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IanT
  • IanT
  • Advanced Member
14 January 2019 20:31:28
Long time member. Infrequent poster. May I ask a question here that does not concern current model output? If it should be somewhere else, I’m sorry.

I have some background with quant financial markets modelling. The models seen there tend to under-predict the incidence of extreme outcomes/conditions. Unlikely events occur more frequently in real life than they do in the models.

With NWM models however, it is my distinct impression that extreme (ie. “widespread winter weather”) conditions appear far more frequently in model output than they do in reality.

Is this correct? If so, why?

Woking, Surrey. 40m asl.
Gavin D
14 January 2019 20:32:37

The ECM weeklies are below average for the entire run


Week 1


pkMKi8o.png


Week 2


mK9xPvR.png


Week 3


qrp5PYN.png


Week 4


34SthS4.png

Ally Pally Snowman
14 January 2019 20:32:45


http://www.meteociel.fr/modeles/ecmwf/runs/2019011412/EDH1-240.GIF?14-0 

Normally I don’t pay massive amounts of attention to these means as they are a blend of all the scenarios so can hide details in individual members, however when the mean is notably different to the climatic norm they are worth a second glance.


Originally Posted by: doctormog 


 


Yes stunning means tonight a real upgrade from the ECM this evening. 


Bishop's Stortford 85m ASL.
Robertski
14 January 2019 20:41:55


 


That T+216 chart would give rain for most, snow on the hills with blizzards above about 300m.


In a cyclonic, Atlantic pattern like that we really need uppers approaching -10C to give snow to low levels. 


Originally Posted by: Joe Bloggs 


 


I don't believe that is correct. It is down to so many factors, dew points, evaporative cooling, boundary lair temps, the list is long!

jhall
14 January 2019 20:42:58

Long time member. Infrequent poster. May I ask a question here that does not concern current model output? If it should be somewhere else, I’m sorry.

I have some background with quant financial markets modelling. The models seen there tend to under-predict the incidence of extreme outcomes/conditions. Unlikely events occur more frequently in real life than they do in the models.

With NWM models however, it is my distinct impression that extreme (ie. “widespread winter weather”) conditions appear far more frequently in model output than they do in reality.

Is this correct? If so, why?

Originally Posted by: IanT 


Doesn't it seem that way because the situation for a particular time in the future will have been forecast umpteen times in different model runs before that time is reached? It wouldn't be surprising if the random "noise" was to occur in a few of those model runs in such a way as to result in a considerably more extreme outcome than the actuality will turn out to be. (Chaos theory suggests that randomness can take over to a large extent sometimes as little as a week or so out.) And of course that handful of extreme runs tend to be the ones that attract most attention.


Cranleigh, Surrey
Arcus
14 January 2019 20:43:08

Long time member. Infrequent poster. May I ask a question here that does not concern current model output? If it should be somewhere else, I’m sorry.

I have some background with quant financial markets modelling. The models seen there tend to under-predict the incidence of extreme outcomes/conditions. Unlikely events occur more frequently in real life than they do in the models.

With NWM models however, it is my distinct impression that extreme (ie. “widespread winter weather”) conditions appear far more frequently in model output than they do in reality.

Is this correct? If so, why?

Originally Posted by: IanT 


I think it's more the case that what we regard as extreme events in terms of NWP modelling is skewed toward desired outcomes (extreme cold, heatwave, thunderstorm etc), and those extreme events get the attention when modelled correctly or not.


Quite often extreme flips in outcome go unnoticed as the previous scenario and end scenario do not fall within those "extreme/interesting" parameters. The tree falls over, but no-one is there to see it.


Ben,
Nr. Easingwold, North Yorkshire
30m asl
Gavin D
14 January 2019 21:04:42

Polar Low
14 January 2019 21:12:14

From Matt H


For what it's worth, given current model volatility, but some very interesting clusters now with a bias towards a mean flow from the E and NE in the 12Z EC ENS next week. The final few frames of the 12Z EC does have some support. Some 'wild' solutions within the ENS longer term.


