Fechar

@MastersThesis{Simões::InVaIn,
               author = "Sim{\~o}es, Paloma Angelina",
                title = "Influ{\^e}ncia da variabilidade intrasazonal na variabilidade 
                         interanual do sistema de mon{\c{c}}{\~a}o da Am{\'e}rica do 
                         Sul",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2024-02-08",
             keywords = "precipita{\c{c}}{\~a}o, ver{\~o}es mais secos, ver{\~o}es mais 
                         chuvosos, escalas, variabilidade intrasazonal, precipitation, more 
                         dry summers, more rainy summers, scales, intraseasonal 
                         variability.",
             abstract = "O Sistema de Mon{\c{c}}{\~a}o da Am{\'e}rica do Sul (SMAS) 
                         {\'e} um dos principais sistemas que contribui para a 
                         precipita{\c{c}}{\~a}o, durante os meses de ver{\~a}o austral, 
                         sobre grande parte da regi{\~a}o tropical da Am{\'e}rica do Sul 
                         (AS), al{\'e}m de influenciar a circula{\c{c}}{\~a}o 
                         atmosf{\'e}rica de grande escala sobre a regi{\~a}o. Perante 
                         isso, o principal objetivo deste estudo foi investigar a 
                         contribui{\c{c}}{\~a}o de oscila{\c{c}}{\~o}es dentro da 
                         escala intrasazonal para a ocorr{\^e}ncia de ver{\~o}es mais 
                         secos e mais chuvosos, durante o per{\'{\i}}odo de 1979 a 2022, 
                         e avaliar a diferen{\c{c}}a nessas an{\'a}lises em tr{\^e}s 
                         sub-regi{\~o}es distintas, que s{\~a}o afetadas pelo SMAS, sendo 
                         elas: Sudeste da Bacia Amaz{\^o}nica (SBA), Centro-Oeste (COB) e 
                         Sudeste (SE) do Brasil. Para tais analises, utilizou-se a 
                         t{\'e}cnica de quantis, para classificar os ver{\~o}es, a 
                         transformada de ondeletas, para avaliar a contribui{\c{c}}{\~a}o 
                         da escala sazonal temporalmente, e compostos de dados filtrados, 
                         para avaliar a contribui{\c{c}}{\~a}o destas escalas com 
                         rela{\c{c}}{\~a}o aos padr{\~o}es an{\^o}malos m{\'e}dios. Os 
                         resultados obtidos indicam que existe uma poss{\'{\i}}vel 
                         tend{\^e}ncia de aumento de ver{\~o}es mais secos e 
                         diminui{\c{c}}{\~a}o de ver{\~o}es mais chuvosos nas tr{\^e}s 
                         regi{\~o}es de an{\'a}lise e que os ver{\~o}es mais secos 
                         destas regi{\~o}es possuem uma rela{\c{c}}{\~a}o com anomalias 
                         positivas da temperatura da superf{\'{\i}}cie do mar sobre o 
                         Atl{\^a}ntico Sul Equatorial. Al{\'e}m disso, os ver{\~o}es 
                         mais secos das tr{\^e}s sub-regi{\~o}es s{\~a}o influenciados 
                         por um padr{\~a}o de um poss{\'{\i}}vel bloqueio, ao sul da AS, 
                         o qual est{\'a} relacionado {\`a} escala entre 11-30 dias. A 
                         an{\'a}lise de ondeletas para o SBA mostrou que a alta 
                         frequ{\^e}ncia exerce influ{\^e}ncia na ocorr{\^e}ncia de 
                         anomalias positivas e negativas de precipita{\c{c}}{\~a}o, 
                         indicando uma poss{\'{\i}}vel atua{\c{c}}{\~a}o de ondas 
                         equatoriais sobre a regi{\~a}o. J{\'a} sobre o COB e SE, 
                         notou-se na maioria dos casos aumento (diminui{\c{c}}{\~a}o) de 
                         precipita{\c{c}}{\~a}o associado ao aumento 
                         (diminui{\c{c}}{\~a}o) de energia nesta escala, sugerindo uma 
                         maior influ{\^e}ncia de sistemas transientes. Com 
                         rela{\c{c}}{\~a}o a escala submensal (11-30 dias) e intrasazonal 
                         (31-90 dias), as mesmas por vezes contribuem para o aumento da 
                         convec{\c{c}}{\~a}o, por vezes para a diminui{\c{c}}{\~a}o, 
                         sugerindo que estas escalas agem de forma a amplificar um sinal 
                         j{\'a} preexistente ao inv{\'e}s de gerar ou inibir a 
                         convec{\c{c}}{\~a}o sobre as regi{\~o}es. Al{\'e}m disso, a 
                         OMJ parece contribuir para a ocorr{\^e}ncia de v{\'a}rios picos 
                         negativos/positivos das anomalias de precipita{\c{c}}{\~a}o. Com 
                         rela{\c{c}}{\~a}o aos padr{\~o}es espaciais, sobre a 
                         regi{\~a}o SBA n{\~a}o se nota nenhuma circula{\c{c}}{\~a}o 
                         associada a ver{\~o}es mais secos e mais chuvosos, ou seja, 
                         padr{\~o}es de teleconex{\~o}es podem estar mais associados 
                         {\`a} din{\^a}mica destes ver{\~o}es, no que tange a escala 
                         sazonal. J{\'a} sobre o COB e SE notamse padr{\~o}es de 
                         circula{\c{c}}{\~o}es anticicl{\^o}nicas/cicl{\^o}nicas em 
                         altos e baixos n{\'{\i}}veis, associadas a escala submensal e 
                         intrasazonal, e que parecem contribuir para a ocorr{\^e}ncia de 
                         ver{\~o}es mais secos e mais chuvosos sobre as regi{\~o}es. 
