At some point it may be but with this inverted trough that pinches off a low, we're essentially facing the same outcome as a low hugging the coast and coming inland. The offshore low needs to take over very quickly to mute that effect but models show now that it won't, either from the southern stream flung way out at sea, chasing convection, sloppy phase, whatever the problem. There's always a problem this "winter"/turd in the punchbowl.