{"refrec":{"BRefID":132330,"RR":"<b>de Kok, J.M.</b> (1997). Baroclinic eddy formation in a Rhine plume model. <i>J. Mar. Syst. 12(1-4)</i>: 35-44, 49-52. <a href=\"https://dx.doi.org/10.1016/S0924-7963(96)00087-5\" target=\"_blank\">https://dx.doi.org/10.1016/S0924-7963(96)00087-5</a>","BEntID":126341,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Mar. Syst. 12(1-4)</i>: 35-44, 49-52. <a href=\"https://dx.doi.org/10.1016/S0924-7963(96)00087-5\" target=\"_blank\">https://dx.doi.org/10.1016/S0924-7963(96)00087-5</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":1,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"de Kok, J.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"de Kok, J.M.","Englishabstract":"A three-dimensional finite difference tidal model, including advective and diffusive transport of salinity, is used in the two-layer model for simulation of Rhine water outflow. 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