Abstract

The rainy season of north-Northeastern Brazil (NE), one of the tropical regions with the largest rainfall interannual variability, is associated with the Intertropical Convergence Zone (ITCZ) influence, which is located in the southermost position during this season (March-April-May). However, there is a large interannual variability in the ITCZ position, associated with atmospheric and oceanic anomalies, responsible for dry or wet years in the region. Besides the tropical Pacific Sea Surface Temperature (SST) anomalies and the Tropical Atlantic SST gradient influences on this variability, extratropical atmospheric influences are identified over the North and South Atlantic. Composites of cases with anomalous precipitation during the middle of the rainy season (April) indicate the El Nino-Southern Oscillation (ENSO) features and northern and southern Atlantic atmospheric anomalies in December-January-February (DJF). When El Nino and La Nina years are removed from the composites of dry and wet cases, respectively, the centers of action over the extratropical North Atlantic in DJF remain, and features of extratropical South Hemisphere become more evident. The tropical SST dipole is still present with inverted signs in each case, consistent with the NE precipitation anomalies. The main mode of variability in the Southern Hemisphere (South Annular Mode) and in the Northern Hemisphere (North Annular Mode) is present in DJF during the dry cases. These annular patterns occur in the composites of Northeast Brazil precipitation anomalies including or excluding ENSO years. Therefore, besides ENSO relations with SAM discussed in previous studies, another connection exists over the South Atlantic, linking anomalies between high and tropical latitudes. The precipitation anomalies over NE have contributions of the two extratropical Atlantic hemispheres regions. The atmospheric anomalies observed in the pre-rainy season can be a helpful tool in monitoring the North Northeastern B

Highlights

  • The rainy season in the northern sector of Northeastern Brazil (NE) occurs in March-April-May (MAM), associated with the displacement of the Intertropical Convergence Zone (ITCZ) along the year, following the seasonal warm Sea Surface Temperature (SST) displacement north-south (Hastenrath, 1984)

  • The Sea Level Pressure (SLP) anomalies composites in DJF for wet and dry cases display the North Atlantic extratropical high-low dipole, with opposite signs in each category (Figure 3, contour), similar to that found in Souza and Cavalcanti (2009) in cases of the ITCZ displacement

  • Removing the El Niño-Southern Oscillation (ENSO) influence, both Atlantic hemispheres contribute to the precipitation anomalies over NE

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Summary

Introduction

The rainy season in the northern sector of Northeastern Brazil (NE) occurs in March-April-May (MAM), associated with the displacement of the Intertropical Convergence Zone (ITCZ) along the year, following the seasonal warm Sea Surface Temperature (SST) displacement north-south (Hastenrath, 1984). The ITCZ variability depends on the tropical inter-hemispheric Atlantic SST and atmospheric circulation mechanisms

Wet and Dry NE Brazil
Data and Method
Composites without ENSO Years
ASLP ATLSUL
La Niña El Niño
Conclusion
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