A cold 2nd half to winter IMO. The full influence of the SSW has yet to be 'felt', given the slow downwelling, the AAM remains interesting and with the MJO back into phases 4-5-6 then all the ingredients there for cold synoptics in coming weeks. To what extent is the unknown


 

Brian Gaze
14 January 2019 21:15:39


Just clicked on Data > Model Launcher, and got the following - with loads more in a similar vein. (Cutting and pasting it here seems to have nuked my sig.)


 


Server Error in '/' Application.




Runtime Error


Description: An application error occurred on the server.


Originally Posted by: jhall 


Should be ok now. I'm rewriting a lot of the back-end services at the moment and adding in new features. 


Brian Gaze
Berkhamsted
TWO Buzz - get the latest news and views 
"I'm not socialist, I know that. I don't believe in sharing my money." - Gary Numan
Arcus
14 January 2019 21:19:41

Long time member. Infrequent poster. May I ask a question here that does not concern current model output? If it should be somewhere else, I’m sorry.

I have some background with quant financial markets modelling. The models seen there tend to under-predict the incidence of extreme outcomes/conditions. Unlikely events occur more frequently in real life than they do in the models.

With NWM models however, it is my distinct impression that extreme (ie. “widespread winter weather”) conditions appear far more frequently in model output than they do in reality.

Is this correct? If so, why?

Originally Posted by: IanT 


I'd also add that whatever the NWP predicts has absolutely zero effect on how the weather actually turns out. Unlike financial modelling.


Ben,
Nr. Easingwold, North Yorkshire
30m asl
RobN
  • RobN
  • Advanced Member
14 January 2019 21:30:17

Long time member. Infrequent poster. May I ask a question here that does not concern current model output? If it should be somewhere else, I’m sorry.

I have some background with quant financial markets modelling. The models seen there tend to under-predict the incidence of extreme outcomes/conditions. Unlikely events occur more frequently in real life than they do in the models.

With NWM models however, it is my distinct impression that extreme (ie. “widespread winter weather”) conditions appear far more frequently in model output than they do in reality.

Is this correct? If so, why?

Originally Posted by: IanT 


That's a very profound question and deserves its own thread.


My guess is that financial markets modelling is limited by the uncertainty in "sentiment" i.e human psychology which is way much more difficult to model than the physical world which obeys well understood laws of physics. The numerical modelling of the atmosphere is limited by the fact that the models are hugely approximating by using grids containing big parcels of air rather than individual molecules of air. The real atmosphere being a continuous medium "smooths" the atmospheric response a lot more than the models, so extremes appearing in the modelling output are less likely to occur in reality.


Rob
In the flatlands of South Cambridgeshire 15m ASL.
Polar Low
14 January 2019 21:44:27

Taken from NW 


 



Absolute stonker of a set of ECM ensembles tonight. For the 24th January, 42 out of 51 members are certainly cold enough for snow in most places. Up from 27 out of 51 this morning!! 


What's noticeable is pretty good agreement on the pattern - deep trough just SE of the UK. In the sweet spot! But will it stay there? end







Got a feeling IF will comment soon


 





Gooner
14 January 2019 21:58:43

O/T apologies D 'MILD' Bett


"The cold air to come could last quite some time ",


 


I always follow the Beeb and Met , they see much more data than most of us ever will


 


Remember anything after T120 is really Just For Fun



Marcus
Banbury
North Oxfordshire
378 feet A S L


14 January 2019 22:00:04


 


 


Yes stunning means tonight a real upgrade from the ECM this evening. 


Originally Posted by: Ally Pally Snowman 


Definitely the coldest set of ENS for De Bilt that I have seen this year.


The snow depth chart from Weather US for the UK (based on the ECM 12z) for midday on 24 Jan shows most places away from Central Southern and SE England having significant snow depths. Many parts of Wales, northern England and Scotland have a good 3+ inches of snow with over a foot on high ground and 28 inches showing on the peaks of the Lake District.


https://weather.us/model-charts/euro/england/snow-depth-in/20190124-1200z.html

Polar Low
14 January 2019 22:02:21

That means freeze-up if that came from him



O/T apologies D 'MILD' Bett


"The cold air to come could last quite some time ",


 


I always follow the Beeb and Met , they see much more data than most of us ever will


 


Originally Posted by: Gooner 

Joe Bloggs
14 January 2019 22:04:56


 


 


I don't believe that is correct. It is down to so many factors, dew points, evaporative cooling, boundary lair temps, the list is long!


