Troca estratosfera-troposfera e sua influência no conteúdo de ozônio sobre a região central do Rio Grande do Sul

• Ano de defesa: 2016
• Autor(a) principal: Santos, Letícia de Oliveira dos
• Tipo de documento: Dissertação
• Tipo de acesso: Acesso aberto
• Idioma: por
• Instituição de defesa: Universidade Federal de Santa Maria; BR; Meteorologia; UFSM; Programa de Pós-Graduação em Meteorologia
• Palavras-chave em Português: Troca estratosfera-troposfera; Coluna total de ozônio; Corrente de jato em altos níveis; Sul da América do Sul; Região central do Rio Grande do Sul; Stratosphere-troposphere exchange; Ozone total column; Upper-level jet stream; Southern South America; Central region of Rio Grande do Sul; CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA
• Link de acesso: http://repositorio.ufsm.br/handle/1/10289

It was identified Stratosphere-Troposphere Exchange (STE) events on Southern South America and their effects in the Ozone Total Column (OTC) above Central Region of Rio Grande do Sul (CRRS), Brazil, in the period between 2005 and 2014. To this end, it was developed a methodology able to verify the tropopause height and the descend mass flux in this region, using reanalysis 2 data provided by NCEP/DOE. Furthermore, these cases must have wind cores above 40m/s (Upper-level Jet Stream - ULJS) acting between 30 and 80°W and 20 and 50°S. The arrival confirmation of air parcels from the STE at the CRRS was made through HYSPLIT trajectory analysis model from NOAA. For cases that acted at the CRRS, it was computed the OTC variation in relation to five days prior to the STE effects, through daily OTC data obtained from the OMI instrument for Santa Maria city (29.72°S; 53.72°W). This methodology proved to be effective in identifying 755 STE events on Southern South America, from which 103 came to act on CRRS, with 65% of cases increasing and 35% reducing the OTC in this region. Seasonal analysis showed that most cases happens in winter, followed by spring and in less quantity in summer and fall. Averaged fields of the vertical wind profile, mass flux, temperature and potential vorticity, showed that STE events occur more often in post-frontal situations at the Bacia do Prata region. Moreover, it was analyzed the convergence role in relation to jet streak s vertical transversal circulations, demonstrating that, in STE cases, these circulations increase even more the stratospheric air intake into the troposphere by strong convergence in the ULJS level. In short, it was verified that STE events on Southern South America act as a stratospheric ozone-rich air source to the CRRS, having as an allied the ULJS, which increase the phenomena.