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Cold season synoptic scale waves over Subtropical South America

Vera, Carolina Susana et al · Amer Meteorological Soc · 2002

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The most active winter synoptic-scale wave patterns over South America are identified using an extended empirical orthogonal function (EEOF) technique and are physically diagnosed using composite methods. Results show that the leading modes of short timescale variability propagate along two main paths: over the subtropical jet latitudes (;308S) and over the subpolar jet latitudes (;608S). This research focuses on the subtropical mode and its evolution over South America. The observed structure of the systems associated with the subtropical mode resembles that of midlatitude baroclinic waves. Both cyclonic and anticyclonic perturbations display significant modifications in their threedimensional structure as they evolve over extratropical and subtropical South America. While the upper-level perturbations are mostly unaffected when moving eastward, the lower-level perturbations advance following the shape of the Andes Mountains and exhibit an abrupt equatorward migration at the lee side of the mountains. As a result of such detachment, smaller eddy heat fluxes are observed in the vicinity of the orography and consequently a weaker eddy baroclinic growth is observed. Once the upper-level system is on the lee side, the perturbations acquire a more typical baroclinic wave structure and low-level intensification of the system occurs. The latter is largest around 1000 km east of the orography, where enhanced moisture transports from tropical latitudes along the eastern portion of the low-level cyclone favor precipitation occurrence over southeastern South America. Those precipitation processes seem to provide a diabatic source of energy that further contributes to the strengthening of the low-level cyclone. In addition, an intensification of the cyclone once over the ocean was found in 60% of the situations considered, which is consistent with previous research suggesting an additional source of moisture and heat flux due to the warm waters of the Brazil Current.
Fil: Vera, Carolina Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Fil: Viglirarolo, Paula K.. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina

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APA 7

Vera, C. S. E. A. (2002). Cold season synoptic scale waves over Subtropical South America. http://hdl.handle.net/11336/147368

MLA

Vera, Carolina Susana et al. "Cold season synoptic scale waves over Subtropical South America." 2002. http://hdl.handle.net/11336/147368.

Chicago

Vera, Carolina Susana et al. 2002. "Cold season synoptic scale waves over Subtropical South America.". http://hdl.handle.net/11336/147368.

Harvard

Vera, C. S. E. A. 2002, Cold season synoptic scale waves over Subtropical South America, Amer Meteorological Soc, available at: http://hdl.handle.net/11336/147368 [Accessed 22 Jun. 2026].

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Título
Cold season synoptic scale waves over Subtropical South America
Autor / colaboradores
Vera, Carolina Susana et al
Editorial
Amer Meteorological Soc
Año de publicación
2002
ISSN
0027-0644
ISSN
0027-0644
Idioma
eng

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