valkhorn Posted January 16, 2013 Share Posted January 16, 2013 SV snow map certainly does. Thus why I posted that exact same map and said, "this seems more reasonable". I double checked your map. It doesn't show a foot for Raleigh or anywhere outside of the NC mountains. Re-check your scale. Link to comment Share on other sites More sharing options...
valkhorn Posted January 16, 2013 Share Posted January 16, 2013 SV snow map certainly does. Thus why I posted that exact same map and said, "this seems more reasonable". White after green is 3". Dark red to bright yellow approaches and eclipses 12". It isn't anywhere near Brick. Link to comment Share on other sites More sharing options...
chapelhillwx Posted January 16, 2013 Share Posted January 16, 2013 White after green is 3". Dark red to bright yellow approaches and eclipses 12". It isn't anywhere near Brick. Uhhhhh, pretty sure he was referring to a different map than the SV map. Link to comment Share on other sites More sharing options...
valkhorn Posted January 16, 2013 Share Posted January 16, 2013 I'll eat some crow over this if we actually get an 1" accumulation in Knoxville. I'm very surprised the GFS is bending towards the NAM and not the other way around. Link to comment Share on other sites More sharing options...
rduwx Posted January 16, 2013 Share Posted January 16, 2013 I double checked your map. It doesn't show a foot for Raleigh or anywhere outside of the NC mountains. Re-check your scale. I don't think burger is saying the SV maps are showing a foot for RDU. That was a different snow map he was talking about. That's the reason he said this is more reasonable when he posted the SV map. This is the way I took it atleast. Link to comment Share on other sites More sharing options...
valkhorn Posted January 16, 2013 Share Posted January 16, 2013 Uhhhhh, pretty sure he was referring to a different map than the SV map. The soundings show he was incorrect. Unless the models really change 1-3" is about all you can expect for the Raleigh area. You can't just go by the maps alone. You need to look at the soundings. Sometimes you have to be conservative with the maps and take off a few inches, too. Link to comment Share on other sites More sharing options...
Jon Posted January 16, 2013 Share Posted January 16, 2013 Text extraction for raleigh 0z gfs 39 01/17 03Z 59 59 232 7 0.00 0.00 562 573 10.7 -10.8 1013.1 58 006SCT030 121FEW141 366FEW420 60 59 0.5 0.0 42 01/17 06Z 58 58 308 6 0.01 0.00 561 572 9.7 -10.8 1013.4 73 -RA 007BKN050 133FEW157 370FEW423 60 58 0.0 0.0 45 01/17 09Z 52 50 0 9 0.01 0.00 558 571 8.7 -12.0 1014.5 93 -RA 014BKN075 CLR 416FEW268 58 52 3.1 0.0 48 01/17 12Z 47 40 5 8 0.00 0.00 556 571 7.7 -13.2 1016.7 92 -RA 025BKN078 CLR 425SCT269 58 47 16.8 0.0 51 01/17 15Z 44 37 18 10 0.06 0.00 556 571 6.8 -12.6 1018.7 98 -RA 048BKN103 144BKN215 361BKN414 47 43 18.4 0.0 54 01/17 18Z 38 35 0 9 0.30 0.00 552 568 3.7 -12.6 1019.5 99 RA 051BKN105 127BKN219 323BKN426 47 38 3.8 0.0 57 01/17 21Z 38 36 1 11 0.36 0.00 549 565 3.4 -13.6 1018.8 100 RA 072BKN116 116BKN228 263OVC446 39 38 1.0 0.0 60 01/18 00Z 39 37 12 11 0.58 0.00 548 565 3.0 -16.3 1020.8 100 RA 077BKN115 117BKN230 247OVC419 39 38 0.5 0.0 63 01/18 03Z 39 37 10 7 0.17 0.00 546 564 0.7 -14.9 1023.0 100 RA 075SCT094 123OVC232 233BKN314 39 38 0.9 0.0 66 01/18 06Z 38 36 18 7 0.00 0.00 546 565 -0.5 -16.2 1023.9 98 -RA FEW 143BKN229 233BKN312 39 38 1.6 0.0 69 01/18 09Z 34 32 356 8 0.00 0.00 546 567 -0.2 -15.6 1025.9 32 CLR 178FEW232 232SCT259 38 34 5.9 0.0 72 01/18 12Z 31 29 0 6 0.00 0.00 546 569 0.8 -15.5 1029.0 16 CLR 179FEW233 233FEW259 38 31 10.4 0.0 That's not the last run? I have this 00Z JAN16 * - APPROXIMATED 2 M 850 SFC SFC 700 6 HR 500 1000 TMP TMP PRS RHU RHU QPF HGT 500 © © (MB) (PCT) (PCT) (IN) (DM) THK FRI 00Z 18-JAN 4.1 0.9 1012 94 98 0.62 561 552 FRI 06Z 18-JAN 0.9 -2.8 1020 99 56 0.51 557 540 Link to comment Share on other sites More sharing options...
