Convective Chat Sunday 3rd June 2012
#1
Posted 02 June 2012 - 12:29
An elongated area of low pressure will spread rain northwards across England and Wales overnight. The low is expected to stall across southern England during Sunday, and bifurcate, with one centre remaining near west Wales, whilst a second centre runs away eastwards into Europe.
This will leave southern counties in a 'col', this containing plenty of moisture throughout the layers, and more to evaporate after the overnight rain. A well marked zone of convergence is expected to lie WNW-SSE across southern England, which may become the focus of some slow moving heavy downpours.
Models are indicating just modest CAPE and LI, but moisture would suggest, cloud efficiency will be high within a convective regime. Some thunder is possible.
Convection will depend very much on how much the cloud layers thin and break across southern areas. A grey day with low stratus will produce nothing. However if cloud does break, temperature will soon lift to initiate convection that will be forced by convergence. Well broken cloud may induce an augmented sea breeze, stronger convergence, a narrow line of intense rain, a risk of funnel clouds and a low risk of one or two weak tornadoes.
Areas at risk, Wilts, Berks, north Hants, Surrey, Sussex and Kent.
N.
#2
Posted 02 June 2012 - 13:59
Didn't really seem worth having another thread for my question.
This post has been edited by Lightningfox92: 02 June 2012 - 14:00
#4
Posted 02 June 2012 - 21:13
PS. If temps can spike up on some cells moving into the boundary the low level spin cud be quite phenomenal!
Not really mentioned the word funnel in the forecast but the potential is certainly there if the desired conditions can come together simultaneously!
This post has been edited by Tony Gilbert: 02 June 2012 - 21:18
#5
Posted 03 June 2012 - 09:49
#6
Posted 03 June 2012 - 13:37
bensainsbury, on 03 June 2012 - 09:49, said:
Surface obs currently show nearest convergence to you closer to Swindon region ATM. CAPE looks to remain rather lean based on limited surface warming today though still some potential for a few sharp showers under developing congestus clouds.
#7
Posted 03 June 2012 - 13:51
As they cross the convergence zone, there will be a (short) period, where the low level helicity will be considerable, in the correct direction for separation from updraft from downdraft along with tornadogenesis. i.e. veering round from east to southwest in the lowest leyers of the cloud. Although relatively weak, they could for a time develop supercellular charactoristics.
This is not too dissimilar from the day that the Birmingham tornado developed, this being the 28th July 2005, when a thunderstorm in a SSW'ly airflow along a line of convergence, ran up a warm front, this overrunning a zone of cold easterlies.
Look for hard echoes on their southeastern flank.
N.
This post has been edited by Nigel Bolton: 03 June 2012 - 13:53
#8
Posted 03 June 2012 - 14:24
Nigel Bolton, on 03 June 2012 - 13:51, said:
As they cross the convergence zone, there will be a (short) period, where the low level helicity will be considerable, in the correct direction for separation from updraft from downdraft along with tornadogenesis. i.e. veering round from east to southwest in the lowest leyers of the cloud. Although relatively weak, they could for a time develop supercellular charactoristics.
This is not too dissimilar from the day that the Birmingham tornado developed, this being the 28th July 2005, when a thunderstorm in a SSW'ly airflow along a line of convergence, ran up a warm front, this overrunning a zone of cold easterlies.
Look for hard echoes on their southeastern flank.
N.
Some sharpened radar returns already!
#11
Posted 03 June 2012 - 15:35
#12
Posted 03 June 2012 - 17:07
N.
#13
Posted 03 June 2012 - 17:10
Nigel Bolton, on 03 June 2012 - 17:07, said:
N.
That cell has just passed overhead; didn't hear no thunder but torrential rain and hail. Doesn't have a good structure either.
This post has been edited by bensainsbury: 03 June 2012 - 17:12












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