Originally Posted by: Robertski 


Yes the second part of my post may have been too simplistic, however I maintain that for most low lying parts of the UK, if the wind is strong and from an Atlantic source, with no continental influence present, you really need deep cold uppers (ideally below -8C, preferably close to -10C) to allow for snow below 100m ASL, especially close to western coasts. Yes evaporate cooling allows for snow, but only if winds fall very light. 


If T+216 ECM came to fruition I maintain that most of us in low lying areas would see rain (850s below) 


 


http://www.wetterzentrale.de/maps/ECMOPEU12_216_2.png


However we’re talking FI so totally hypothetical regardless. 



Manchester City Centre, 31m ASL

Gooner
14 January 2019 22:05:46


That means freeze-up if that came from him


 


Originally Posted by: Polar Low 


It was the LP next week that showed ppn crossing the country , he wasn't bigging it up though 


Remember anything after T120 is really Just For Fun



Marcus
Banbury
North Oxfordshire
378 feet A S L


Joe Bloggs
14 January 2019 22:07:01


 


Definitely the coldest set of ENS for De Bilt that I have seen this year.


The snow depth chart from Weather US for the UK (based on the ECM 12z) for midday on 24 Jan shows most places away from Central Southern and SE England having significant snow depths. Many parts of Wales, northern England and Scotland have a good 3+ inches of snow with over a foot on high ground and 28 inches showing on the peaks of the Lake District.


https://weather.us/model-charts/euro/england/snow-depth-in/20190124-1200z.html


Originally Posted by: Global Warming 


If only those charts were even in a tiny way accurate! 



Manchester City Centre, 31m ASL

some faraway beach
14 January 2019 23:03:52

Long time member. Infrequent poster. May I ask a question here that does not concern current model output? If it should be somewhere else, I’m sorry.

I have some background with quant financial markets modelling. The models seen there tend to under-predict the incidence of extreme outcomes/conditions. Unlikely events occur more frequently in real life than they do in the models.

With NWM models however, it is my distinct impression that extreme (ie. “widespread winter weather”) conditions appear far more frequently in model output than they do in reality.

Is this correct? If so, why?

Originally Posted by: IanT 


The weather models are mechanical - they calculate how conditions should evolve on the basis of laws of physics. Each set of inputs can only produce one outcome. The trouble is that the range of measurements you start with is never complete, so you're bound occasionally to miss one or two data points which might in reality have moderated an extreme outcome. 


The ensemble is supposed to be a way of testing whether this is the case. By tweaking your initial conditions 20 or 50 times, you're supposed to cover the effects of possible gaps in your initial data. But every one of those ensemble runs is another one-off event with only one possible outcome. None of the 20 or 50 runs is more likely to occur in reality than any other. So we have to treat every one, including the most extreme ones, as equally possible. Thus we have every right to examine extreme model runs as much as boring runs. And we do!


As I understand it, financial modelling, by contrast, is essentially statistical. You're looking for what is more likely or less likely to happen, and applying percentages to that, and comparing it with the possible financial gain to be made by taking different positions. To put it in horse racing term you're looking for which outcome should be the favourite, and determining whether the potential gain of backing that outcome outweighs the risk of one of the outsiders coming in instead. 


As you say, the favourite (as in horse racing) tends to be priced up just that little bit too short, as everyone piles in for the easy money, or the short-term gain. And when an outsider does come in, then everyone is shocked, even though a 1-in-a-thousand event had every right to occur at some point.


 


It takes me back to my grammar school, and doing my applied maths A level 42 years ago. There was a choice of two papers to take with the Oxford board back then: statistics or mechanics. Our maths teacher told us that statistics is a very straightforward subject, but essentially useless in scientific terms, so we covered the whole subject in four weeks, to a level which would have been enough to pass the exam. Then we spent the rest of the year studying mechanics, on the basis that it was much more difficult, but much more useful, so that would be the paper for which we would be entered.


It was a different world back then.


