French Imports - What went wrong?
#1
Posted 23 August 2011 - 11:49
Robbie |
@ London Biggin Hill Airport! Follow me on Twitter | @RobbiePPLPilot
Weather Extremes London 2009+ -
2009 - 5 Snowfalls, 6 Thunderstorms, 32.0 °C 2010 - 5 Snowfalls, 4 Thunderstorms, 31.7 °C 2011 - , 1 Snowfall, 3 Thunderstorms, 33.1 °C
2012, 2 Snowfalls, 11 Thunderstorms + 1 odd rumble (12), 26.9°C.
#2
Posted 23 August 2011 - 11:55
(='.'=) This is Bunny. Copy and paste bunny into your
(")_(") signature to help him gain world domination
#3
Posted 23 August 2011 - 11:56
Sorry that should say " what could be improved "
SnowDepth: 2008 5-10CM / 2009/10 20CM+ / 2011 An amazing Winter start! 15cm+ / FEB 4-5th 2012 10CM+
#4
Posted 23 August 2011 - 11:59
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A glance at the 00z (1AM BST) soundings for Trappes (Paris) and Herstmonceux (Sussex) is quite revealing, demonstrating why N France received so many active storms overnight and why Sussex did not. As can be seen on the (modified) Trappes ascent, there is a warm nose of temps at ~850mb followed by steep lapse rates between there and 500mb. I have analysed a most unstable, elevated CAPE situation which demonstates the HUGE amount of CAPE available to a parcel of air rising from the 850mb plume. The boundary layer (lowest 1km or ~150mb) near Paris was already much cooler by 00z (probably cooled by rain/outflow from earlier storms) and storms were therefore decoupled from the boundary layer. However, this did not prevent storms forming and persisting as they were growing from out of the plume above. This situation does happen in the UK too, explaining how we (sometimes!!) get active overnight storms.
Now looking at Herstmonseux, Sussex - a sounding which is likely to be quite typical of an ascent over SE England. For an appreciable storm risk we really needed to advect some of the warm 850mb plume in from the south to generate the necessary instability to maintain storm cells that were travelling up from France. There is a very slight warm bulge at 850mb but it is very insignificant compared with the Trappes ascent and crucially we don't have those steep lapse rates between 850mb and 500mb to help create that store of elevated CAPE.
It was always going to be a knife edge scenario last night as the very unstable air was sneaking right past the far SE of the UK and there was a small risk (accounted for in my forecast) that some of this instability could get advected over the far SE for a time. It is far easier to predict thunderstorms when all the forecast parameters are 'red lining' and the only thing that can go wrong is that the storms are slightly less numerous or active than you forecast.
The position of the UK relative to the Atlantic and France/Spain often means we are clipped by the edges of these plumes and a slight shift west or east in the plume can make a HUGE amount of difference to the weather experienced and forecast success.
The extensive (and largely unforecast 12 hrs before) raft of elevated thunderstorms that affected the SE and East Anglia on Tuesday 28th June this year is an example where the plume was slower to clear than forecast, with an approaching upper trough rapidly destabilising it creating many thunderstorms over a short time period.
#5
Posted 23 August 2011 - 12:04
All well and said, but I agree the MetOffice was slow to update last night and should created a better website of showing us why things didn't go to plan.
Robbie |
@ London Biggin Hill Airport! Follow me on Twitter | @RobbiePPLPilot
Weather Extremes London 2009+ -
2009 - 5 Snowfalls, 6 Thunderstorms, 32.0 °C 2010 - 5 Snowfalls, 4 Thunderstorms, 31.7 °C 2011 - , 1 Snowfall, 3 Thunderstorms, 33.1 °C
2012, 2 Snowfalls, 11 Thunderstorms + 1 odd rumble (12), 26.9°C.
#6
Posted 23 August 2011 - 12:14
Its just one of those things you have to take as a storm-chaser or even if your just interested in the weather. As Matt D's post proves all it takes is one elevated parcel of CAPE that was progged by models to shift or even dissipate with capping, and its watching the light show on the laptop instead while outside you could be seeing stars and satellites.
Low Temperature -11.0°C at 07:35 on 20th December 2010
Highest Daily Rainfall 77 mm (3.03 inches) on 10th August 2004
Highest Monthly Rainfall 287 mm (11.30 inches) in August 2004
#7
Posted 23 August 2011 - 12:21
#8
Posted 23 August 2011 - 12:24
pottyprof, on 23 August 2011 - 12:21 , said:
But in the last few years even the simplist of weather forecasts have been difficult for the top end pros. For example forecasting a sunny day clear blue skies and you get 3 days of cloud across the south east corner
SnowDepth: 2008 5-10CM / 2009/10 20CM+ / 2011 An amazing Winter start! 15cm+ / FEB 4-5th 2012 10CM+
#9
Posted 23 August 2011 - 12:31
Victor Meldrew, on 23 August 2011 - 12:24 , said:
But in the last few years even the simplist of weather forecasts have been difficult for the top end pros. For example forecasting a sunny day clear blue skies and you get 3 days of cloud across the south east corner
Perhaps someone could shed some light as to if this is the case or not?
