A General Model for the Helical Structure of Geophysical Flows in Channel Bends

Author:

Azpiroz-Zabala M.12ORCID,Cartigny M. J. B.3ORCID,Sumner E. J.1,Clare M. A.2,Talling P. J.3,Parsons D. R.4ORCID,Cooper C.5ORCID

Affiliation:

1. Ocean and Earth Sciences; University of Southampton; Southampton UK

2. National Oceanography Centre; Southampton UK

3. Departments of Earth Sciences and Geography; University of Durham; Durham UK

4. Department of Geography, Environment and Earth Sciences; University of Hull; Hull UK

5. Formerly at Chevron Energy Technology Company; San Ramon CA USA

Funder

National Oceanography Centre

Natural Environment Research Council

HEIF at University of Hull

Natural Environment Research Council Project

HEIF at the University of Hull

Graduate School of National Oceanography Centre Southampton

National Oceanography Centre Southampton

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference43 articles.

1. Secondary current of saline underflow in a highly meandering channel: Experiments and theory;Abad;Journal of Sedimentary Research,2011

2. Newly recognized turbidity current structure can explain prolonged flushing of submarine canyons;Azpiroz-Zabala;Science Advances,2017

3. Bed load transport by natural rivers;Bagnold;Water Resources Research,1977

4. A simple model for vertical profiles of velocity and suspended sediment concentration in straight and curved submarine channels;Bolla Pittaluga;Journal of Geophysical Research: Earth Surface,2014

5. A field study on turbidity currents initiated from spring runoffs;Chikita;Water Resources Research,1989

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