valkhorn Posted January 16, 2013 Share Posted January 16, 2013 Not related to the thread, but the cold air after this system doesn't look as deep as it had been. 850 temps over Knoxville have gone from a possible -22C a day ago to -18C. This next ULL has something to do with it. I'll bet if it went further south the next trough would have been sharper and further south, too. Plus, now that this system is more energetic, it's going to be harder to see the trough around the 22nd. Interesting methinks. Link to comment Share on other sites More sharing options...
chapelhillwx Posted January 16, 2013 Share Posted January 16, 2013 GFS snow maps put down almost a foot around RDU. If Brick gets a foot of snow out of this I'm never coming back to the boards. . The soundings show he was incorrect. Unless the models really change 1-3" is about all you can expect for the Raleigh area. You can't just go by the maps alone. You need to look at the soundings. Sometimes you have to be conservative with the maps and take off a few inches, too. Again, it's pretty obvious that he was making this comment in jest. Burger has probably figured out that NAM clown maps are not to be taken verbatim by this point. Link to comment Share on other sites More sharing options...
rduwx Posted January 16, 2013 Share Posted January 16, 2013 That's not the last run? I have this 00Z JAN16 * - APPROXIMATED 2 M 850 SFC SFC 700 6 HR 500 1000 TMP TMP PRS RHU RHU QPF HGT 500 © © (MB) (PCT) (PCT) (IN) (DM) THK FRI 00Z 18-JAN 4.1 0.9 1012 94 98 0.62 561 552 FRI 06Z 18-JAN 0.9 -2.8 1020 99 56 0.51 557 540 I'm showing the samething Jon. Link to comment Share on other sites More sharing options...
BullCityWx Posted January 16, 2013 Author Share Posted January 16, 2013 I'm showing the samething Jon. Ditto Not sure where the other numbers came from. Link to comment Share on other sites More sharing options...
SN_Lover Posted January 16, 2013 Share Posted January 16, 2013 That's not the last run? I have this 00Z JAN16 * - APPROXIMATED 2 M 850 SFC SFC 700 6 HR 500 1000 TMP TMP PRS RHU RHU QPF HGT 500 © © (MB) (PCT) (PCT) (IN) (DM) THK FRI 00Z 18-JAN 4.1 0.9 1012 94 98 0.62 561 552 FRI 06Z 18-JAN 0.9 -2.8 1020 99 56 0.51 557 540 whops , your right. sorry. Link to comment Share on other sites More sharing options...
valkhorn Posted January 16, 2013 Share Posted January 16, 2013 . Again, it's pretty obvious that he was making this comment in jest. Burger has probably figured out that NAM clown maps are not to be taken verbatim by this point. If it was then I stand corrected. Something else I thought is that over East TN we've had a lot of cold rain. I'm guessing it might have lowered the soil temperatures a bit from the warm spell we had earlier. Five inches of rain at 38 degrees F ought to do something to the soil temps. Link to comment Share on other sites More sharing options...
Wow Posted January 16, 2013 Share Posted January 16, 2013 The March 09 event is becoming a good analog for this storm, though a little weaker with the ULL. Overall, I do like the idea of a nice deformation band setting up over the same areas. Would be great to get some thundersnow again. Link to comment Share on other sites More sharing options...
BullCityWx Posted January 16, 2013 Author Share Posted January 16, 2013 The March 09 event is becoming a good analog for this storm, though a little weaker with the ULL. Overall, I do like the idea of a nice deformation band setting up over the same areas. I think we're battling a warmer boundary layer though, John. Link to comment Share on other sites More sharing options...
Jon Posted January 16, 2013 Share Posted January 16, 2013 The March 09 event is becoming a good analog for this storm, though a little weaker with the ULL. Overall, I do like the idea of a nice deformation band setting up over the same areas. Do you have a link to a pretty deep analysis of that storm? I can't find anything substantial other than a snow map and maybe the trace of the low... Link to comment Share on other sites More sharing options...
SN_Lover Posted January 16, 2013 Share Posted January 16, 2013 Do you have a link to a pretty deep analysis of that storm? I can't find anything substantial other than a snow map and maybe the trace of the low... here is a good link http://www4.ncsu.edu/~nwsfo/storage/cases/20090302/ Link to comment Share on other sites More sharing options...
JQPublic Posted January 16, 2013 Share Posted January 16, 2013 Fishel is thinking rain will end as snow Thursday nigh with the chance of limited accumulations on grassy and elevated surface. Link to comment Share on other sites More sharing options...
beanskip Posted January 16, 2013 Share Posted January 16, 2013 Well, I will take my 9 inches again in a heartbeat, but I think we're going to come up about 5 degrees F short of where we were in 2009. The March 09 event is becoming a good analog for this storm, though a little weaker with the ULL. Overall, I do like the idea of a nice deformation band setting up over the same areas. Would be great to get some thundersnow again. Link to comment Share on other sites More sharing options...
tnweathernut Posted January 16, 2013 Share Posted January 16, 2013 http://www.erh.noaa.gov/gsp/localdat/cases/2009/1-2March2009Snow/1-2MarchSnow.html Another good one. I don't think KTRI got anything from that one Link to comment Share on other sites More sharing options...
