jiharris0220
Member
I wouldn’t be surprised to see a 30% moderate, or perhaps a high risk if models stay as they are now or trend even worse up until tomorrow.
Oh I know haha I’m just being silly.The earth is going to do what the earth is gong to do. Not talking about it (on a forum about Severe weather hahaha) is not going to keep us safer lol
They won't go 30% here without adding a high, the threat for significant tornadoes is too high for that.I wouldn’t be surprised to see a 30% moderate, or perhaps a high risk if models stay as they are now or trend even worse up until tomorrow.
Really very not great (newest SPC outlook).Most current guidance maximizes the STP at 8-10 around 03Z over south-central OK.
Good googly moogly
I’m seeing a pink sharpie tomorrow.Let's not and say we did.
*edited to reduce the heatFYI, there is such thing as the ignore button for people who's posts you don't want to see. Click profile, click ignore - on XenForo it works really well.
Whereas complaining about other poster's posting becomes itself annoying.
Mean closer purple … know what u meanI’m seeing a pink sharpie tomorrow.
The convective inhibition being talked about here isn't a capping inversion. It's the nightly nocturnal low-level inversion that develops on the Plains from boundary layer decoupling. It happens after sunset; so, the amount of sunshine tomorrow has nothing to do with it. We're not looking for it to be broken or eroded because it won't be (although it may not build in as fast, the stronger the low-level winds are). We are looking for supercellular updrafts to get rooted in the surface-based inflow layer prior to it getting established.If low level lapse rates are high enough and cloud cover is marginal then that CIN will be meaningless. Of course, the key word is “if”.
Look for a very large 30 percent area on Wednesday s threat … the lapse rates 12z models r showing r nearly off chart , going be a very serious big hail threstI’m seeing a pink sharpie tomorrow.
Moisture advection helps counter this, and boy do I see a lot of it through the day and into tomorrow evening.The convective inhibition being talked about here isn't a capping inversion. It's the nightly nocturnal low-level inversion that develops on the Plains from boundary layer decoupling. It happens after sunset; so, the amount of sunshine tomorrow has nothing to do with it. We're not looking for it to be broken or eroded because it won't be (although it may not build in as fast, the stronger the low-level winds are). We are looking for supercellular updrafts to get rooted in the surface-based inflow layer prior to it getting established.