#10
Posted 23 August 2011 - 12:40


Now, you listen here:'e's not the Messiah,'e's a very naughty boy!
Views & opinions expressed in any of my posts are my own - but the voices made me do it
#11
Posted 23 August 2011 - 12:57
Just to comment on last night they got it wrong simple as that why then you best ask them not me? A clue is the item above about the Trappes and Herstmanceaux ascents.
But I'll attempt a constructive comment on the other thread later today.
here is my weather station, for local written forecasts or simply browsing further afield.
http://www.johnholmes-weather.co.uk/
see my blog for weather updates as I get time and also my plea for preventing getting skin cancer.
#12
Posted 23 August 2011 - 13:05
#13
Posted 23 August 2011 - 13:14
#14
Posted 23 August 2011 - 17:33
Looking at Frenchie yesterday, we almost did - but it decayed over the channel and stayed there for quite a few hours.
Something is very wrong with the climate, either if that's normal 'Climate Change' or this rubbish theory behind 'Global Warming' - we should investigate?
Robbie |
@ London Biggin Hill Airport! Follow me on Twitter | @RobbiePPLPilot
Weather Extremes London 2009+ -
2009 - 5 Snowfalls, 6 Thunderstorms, 32.0 °C 2010 - 5 Snowfalls, 4 Thunderstorms, 31.7 °C 2011 - , 1 Snowfall, 3 Thunderstorms, 33.1 °C
2012, 2 Snowfalls, 11 Thunderstorms + 1 odd rumble (12), 26.9°C.
#15
Posted 24 August 2011 - 09:10
Bumbulus Londonicus says: rhubarb, rhubarb, rhubarb...
Non cogito ergo non sum!
Views and opinions expressed in this or any other of my posts are my own
http://www.don-linds.../arguments.html
CCCP
#16
Posted 24 August 2011 - 09:45
Robbie Garrett, on 23 August 2011 - 17:33 , said:
Looking at Frenchie yesterday, we almost did - but it decayed over the channel and stayed there for quite a few hours.
Something is very wrong with the climate, either if that's normal 'Climate Change' or this rubbish theory behind 'Global Warming' - we should investigate?
As we've discussed before...the Atlantic has been considerably quieter in the past few years (unlike the 90s) and IMO we need a +NAO, high octane Atlantic if we are going to improve our chances of seeing storms.
The last few years have been primarily -NAO and accordingly weather systems weaker. This IMO (emphasise this is just my opinion and I have little scientific evidence to back it up, just theory) is what has contributed to a less typical distribution of storms but furthermore, fewer storms generally.
+NAO is associated with stronger pressure systems, which if you think about it means our chances of storms increases. It means depressions and anticyclones are more pronounced, meaning wind distribution between to two areas tends to be stronger! If you picture a pronounced, strong depression in the atlantic moving towards a strong, pronounced anticyclone to our East, it helps provide two things which we have lacked of late - one, is a deeper fetch of winds...a large depression is likely to draw in much cooler winds on the western flank and much deeper, warmer winds on the East (with the anticyclone doing the opposite). This means we have greater potential for heightened lapse rates, bigger differences between the moisture (which has been pumped out of the Med/N Africa and the cooler drier air fed from the polar regions), bigger differences between temperature.
Most critically, it enables us to have a more N-S orientated plume than the weaker SW to NE as we've been seeing. The prevailing wind at our latitude is a SW'erly...unless you have synoptics strong enough to drive, in particular storm cells and warm, moist air, in a northerly direction, they will be influenced to a greater degree by the prevailing SW to NE winds, particularly those which often blow through the Channel (which funnily enough is orientated towards WSW to ENE, narrowing at the eastern tip)...this may help explain why our storms once nearing the channel are both falling apart and/or flinging NE'wards.
IMO, the North Atlantic Oscillation is the biggest player in respect of our chances at bigger, night time thunderstorms. If we have a bitterly cold, snowy winter, it's more than likely we are at the mercy of a -NAO. A much milder, stormier winter, then we have +NAO! The last few years in particular have seen colder, more snowy winters, followed by generally mixed bag summers and reduced thunderstorm activity. The 90s were dominated by not only +NAO scenarios (8 out of the 10 years), but particularly strong +NAOs. Since the turn of the millennium, we've had fewer AND weaker +NAOs in relation to the 90s. I'm not suggesting at all that the NAO defines solely our chances - we've no doubt have cracking storms during -NAO years and hardly in +NAO years...however, the frequency of the 90s storms (and their intensity) compared with the 00s does strike me as somewhat suspicious....
