Azpiroz-Zabala, M. and Cartigny, M.J.B. and Sumner, E.J. and Clare, M.A. and Talling, P.J. and Parsons, D.R. and Cooper, C. (2017) 'A general model for the helical structure of geophysical flows in channel bends.', Geophysical research letters., 44 (23). 11,932-11,941.
Meandering channels formed by geophysical flows (e.g. rivers and seafloor turbidity currents) include the most extensive sediment transport systems on Earth. Previous measurements from rivers show how helical flow at meander bends plays a key role in sediment transport and deposition. Turbidity currents differ from rivers in both density and velocity profiles. These differences, and the lack of field measurements from turbidity currents, have led to multiple models for their helical flow around bends. Here we present the first measurements of helical flow in submarine turbidity currents. These ten flows lasted for 1-to-10 days, were up to ~80-metres thick, and displayed a consistent helical structure. This structure comprised two vertically-stacked cells, with the bottom cell rotating with the opposite direction to helical flow in rivers. Furthermore, we propose a general model that predicts the range of helical flow structures observed in rivers, estuaries and turbidity currents based on their density stratification.
|Full text:||(AM) Accepted Manuscript|
Download PDF (766Kb)
|Full text:||(VoR) Version of Record|
Available under License - Creative Commons Attribution.
Download PDF (2328Kb)
|Publisher Web site:||https://doi.org/10.1002/2017GL075721|
|Publisher statement:||© 2017. 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.|
|Date accepted:||21 November 2017|
|Date deposited:||08 December 2017|
|Date of first online publication:||11 December 2017|
|Date first made open access:||04 January 2018|
Save or Share this output
|Look up in GoogleScholar|