B
Brick Tamland
Guest
I had a whole lot of sound and fury with the passing storm earlier, but only 0.10” to show for it. Maybe something this afternoon.
I experienced that the last time I had Mexican.
I had a whole lot of sound and fury with the passing storm earlier, but only 0.10” to show for it. Maybe something this afternoon.
Interesting…View attachment 90362
Spc mesoanalysis says we are fairly unstable now and there is an obvious differential heating boundary along US1. I hope we start to see things fire along US1 as that approaches in the next couple of hours but I think we may see the better coverage just to our east where a little more sun has been realized.Storms looks like they are going to be developing on this little MCV moving through … it’s a bare skeleton right now but soon enough HRRR develops a band of storms along this skeleton…. Will be interesting to watch when they start to formView attachment 90401
What is CINMan even with the sun out you can feel the CIN in the air
What is CIN
Would expect a similar feature causing the overnight stuff tonight maybe a bit more East?Cool to see the feature that caused the morning storms View attachment 90402
Would expect a similar feature causing the overnight stuff tonight maybe a bit more East?
Thanks. It’s good to learn these terms in here from time to time. Maybe we should have a thread with meteorology terms??Convective inhibition. But I am not too worried about it affecting us later on. We should be able to get some more CAPE as the afternoon progresses.
Thanks. It’s good to learn these terms in here from time to time. Maybe we should have a thread with meteorology terms??
Thanks. It’s good to learn these terms in here from time to time. Maybe we should have a thread with meteorology terms??
Man even with the sun out you can feel the CIN in the air
As in the CIN I felt, I meant SBCIN and feeling the stableness in the air from early morning convection.How can you *feel* CINH? Meaning how can you feel the difference between it and uncapped unstable air?
It's essentially just air so warm aloft that moisture evaporates before it can organize into an updraft.