Influence of the PDO and AMO patterns on the air temperature in Brazil during the austral winter
DOI:
https://doi.org/10.5902/2179460X55312Keywords:
Climatic variability, SST, Teleconnections, PDO, AMOAbstract
Anomalies of sea surface temperature (SST) favor the emergence of climatic variability modes, which can be transferred by atmospheric teleconnections to different regions of the globe. The present study sought to identify influences of the Pacific Decadal Oscillation (PDO) and the Atlantic Multidecadal Oscillation (AMO) on the air temperature in Brazil, during the period from 1901 to 2012. It was found that the negative periods of the PDO and AMO (1901-2012) have a greater influence on the South and North regions of Brazil. When these modes of variability are in opposite phases (1901-1927), they mainly interfere in the southern region of Brazil. On the other hand, when the PDO is in the negative phase and the AMO is moving from the positive to the negative phase (1944-1975), the northern region of Brazil is more influenced.
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