 


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.
Lionel Hutz
14 January 2019 23:05:20


 


Yes the second part of my post may have been too simplistic, however I maintain that for most low lying parts of the UK, if the wind is strong and from an Atlantic source, with no continental influence present, you really need deep cold uppers (ideally below -8C, preferably close to -10C) to allow for snow below 100m ASL, especially close to western coasts. Yes evaporate cooling allows for snow, but only if winds fall very light. 


If T+216 ECM came to fruition I maintain that most of us in low lying areas would see rain (850s below) 


 


http://www.wetterzentrale.de/maps/ECMOPEU12_216_2.png


However we’re talking FI so totally hypothetical regardless. 


Originally Posted by: Joe Bloggs 


As regards uppers, I may have misinterpreted, but I seem to recall over the weekend Retron saying that snow could fall to low levels with not so cold uppers. You need colder upper temperatures in high pressure conditions. He seemed to think that uppers of - 6 could be cold enough for snow with air pressure of 985 mbs. 


Lionel Hutz
Nr.Waterford , S E Ireland
68m ASL



tallyho_83
14 January 2019 23:33:56




Originally Posted by: Gavin D 


Just checked them a day or so back and shows below average for Feb and March?




And with quite an extensive northern block:




 


Home Location - Kellands Lane, Okehampton, Devon (200m ASL)
---------------------------------------
Sean Moon
Magical Moon
www.magical-moon.com


tallyho_83
14 January 2019 23:47:35

Quite a difference in temps between the GFS Para 18z and the OP run firstly the OP @ 210:



 


Temps struggling to get much above freezing in the still north to north westerly wind! Maybe mid single figures at best! Perhaps lot's of sleet to snow showers or even soft hail! (not seen this sort of precipitation in a while).



 


Then the 18z Para - temps in double figures midday in the south and low pressure slower sinking southwards:


But eventually does it but later time than the Op run!




 


Home Location - Kellands Lane, Okehampton, Devon (200m ASL)
---------------------------------------
Sean Moon
Magical Moon
www.magical-moon.com


Solar Cycles
14 January 2019 23:48:17
If the GFS turns out correct it will turn out to be its finest hour. In other news Elvis was spotted down our local chip shop earlier.
tallyho_83
15 January 2019 00:08:38

18Z Para @ 360 is showing more like a northern block developing over Pole and into Greenland:



Home Location - Kellands Lane, Okehampton, Devon (200m ASL)
---------------------------------------
Sean Moon
Magical Moon
www.magical-moon.com


Retron
15 January 2019 04:34:45


As regards uppers, I may have misinterpreted, but I seem to recall over the weekend Retron saying that snow could fall to low levels with not so cold uppers. You need colder upper temperatures in high pressure conditions. He seemed to think that uppers of - 6 could be cold enough for snow with air pressure of 985 mbs. 


Originally Posted by: Lionel Hutz 


Yes indeed. Down here at least I usually look for -10C at 850, but as I mentioned the lower the pressure the closer to the ground that 850 line becomes and thus the higher a temperature you can get away with.


Here's an example (note: NOT based on any particular model).


Say that it needs to be -7C at 4000 feet for snow to make it to the ground. The ground temperature is 2C. I'm using this calculator.


At an SLP of 1025hPa, the 850 line is at 4860 feet (therefore it'd need to be colder than -7 at 850 for snow to fall - probably closer to -10)


At 1005 hPa, it's at 4350 feet (so -8 or so would do)


At 985, it's 3840 feet (so you could get away with -6)


And at 965, it's 3300 feet (so -4 or -5 would do).


Obviously there's a lot more to it than just that (lapse rates, evaporative cooling, boundary layer modification via a warm sea etc), but it gives a rough idea of why the models have been so snowy with relatively modest 850s - this is the polar opposite of a typical "driven by a massive high" cold spell.


Incidentally the ECM showed this beautifully a couple of days ago. 850s under lowish pressure were -5C or so, then as a high built in situ, without pulling in a colder airmass, the 850s fell to -8C over the course of a day - just because the 850 line was getting progressively higher.


We could really do with seeing temperature charts at x height rather than x pressure.


 


Leysdown, north Kent
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