Abstract
This study shows, from the mesoscale analysis perspective that Mesoscale Cyclonic Vortex (MCV) is associated to the South Atlantic Convergence Zone (SACZ) through a feedback process. This system, simulated by the BRAMS regional model, is generated embedded in a stratiform environment within the SACZ region, during the January 2009 austral summer. MCVs present similar characteristics which could be considered as a “signature” for such systems. The case study also presents a lifetime shorter than 24 h and spatial scale of approximately 200 km2 in addition to intense precipitation, shifting in the flow direction in the lower troposphere. In the case occurred in the Mato Grosso State, the presence of this system was associated with heavy rain, relative vorticity of the same order as the Coriolis parameter (10−4 s−1), warm core above the level of maximum intensity and rapid growth of the cyclonic vorticity center mostly in the lower levels. The simulated precipitation is compared against the Hidroestimador precipitation product. The results suggest that the BRAMS model, configured with high spatial and temporal resolutions improves the representation of the MCVs when compared to the NCEP CFSR reanalysis.
Keywords:
mesoscale cyclonic vortex; SACZ; precipitation
