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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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#1
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cold gone.
sucker gap wider will? |
#2
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![]() "Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? A return to raging zonality. Where did that come from? Seemingly completely at odds with all the other models, for now at least, or perhaps it's the start of a trend. Ridiculously mild outlier perhaps. -- Col Bolton, Lancashire 160m asl |
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Col wrote:
"Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? A return to raging zonality. Where did that come from? Seemingly completely at odds with all the other models, for now at least, or perhaps it's the start of a trend. Ridiculously mild outlier perhaps. Hoorah! Here's hoping... -- Chris Swaffham, Norfolk |
#4
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On Jan 20, 8:32*pm, Chris Smith wrote:
Col wrote: "Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? A return to raging zonality. Where did that come from? Seemingly completely at odds with all the other models, for now at least, or perhaps it's the start of a trend. Ridiculously mild outlier perhaps. Hoorah! Here's hoping... -- Chris Swaffham, Norfolk It came from a 3-run development of the ECM Col. It's not out of nowhere, though it is an extension of what had happened on the previous 12z and the 00z runs and, as you say, it is at odds with other models. The 00z ens show that the operational was close to the mean (if a little warmer) and the mean trend, gfs+ECM, past 8 days, is milder, rather than colder. Still nothing is sorted, but there has been some real changes in the ECM output over the last 24 hours, whereas the gfs (and GEM) still show colder. I have a feeling there may be a believable 10-day solution tomorrow (or am I just hoping for this) |
#5
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![]() "Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? The ECM is going a tad wild recently with deep low developments popping up all over the place all depending on how the upper trough in the western atlantic disrupts. Trough disruption there should tend to build a Scandi high under normal circumstances, perhaps that's where the problem lies, the usual difficult trough disruption process. The most consistent model of late has been UKMO but you only see that to T+144. That model is basically going for an anticyclonic easterly. A lot of dry weather but snow showers in east and south. I'm sticking with that for the time being as it is the simplest and what one would predict from first principles without models to confuse us. No sucking from me :-) Will -- |
#6
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Will Hand wrote:
"Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? The ECM is going a tad wild recently with deep low developments popping up all over the place all depending on how the upper trough in the western atlantic disrupts. Trough disruption there should tend to build a Scandi high under normal circumstances, perhaps that's where the problem lies, the usual difficult trough disruption process. The most consistent model of late has been UKMO but you only see that to T+144. That model is basically going for an anticyclonic easterly. A lot of dry weather but snow showers in east and south. I'm sticking with that for the time being as it is the simplest and what one would predict from first principles without models to confuse us. No sucking from me :-) Will GFS has been quite consistent with an easterly as well. Strange how ALL models have their good and bad points / weather favourites. -- Keith (Southend) http://www.southendweather.net e-mail: kreh at southendweather dot net |
#7
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![]() "Keith(Southend)" wrote in message ... Will Hand wrote: "Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? The ECM is going a tad wild recently with deep low developments popping up all over the place all depending on how the upper trough in the western atlantic disrupts. Trough disruption there should tend to build a Scandi high under normal circumstances, perhaps that's where the problem lies, the usual difficult trough disruption process. The most consistent model of late has been UKMO but you only see that to T+144. That model is basically going for an anticyclonic easterly. A lot of dry weather but snow showers in east and south. I'm sticking with that for the time being as it is the simplest and what one would predict from first principles without models to confuse us. No sucking from me :-) Will GFS has been quite consistent with an easterly as well. Strange how ALL models have their good and bad points / weather favourites. It's not so much the models Keith it is the handling of complex situations. What seems to be happening is that the wavelength has shortened over Canada this weekend with an upper trough coming east. Just downstream of this (over western Atlantic) is another upper trough which has a strong SSW flow on its eastern edge, in other words a confluent but relaxing and eventually disrupting upper trough. The strong SSW flow causes and helps to reinforce the downstream Scandi/continental high through ageostrophic effects at the right exit. Under normal circumstances this disruption process would force any Atlantic lows to southern or even west of Greenland and build the Scandi high to the north. Unfortunately the complication of the Canadian shortwave means that the confluent/disrupting Atlantic trough gets a "kick up the backside" which crucially alters its orientation to more SW'ly or even WSW'ly bringing more flow into the Euro high preventing it from building northwards. Thus it is a fine balance as to how it builds and all depends on the western Atlantic developments. Interestingly 18Z GFS builds the high in the short term (rest of run not in yet), but I fancy maybe a strong SW flow eventually getting into NW Scotland so *could* end up milder there. Will -- |
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On Jan 20, 10:15*pm, "Will Hand" wrote:
