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The Beast from the East
31 December 2014 14:34:47


As a passing thought,I wonder if in the days ahead we'll be adding to 'that' list that gets posted on here about Easterlies and 'Where did they come from'


 


Originally Posted by: Snow Hoper 


More 06z GEFS members go for it than the 00z set, not enough to be significant, but I wonder...


It seems a race against time, but as mentioned, Greece is probably the place to be in 10 days time. Wont do their economy any good!


"We have some alternative facts for you"
Kelly-Ann Conway - special adviser to the President
nsrobins
31 December 2014 14:45:00


 


Neil, will you be introducing the cayenne pepper at the 1hPa level in anticipation of a propagation of warming downward through the system, possibly leading to reversal of westward stirring technique?


Originally Posted by: Arcus 


LOL. At the very highest layers I've input the Cumin Calibration Factor derived from land-based measurements plus an adjustment for atmospheric heat content as proposed by Schofield, et al (The Journal of Curry Cuisine, vol 34, 345-3). The process by which chilli propagates down the system into the lowest layers is little understood, but it is believed there is a lag of several hours before the effects are known. Once the wave cycles right down to the bottom, the output can be quite remarkable especially if accompanied by a SRW (Sudden Rectal Warming). There are as you said also marked changes in wind direction, switching erratically from west to east and in the worst cases north to south. This process has also been described in several toilet papers, including the famous essay by the team at the Instituto Tecnológico Autonomo de México headed by Montezuma.



Neil
Fareham, Hampshire 28m ASL (near estuary)
Stormchaser, Member TORRO
Gooner
31 December 2014 14:45:52


I don't think there's a single person in here who doesn't understand SSW can be a factor, and at the risk of sounding like a broken record and repeating a point made countless times in the last couple of days alone, people also understand it's one tiny part of a weather jigsaw puzzle containing many, many pieces, and actually even the most intense SSW event doesn't even come close to guaranteeing cold for these shores. 


Originally Posted by: Matty H 


Thanks for posting that view for the 100th time


It isn't sinking in though


Remember anything after T120 is really Just For Fun



Marcus
Banbury
North Oxfordshire
378 feet A S L


Arcus
31 December 2014 15:03:47


 


LOL. At the very highest layers I've input the Cumin Calibration Factor derived from land-based measurements plus an adjustment for atmospheric heat content as proposed by Schofield, et al (The Journal of Curry Cuisine, vol 34, 345-3). The process by which chilli propagates down the system into the lowest layers is little understood, but it is believed there is a lag of several hours before the effects are known. Once the wave cycles right down to the bottom, the output can be quite remarkable especially if accompanied by a SRW (Sudden Rectal Warming). There are as you said also marked changes in wind direction, switching erratically from west to east and in the worst cases north to south. This process has also been described in several toilet papers, including the famous essay by the team at the Instituto Tecnológico Autonomo de México headed by Montezuma.



Originally Posted by: nsrobins 


I may take a baroclinic leaf out of your book and indulge in some anthropomorphicly warmed digestibles myself, but as you mention I am somewhat concerned that excessive advection aloft may cause undue rooting in the lower layers later, possibly leading to complete convective instability and the subsequent dynamic lifting of trouser cloth.


 


 


Ben,
Nr. Easingwold, North Yorkshire
30m asl
Nick2373
31 December 2014 15:08:28


 


Thanks for posting that view for the 100th time


It isn't sinking in though


Originally Posted by: Gooner 

Sorry i know this as gone on for a while but here is some information on which way a SSW Could go.


Typically stratospheric meteorologists classify the vortex breakdown into three categories: major, minor, and final.


Sometimes a fourth category, the Canadian warming, is included because of its unique and distinguishing structure and evolution.


Major


These occur when the westerly winds at 60N and 10hPa (geopotential height) reverse, i.e. become easterly. A complete disruption of the polar vortex is observed and the vortex will either be split into daughter vortices, or displaced from its normal location over the pole.


