Forecaster: Dan
Last Updated: 18:58 Friday, 5th August 2011
Valid: 00:00 Saturday, 6th August 2011 - 23:59 Saturday, 6th August 2011
MDT: S + E Ireland
SLGT: N + E England, Borders, Ireland, Northern Ireland, Wales, SW England, West Country
Synopsis:
A large, elongated, vertically-stacked and multi-centred upper low becomes established across the British Isles on Saturday. Convection will be widespread, with a few thunderstorms expected.
Discussion:
Beneath the upper low, lowering geopotential heights and a cold pool will overspread the country, with T500's as low as -25C, steepening lapse rates. Diurnal heating will aid convection development, with as much as ~600 J/kg CAPE available. Consequently, showers will become widespread across Ireland and western Britain, and with ELT's as low as -30C over Ireland, thunder and lightning is likely in quite a few showers.
DLS of up to 50kts is forecast over Wales and W England during the day, which is likely to help organise the convection. However, relatively weaker DLS (less than 20kts) is likely across Ireland, and this will slowly spread eastwards into Wales by evening. Meagre LLS will preclude a tornado risk. Given the cold mid levels, small hail is likely in some of the showers, particularly over Ireland. Concern exists that excessive cloud cover may inhibit convection, particularly over Ireland. Strong steering winds will mean any showers that do develop will move fairly quickly, but much lighter upper level winds over Ireland, particularly the W, will allow slow-moving showers and local thunderstorms to exist. Showers that do develop will continue well into the evening, becoming mostly confined to coastal parts where the risk of lightning continues to exist.
A developing trough feature is also forecast to move northwards across England, into southern Scotland during the forecast period.
Whilst high precipitation totals are likely over the Borders/NE England, the lack of any other severe conditions prevent us from issuing a SVR threat level. There are indications that there may be an increase in convection along this feature during the afternoon and early evening, but ELT's of only -20C and excessive cloud cover, combined with lower surface temperatures, are likely to mean that lightning, if any, will be quite isolated in nature.