Convective Outlook: Sun 30 Apr 2023
LOW
SLGT
MDT
HIGH
SVR
What do these risk levels mean?
Convective Outlook

VALID 06:00 UTC Sun 30 Apr 2023 - 05:59 UTC Mon 01 May 2023

ISSUED 07:02 UTC Sun 30 Apr 2023

ISSUED BY: Dan

A pronounced upper trough will crest the western Europe upper ridge as it slides eastwards across the British Isles on Sunday. A moist low-level airmass will persist across most areas, with the exception of central and northern Scotland, with dewpoints typically 10-12C. Ireland/Northern Ireland will have the benefit of early occlusion debris clearing eastwards leading to better insolation and surface heating, coupled with being under the upper trough (and associated cold pool) during peak heating hours. As such, an unstable environment is anticipated here, yielding generally 500-1,000 J/kg MLCAPE and resulting in numerous heavy showers and thunderstorms developing through the day, especially in Ulster and Leinster aided in places by orographic forcing and some areas of low-level wind convergence as a surface trough develops through the afternoon. Modified forecast soundings reveal fairly unidirectional winds with height leading to rather weak cloud layer shear (typically 20kts), but potential for cloud tops to reach around 30,000ft (ELTs around -50C). As such, some fairly active thunderstorms will be possible, perhaps more especially in the north and east of Northern Ireland. Cells initially will probably be steered towards the east or northeast on the forward side of the upper trough, but as the trough departs towards Britain during the evening the steering flow may take cells more to the southeast later in the day and through the evening. While shear may not be particularly strong, some fairly robust updrafts in the most organised cells could produce hail up to 1.5cm in diameter (sub-severe). Thunderstorms may spread into or develop over portions of southern Scotland later in the afternoon and into the evening hours.

Over England and Wales, rather extensive cloud (and outbreaks of rain) associated with occlusion debris may limit surface heating and therefore casts a lot of uncertainty over whether deep convection can develop. Ahead of this, some modest surface heating is possible in eastern England for a time, and may just be sufficient to develop a few heavy showers/weak thunderstorms in conjunction with breeze convergence in the area. The risk area will shift southwards from Northumberland towards Lincolnshire through the afternoon, and is still a possibility until around mid-evening for Lincolnshire/The Wash, but confidence on much lightning activity occurring is rather low. Elsewhere, some modest build-up of CAPE is possible across northern England, Wales and SW England in the vicinity/towards the rear of the occlusion in response to diurnal heating if sufficient cloud thinning/breaking occurs as the leading edge of the upper trough/cold pool arrives from the west, and may provide the focus for additional heavy showers/weak thunderstorms - a few isolated lightning strikes are possible from the most intense cells, and a couple of low-end SLGTs have been introduced to highlight this risk. In addition, during the evening and night activity over eastern Ireland will eventually migrate across the Irish Sea into Wales/NW England albeit probably with a weakening trend in lightning activity.