{"refrec":{"BRefID":7390,"RR":"<b>Trouw, K.; Williams, J.J.; Rose, C.P.</b> (2000). Modelling sand resuspension by waves over a rippled bed. <i>Est., Coast. and Shelf Sci. 50(1)</i>: 143-151. <a href=\"http://dx.doi.org/10.1006/ecss.1999.0542\" target=\"_blank\">dx.doi.org/10.1006/ecss.1999.0542</a>","BEntID":7390,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Est., Coast. and Shelf Sci. 50(1)</i>: 143-151. <a href=\"https://dx.doi.org/10.1006/ecss.1999.0542\" target=\"_blank\">https://dx.doi.org/10.1006/ecss.1999.0542</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Trouw, K.; Williams, J.J.; Rose, C.P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Trouw, K. <i>et al.</i>","Englishabstract":"With a two-dimensional <i>Kappa-Epsilon</i>-model and equations to describe sediment entrainment, diffusion, convection and settling, wave-induced flow velocities and sediment concentration fields over rippled beds have been calculated. Results from the simulations are compared with time-averaged vertical suspended sediment concentration profiles, C-profiles, measured in a large wave flume using the autonomous multi-sensor instrument STABLE. The simulations make it possible to examine in detail the mechanisms of sediment entrainment, vortex formation and advection. The resulting animations of model output allow a quasi-3-D visualization of sediment resuspension processes and aid quantification of the resulting vertical suspended sediment concentration field due to regular waves, asymmetric waves and wave groups. 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