Clem282340
Member
Can someone post the GEFS snow maps
About the same for me. No shortage of opportunity. You can add one for me next week.Well in looking at GFS for me, looks like a busy" first week "of 2018. With borderline ZR/IP event (off by couple of degrees 192 to 228), followed by mid to upper teens (ground freeze) which would lead to a significant "Impact" event (264-288), then #3 as a heavy snow event (324-348) , but then this is the 18Z GFS...
I use to go there as a kid myself. Always preferred there rather than 3 fountains. I'm right across from the elementary school. That's pretty cool man.I'm about 20 min from there. Spent a large portion of my childhood at Skate Station and at a friend's house in the Grove.
Sleet can be fun. I'm sure you know since you like hockey. In Feb 2014, CAE was on the transition zone and we picked up nearly 3 inches of sleet. I remember having my skimboard out there and ive never had more fun in a winter storm than with that storm. It was just like skimming the ocean but better haha.Not so amazing if you like getting another sleet fest in or around RDU.
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Ice storm remains on the table...Going to be interesting CAD setup depending on strength of the HP in the NE this very well could extend over into E AL and N GA esp in the higher terrain seen it numerous times. Outside of this possible event not seeing much hope for wintry precip of any consequence for other areas in this pattern setup...
...Carry on
It's certainly unusual but like we saw in the most recent winter storm it's possible. The precipitation was so intense that we created an in-situ CAD dome as melting hydrometeors amidst modest CAA cooled the low levels while deposition of water vapor into snow crystals and condensational heating warmed the mid levels so it created a weak inversion that led to mixed precipitation and a weak CAD dome despite there was just a primary coastal low. Thus, we can do that even in Miller As, eventually you reach a point where latent heating from deposition and condensation overwhelms the melting you'd see in the low levels as aforementioned and observed in the storm earlier this month. It's an extreme case but it does happen from time to time. On the flip side of this, there's actually a way you can still technically get all snow even with a big inversion and well above freezing warm nose associated with CAD. In the beginning of the February 2003 presidents Day storm the inversion over RDU was so intense despite the 5C ish temps aloft, light snow fell at the surface because as the rain drops fell into the cold low level CAD dome, they froze so quickly that they shattered instead of freezing into solid ice pellets. This shattering of new ice nuclei kickstarted the Bergeron process yet again and we got snow instead of ZR or IP as the sounding at the time suggestedLol mystery 850 bubble
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You wanna see some real cold, don't have to go very far. EPS keeps Roanoke, VA below freezing for nearly a week and a half and the mean is already depicting single digits lows haha
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To get shattering of the rain drops as they enter the CAD dome and generate snow at the low levels you want the coldest low level temps in the shallow cad dome to be at least 8-10C (or more) below freezing and the cloud condensation nuclei (CCN) that the water freezes onto needs to have a high freezing temperature when water is contact w/ it. Water in contact with CCN like pollen, dust grains, soot, and salt crystals will freeze at different temperatures. Henceforth, even if you got the temperature profile, moisture, lift, etc exactly right you still could screw up the precipitation type at the surface (esp determining sleet vs freezing rain) because you don't know the distribution of CCN in the cloud that's producing the precipitation. Even with current observational techniques we can't adequately observe CCN, thus it is parameterized in NWP models and most assume models stereotypical marine CCN distributions (which isn't correct for us on the continental landmass). It's just another limitation of NWP modeling for winter stormsIt's certainly unusual but like we saw in the most recent winter storm, wherein the precipitation was so intense that we created an in-situ CAD dome as melting hydrometeors amidst modest CAA cooled the low levels while deposition of water vapor into snow crystals and condensational heating warmed the mid levels so it created a weak inversion that led to mixed precipitation despite there was just a primary coastal low. Thus, we can do that even in Miller As, eventually you reach a point where latent heating from deposition and condensation overwhelms the melting you'd see in the low levels as aforementioned and observed in the storm earlier this month. It's an extreme case but it does happen from time to time. On the flip side of this, there's actually a way you can still technically get all snow even with a big inversion and well above freezing warm nose associated with CAD. In the beginning of the February 2003 presidents Day storm the inversion over RDU was so intense despite the 5C ish temps aloft, light snow fell at the surface because as the rain drops fell into the cold low level CAD dome, they froze so quickly that they shattered instead of freezing into solid ice pellets. This shattering of new ice nuclei kickstarted the Bergeron process yet again and we got snow instead of ZR or IP as the sounding at the time suggested
I wouldn't say that at all, Atlanta and points NE should be keeping a close eye on this, because it would take next to nothing verbatim to give the metro area a big ice storm
Could you try Columbia,SC?The EPS is already trying to pick up on yet another threat for wintry weather in RDU sometime around January 2-6.
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Could you try Columbia,SC?