According to the World Meteorological Organization's Commission for Atmospheric Sciences (Mclnturff, 1978): a stratospheric warming can be said to be major if 10 mb or below the latitudinal mean temperature increases poleward from 60 degree latitude and an associated circulation reversal is observed (that is, the prevailing mean westerly winds poleward of 60 latitude are succeeded by mean easterlies in the same area).


Minor


Minor warmings are similar to major warmings however they are less dramatic, the westerly winds are slowed, however do not reverse. Therefore a breakdown of the vortex is never observed.


Mclnturff states: a stratospheric warming is called minor if a significant temperature increase is observed (that is, at least 25 degrees in a period of week or less) at any stratospheric level in any area of winter time hemisphere. The polar vortex is not broken down and the wind reversal from westerly to easterly is less extensive.


Final


The radiative cycle in the stratosphere means that during winter the mean flow is westerly and during summer it is easterly (westward). A final warming occurs on this transition, so that the polar vortex winds change direction for the warming, however do not change back until the following winter. This is because the stratosphere has entered the summer easterly phase. It is final because another warming cannot occur over the summer, so it is the final warming of the current winter.

squish
31 December 2014 15:47:08
12z GME/DWD shows the same 'hinted at' pressure rise over Scandi. Hard to compare it as there are no Northern Hemisphere charts for this model on Meteociel. They'll be out soon on WZ.


http://modeles.meteociel.fr/modeles/gme/run/gme-0-132.png?31-12 
D.E.W on Dartmoor. 300m asl
31 December 2014 16:09:41


 


interesting to note that you can still have a shot of cold even without completely destroying the polar vortex- indeed a weakened Atlantic has often given us some very noteworthy marginal snowfall events at this time of year. Having said that, the 10th January chart above in Fothergills excellent post shows a very flat and zonal look with no weakening at all. This SSW could be a close but no cigar event, and interestingly Greece and the Balkans look like getting a good taste of winter into January.  


Originally Posted by: JACKO4EVER 


 


Indeed Jacko I think sometimes it is easy to become obsessed with SSW as the only way to get decent cold and snow for the UK.


When as 2013 proved all you really need is a weakened Atlantic flow and relatively weak heights to our north east to set the rain in motion.

Quantum
31 December 2014 16:17:31

12z GME/DWD shows the same 'hinted at' pressure rise over Scandi. Hard to compare it as there are no Northern Hemisphere charts for this model on Meteociel. They'll be out soon on WZ.


Originally Posted by: squish 

">http://modeles.meteociel.fr/modeles/gme/run/gme-0-132.png?31-12


For the last day or two there has been a hint of height rise at about 192 hours in the scandi-siberia domain, but I thought it so megre I wouldn't mention it. Alone it will do nothing, but if the trends continue I might become interested.


 


2023/2024 Snow days (approx 850hpa temp):
29/11 (-6), 30/11 (-6), 02/12 (-5), 03/12 (-5), 04/12 (-3), 16/01 (-3), 18/01 (-8), 08/02 (-5)

Total: 8 days with snow/sleet falling.

2022/2023 Snow days (approx 850hpa temp):

18/12 (-1), 06/03 (-6), 08/03 (-8), 09/03 (-6), 10/03 (-8), 11/03 (-5), 14/03 (-6)

Total: 7 days with snow/sleet falling.

2021/2022 Snow days (approx 850hpa temp):

26/11 (-5), 27/11 (-7), 28/11 (-6), 02/12 (-6), 06/01 (-5), 07/01 (-6), 06/02 (-5), 19/02 (-5), 24/02 (-7), 30/03 (-7), 31/03 (-8), 01/04 (-8)
Total: 12 days with snow/sleet falling.
JACKO4EVER
31 December 2014 16:49:05


">http://modeles.meteociel.fr/modeles/gme/run/gme-0-132.png?31-12

Originally Posted by: Quantum 


For the last day or two there has been a hint of height rise at about 192 hours in the scandi-siberia domain, but I thought it so megre I wouldn't mention it. Alone it will do nothing, but if the trends continue I might become interested.



you need those yellows a bit further North- East,  and well I suppose anything could happen. A 5% chance ATM, and I think that is being generous. Still, something to cast my eye on in the next day or two. 

