Yeah right.
I wonder though if in the modeling world if there are any hypotheses as to why the GFS likes to overmix in the medium/long-range. Hell, the GFS can even tend to overmix in the short range. I find it interesting how the NAM tends to undermix while the GFS tends to overmix. There must be something within the boundary layer physics of each model contributing to this.
I mean look at this sounding right around the 102°F in northeast Mass. We're mixing up to ~750mb there and that's gotta be as close to superadiabatic lapse rate as you can get. I doubt there are any records on this anywhere but I would go out and wager we hardly, if ever, even came close to mixing to such a level. This is the type of sounding you would expect to see within the Southwest.
As dendrite always mentions to keep reality in check, we almost always see the outcome be temperatures several degrees cooler with dewpoints several degrees warmer.
925 temps are modeled to be around 30°C with 850 temps around 23°C. Don't you want to see 850 temps more around 26 or so to get a legit shot for 100 here (assuming full sun/mixing)?