GFS handling of the initial interaction doesn't really differ from other models. But its upper level setup? Night and day.
Take a look at the GFS' shear early on August 1st, while the wave is just northeast of PR. The wave would be dealing with 20kt of shear at this point, decoupling the developing area of vorticity severely and injecting dry air.

The Euro at the same time? Vastly different. There is an anticyclone situated over the wave envelope. Shear is almost negligible. The wave starts slowly building momentum starting here on the model.

The CMC is quite similar to the Euro as well.

The end result? By this frame, the 500mb and 850mb vorticity maxima are displaced by over 400 miles (!) on the GFS. The GFS is all alone in this short term high-shear solution.