
So last night was interesting. The area of stratiform rain ended up lasting until 4am and was way larger than any model had. Hence, the higher rain totals. But also, there were a lot of positive lightning strikes, some bolt of the blue... which are VERY unusual.
Per the nws... a large area of stratiform rain continues over the
eastern half of the CWA. Lightning activity within this shield
continues to be impressive and there are actually some cloud-to-
ground strikes behind the the precip area which seems like a pretty
rare occurrence. In addition, we are also seeing some rapid pressure
falls on the back edge of the rain with northeast winds increasing to
near 35-40 mph. This is indicative of a wake low which sometimes can
form with these system. These two interesting features likely go
together. There are radar returns above 15kft where these dry
lightning bolts are happening, which is expected since you need ice
for lightning production. However, no radar returns on the lowest
radar scans, tells us that all the precip here on the back side is
evaporating before reaching the surface. This is indicative of dry-
air subsidence which is what you need to get a wake-low to form. This
is quite an interesting setup.
Weather geek and a storm spotter in West Austin. Not a degreed meteorologist. Big snow fan. Love rain and cold! Despise heat!