Have a look at this chart depicting NAO below and draw your own conclusions....(if indeed there are any to be made)
Edited by Harry, 24 August 2011 - 09:49 .
Supercells - 6
Tornadoes - 3
States Visited - 7 (TX,OK,KS,NE,MO,AR,TN)
Snow and Thunder Totals - 2012 (2011 in brackets for comparison)
Highest snowfall recorded - 8 inches (2011 - 6 inches)
Thunder - storms/showers/rain - 8 (2011 - 8 days)
Thunder/Lightning Days - 6 days/1 Night - 10/4, 11/4, 12/4, 13/4, 19/4, 15/5 / 30/4 (2011 - 8 days)
#17
Posted 24 August 2011 - 09:52
Harry, on 24 August 2011 - 09:45 , said:


Now, you listen here:'e's not the Messiah,'e's a very naughty boy!
Views & opinions expressed in any of my posts are my own - but the voices made me do it
#18
Posted 24 August 2011 - 09:59
Harry, on 24 August 2011 - 09:45 , said:
IMO, the North Atlantic Oscillation is the biggest player in respect of our chances at bigger, night time thunderstorms. If we have a bitterly cold, snowy winter, it's more than likely we are at the mercy of a -NAO. A much milder, stormier winter, then we have +NAO! The last few years in particular have seen colder, more snowy winters, followed by generally mixed bag summers and reduced thunderstorm activity. The 90s were dominated by not only +NAO scenarios (8 out of the 10 years), but particularly strong +NAOs. Since the turn of the millennium, we've had fewer AND weaker +NAOs in relation to the 90s. I'm not suggesting at all that the NAO defines solely our chances - we've no doubt have cracking storms during -NAO years and hardly in +NAO years...however, the frequency of the 90s storms (and their intensity) compared with the 00s does strike me as somewhat suspicious....
Have a look at this chart depicting NAO below and draw your own conclusions....(if indeed there are any to be made)
But you could argue that some areas of Britain this year have had a fair bit of thundery activity, expecially NE England and probably some other areas too. While at the same time, for sake of keeping to the subject of the title of this thread, 'French Imports' appear to have drastically reduced in recent summers which coincides with a reduction of slow-moving troughs setting up just to our west and SW which allows those classic thundery Spanish Plumes to spread across the UK. This may bring a reduction of storms to the SE corner of the UK, but not necessarily to some other parts of the UK.
Not so sure that the NAO state has any role, though could be part of the reason, along with SSTs in the Atlantic - which can influence the tendency for a pressure/height pattern to develop each summer across W Europe. And generally teleconnections in the northern hemispehere may have an influence along with other cycles.
Fredericksburg (TX) 01/05/07, Stafford (KS) 05/05/07, Medicine Lodge (KS) 06/05/08, Hooker (OK) 05/05/08, Stuttgart (AR) 10/05/08, Big Spring (TX) 14/05/08, Sielbert (CO) 21/05/08, Hoxie (KS) 22/05/08, Collyer (KS) 22/05/08, Dighton (KS) 23/05/08, Ness City (KS) 23/05/08, Ellis (KS) 23/05/08, Quinter (KS) 23/05/08, Pratt (KS) 26/05/08, Kearney (NE) 29/05/08, Aurora (NE) 29/05/08.
#19
Posted 24 August 2011 - 11:06
Coast, on 24 August 2011 - 09:52 , said:
Linking your observations, Coast, with Nick F's above, the 60s (if that chart I posted was accurate) was a heavily -NAO period...interesting.
Supercells - 6
Tornadoes - 3
States Visited - 7 (TX,OK,KS,NE,MO,AR,TN)
Snow and Thunder Totals - 2012 (2011 in brackets for comparison)
Highest snowfall recorded - 8 inches (2011 - 6 inches)
Thunder - storms/showers/rain - 8 (2011 - 8 days)
Thunder/Lightning Days - 6 days/1 Night - 10/4, 11/4, 12/4, 13/4, 19/4, 15/5 / 30/4 (2011 - 8 days)
#20
Posted 24 August 2011 - 13:07
" Cloudy morning with the odd patchy light drizzle will clear by early afternoon with sunny spells "
We've got HEAVY SHOWERS, Nice one met office keep chucking the rubbish.
Even now it says A dull start for most places with a few showers likely but it should become mostly dry by the afternoon and the cloud should lift and break to give some warm sunny spells.
We had drizzle in the morning followed by some pretty hefty showers in the afternoon.
So if they struggle with french imports and struggle with the 12hr forecast we have no hope!
Edited by Victor Meldrew, 24 August 2011 - 13:08 .
SnowDepth: 2008 5-10CM / 2009/10 20CM+ / 2011 An amazing Winter start! 15cm+ / FEB 4-5th 2012 10CM+
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