@article{fdi:010063604,
  title = {{R}econstruction of southwestern {A}tlantic sea surface temperatures during the last century : {C}abo {F}rio continental shelf ({B}razil)},
  author = {{C}ordeiro, {L}gms and {B}elem, {A}. {L}. and {B}ouloubassi, {I}. and {R}angel, {B}. and {S}ifeddine, {A}bdelfettah and {C}apilla, {R}. and {A}lbuquerque, {A}. {L}. {S}.},
  editor = {},
  language = {{ENG}},
  abstract = {{M}odern sea surface temperatures ({SST}s) were estimated from {U}-37({K}') values often core-top sediment samples collected under the {C}abo {F}rio upwelling system and validated by comparison with satellite-derived {SST}s. {U}-37({K}')-{SST}s were found to reflect annual {SST} means in the offshore area and seasonal means (winter/spring) in the inshore and central areas. {T}he latter areas are mainly influenced by upwelling processes whereas the offshore area is under the influence of the thermal front of the {B}razil {C}urrent ({BC}). {SST} variability during the last century was then reconstructed from three short sediment cores. {T}he record showed a general cooling trend in the inshore and central areas, suggesting intensification of the upwelling process. {T}he trends at the offshore area reflected oscillations of the {BC} thermal front, with piling up of warmer {BC} waters closer to the coast since ca. 1950.},
  keywords = {{U}-37({K}')-{SST} ; {SW} {A}tlantic ; {C}abo {F}rio ; {W}estem boundary upwelling system ; {BRESIL} ; {ATLANTIQUE} {SUD}},
  booktitle = {},
  journal = {{P}alaeogeography {P}alaeoclimatology {P}alaeoecology},
  volume = {415},
  numero = {{SI}},
  pages = {225--232},
  ISSN = {0031-0182},
  year = {2014},
  DOI = {10.1016/j.palaeo.2014.01.020},
  URL = {https://www.documentation.ird.fr/hor/fdi:010063604},
}