Wow Posted January 16, 2013 Share Posted January 16, 2013 Well, I will take my 9 inches again in a heartbeat, but I think we're going to come up about 5 degrees F short of where we were in 2009. No, we def won't have the sfc temps where we want and it'll be more rain than snow, but I think we'll see something here. Whether it's measurable, eh.. we'll see. Link to comment Share on other sites More sharing options...
Snowless in Carrollton Posted January 16, 2013 Share Posted January 16, 2013 If March 09 is a good analog for this storm, that is great news for Central and North GA. Link to comment Share on other sites More sharing options...
rduwx Posted January 16, 2013 Share Posted January 16, 2013 Fishel is thinking rain will end as snow Thursday nigh with the chance of limited accumulations on grassy and elevated surface. At this point I think that's a good call. The nam and gfs were a giant step in the right direction but I personally would like to see this continue to show up on the models on tomorrows runs. With the BL issues this is a true thread the needle situation for our area. Link to comment Share on other sites More sharing options...
Wow Posted January 16, 2013 Share Posted January 16, 2013 If March 09 is a good analog for this storm, that is great news for Central and North GA. Analog doesn't mean repeat. Link to comment Share on other sites More sharing options...
FoothillsNC Posted January 16, 2013 Share Posted January 16, 2013 If I lived between Asheville, Boone, to Danville, maybe Richmond corridor, I'd be getting a little nervous and maybe checking out the trees around my house tomorrow. 2 to 3" per hour snow rates of wet snow is nothing to mess around with. I don't see this lasting as long as Mar 09. Thundersnow? Yes! For some areas. Hope everyone who gets hit enjoys the snow without the aggravation. I'm looking for mostly rain this go around in my area, unless the temps really come down more than shown. Link to comment Share on other sites More sharing options...
BullCityWx Posted January 16, 2013 Author Share Posted January 16, 2013 Analog doesn't mean repeat. Not sure if you remember it but 2/19/99 could be similar, also. Link to comment Share on other sites More sharing options...
Thrasher Fan Posted January 16, 2013 Share Posted January 16, 2013 If March 09 is a good analog for this storm, that is great news for Central and North GA. I was about to type the same thing. However, that storm looked to have tracked a bit further south than the one have coming. Link to comment Share on other sites More sharing options...
Jon Posted January 16, 2013 Share Posted January 16, 2013 here is a good link http://www4.ncsu.edu/~nwsfo/storage/cases/20090302/ http://www.erh.noaa.gov/gsp/localdat/cases/2009/1-2March2009Snow/1-2MarchSnow.html Another good one. I don't think KTRI got anything from that one Thanks, guys. This will definitely be different than March 09, but certainly a good analog to take a look at. Link to comment Share on other sites More sharing options...
WhiteoutWX Posted January 16, 2013 Share Posted January 16, 2013 This is about as good as I see this getting since we are now within 36 hours. Temps aren't going to change drastically enough to give significant snow to anyone outside the mountains in NC (barring maybe the northern border counties). With that said I think areas in the piedmont could definitely see a changeover at the end for a few hours, which would already be the most snow we have seen in almost two years now. Link to comment Share on other sites More sharing options...
calculus1 Posted January 16, 2013 Share Posted January 16, 2013 http://www.erh.noaa.gov/gsp/localdat/cases/2009/1-2March2009Snow/1-2MarchSnow.html Another good one. I don't think KTRI got anything from that one Here's the authors' take on the low snow totals in the lee of the mountains in NC during that March 2009 event: The snow level lowered sufficiently so that a transition of precipitation types occurred at most locations outside the mountains. One notable exception was the North Carolina Foothills where the RUC13 925 mb temperature analysis and forecasts (not shown) indicated that a small area of relatively warm temperatures persisted throughout the afternoon. The slightly warmer temperatures delayed the onset of accumulating snow and contributed to the smaller snow totals depicted just east of the mountains in Fig. 1. Rain changed to snow at HKY around 1800 UTC, but it changed to rain again around 2000 UTC when the surface temperature increased to 36o F. Rain continued at HKY until 0047 UTC on 2 March when snow returned. The origin of the warmer air in the foothills was not clearly understood. Wind direction in the vertical veered from northeast to south from the surface to 500 mb and above, so an obvious downslope wind component to produce warming by subsidence did not exist. An untested hypothesis suggested that the predominant cooling in the cold air damming occurred farther to the east near the axis of the low-level jet in Fig. 10. The cooling progressed slowly along the foothills and did not lower surface temperatures close to freezing until late in the precipitation event. Apparently, they are still not sure why the northern foothills missed out on the snow. It wasn't due to downsloping, according to their analysis. Since BL temps are so marginal in this upcoming event as well, I must confess that I am a little worried that we might experience a similar phenomenon as occurred during this March 2009 event: If the surface temps aren't able to cool enough, we could be staring at the remnants of melted snowflakes (i.e., rain) as they smack into the ground. Link to comment Share on other sites More sharing options...
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