Ian Docwra
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Depends where you are - how thick the cloud is, etc. Heavier snow showers will both cut out the solar warming and bring colder air down with the snow, lowering the temperature. The same cycle can continue until late afternoon when the sun's warmth is gone. Then the opposite effect takes over - clear skies lead to rapid cooling as the earth radiates heat away, but clouds limit the cooling through their insulating effect.
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Regarding temperatures, something that may be worth bearing in mind is that the sun at the moment is getting high enough to provide a little warmth even through moderate cloud. This means that its radiative effect can warm many surfaces and objects enough to raise them a little above freezing even when it's snowing lightly. This includes cars and conservatories, paths with some bare areas showing (dark absorbs heat much more than snow) and metal garden furniture, for example. These can all be sitting at a degree or so above freezing even if the air temperature is not. The stronger wind reduces the effect as it drags the heat away and evaporation cools the surface. Today's wind is much lighter than yesterday's and the warming effect is more apparent. If we were in mid-December, solar warming would be much less significant.
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A number of reasons are possible - for a start: 1. Drains or pipes running underneath (we have this with our front path) 2. The ground still has some deeper warmth from the mild weather before the snow and this leaches upwards 3. Salt residue 4. Generally, slabs and concrete transmit heat better than grass, and heat leaks from houses' foundations to surrounding areas and warms them enough to prevent anything but brief freezing in strong winds, when the heat leaking out is overwhelmed by the constant influx of colder air. Lighter winds can't take that heat away fast enough.
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At the moment it looks as if the colder influence will dominate for the foreseeable future - how cold exactly is unclear, but we are getting to mid-February soon and the sun is getting stronger. However, clear nights can still produce some very low minima over snow cover (-15C last night in Scotland, and the same tonight).
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The wind has been coming off the North Sea for the entire cold spell. An E, rather than NE, wind has a shorter sea track so should make it colder still, but there are other factors at play - the wind is a little lighter today and there is a little more solar warming through the thinner clouds, pushing the temperature up a tad. Remember we are now nearly a month and a half on from the shortest day so the sun is gaining a little more power. We are now at -0.6c here (from -1.2C an hour ago) in NE Surrey with a few flakes falling, but the sky is much brighter than yesterday - i.e. more insolation reaching the surface.
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The radar echoes from the EA/Essex area of snowfall seems to have several gaps where it goes from heavy snow to nothing without any gradation at all, almost as if in a dead zone. What's causing this, as I can't see it actually being the case that there are small fixed areas embedded in heavy snow where it's bone dry without any tail-off into those areas? In the screenshot they are the white patches in the leading area of green, which, on the animation, stay where they are as the green echoes pass by (like rocks in a stream).