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Journal of Climate
The tropical Atlantic wind response to El Niñ o forcing is robust, with weakened northeast trade winds north of the equator and strengthened southeast trade winds along and south of the equator. However, the relationship between sea surface temperature (SST) anomalies in the eastern equatorial Pacific and Atlantic is inconsistent, with El Niñ o events followed sometimes by warm and other times by cold boreal summer anomalies in the Atlantic cold tongue region. Using observational data and adoi:10.1175/jcli-d-11-00553.1 fatcat:kgs7yczsxna75pwk44mjitqnou