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43:, and convergent winds oriented in a northwest–southeast manner across southeast Brazil into the southwest Atlantic Ocean. By definition, the feature is a
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141:"The South Atlantic Convergence Zone: Intensity, Form, Persistence, and Relationships with Intraseasonal to Interannual Activity and Extreme Rainfall"
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63:, while easterly wind anomalies indicate breaks of activity along the SACZ. The feature is also strongest with negative anomalies in the
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are tied to the strength of this zone, where westerly wind anomalies correlate to active phases of the South
American
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pattern lie over the southern
Atlantic Ocean, while opposite conditions prevail across the northern Atlantic Ocean.
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passes into the region, due to the enhanced upper divergence. Low level winds over
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activity along the feature magnifies over three or more days when the
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172:"Impact of SST Anomalies on the South Atlantic Convergence Zone"
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Leila M. V. Carvalho; Charles Jones & Brant
Leibman (2003).
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R. De
Almeida; R. Haarsma; E. Campos & A. Sterl.
24:"SACZ" redirects here. For the city in Poland, see
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47:. It is strongest in the warm season.
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39:, is an elongated axis of clouds,
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86:"South Atlantic convergence zone"
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109:Glossary of Meteorology (2009).
84:Glossary of Meteorology (2009).
115:American Meteorological Society
90:American Meteorological Society
33:South Atlantic convergence zone
1:
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53:Madden–Julian oscillation
322:Regional climate effects
65:sea surface temperature
261:-related article is a
204:–related article is a
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20:SACZ in December 2022
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317:Atmospheric dynamics
312:Tropical meteorology
149:Journal of Climate
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332:Climatology stubs
327:Meteorology stubs
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154:. Retrieved
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123:. Retrieved
119:the original
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93:. Retrieved
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49:Thunderstorm
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259:climatology
202:meteorology
306:Categories
156:2009-06-05
125:2009-06-04
95:2009-06-05
71:References
26:Nowy SÄ…cz
57:RondĂ´nia
61:monsoon
257:This
200:This
175:(PDF)
144:(PDF)
35:, or
263:stub
206:stub
37:SACZ
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