Abstract
In this chapter, the meteorological characteristics of the South-Southeast Brazilian coast are analysed, in particular the frontal systems and their influence on ocean circulation and sea level. The analyses are based on meteorological fields (pressure, temperature and wind) and oceanic fields (ocean currents and sea level) calculated by the CFS-v2 – Climate Forecast System (version 2), as well as on the synoptic analyses of the (Brazilian) Center for Weather Forecasting and Climatic Studies/National Institute of Space Research (CPTEC/INPE). Regarding the temporal evolution of the meteorological and oceanographic variables, it was chosen the month of September 2009, which registered several frontal systems of great intensity.
The intensity, duration, and time interval between these events have seasonal and interannual variability, and can be predicted only a few days in advance. Sea surface currents in the coastal region between 23°S and 27°S are to the South with a low intensity before the fronts (typically 0.2 m/s) and are to the North and very intense after the passage of the frontal systems (maximum above 0.4 m/s); sea surface level at the coast may vary from −0.1 m before the passage of the fronts, exceeding +0.5 m after their passage.
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Harari, J., de Camargo, R. (2019). Patterns of Evolution of Frontal Systems Along the South-Southeastern Brazilian Coast. In: Nunes, L., Greco, R., Marengo, J. (eds) Climate Change in Santos Brazil: Projections, Impacts and Adaptation Options. Springer, Cham. https://doi.org/10.1007/978-3-319-96535-2_2
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DOI: https://doi.org/10.1007/978-3-319-96535-2_2
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