This is not like the easterlies you have in mind as the wind at the 1000 - 900 hPa is very strong and directly from a very large body of cold water. It doesn't allow for vertical mixing either upwards or downwards.
I have seen something similar even in the Greek islands; T850 > 25C, yet surface temps in the mid to high 20s (same as the SSTs). The locals call it natural air con and they love it.
If this is truly the case... then it implies the forecasters at the Met Office are inadequately educated on such things. I can't see why else their video forecast maximums are widely 2-5*C above the numerical modelling; they have the same orientation of the high and resulting winds.
So I'm not sure there can actually be zero vertical mixing. Just less of it than in a weaker, drier easterly. It seems some must have managed to happen today, despite the short heated ground fetch enforced by the low cloud belt, to permit 23-25*C in the far south and southwest today in what were unusually windy conditions for late June (most of the local small-talk this afternoon has begun with how weird it feels).
Tomorrow brings the greatest test of the Met Office forecasting so far in this spell of weather, assuming the low cloud dissipates or clears away overnight (and I'm not 100% sure about that as it was supposed to be mostly absent by now, but there's loads of it persisting!).
If tomorrow proves sunny yet only maxes out in the low-mid 20s across central and western parts of England and most of Wales, then it will be time to start wondering what on Earth those who modified the raw model data so far upward were thinking of.
...although I must admit, I've already thought that a little bit today with respect to the central-third of England, but have put that down to another classic case of underestimating the stubbornness of British low cloud formations .
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