead of solely being dependent on latitude. Thus, thick and dense (≥1% bulk sediment concentration) flows traveling within steep-gradient, small-scale channels were shown to be relatively less susceptible to flow modification by Coriolis forcing even at high latitudes. On the other hand, thin and dilute (≪1% bulk sediment concentration) flows in shallow-gradient, large-scale channels showed susceptibility to Coriolis forcing at all latitudes. These results offer new insights into submarine channel evolution and intra-channel sedimentation patterns.

Citation

Crisóstomo-Figueroa, A., Dorrell, R. M., Amy, L., McArthur, A. D., & McCaffrey, W. D. (2024). Modeling the Tilt of Bend-Traversing Turbidity Currents: Implications for Sinuous Submarine Channel Development. Journal of Geophysical Research: Oceans, 129(10), Article e2023JC020131. https://doi.org/10.1029/2023JC020131

Journal Article Type Article
Acceptance Date Nov 1, 2024
Publication Date Oct 1, 2024
Deposit Date Nov 20, 2024
Publicly Available Date Nov 21, 2024
Journal Journal of Geophysical Research: Oceans
Print ISSN 2169-9291
Publisher American Geophysical Union
Peer Reviewed Peer Reviewed
Volume 129
Issue 10
Article Number e2023JC020131
DOI https://doi.org/10.1029/2023JC020131
Keywords Turbidity currents; Submarine channels; Coriolis; Sinuous channels; Upper interface tilt; Modeling
Public URL https://hull-repository.worktribe.com/output/4868632

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Publisher Licence URL
http://creativecommons.org/licenses/by/4.0

Copyright Statement
© 2024. The Author(s).
This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.




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