Convective Outlook: Tue 31 May 2022
LOW
SLGT
MDT
HIGH
SVR
What do these risk levels mean?
Convective Outlook

VALID 06:00 UTC Tue 31 May 2022 - 05:59 UTC Wed 01 Jun 2022

ISSUED 06:38 UTC Tue 31 May 2022

ISSUED BY: Dan

A broad upper trough covers the British Isles on Tuesday, its orientation changing from NNW-SSE at 06z to become almost W-E by 06z Wednesday. Cooler air in the mid-levels will advect further south than on Monday, and the net result is a deeper convective layer yielding 400-700 J/kg CAPE in response to modest surface heating and cloud tops potentially around 20,000-25,000ft. While CAPE is higher than Monday, and encompasses more of the mixed phase region, it is also stretched over a much deeper layer. Areas of showery rain will already be present in the morning, these turning more convective through the day with numerous other showers developing with time. By the afternoon showers will become widespread with a few thunderstorms likely too, although fewer showers across much of southern Ireland, south Wales and SW England as profiles here become increasingly subsided. The greatest risk of lightning, which is likely to be more widespread than the past couple of days, will be associated with the belt of steep mid-level lapse rates from western Scotland southeastwards to SE England - as broadly depicted by the SLGT issued. However, shear will be fairly weak in this region within the upper trough axis, and the tall skinny CAPE profiles will likely lead to slow-moving heavy showers with locally high rainfall totals, but perhaps limited lightning/morphing into areas of showery rain.

Strong northwesterly flow aloft, around the west/southwest flank of the upper trough, will edge slowly eastwards across the Midlands and southern England during the afternoon, and so the best overlap of CAPE/shear is likely in a zone broadly from Birmingham to London during the mid-late afternoon - and here the better potential of some organisation/longevity of cells. Any further west, and convection becomes increasingly restricted in depth due to warming aloft. The strongest cells could produce hail up to 1.0cm in diameter and wind gusts 35-45mph. The slack flow with areas of low-level convergence will create a favourable environment for a few funnel clouds. Where several showers occur, rainfall accumulations could locally exceed 30mm bringing the risk of some surface water flooding. Showers will weaken in intensity during the evening hours as nocturnal cooling of the boundary layer commences.