Extension of <mml:math altimg="si85.gif" overflow="scroll" xmlns:xocs="http://www.elsevier.com/xml/xocs/dtd" xmlns:xs="http://www.w3.org/2001/XMLSchema" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://www.elsevier.com/xml/ja/dtd" xmlns:ja="http://www.elsevier.com/xml/ja/dtd" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:tb="http://www.elsevier.com/xml/common/table/dtd" xmlns:sb="http://www.elsevier.com/xml/common/struct-bib/dtd" xmlns:ce="http://www.elsevier.com/xml/common/dtd" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:cals="http://www.elsevier.com/xml/common/cals/dtd" xmlns:sa="http://www.elsevier.com/xml/common/struct-aff/dtd"><mml:mrow><mml:mi>k</mml:mi><mml:mo>-</mml:mo><mml:mi>ω</mml:mi></mml:mrow></mml:math> turbulence closure to two-phase sediment transport modelling: Application to oscillatory sheet flows-Reference-Cited by-同舟云学术

Extension of k-ω turbulence closure to two-phase sediment transport modelling: Application to oscillatory sheet flows

Author:

Amoudry Laurent O.

Funder

Natural Environment Research Council

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference44 articles.

4. Effects of wave shape on sheet flow sediment transport;Hsu;J Geophys Res,2004

5. Sediment transport under wave groups – the relative importance between wave shape and nonlinear boundary layer streaming;Yu;J Geophys Res,2010

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