@Article{VenâncioSSLDCMKTVBBSAN:2020:OcInOv,
               author = "Ven{\^a}ncio, Igor Martins and Shimizu, Mar{\'{\i}}lia Hamuri 
                         and Santos, T. P. and Lessa, D. O. and Dias, B. B. and Chiessi, C. 
                         M. and Mulitza, S. and Kuhnert, H. and Tiedemann, R. and 
                         Vahlenkamp, M. and Bickert, T. and Belem, A. L. and Sampaio, 
                         Gilvan and Albuquerque, A. L. S. and Nobre, Carlos Afonso",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Universidade Federal 
                         Fluminense (UFF)} and {Universidade Federal Fluminense (UFF)} and 
                         {Universidade Federal Fluminense (UFF)} and {Universidade de 
                         S{\~a}o Paulo (USP)} and {University of Bremen} and {University 
                         of Bremen} and {Alfred Wegener Institute for Polar and Marine 
                         Research} and {University of Bremen} and {University of Bremen} 
                         and {Universidade Federal Fluminense (UFF)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Universidade Federal 
                         Fluminense (UFF)} and {Universidade de S{\~a}o Paulo (USP)}",
                title = "Ocean-atmosphere interactions over the western South Atlantic 
                         during Heinrich stadials",
              journal = "Global and Planetary Change",
                 year = "2020",
               volume = "195",
                pages = "e103352",
                month = "Dec.",
             abstract = "Slowdowns of the Atlantic meridional overturning circulation 
                         during Heinrich stadials (HS) caused reductions in 
                         cross-equatorial heat transport, southward shifts of the 
                         Intertropical Convergence Zone and intensification of 
                         precipitation over eastern tropical South America. While these 
                         changes are well described, the associated spatial sea surface 
                         temperature (SST) patterns are still unclear. Here, we analyze 
                         proxy data to assess changes in ocean-atmosphere interactions 
                         during HS over the western South Atlantic. Our SST proxy records 
                         show contrasting patterns between the tropical (warming) and the 
                         subtropical (no change) western South Atlantic during HS. We 
                         propose that the distinct SST behavior in the subtropics was 
                         associated with the cloud cover effect of the South Atlantic 
                         Convergence Zone over the upper ocean.",
                  doi = "10.1016/j.gloplacha.2020.103352",
                  url = "http://dx.doi.org/10.1016/j.gloplacha.2020.103352",
                 issn = "0921-8181",
             language = "en",
           targetfile = "venancio_ocean.pdf",
        urlaccessdate = "27 abr. 2024"
}