Surface winds and surface ocean hydrography in the subpolar North Atlantic
appear to have been influenced by variations in solar output through the en
tire Holocene. The evidence comes from a close correlation between inferred
changes in production rates of the cosmogenic nuclides carbon-14 and beryl
lium-10 and centennial to millennial. time scale changes in proxies of drif
t ice measured in deep-sea sediment cores. A solar forcing mechanism theref
ore may underlie at least the Holocene segment of the North Atlantic's "150
0-year" cycle. The surface hydrographic changes may have affected productio
n of North Atlantic Deep Water, potentially providing an additional mechani
sm for amplifying the solar signals and transmitting them globally.