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Pattern May-hem

SD said:
Disturbance just getting into NE Ga now we will see what the rest of the evening brings

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It's rolling right up 85, and some discretes trying to roll off the mountains! Could be a rainy evening
 
For May as a whole, it now looks practically certain that parts of SW GA into S AL, Anniston, Tuscaloosa, W TN, much if not all of AR, and most of MS will end up slightly cooler than normal. BHM will be close. The rest of the SE will be mainly slightly warmer than normal. The long warmer than normal streaks at ATL, SAV, and GNV continue!
 
Tarheel1 said:
It's rolling right up 85, and some discretes trying to roll off the mountains! Could be a rainy evening
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Unless things change me and you will be lucky to get .10 out of this. A classic upstate SC split with the stronger storms.
 
I think this latest batch of rain is going to miss me. :mad:
I feel like I'm slowly baking, even when I'm in the house, so this isn't fun...
 
Lame ass storms! The STW kiss of death! No thunder and light rain. Weakened dramatically as the entered GSP area! :(
 
Tarheel1 said:
Lame ass storms! The STW kiss of death! No thunder and light rain. Weakened dramatically as the entered GSP area! :(
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The 61-64 degree dewpoints hurt. The storms hit the drier air and dried up. Hopefully this does not signal how our summer will go, but I would not bet against it.
 
This storm near Columbia has a classic Flare Echo/Three Body Scatter Signature (TBSS) that's characterized as an elongated echo region orientated downstream from a (often strong) thunderstorm core that's a a result of very large hydrometeors (water-based particles, (typically hail)) and tends to occur in conjunction with large-very large hail and very destructive straight line winds in concomitant downdrafts. See Lemon (1998) for more information. I learn something new everyday! http://journals.ametsoc.org/doi/full/10.1175/1520-0434(1998)013<0327:TRTBSS>2.0.CO;2
 
Webberweather53 said:
This storm near Columbia has a classic Flare Echo/Three Body Scatter Signature (TBSS) that's characterized as an elongated echo region orientated downstream from a (often strong) thunderstorm core that's a a result of very large hydrometeors (water-based particles, (typically hail)) and tends to occur in conjunction with large-very large hail and very destructive straight line winds in concomitant downdrafts. See Lemon (1998) for more information. I learn something new everyday! http://journals.ametsoc.org/doi/full/10.1175/1520-0434(1998)013<0327:TRTBSS>2.0.CO;2
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We do too!
 
Merry Fing Christmas LOL!
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