{"refrec":{"BRefID":362734,"RR":"<b>Marquart, R.; Bogaers, A.; Skatulla, S.; Alberello, A.; Toffoli, A.; Schwarz, C.; Vichi, M.</b> (2021). A computational fluid dynamics model for the small-scale dynamics of wave, ice floe and interstitial grease ice interaction. <i>Fluids 6(5)</i>: 176. <a href=\"https://dx.doi.org/10.3390/fluids6050176\" target=\"_blank\">https://dx.doi.org/10.3390/fluids6050176</a>","BEntID":360452,"PublicFlag":1,"CheckedFlag":1,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Fluids 6(5)</i>: 176. <a href=\"https://dx.doi.org/10.3390/fluids6050176\" target=\"_blank\">https://dx.doi.org/10.3390/fluids6050176</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Marquart, R.; Bogaers, A.; Skatulla, S.; Alberello, A.; Toffoli, A.; Schwarz, C.; Vichi, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Marquart, R. <i>et al.</i>","Englishabstract":"The marginal ice zone is a highly dynamical region where sea ice and ocean waves interact. Large-scale sea ice models only compute domain-averaged responses. As the majority of the marginal ice zone consists of mobile ice floes surrounded by grease ice, finer-scale modelling is needed to resolve variations of its mechanical properties, wave-induced pressure gradients and drag forces acting on the ice floes. A novel computational fluid dynamics approach is presented that considers the heterogeneous sea ice material composition and accounts for the wave-ice interaction dynamics. Results show, after comparing three realistic sea ice layouts with similar concentration and floe diameter, that the discrepancy between the domain-averaged temporal stress and strain rate evolutions increases for decreasing wave period. 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