 11-year solar cycle influences on winter climate over the North Atlantic European region have been studied using lead-lag multilinear regression technique with a sliding window of 44 years over the period 1751-2016, and results confirm previous analyses showing a statistically significant 2- to 4-year lagged mean sea-level pressure response centered over the Azores region. Stronger SC signals tend to appear in periods when the SC forcing amplitudes are relatively larger, an individual month analysis indicates that the consistent lagged response in December, January, February average arises primarily from early winter months associated with ocean feedback processes. This article was authored by Hedy Ma, Aishin Chen, Leslie Gray, and others.