                         Sobre o SE, os padr{\~o}es, no caso de anos chuvosos, est{\~a}o 
                         associados a modos do tipo PSA e poss{\'{\i}}vel deslocamento da 
                         ZCAS mais ao sul ou pr{\'o}ximo da sua posi{\c{c}}{\~a}o 
                         climatol{\'o}gica. Notam-se padr{\~o}es opostos no HN entre os 
                         anos secos e chuvosos nas regi{\~o}es COB e SE, e que sobre o SE, 
                         estes padr{\~o}es est{\~a}o associados as escalas submensal e 
                         intrasazonal, podendo agir como padr{\~o}es de teleconex{\~o}es 
                         dada a similaridade e sinais opostos. Em s{\'{\i}}ntese, este 
                         trabalho contribui para uma vis{\~a}o abrangente dos padr{\~o}es 
                         intrasazonais que impactam os ver{\~o}es mais secos e mais 
                         chuvosos em diferentes regi{\~o}es do Brasil. ABSTRACT: The South 
                         American Monsoon System (SAMS) is one of the main systems that 
                         contribute to the precipitation, during the southern summer 
                         months, over a large part of the tropical region of South America 
                         (SA), and exerts influence on the large scale atmospheric 
                         circulation over the region. In view of this, the main objective 
                         of this study was to investigate the contribution of oscillations 
                         within the intraseasonal scale to the occurrence of more dry and 
                         more rainy summers, during the period from 1979 to 2022, and to 
                         evaluate the differences in these analyzes in three distinct 
                         sub-regions, which are affected by SMAS, namely: Southeast of the 
                         Amazon Basin (SBA), Central-West (COB) and Southeast (SE) of 
                         Brazil. For such analyses, a quantile technique was used to 
                         classify summers, a wavelet transform to evaluate the contribution 
                         of the seasonal scale and composites of filtered data to evaluate 
                         the contribution of these scales in relation to the average 
                         anomalous patterns. The results obtained indicate that there is a 
                         possible tendency towards an increase in more dry summers and a 
                         decrease in more rainy summers in all three regions. More dry 
                         summers in these regions are related to positive sea surface 
                         temperature anomalies over the South Equatorial Atlantic. 
                         Furthermore, the more dry summers of the three sub-regions are 
                         influenced by a pattern of possible blocking to the south of SA, 
                         related to the scale between 11-30 days. The wavelet analysis for 
                         the SBA showed that high frequency influences the occurrence of 
                         positive and negative precipitation anomalies, indicating a 
                         possible action of equatorial waves over the region. Regarding COB 
                         and SE, an increase (decrease) in precipitation associated with an 
                         increase (decrease) in energy on this scale was noted in most 
                         cases, suggesting a greater influence of transient systems. 
                         Regarding the submonthly (11-30 days) and intraseasonal scales 
                         (31-90 days), they sometimes contribute to an increase in 
                         convection and sometimes to a decrease, suggesting that these 
                         scales act to amplify a pre-existing signal rather than generating 
                         or inhibiting the convection over the regions. Furthermore, the 
                         OMJ appears to contribute to the occurrence of diverses 
                         negative/positive peaks of precipitation anomalies. Regarding 
                         spatial patterns, over the SBA region there is no circulation 
                         associated with more dry and more rainy summers, that is, 
                         teleconnection patterns may be more associated with the dynamics 
                         of these summers, in terms of the seasonal scale. Over the COB and 
                         SE, anticyclonic/cyclonic circulations are noted at high and low 
                         levels, associated with a submonthly and intraseasonal scale, and 
                         which seem to contribute to the occurrence of more dry and more 
                         rainy summers over the regions. In the SE, the patterns are 
                         associated with PSA pattern and possible displacement of the SACZ 
                         further south or close to its climatological position are observed 
                         in rainy years. Opposite patterns are noted in H.N between dry and 
                         rainy years in the COB and SE regions, and over the SE, these 
                         patterns are associated with submonthly and intraseasonal scales, 
                         and can act as teleconnection patterns given the similarity and 
                         opposite signs. In summary, this work contributes to a 
                         comprehensive view of the intraseasonal patterns that impact the 
                         more dry and more rainy summers in different regions of Brazil.",
            committee = "Ferreira, Nelson Jesuz (presidente) and Gan, Manoel Alonso 
                         (orientador) and Seluchi, Marcelo Enrique and Calheiros, 
                         S{\^a}mia Regina Garcia",
         englishtitle = "Influence of intraseasonal variability on the inter-anual 
                         variability of the South American monsoon system",
             language = "pt",
                pages = "186",
                  ibi = "8JMKD3MGP3W34T/4APH8N8",
                  url = "http://urlib.net/ibi/8JMKD3MGP3W34T/4APH8N8",
           targetfile = "publicacao.pdf",
        urlaccessdate = "19 maio 2024"
}


Fechar