I think what's deceiving with the surface low placement on both the operational and ensemble maps is the surface low feature is actually elongated (occluded?) and the location of the absolute lowest pressure is irrelevant. It's better to look at the surface wind barbs to get a handle on how the low-level flow is interacting with the low from the CAD high. Then once in Georgia, it of course begins the handoff to the coastal in SC.I need to see these gulf members please. This is what I have:
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That said, the GFS did take another tick south with the overall surface flow although it didn't appear to change the model's thermal profiles much at all...yet.