Update: confirmed tornadoes today (see foot!)
Potentially interesting, albeit tricky, weather tomorrow for UK, Wednesday. A deep surface LOW sits to the SW of Ireland and is dragging through complex series of fronts associated with various airmasses. Occluded fronts are tightly wrapped around the LOW, which is due to migrate NE away from the UK during the weekend and pressure to rise. For the SE tomorrow it’s not so much the fronts but an unstable mass of warm southerly surface air that will be the main cause of any heavy showers tomorrow and some potentially thundery weather, especially when this warm air is forced up by anything… coast, hills or fronts.
jetstream lowers pressure
bands of showers follow S winds
Here’s likely scenario for us in Reigate, Surrey SE: Rain is likely, possibly exceeding 10mm, which is fairly wet for SE: higher is possible. Most of this is likely to be convective rainfall due to unstable and moist air moving in from the south overnight. Showers, possibly heavy and thundery, are most likely in the morning as the warm surface air moves into our area, causing lapse rates to increase moderately and this encourages lift and cumuliform clouds. If the sun comes out then surface heating could spark heavy showers and thunderstorms as warm air rises freely through the atmosphere, encouraged by the jetstream overhead that effectively drags air off the ground. One of the ingredients for thunderstorms, LIFT, is therefore partly in place tomorrow, although it will depend on sunshine for greatest effect. If it stays overcast, which is possible, then little exciting weather action beyond just rain is likely.
convergence on coast and hills
totals could be high in SE
The above charts also show that the southerly / SW airstream is humid because, as it converges on the coast, the model shows rainfall increasing significantly. This increased rainfall on coasts is often caused by convergence which is due to air arriving onto the coast quicker than it is leaving (check the lower wind speeds inland) so the wind effectively PILES UP on the coast and is forced to rise as it has nowhere else to go except UP! This is called convergence. It is clear from the charts above that any HILLS also encourage lift as South Wales and even the South and North Downs appear to be pushing rainfall totals up locally: this is orographic or relief rainfall. The charts below shows another feature of the weather tomorrow: the winds are shown to be VEERING with height (left diag) which allows WARM air to advect (move into) into our region (right diag). Read on for more about how veering winds and WARM AIR ADVECTION can encourage stormy weather.
VEERING winds: warm air advection
warm air advection
Another ingredient for potentially unstable weather is that winds are VEERING tomorrow, albeit not dramatically, which means they are rotating clockwise directionally with height thus allowing warmer air from the south to move into a location: it is like opening the door to warm air: winds move through a southerly direction and therefore allow warm air to “advect” into our area. A moderate wind veer is taking place overnight and into tomorrow morning. Warmer air at the surface is overrun by cooler westerlies aloft that increases lapse rates: steepens the temperature difference between surface and air at altitude. The air at altitude tends to stay the same temperature and is associated more with direction and origin of airmass than it is with surface heating or advection of warmer air at the surface. An increase in lapse rates adds to instability which encourages air parcels to LIFT off the ground, should surface heating occur if the sun comes out. The chart above right shows how WARM air is ADVECTED into the South of the UK and migrates NORTH during the day. This has nothing to do with solar heating… it is an 850hPa chart (1500m) and shows the airmass temperature which is largely independent of surface influences. It’s a good example of WARM AIR ADVECTION with a moist air stream increasing instability causing showers and possible thunderstorms.
Finally, the warm relatively unstable airmass is being overridden by a NE turning jetstream that will encourages lift and wind shear. Wind shear is the vertical change of direction and/or speed with height: rotation. Shear is moderate tomorrow which might also add a twist to rising air that could even produce the odd tornado. Nice 🙂 After writing this Estofex issued a tornado warning Level 1.
spot wind veer
cape shows unstable air
jet overhead adds pazzaz
Estofex.. Level 1 tornado
Update 8 Oct: confirmed tornados from today 8 October 2014
Alfreton (T4) tornado
Likely radar signature for Bromborough
Haverthwaite Cumbria 8 Oct
Plymouth spout 7 Oct
approx locations of tornados 8 October 2014 UK