As previsões dos níveis do mar no Atlântico NE são baseadas na aplicação do modelo SCHISM (http://ccrm.vims.edu/w/index.php/Main_Page). O modelo é corrido em modo 2D barotrópico, e forçado por marés calculadas com o modelo FES2012 (http://www.aviso.altimetry.fr/en/data/products/auxiliary-products/global...) e ventos e pressão atmosférica do modelo GFS do NCEP (http://mag.ncep.noaa.gov/). A resolução espacial na costa Portuguesa é de cerca de 250 m. Para mais detalhes, consultar aqui. Referência Fortunato, A.B., Li, K., Bertin, X., Rodrigues, M., Miguez, B.M. (2016). Determination of extreme sea levels along the Iberian Atlantic Coast, Ocean Eng., 111: 471-482. The forecasts of water elevation in the NE Atlantic are based on the application of the model SCHISM (http://ccrm.vims.edu/w/index.php/Main_Page). The model is run in 2D arotropic mode, and forced by tides from FES2012 (http://www.aviso.altimetry.fr/en/data/products/auxiliary-products/global...) and winds and atmospheric results from the NCEP GFS model (http://mag.ncep.noaa.gov/). The grid resolution is about 250 m in the Portugese coast. For further details see here. Reference Fortunato, A.B., Li, K., Bertin, X., Rodrigues, M., Miguez, B.M. (2016). Determination of extreme sea levels along the Iberian Atlantic Coast, Ocean Eng., 111: 471-482. |
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