"Keith(Southend)" wrote in message ... Will Hand wrote: "Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? The ECM is going a tad wild recently with deep low developments popping up all over the place all depending on how the upper trough in the western atlantic disrupts. Trough disruption there should tend to build a Scandi high under normal circumstances, perhaps that's where the problem lies, the usual difficult trough disruption process. The most consistent model of late has been UKMO but you only see that to T+144. That model is basically going for an anticyclonic easterly. A lot of dry weather but snow showers in east and south. I'm sticking with that for the time being as it is the simplest and what one would predict from first principles without models to confuse us. No sucking from me :-) Will GFS has been quite consistent with an easterly as well. Strange how ALL models have their good and bad points / weather favourites. It's not so much the models Keith it is the handling of complex situations. What seems to be happening is that the wavelength has shortened over Canada this weekend with an upper trough coming east. Just downstream of this (over western Atlantic) is another upper trough which has a strong SSW flow on its eastern edge, in other words a confluent but relaxing and eventually disrupting upper trough. The strong SSW flow causes and helps to reinforce the downstream Scandi/continental high through ageostrophic effects at the right exit. Under normal circumstances this disruption process would force any Atlantic lows to southern or even west of Greenland and build the Scandi high to the north. Unfortunately the complication of the Canadian shortwave means that the confluent/disrupting Atlantic trough gets a "kick up the backside" which crucially alters its orientation to more SW'ly or even WSW'ly bringing more flow into the Euro high preventing it from building northwards. Thus it is a fine balance as to how it builds and all depends on the western Atlantic developments. Interestingly 18Z GFS builds the high in the short term (rest of run not in yet), but I fancy maybe a strong SW flow eventually getting into NW Scotland so *could* end up milder there. Will --- Hide quoted text - - Show quoted text - The 00z gfs shows what I was thinking yesterday that it might; a sinking high and milder, west to north-westerly conditions affecting us at 10 days around the top of the high. Is the death knell of the deep cold being tolled? Or is this just another model twist? |
#9
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On Jan 21, 6:09*am, Dawlish wrote:
On Jan 20, 10:15*pm, "Will Hand" wrote: "Keith(Southend)" wrote in message ... Will Hand wrote: "Terry Tibbs" wrote in message ... cold gone. sucker gap wider will? The ECM is going a tad wild recently with deep low developments popping up all over the place all depending on how the upper trough in the western atlantic disrupts. Trough disruption there should tend to build a Scandi high under normal circumstances, perhaps that's where the problem lies, the usual difficult trough disruption process. The most consistent model of late has been UKMO but you only see that to T+144. That model is basically going for an anticyclonic easterly. A lot of dry weather but snow showers in east and south. I'm sticking with that for the time being as it is the simplest and what one would predict from first principles without models to confuse us. No sucking from me :-) Will GFS has been quite consistent with an easterly as well. Strange how ALL models have their good and bad points / weather favourites. It's not so much the models Keith it is the handling of complex situations. What seems to be happening is that the wavelength has shortened over Canada this weekend with an upper trough coming east. Just downstream of this (over western Atlantic) is another upper trough which has a strong SSW flow on its eastern edge, in other words a confluent but relaxing and eventually disrupting upper trough. The strong SSW flow causes and helps to reinforce the downstream Scandi/continental high through ageostrophic effects at the right exit. Under normal circumstances this disruption process would force any Atlantic lows to southern or even west of Greenland and build the Scandi high to the north. Unfortunately the complication of the Canadian shortwave means that the confluent/disrupting Atlantic trough gets a "kick up the backside" which crucially alters its orientation to more SW'ly or even WSW'ly bringing more flow into the Euro high preventing it from building northwards. Thus it is a fine balance as to how it builds and all depends on the western Atlantic developments. Interestingly 18Z GFS builds the high in the short term (rest of run not in yet), but I fancy maybe a strong SW flow eventually getting into NW Scotland so *could* end up milder there. Will --- Hide quoted text - - Show quoted text - The 00z gfs shows what I was thinking yesterday that it might; a sinking high and milder, west to north-westerly conditions affecting us at 10 days around the top of the high. Is the death knell of the deep cold being tolled? Or is this just another model twist?- Hide quoted text - - Show quoted text - And then when you think you may be seeing something that may be an actual solution, the ECM doesn't sink the high and suggests, instead, the northerly that has been hinted at a couple of times in the last 2 days by the ECM and once in a gfs run. Nothing sorted at 10 days still. Back to the lookout post! |
#10
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In article
, Dawlish writes: And then when you think you may be seeing something that may be an actual solution, the ECM doesn't sink the high and suggests, instead, the northerly that has been hinted at a couple of times in the last 2 days by the ECM and once in a gfs run. Nothing sorted at 10 days still. Back to the lookout post! Things are improving, though. Yesterday, things didn't even seem to be sorted at five days, never mind at ten! ![]() -- John Hall "Acting is merely the art of keeping a large group of people from coughing." Sir Ralph Richardson (1902-83) |
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