Stormchaser
31 December 2014 17:32:14

The location of the strongest strat. warming and attempt at splitting the vortex at 30hPa extends from SW of Iceland to the near side of Scandinavia day 10 onward, as opposed to sticking around over Greenland.


This continues a trend which began this morning but which I forgot to account for (I'm only human, and it is New Year's Eve after all), and shifts the focus for a weaker jet further east, which then opens the door for height rises to our NE.


The past two GFSP runs were too weak with the warming to have much effect within the 16 day range, but the 12z has stepped it up a gear and this seems to produce a faster, more pronounced trop. response.


This allows the Siberian High to finally emerge from it's long slumber and start smashing up the polar vortex. That would be quite a result given that this is how Cohen originally thought it would unfold in the November outlook (but delayed by two weeks).


 


Nice to see an entertaining bit of trop. output for a change, even if it is way outside of the reliable. The response does seem to be rather strong given that the vortex is only displaced and elongated rather than split, and the GFS 06z, which had similar intensity of warming (though a bit less than GFSP has later on), produced far less of a response, so the usual truckload of salt needs to be taken with this GFSP 12z run.


Given that ECM was showing a similar progression out to day 10 this morning, it seems we should hope for this warming, starting near or over Greenland in 6 days time (below left - note that the strongest warming is at higher levels at this point in time) and traversing the Atlantic to Scandinavia during the following 10 days (below right), to be as strong and persistent as possible. That improves the odds of reversing the zonal wind at 60*N and also seems to allow for more of the warming to propagate downward - which may explain how the 30hPa warming grows stronger during days 10-16 of the GFSP run.


Netweather GFS Image  Netweather GFS Image


Cohen stated yesterday that GFS persistently underestimates the strat. warming, so perhaps we shouldn't worry too much about what that model shows. The updates for GFSP, on the other hand, might have accounted for that bias - though it would be handy right now if they haven't!


 


Those reading my recent posts can probably tell that my understanding of the stratosphere and how it impacts the troposphere is still rather sketchy so it's probably best not to pay too much attention to how I think the troposphere may be impacted - I'm still learning, and I'm hoping that events this month will prove to be a useful case study. What makes it so tricky to understand is the fact that key developments happen at a range of different heights.


If you have any problems or queries relating to TWO you can Email [email protected]

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T-Max: 30.2°C 9th Sep (...!) | T-Min: -7.1°C 22nd & 23rd Jan | Wettest Day: 25.9mm 2nd Nov | Ice Days: 1 (2nd Dec -1.3°C in freezing fog)
Keep Calm and Forecast On
roger63
31 December 2014 18:23:00


 


For the last day or two there has been a hint of height rise at about 192 hours in the scandi-siberia domain, but I thought it so megre I wouldn't mention it. Alone it will do nothing, but if the trends continue I might become interested.


Originally Posted by: JACKO4EVER 


you need those yellows a bit further North- East,  and well I suppose anything could happen. A 5% chance ATM, and I think that is being generous. Still, something to cast my eye on in the next day or two. 



Little support from GEFS for any persistence.Around 50% ENS show at 120h HP close to UK with ridging NE.In just 24 hours  just most have flattened /pushed  away by Atlantic flow.

Zubzero
31 December 2014 18:32:10

If only we could get an easterly 


http://www.meteociel.fr/modeles/ecmwf/runs/2014123112/ECH0-144.GIF?31-0


 

Whether Idle
31 December 2014 18:40:54


If only we could get an easterly 


http://www.meteociel.fr/modeles/ecmwf/runs/2014123112/ECH0-144.GIF?31-0


 


Originally Posted by: Zubzero 


The high will get bulldozed and pummelled out of the way by the Atlantic jet bully.


Dover, 5m asl. Half a mile from the south coast.
squish
31 December 2014 18:41:04
http://www.wetterzentrale.de/pics/Recm1441.gif 

Interesting
D.E.W on Dartmoor. 300m asl
JACKO4EVER
31 December 2014 18:53:33

http://www.wetterzentrale.de/pics/Recm1441.gif

Interesting

Originally Posted by: squish 


very.


thats not as straight forward as you would think. 


