Evidence is presented for local and remote wind-forcing of deep ocean currents in three frequency bands (corresponding to 3.7--8 day, 8--22 day, and 23--82 day periods) at a two-year mooring in the eastern North Atlantic. Coherence between current meter velocities and estimated wind stress curl is largest for the deepest instrument (3000 m) and decreases toward the surface. The strongest evidence is found at 3000 m depth in the high frequency (3.7--8 day) band, where both components of velocity are significantly coherent with wind stress curl. Meridional velocity at 3000 m is also significantly coherent with wind stress curl in the low frequency (23--82 day) band, while zonal velocity in the low frequency band and both velocity components in the intermediate frequency (8--22 day) band are only marginally coherent. The results are compared with a stochastically-forced linear quasi-geostrophic model that includes a simple representation of the mid-Atlantic Ridge. Good agreement between predicted and observed coherences is found for the 3000 m currents in the high frequency band, but only partial agreement is found between predicted and observed coherences in the low frequency band, and little agreement in the intermediate band. Kinetic energy levels at 3000 m are well predicted in all three bands. For the shallower instruments (1100 m and 500 m), observed coherences are at most marginally significant and energy levels are considerably higher than the theory predicts. Including an upper-layer mean flow in the model improves the prediction of energy levels at the shallower instruments. ¿ American Geophysical Union 1990