Sophie Hage
Direct monitoring reveals initiation of turbidity currents from extremely dilute river plumes
Hage, Sophie; Cartigny, Matthieu J.B.; Sumner, Esther J.; Clare, Michael A.; Hughes Clarke, John E.; Talling, Peter J.; Lintern, D. Gwyn; Simmons, Stephen M.; Silva Jacinto, Ricardo; Vellinga, Age J.; Allin, Joshua R.; Azpiroz‐Zabala, Maria; Gales, Jenny A.; Hizzett, Jamie L.; Hunt, James E.; Mozzato, Alessandro; Parsons, Daniel R.; Pope, Ed L.; Stacey, Cooper D.; Symons, William O.; Vardy, Mark E.; Watts, Camilla
Authors
Dr Matthieu Cartigny matthieu.j.cartigny@durham.ac.uk
Associate Professor
Esther J. Sumner
Michael A. Clare
John E. Hughes Clarke
Professor Peter Talling peter.j.talling@durham.ac.uk
Professor
D. Gwyn Lintern
Stephen M. Simmons
Ricardo Silva Jacinto
Age J. Vellinga
Joshua R. Allin
Maria Azpiroz‐Zabala
Jenny A. Gales
Jamie L. Hizzett
James E. Hunt
Alessandro Mozzato
Daniel R. Parsons
Edward Pope edward.pope@durham.ac.uk
Honorary Fellow
Cooper D. Stacey
William O. Symons
Mark E. Vardy
Camilla Watts
Abstract
Rivers (on land) and turbidity currents (in the ocean) are the most important sediment transport processes on Earth. Yet, how rivers generate turbidity currents as they enter the coastal ocean remains poorly understood. The current paradigm, based on laboratory experiments, is that turbidity currents are triggered when river plumes exceed a threshold sediment concentration of ~1 kg.m‐3. Here we present direct observations of an exceptionally dilute river‐plume, with sediment concentrations one order of magnitude below this threshold (0.07 kg.m‐3), which generated a fast (1.5 m.s‐1), erosive, short‐lived (6 min) turbidity current. However, no turbidity current occurred during subsequent river‐plumes. We infer that turbidity currents are generated when fine‐sediment, accumulating in a tidal turbidity maximum, is released during spring tide. This means that very dilute river‐plumes can generate turbidity currents more frequently and in a wider range of locations, than previously thought.
Citation
Hage, S., Cartigny, M. J., Sumner, E. J., Clare, M. A., Hughes Clarke, J. E., Talling, P. J., Lintern, D. G., Simmons, S. M., Silva Jacinto, R., Vellinga, A. J., Allin, J. R., Azpiroz‐Zabala, M., Gales, J. A., Hizzett, J. L., Hunt, J. E., Mozzato, A., Parsons, D. R., Pope, E. L., Stacey, C. D., Symons, W. O., …Watts, C. (2019). Direct monitoring reveals initiation of turbidity currents from extremely dilute river plumes. Geophysical Research Letters, 46(20), 11310-11320. https://doi.org/10.1029/2019gl084526
Journal Article Type | Article |
---|---|
Acceptance Date | Sep 2, 2019 |
Online Publication Date | Sep 13, 2019 |
Publication Date | Oct 28, 2019 |
Deposit Date | Oct 10, 2019 |
Publicly Available Date | Nov 4, 2019 |
Journal | Geophysical Research Letters |
Print ISSN | 0094-8276 |
Electronic ISSN | 1944-8007 |
Publisher | Wiley |
Peer Reviewed | Peer Reviewed |
Volume | 46 |
Issue | 20 |
Pages | 11310-11320 |
DOI | https://doi.org/10.1029/2019gl084526 |
Public URL | https://durham-repository.worktribe.com/output/1283261 |
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Copyright Statement
Advance online version © 2019. The Authors.
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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