Abstract
A frontal structure in the tropical region is different than in the extratropical region and traditional methods of frontal identification are not accurate. The use of a horizontal distribution of the equivalent potential temperature and its advection is the new aspect in frontal identification and will support forecasters in their daily operational practice. Six fronts over 3 years were identified by the method used in operational practice. Twenty fronts were registered by cloud bands together with the equivalent potential temperature and its advection maps. A cold front separated from the cyclone’s center and affected weather on the Northeast Brazil.
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Partial financial support (student grant) was provided by CAPES (Coordination of the Level Superior Personal Improvement).
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Fedorova, N., Levit, V. & da Cruz, C.D. On Frontal Zone Analysis in the Tropical Region of the Northeast Brazil. Pure Appl. Geophys. 173, 1403–1421 (2016). https://doi.org/10.1007/s00024-015-1166-y
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DOI: https://doi.org/10.1007/s00024-015-1166-y