@MastersThesis{Mattos:1987:PaDeHo,
               author = "Mattos, Luiz Fernando de",
                title = "O papel de deforma{\c{c}}{\~a}o horizontal na frontog{\^e}nese 
                         na Regi{\~a}o Sul brasileira",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "1987",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "1987-11-04",
             keywords = "previs{\~a}o de tempo e estudos clim{\'a}ticos, 
                         frontog{\^e}nese, deforma{\c{c}}{\~a}o horizontal, 
                         climatologia, frontogenetic, horizontal deformation, 
                         climatology.",
             abstract = "Um estudo climatol{\'o}gico dos efeitos frontogen{\'e}tico e 
                         frontol{\'{\i}}tico que os campos de deforma{\c{c}}{\~a}o 
                         horizontal e de diverg{\^e}ncia provocam na baixa troposfera na 
                         Am{\'e}rica do Sul em particular e na regi{\~a}o do planeta 
                         compreendida entre 45N e 45S e elaborado. No Hemisf{\'e}rio Norte 
                         as mais conhecidas regi{\~o}es de fontogen{\'e}ticas foram 
                         reproduzidas e coincidem satisfatoriamente no centro da 
                         Am{\'e}rica do Norte e no mar do Jap{\~a}o. Quatro bandas de 
                         frontog{\^e}nese, orientadas de noroeste para sudeste, s{\~a}o 
                         localizadas no Hemisf{\'e}rio Sul, e uma delas se relaciona com a 
                         bem conhecida Zona de Converg{\^e}ncia do Pacifico Sul. A 
                         fun{\c{c}}{\~a}o fontogen{\'e}tica e de maior intensidade 
                         positiva na Patag{\^o}nia no ver{\~a}o (janeiro), n{\~a}o no 
                         inverno como acontece no Hemisf{\'e}rio Norte. Sobre a 
                         Am{\'e}rica do Sul, a linha que separa a {\'a}rea 
                         frontogen{\'e}tica da frontol{\'{\i}}tica passa pelo Estado do 
                         Rio de Janeiro e tamb{\'e}m esta orientada de noroeste para 
                         sudeste. E feito um estudo de caso de frontog{\^e}nese ocorrido 
                         de 28 a 31 de julho de 1980 sobre a Regi{\~a}o Sul do Brasil. E 
                         mostrado claramente como o papel da deforma{\c{c}}{\~a}o 
                         horizontal e importante na forma{\c{c}}{\~a}o, 
                         intensifica{\c{c}}{\~a}o, orienta{\c{c}}{\~a}o e movimento da 
                         frente. Na analise da se{\c{c}}{\~a}o vertical do campo de 
                         temperatura potencial ao longo do meridiano 50 W, que passa 
                         pr{\'o}ximo a Porto Alegre, e observada forte 
                         advec{\c{c}}{\~a}o fria atr{\'a}s do sistema frontal junto a 
                         superf{\'{\i}}cie e na baixa e media troposfera observa-se forte 
                         advec{\c{c}}{\~a}o quente. No estagio da matura{\c{c}}{\~a}o a 
                         frente se apresenta com todas as caracter{\'{\i}}sticas 
                         observadas por Sanders. ABSTRACT: A climatological study of the 
                         frontogenetic and frontolytic effects of the horizontal 
                         deformation and divergence fields in the lower troposphere over 
                         the part of the globe enclosed between 45N and 45S is made. The 
                         well-known frontogenetic regions of the Northern Hemisphere off 
                         the Rockies and the Japan Sea area are reproduced satisfactorily. 
                         Four bands of frontogenesis, aligned northwest to southeast, are 
                         clearly seen, and one of them agrees closely with the South 
                         Pacific Convergence Zone. The frontogenetic funtion over the 
                         central. and southern Argentina is strongest in sumner (January), 
                         which is in contrast to the Northern Hemispheric situation. Over 
                         South America, a northwest to southeast oriented line passing 
                         through the State of Rio de Janeiro divides the regions of 
                         frontogenesis to the southwest and frontolysis to the northeast. A 
                         case study of frontogenesis which occurred in the period 28-31 
                         July 1980 over South Brazil is presented. It shows clearly the 
                         importance of the horizontal deformation field in the formation, 
                         intensification, orientation and movement of the front. In the 
                         formative stage, strong warm advection ahead of the front-is 
                         observed in the lower middle troposphere and strong cold advection 
                         behind the front in the surface layers. In the mature stage the 
                         front presents all the characteristics observed by Sanders.",
            committee = "Rao, Vadlamudi Brahamananda (presidente) and Satyamurty, Prakki 
                         (orientador) and Silva Dias, Pedro Leite da and Ferreira, Marlene 
                         Elias and Lorenzzetti, Jo{\~a}o Antonio",
           copyholder = "SID/SCD",
         englishtitle = "The paper of horizontal deformation in the frontogenesis in South 
                         Brazilian regions",
             language = "pt",
                pages = "118",
                  ibi = "6qtX3pFwXQZGivnJSY/HettM",
                  url = "http://urlib.net/ibi/6qtX3pFwXQZGivnJSY/HettM",
           targetfile = "publicacao.pdf",
        urlaccessdate = "06 maio 2024"
}