摘要：The Atlantic multidecadal oscillation (AMO) is a 60–70 year pattern of sea-surface temperature (SST) variability in the North Atlantic commonly ascribed to internal ocean dynamics and changes in northward heat transport. Recent modeling studies; however; suggest that SSTs fluctuate primarily in response to major volcanic eruptions and changes in atmospheric circulation. Here; we utilize historical SST; atmospheric reanalysis; and stratospheric aerosol optical depth data to examine the basic evidence supporting a volcanic link. We find that cool intervals across the North Atlantic coincide with two distinct episodes of explosive volcanic activity (1880s–1920s and 1960s–1990s); where key eruptions include 1883 Krakatau; 1902 Santa María; 1912 Novarupta; 1963 Agung; 1982 El Chichón; and 1991 Pinatubo. Cool SST patterns develop in association with an increased prevalence of North Atlantic Oscillation (NAO) atmospheric patterns caused by stratospheric aerosol loading and a steepened poleward temperature gradient. NAO patterns promote wind-driven advection; evaporative cooling; and increased albedo from enhanced Saharan dust transport and anthropogenic aerosols. SSTs across the subpolar gyre are regulated by strength of low pressure near Iceland and the associated wind-driven advection of cold surface water from the Labrador Sea. This is contrary to an interpretation that subpolar SSTs are driven by changes in ocean overturning circulation. We also find that North Pacific and global mean SST declines can be readily associated with the same volcanic triggers that affect the North Atlantic. Thus; external forcing from volcanic aerosols appears to underpin multi-decade SST variability observed in the historical record.
