I would be inclined to agree. As part of observed data assimilation the model values would be "nudged" towards the observed values.
I think today may be a good example of that. It's been unbroken sunshine in Penzance (so far - it's now 13:00) This was correctly forecast. At 09:00 the temperature prediction for Penzance at 13:00 was 14C. At noon the forecast was lowered to 12C, whilst when I checked a moment ago it was 15.2C with a light F2 NE breeze.
However it is a fair bit cooler along the north coast with a directly onshore N sea breeze.
In addition there is now some cloud build up near the north coast, where the northerly sea breeze hits the ENE gradient wind.
A big advantage with being on the south coast, as opposed to the north, is that any cloud build up down the spine of the peninsula, or along the sea breeze front, is the opposite side of the sky to the sun!
I would be interested in any recommended reading on how the models work for actual weather at a location, what they include and what they don't (like salt spray in visibility forecasts). I think the models are remarkably good now at forecasting the synoptic situation 3 or 4 days ahead, but actual weather in a rather complicated area like coastal Cornwall can still be fairly poor. Certainly understanding of the sea breeze is still very limited. Long Rock, 1 mile east of Penzance and Marazion have some of the strongest sea breezes in Cornwall, with the marsh behind offering no resistance. Penzance sees only limited sea breeze development with the hills behind, and a different aspect. Something widely known (hence all the windsurfing at Long Rock) but not really appreciated by the models. Mid afternoon a fresh onshore sea breeze can become a N offshore in just a few minutes, due to the afternoon heating of the NW facing N coast. A quick look at forecast winds & actual on sunny days under very slack pressure, quickly reveals the limitations of the forecast winds.
Graham
Penzance