A little interest tonight and a small hope for coldies

peeps in west oxon
31 December 2014 19:00:46
Could one of you kind people explain why this interesting.😊 Thanks.
West Oxfordshire, 80M ASL
bledur
31 December 2014 19:06:46

 Still looking cool rather than cold after an early mild spell 


Slideshow image

some faraway beach
31 December 2014 19:28:30

Could one of you kind people explain why this interesting.😊 Thanks.

Originally Posted by: peeps in west oxon 


Very basically, see that high over Scandinavia, with the H (= "hoch"/high, it's in German)? Now imagine that expanding, particularly westwards. The low over the UK, with the T (= "tief"/deep, i.e. low), would be forced beneath it (or "undercut" it in the jargon on here). 


Now picture that scenario and follow the resulting isobars (the lines around the T), bearing in mind the direction of wind is anti-clockwise around areas of low pressure. You'd find the consequent airflow would be coming off cool land to the east rather than mild water to the west.


The other noteworthy point is that the high over Scandinavia is coloured green and yellow, indicating warmth and consequently strength in the high. What coldies are looking for is warm air advection (WAA) northwards to promote areas of high pressure to our north (so-called northern blocking). This forces the areas of low pressure southwards and, if everything falls in the right places, a visit from colder Arctic or Continental air rather than mild sea air.


 


It really is that simple.


2 miles west of Taunton, 32 m asl, where "milder air moving in from the west" becomes SNOWMAGEDDON.
Well, two or three times a decade it does, anyway.
sizzle
31 December 2014 19:38:02

 some very great stuff above just before i start getting drunk and my girlfriend starting on me for being on the net,  I want so say HAPPY NEW YEAR TO EVERYONE here on TWO. loving this site loving the upgrades, nice to see the model charts than the old skool links that never worked when clicked on them, thanks to everyone who post to MR BRIAN and MATTY H and the MODS for doing such a good job on this forum and keeping the rampers at bay and away   looking forward to 2015, a great BUZZ update from MR BRIAN RESPECT to you all, and to my buddy gavin partridge for all his great work and time he gives us thru the year. cheers guys,   [ sorry for of topic, ]

Arcus
31 December 2014 19:40:18


 some very great stuff above just before i start getting drunk and my girlfriend starting on me for being on the net,  I want so say HAPPY NEW YEAR TO EVERYONE here on TWO. loving this site loving the upgrades, nice to see the model charts than the old skool links that never worked when clicked on them, thanks to everyone who post to MR BRIAN and MATTY H and the MODS for doing such a good job on this forum and keeping the rampers at bay and away   looking forward to 2015, a great BUZZ update from MR BRIAN RESPECT to you all, and to my buddy gavin partridge for all his great work and time he gives us thru the year. cheers guys,   [ sorry for of topic, ]


MetOffice LRF wrote:


I've only one issue with that post, the rest is fab.


Ben,
Nr. Easingwold, North Yorkshire
30m asl
Snow Hoper
31 December 2014 19:40:50

I dunno, if you took the output from the big three to Mon/Tues next week and no further things may have seemed a little more interesting. Imagine if they modelled the area to our north wrong and its too progressive? That might be all the high building to the n/e and e needs.


Going to war over religion is like killing each other to see who has the better imaginary friend.


Home : Thorndon, Suffolk.
Hungry Tiger
31 December 2014 19:40:55


 


Very basically, see that high over Scandinavia, with the H (= "hoch"/high, it's in German)? Now imagine that expanding, particularly westwards. The low over the UK, with the T (= "tief"/deep, i.e. low), would be forced beneath it (or "undercut" it in the jargon on here). 


Now picture that scenario and follow the resulting isobars (the lines around the T), bearing in mind the direction of wind is anti-clockwise around areas of low pressure. You'd find the consequent airflow would be coming off cool land to the east rather than mild water to the west.


The other noteworthy point is that the high over Scandinavia is coloured green and yellow, indicating warmth and consequently strength in the high. What coldies are looking for is warm air advection (WAA) northwards to promote areas of high pressure to our north (so-called northern blocking). This forces the areas of low pressure southwards and, if everything falls in the right places, a visit from colder Arctic of Continental air rather than mild sea air.


