@Article{OliveiraPeSoSaCuPa:2019:FiMeOc,
               author = "Oliveira, R. R. and Pezzi, Luciano Ponzi and Souza, Ronald Buss de 
                         and Santini, Marcelo Freitas and Cunha, L. C. and Pacheco, Felipe 
                         Siqueira",
          affiliation = "{} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and 
                         {Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Universidade Estadual 
                         do Rio de Janeiro (UERJ)} and {Instituto Nacional de Pesquisas 
                         Espaciais (INPE)}",
                title = "First measurements of the ocean-atmosphere CO2 fluxes at the Cabo 
                         Frio upwelling system region, Southwestern Atlantic Ocean",
              journal = "Continental Shelf Research",
                 year = "2019",
               volume = "181",
                pages = "135--142",
             keywords = "fluxos de carbono, Covari{\^a}ncia de V{\'o}rtices, Oceano 
                         Atl{\^a}ntico Sudoeste, ressurg{\^e}ncia de Cabo Frio, 
                         intera{\c{c}}{\~a}o oceano-atmosfera, camada limite 
                         atmosf{\'e}rica marinha.",
             abstract = "This study presents novel results about ocean-atmosphere 
                         CO2exchanges based upon novel directin situmea-surements of 
                         turbulentfluxes using the eddy covariance (EC) methodology. This 
                         study was carried out on theSoutheast coast of Brazil and the 
                         adjacent open ocean during two days of the austral winter of 2015, 
                         on board theRV Vital de Oliveira. This is thefirst time that the 
                         EC technique was used in this region for CO2flux studies. 
                         Theresults presented illustrate contrasting magnitudes of 
                         CO2fluxes measured on the open sea region(1.22 ± 2.08\μmol 
                         m\−2s\−1), the Brazil Current (\−2.92 ± 
                         1.25\μmol m\−2s\−1) and the coastal 
                         region(\−3.11 ± 1.67\μmol m\−2s\−1). 
                         The main cause of negative CO2fluxes, indicating a mean CO2sink 
                         behavior ofthis region, is due to the occurrence of the coastal 
                         upwelling phenomenon and the atmospheric conditions. Wefound that 
                         lower atmosphere local modulation due to sea surface temperature 
                         (SST) variations along the studyregion combined with the 
                         large-scale atmospheric synoptic conditions contributed to theflux 
                         behavior.",
                  doi = "10.1016/j.csr.2019.05.008",
                  url = "http://dx.doi.org/10.1016/j.csr.2019.05.008",
                 issn = "0278-4343",
                label = "lattes: 0537824080913130 3 OliveiraPeSoSaCuPa:2019:FiMeOc",
             language = "en",
           targetfile = "1-s2.0-S027843431830390X-main.pdf",
        urlaccessdate = "27 abr. 2024"
}