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As for the "cold air is hard to shift" trope, it is true to a limited extent. Today, for example, it's still only 2.1C here (with cold drizzle), despite several hours' worth of Atlantic onslaught. The reason is that ahead of the front the cold drains from the Continent; it was well below zero all morning in northern France and the dregs of that air get dragged across the Channel. It's only a shallow cold layer, but if it was one of those all-too-rare cases of a low approaching, then being deflected, it'd have been enough to maintain the cold.
It'll only be later this evening that the mild stuff really arrives in earnest. It's already there aloft, of course (hence the rain), but the cold wedge of air near the surface does indeed take some shifting... at least in the SE!
Originally Posted by: Retron