 


It really is that simple.


Originally Posted by: some faraway beach 


Excellent description there.


Gavin S. FRmetS.
TWO Moderator.
Contact the TWO team - [email protected]
South Cambridgeshire. 93 metres or 302.25 feet ASL.


peeps in west oxon
31 December 2014 19:52:57


 


Very basically, see that high over Scandinavia, with the H (= "hoch"/high, it's in German)? Now imagine that expanding, particularly westwards. The low over the UK, with the T (= "tief"/deep, i.e. low), would be forced beneath it (or "undercut" it in the jargon on here). 


Now picture that scenario and follow the resulting isobars (the lines around the T), bearing in mind the direction of wind is anti-clockwise around areas of low pressure. You'd find the consequent airflow would be coming off cool land to the east rather than mild water to the west.


The other noteworthy point is that the high over Scandinavia is coloured green and yellow, indicating warmth and consequently strength in the high. What coldies are looking for is warm air advection (WAA) northwards to promote areas of high pressure to our north (so-called northern blocking). This forces the areas of low pressure southwards and, if everything falls in the right places, a visit from colder Arctic of Continental air rather than mild sea air.


 


It really is that simple.


Originally Posted by: some faraway beach 


SFB that is brilliant! Thanks very much, I have learned something today, great description.  I will study the modeland use your description. yes it is quite simple😳 I suppose!😜😀


West Oxfordshire, 80M ASL
Stormchaser
31 December 2014 20:58:44

  


Now that's interesting - more of a split polar vortex pattern emerging on the ECM 12z op run (above left), no word on the strat. charts from this model yet but I would not be surprised to see a better attempt at splitting the strat. vortex at 30mb than was seen on the 00z, with the Canadian vortex suppressed further - more like recent NAVGEM runs perhaps.


Edit: or perhaps similar to the 12z JMA which is really sticking to its guns, now shown above-right. There is little move to transfer a new 10mb trough over to Canada, which is GFS and GFSP have taking place really quite quickly days 7-10.


This version of events seems heavily dependent on having stronger warming over East Asia days 5-6 which seems to stand in the way of the trough transfer event. It might also be helping to get the core of the wave 2 warming all the way up to -8*C.


 


Shifting attention back to the 500mb charts, the ECM evolution is quite literally a different angle to the GFSP 12z in terms of where the build of high latitude blocking begins; it's quite a bit further east on this ECM op run with a strong dig of low heights down into Central Europe already well underway (GFSP shows a similar thing but it's more gradual and closer to the UK). The ridge to the Pole is being sustained by undercutting lows and is nicely placed to try and break up the Atlantic westerlies.


By contrast, there's still no suggestion of high latitude blocking from GFS, which ties in with it's weaker strat warming. GEM looks about the same, so I guess it is similar to GFS at the strat. levels, presuming it models them all.


 


Shifting focus to the shorter range for a moment, Snow Hoper has made an interesting point about the heights to our E and NE in 6 days time. There was a case in late November or early December when we had a similar situation, and the ridge did turn out to be a little more resilient in the end - but not quite enough to save us from the westerlies.


To be honest though, I'd rather see low heights smash through on route to Central Europe as per ECM/GFSP.


 


Overall, I'm just glad to have some interesting changes in the 500mb charts to think about after so many days of 'same old, same old' 


Happy New Year 


If you have any problems or queries relating to TWO you can Email [email protected]

https://twitter.com/peacockreports 
2023's Homeland Extremes:
T-Max: 30.2°C 9th Sep (...!) | T-Min: -7.1°C 22nd & 23rd Jan | Wettest Day: 25.9mm 2nd Nov | Ice Days: 1 (2nd Dec -1.3°C in freezing fog)
Keep Calm and Forecast On
sizzle
31 December 2014 21:13:49

great post storm chaser just nipped on to view your post DAM this forum is like a heavy drug I cant keep away,  anyway thanks storm chaser happy new year to you buddy, back to the JD and coke.

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