{"refrec":{"BRefID":53992,"RR":"<b>Coelho, H.S.; Neves, R.J.J.; White, M.; Leitão, P.C.; Santos, A.J.</b> (2002). A model for ocean circulation on the Iberian coast. <i>J. Mar. Syst. 32(1-3)</i>: 153-179. <a href=\"https://dx.doi.org/10.1016/S0924-7963(02)00032-5\" target=\"_blank\">https://dx.doi.org/10.1016/S0924-7963(02)00032-5</a>","BEntID":29840,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Mar. Syst. 32(1-3)</i>: 153-179. <a href=\"https://dx.doi.org/10.1016/S0924-7963(02)00032-5\" target=\"_blank\">https://dx.doi.org/10.1016/S0924-7963(02)00032-5</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Coelho, H.S.; Neves, R.J.J.; White, M.; Leitão, P.C.; Santos, A.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Coelho, H.S. <i>et al.</i>","Englishabstract":"We used a three-dimensional model with generic vertical coordinate to investigate the structure of flow and transports on the Iberian shelf-slope region. Two different types of experiments were conducted. The first was a process-oriented study to investigate the role of thermohaline forcing in the generation and meridional variability of the poleward slope current. The second experiment was a more realistic simulation for the year of 1994, a period for which there are several long-term current meter data sets available. Comparisons between model, data and other published works have shown a reasonable agreement both qualitatively and quantitatively. The results obtained included the seasonal cycle with upwelling during the summer and a winter surface poleward current over the shelf, with a permanent undercurrent transporting Mediterranean Water along the Portuguese and Spanish slopes. The along-slope transports were predominant especially in the OMEX II-II study area. 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