Ian Docwra
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Sadly, it's probably too much to the N of E to get the heavy stuff there. We've just had a flurry but the main stream is east of us again. It went from a heavy E-W streamer last night to pivoting over us to the current NE streamer, but with it dying out for the period when it pivoted - i.e giving us nothing. Nature can be cruel!
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It's possible where significant snow still remains and with the wind falling much lighter. The night is predicted to be largely clear, giving rapid radiation cooling. London won't get that low, but rural areas, especially frost hollows, could see -10C. It was -16.7C in northern Scotland last night and could be around that there again tonight.
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Again, the very mild and very wet lead up to this has led to much ground snow loss, when a cold, frosty precursor would not have. Bear in mind that if all the snow that fell had accumulated (on frosty, dry ground) many more areas would have a significant depth. That's exactly what happened here on 24 January, when snow from the west settled on a hard frost - not a flake was wasted!
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The Met Office is doing what the BBC does - their SE regional text sumary talks of scattered snow showers in the east of the region overnight, while its forecast map shows a significant streamer NE to SW right across the middle of the region tonight/early tomorrow morning, with nothing to the east of that. Consistency, even if wrong, is far better than such randomness.
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The sun is now about six weeks higher than its minimum in December and is starting to have a noticeable impact. Even in moderate cloud its radiation can melt snow in sub-zero air, whereas in December/early January it is too weak unless fully sunny. February snow in southern Britain is always likely to melt in any sunshine when it's powdery as it has more air/surface area to absorb warmth. A bit of thaw and re-freeze toughens it up a little although reduces the volume/depth.
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Yes, and the fact that the water has been relatively warm recently after what has been a mild winter. We have two large ponds and they are only slushilly(!)-covered. With still, clear nights they should freeze easily. A calm, clear night has a steep temperature gradient from the ground/water up, whereas the wind both keeps the water moving and mixes up the air so that the water surface-level will be exposed to, say, -2C whereas it might be -8C in still air with the steeper gradient.