
It is after 5pm.. and the temp. at the local weather station is 97 DEGREES.
This is definitely our warmest day so far this season.. I almost wonder how many 100 plus degree days we're going to have.


I like the heat.. but we NEED SOME RAIN!
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PTrackerLA wrote:You sure are baking down there in Florida! Today was warm but it only reached 88 degrees. We have yet to hit 90 here possibly because of all the rain we had earlier this month.
USAwx1 wrote:the sounding at CAE also revealed INC moisture mainly above 950 and 650mb as evidenced by lowering Dewpoint depressions, although the boundary layer remians pretty dry with RH's < 50%
Stormsfury wrote:USAwx1 wrote:the sounding at CAE also revealed INC moisture mainly above 950 and 650mb as evidenced by lowering Dewpoint depressions, although the boundary layer remians pretty dry with RH's < 50%
Which pretty yields only about a 20% chance of convection, at BEST... but what, if any, development does occur ... will likely be severe, with frequent to continual lightning, and drier air at the mid-levels conducive for damaging microbursts with pulse activity.
SF
Stormsfury wrote:A couple of things of interest on the ETA are the upper disturbance swinging in from the Southwest, and a small discrete s/w over NC may be a factor tomorrow afternoon for portions of the Carolinas ...
1) IF sufficient moisture can return into the region ...
2) IF the strong subsidence and capping can be broken down enough
3) IF previous convection doesn't suppress maximum insolation with convective cloud debris ...
Dan wrote:By looking at the models and current trends, I feel like moisture will be sufficient enough for some weather. I also believe high and mid level debris will be only a small limiting factor. Jet stream winds are fast enough along with late may sun angle to erode the clouds. I just hope the short wave is strong enough to break the cap.
Since Charleston and Columbia has been mentioned, what does it look like for GSP and areas up towards the mountains? What's your take, SF?
By looking at the models and current trends, I feel like moisture will be sufficient enough for some weather. I also believe high and mid level debris will be only a small limiting factor. Jet stream winds are fast enough along with late may sun angle to erode the clouds. I just hope the short wave is strong enough to break the cap.
Since Charleston and Columbia has been mentioned, what does it look like for GSP and areas up towards the mountains? What's your take, SF?
ummm, well thats the problem, the best moisture is located inb the mid levels w/ dry air closer to the boundary layer per the CAE sounding. The more moisture in the mid levels, the better the potential for heavy rainfall, which you would see manifested in higher K indices, but for convective instability, one would want to see dry air overtop of a moist boundary layer, (which albeit is not as great for heavy rianfall, although heavy raifall CAN still occur given abundant LLVL moisture) but a MUCH better CI signal --- favoring downbursts and wind damage.
I dont forsee the potential for sevrere tomorrow with whatever might develop in response to lift generated by that s/w
Stormsfury wrote:ummm, well thats the problem, the best moisture is located inb the mid levels w/ dry air closer to the boundary layer per the CAE sounding. The more moisture in the mid levels, the better the potential for heavy rainfall, which you would see manifested in higher K indices, but for convective instability, one would want to see dry air overtop of a moist boundary layer, (which albeit is not as great for heavy rianfall, although heavy raifall CAN still occur given abundant LLVL moisture) but a MUCH better CI signal --- favoring downbursts and wind damage.
I dont forsee the potential for sevrere tomorrow with whatever might develop in response to lift generated by that s/w
Downslope component ... forgot about that ... setup is much better up in Western NC. I don't foresee a widespread outbreak either, but I can't exactly rule out a couple of severe cells in NC...
SF
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