Morpheus wrote:Hook wrote:Without warning?
Yeah boy no drizzle before or anything. Just BRAM!
........aaaand it stop less than 5 mins after. Birds achirping again. People resume their morning walks and gardening like it never happen


lemme show yuh a scene, and why you wouldn't get any "warning", and why it happened the way it did.
There's "rain" and then there's "showers". Two completely different types of precipitation, characterized by very specific sources and behaviour, although to the layman, they're one and the same - rain is rain, right? No.
Amongst weathermen, there's an old joke about the difference between "rain showers" and "showers of rain". They're not the same thing.
"Rain" or "showers of rain", comes from stratified cloud - stratocumulus, stratus fractus, nimbo stratus, alto stratus (although precipitation from alto stratus seldom reaches the ground, known as virga, but that's another discussion. There can be ice precipitation from cirro stratus clouds, but that's way higher than concerns you on the ground) etc. - pretty much any type of flat/stratified/layered cloud produces this type of precipitation.
"Drizzle" also falls from this type of cloud, but that particular type of precipitation isn't native to T&T. We can say "rain is drizzling" and be correct because of the intensity of the precipitation, but we can't call it "drizzle" because of the nature of it. I think I already discussed that earlier on in this thread.
Stratified cloud tend to form below a stable layer of atmosphere, where it is difficult for convective activity to penetrate. This is important to identify the possibility of formation of tall convective clouds (cumulonimbus) that can be dangerous if their precipitation is accompanied by lightning, downdrafts, microbursts, twisters.
Aside from identifying the source, it usually falls in one consistent intensity, long duration, smaller droplet size.
"Showers" or "Rain showers", are characterized by the behaviour you noted - sudden onset and cessation, a clearing of the sky afterwards, droplet size varies - mostly because of the dynamic within the convective clouds that produce showers (called collision and coalescence). Note, CONVECTIVE CLOUD.
Cumulus, cumulonimbus (lightning producing). Altocumulus can produce precipitation in rare cases, but more often than not, they're a herald for bad weather to come, and sometimes even form out of the middle layers of a cumulonimbus.
Sometimes it might be in your best interest to identify what's happening to know how to secure your property or plan your movements. Next thing you're thinking it's a small shower that'll clear up in a few minutes, when it's really continuous rain that'll last hours.