I don't think that was the case.
1) When Debbie was a swirl of clouds, forecast models struggled since there was no defined center yet, that's why there was a large disparity in initial track, anywhere from eastern Gulf to the southwest Atlantic. Models would just pick up on random bursts of convection as a "Center". However, once the swirl organized into a tropical wave and eventually developed a more defined center, it was much easier for models to get a handle on the track.
2) With no steering flow, Debbie just sat and spun across the Southeast and meandered into the Atlantic, off the coast. Now that we have somewhat of a trough digging up north, combined with an approaching front, the remnants of Debbie are being driven northwards.
I don't think strength of ATL ridge played much of a factor here.