The current modeled totals for next week probably consist largely of the more persistent rain systems, rather than the convective storms. Recent reading that I've been doing for my dissertation has covered how models with a resolution similar to GFS tend to underestimate rainfall in the moderate-heavy range, though the error reduces as you near 10mm/hr rain rates.
The net effect is to underestimate convective rainfall, however. For that, we'll need to turn to models such as WRF and EURO-4, which can represent convection in far more detail, and with greater accuracy overall, although peak intensities can be rathe overdone.
On to the latest runs... I see GFS has taken a step back on the trend to bring less cold air down the eastern flank of the Atlantic ridge, leading to stronger trough development over the UK and less to the SW - yet the run still features enough of a trough to the SW to promote a bit of a ridge close to the SE then E of the UK, bringing back the warm continental air after a brief absence... renewing the thunder/rain threat.
UKMO seems to see the colder air in the Atlantic having less of an impact on the UK trough, leaving it a weaker feature, and keeping that colder air out to the west rather than drawing it across as convergence occurs near the surface in the low pressure system.
Given the failed projections of strong trough development from interaction with cold air last week, I'm inclined to give UKMO the nod over GFS.
http://www.wetterzentrale.de/pics/Recm1442.gif
Now how about ECM eh? Once again it shows notable low pressure system development, and once again that's not so much down to cold air interaction - there's much more of a ridge to the north of the trough and the whole pattern just seems a bit more amplified to me.
Given that I see ridge progression to the NE from the N/NW as something often underestimated, I'm inclined to give ECM the nod over UKMO...
Originally Posted by: Stormchaser