Just throwing this out there to clarify that all Atlantic ridges, weak and strong, are not created equally. Storm motion has just as much to do with the position and orientation of the ridge axis, as it does its strength.
This is idealized, or course, but a stronger ridge will generally send a TC farther westward at a faster rate of speed, however, this assumes a mostly zonal (W-E) orientation to the ridge. The more meridional (N-S) component there is, or develops, the more poleward a TC can and will move. Even a weaker Atlantic ridge will continue to send a TC generally westward (let's not get into beta-effect or drift

) , just at a slower forward speed, and that motion will continue just as long as there isn't a breach or significant weakness in said ridge.
