Mr. Chapman et Ma. Maslin, Low-latitude forcing of meridional temperature and salinity gradients in the subpolar North Atlantic and the growth of glacial ice sheets, GEOLOGY, 27(10), 1999, pp. 875-878
Sea-surface temperature (SST) and salinity (SSS) records obtained from two
deep-sea cores have been used to reconstruct meridional gradients in the mi
d-latitude North Atlantic over the past 40 k.y. During the buildup of ice s
heets toward the last glacial maximum, SST and SSS gradients between 40 deg
rees and 50 degrees N increased by 6-8 degrees C and similar to 2 parts per
thousand, respectively. This trend represents a two-fold increase in surfa
ce-water gradients between 40 and: 20 ka and strongly overprints the signal
of high-frequency climatic oscillations, We attribute the gradual intensif
ication of meridional SST and SSS gradients to a precession-driven increase
in advection within the glacial North Atlantic Current resulting from chan
ges in low-latitude insolation and seasonality. A strongly zonal ocean circ
ulation pattern, maintained by greater advection and enhanced heat storage
within the subtropical ocean at the last glacial maximum, persisted until c
a. 20 ka, when a decrease in glacial SST gradients, coincident with a reduc
tion in low-latitude climate forcing, marked the initiation of the last deg
laciation.