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Everything posted by Kentish Kiwi
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I've been outside for the last couple of hours on the golf course doing the drinks buggy and can confirm its bloody cold with a strengthening icy wind. Some shallow cumulus/stratocumulus moving in from the east - not the type that looks as though it's going to bubble up anytime soon though. 1C here with a windchill well below zero. Sun coming out has brought a bit of a thaw to yesterday's covering.
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-17 850's was mentioned by Steve Murr as the lowest ever recorded over the UK but this was corrected to -19, during the historic easterly of 1987. The charts earlier this week were quite incredible showing -17/18 on occassions and frankly were always more than likely to be downgraded by a few degrees.
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Heavy snizzle here and very dark, poor visability. Hasn't stopped once today. Putting greens are completely white with a good covering while it is just beginning to accumulate on the grass/fairways. Concrete surfaces etc completely soaked, going to be quite a hazard if temperatures drop quickly this afternoon/evening and it freezes up...
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Yes, I completely agree. The convection is not at all deep or vigorous (although I never claimed it was) and is unlikely to lead to anything noticeable today, but it is convection - just very weak. Certainly not the type of conditions you need for a real streamer to form. It seems quite clear that the air is just not unstable enough for anything significant to develop... Have to say I'm quite worried we wont see any real heavy, prolonged snow from this easterly spell and we may be left to deal with conditions similar to today for the remainder of the week. I'll be very glad to be proved wrong though.
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I think there is a bit of a disparity here of our understanding of convection... My understanding of it was the formation of showers due to rising air away from frontal systems. This certainly seems to be the case with those showers pushing in off the north sea. I'm by no means saying the convection is vigirous but it is at least evident in a very slight way. Am I mistaken with this? I don't see how the precipitation is forming out of thin air if it is not convection. It's also worth noting that while it may be sleet for you on the coast, I'm fairly confident the precipitation will be of snow this far inland. It has been throughout the day so far, well grauple/snizzle anyway, but not sleet.
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From what I've read, the general thoughts are that the wind will dry out significantly by mid-week, even in spite of the increased thermal gradient... I don't fully understand why this is expected, except for it being an intensely cold and dry airmass, presumably differing to the current air we have now which is slightly more... 'moist'. Is this anything to be concerned about in your opinion? Is the air pressure expected to be any higher than it is now by the end of the week?
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So your view on things is that the undeniably high pressure will hardly factor into things given the potential lapse rates on offer? Personally the idea that shower activity will be limited in a general sense but those that break the cap will be quickly develop into intense cells seems a reasonable assumption. It is pretty much unknown territory for the UK though, and will more than likely come down to a now-casting scenario, even more so than usual!
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That was my main concern with the 18z. If the winds turn just a hint too far northerly, East Anglia will eat up all the moisture for my area while Maidstone eastwards gets hammered. It is fair to say an ENEerly is generally a better wind direction for the SE region as a whole, giving a better spread of snowfall, particularly further inland? P20 from the pub run looks like an amazing evolution in terms of potential countrywide snowfall from an undercutting low, it's a shame no other operational run has hinted at something like that. Ahh, your height is probably the significant factor there. If you're looking down on Sevenoaks Town you must be well above 200m.
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I managed >45cm from the November/December 2010 streamer from (if I remember correctly) 70 hours of continuous snowfall, albeit it very light for periods. Noticeably more up at the top of the downs. Also, for me December 2009 was significantly better than February of that year, which, as you mention, illustrates just how subtle changes in the wind direction can have big impacts on the variation in snow depths. This area is pretty well situated for any Thames streamer as long as the wind is a consistent E/ENE and doesn't veer too far north into more of a NEerly. I'm not sure if anyone else will get what I'm talking about, but does anyone have an explanation for why, in easterlies, the wind seems to suddenly turn much more northerly in character as it moves in a westerly direction further inland, particularly so as it becomes lighter?