Challenges to the representation of suspended sediment transfer using a depth-averaged flux-Reference-Cited by-同舟云学术

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Challenges to the representation of suspended sediment transfer using a depth-averaged flux

Published:2016-02-19 Issue:10 Volume:41 Page:1337-1357
ISSN:0197-9337
Container-title:Earth Surface Processes and Landforms
language:en
Short-container-title:Earth Surf. Process. Landforms

Author:

Cheng Chen¹²³,Huang Huiming⁴,Liu Chengyan¹²³,Jiang Weimin¹²³

Affiliation:

1. Polar Climate System and Global Change Laboratory; Nanjing University of Information Science & Technology; Nanjing China

2. School of Marine Sciences; Nanjing University of Information Science & Technology; Nanjing China

3. Jiangsu Research Center for Ocean Survey Technology; Nanjing University of Information Science & Technology; Nanjing China

4. College of Harbor, Coastal and Offshore Engineering; Hohai University; Nanjing China

Funder

Startup Foundation for Introducing Talent of NUIST

Natural Science Foundation of Jiangsu Higher Education Institutions of China

National Natural Science Foundation of China

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/esp.3903/fullpdf

Reference90 articles.

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2. The measurement of sand transport in two inlets of Venice lagoon, Italy;Amos;Estuarine, Coastal and Shelf Science,2010

3. Schmidt number and near-bed boundary condition effects on a two-phase dilute sediment transport model;Amoudry;Journal of Geophysical Research - Oceans,2005

4. Finite element model for cohesive sediment transport;Ariathurai;Journal of the Hydraulics Division,1976

5. A one-dimensional model for the transport of a sediment mixture in non-equilibrium conditions;Armanin;Journal of Hydraulic Research,1988

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