WxUSAF Posted 3 hours ago Share Posted 3 hours ago I missed the action in Columbia due to a funeral… but my son said it was “scary”. As @Herb@MAWS posted in the other thread, about 1” on the day now. Just heard thunder again. 1 Link to comment Share on other sites More sharing options...
vortex95 Posted 3 hours ago Share Posted 3 hours ago 6 hours ago, midatlanticweather said: HRRR has said smoke should improve over the next 2 hours and I am thinking that will help with heat. No problems on moisture outside!! It is thick. Sunshine has been seriously shrouded in fog and smoke here in Loudoun GFS MOS had 93-94 and it got to 93 at DCA. And the GFS does not have smoke integrated into it, so apparent the smoke was not a factor for heating. The Td got to 77 and DCA and IAD. You get more bang for you buck per deg for Td than T when it comes to increasing CAPE. There is a sig difference between say 72 Td and 77 since moisture increase is not linear, and it really goes up fast once in the 70s! 1 1 Link to comment Share on other sites More sharing options...
vortex95 Posted 3 hours ago Share Posted 3 hours ago 4 hours ago, JakkelWx said: What a surprise storm this morning. Some of the loudest thunder ever. 0.3" Probably +CGs and the thunder was enhanced by the nocturnal inversion! Link to comment Share on other sites More sharing options...
vortex95 Posted 3 hours ago Share Posted 3 hours ago 3 hours ago, high risk said: What the heck is that random lightning strike near Damascus??? I attached the VIS image at 1716z (13:15 EDT on the image is 1:15pm EDT, right?) Was this CG verified? Sometimes isolated strikes are misplotted when there is a lot of activity. No anvil overhead or close to Damascus, but +CGs has been known shoot out laterally up to 10 mi from a CB. And when a storm, esp. a supercell, has a thick anvil streaming well downwind (can be well over 100 mi when winds aloft are strong), you can get CGs out of the anvil 50+ miles away. Farthest I have seen reported and verified is 90 mi from the parent cell core out of the anvil (storms near Enid OK and in strikes far NW OKC)! Link to comment Share on other sites More sharing options...
weatherCCB Posted 3 hours ago Share Posted 3 hours ago Nothing but light shower here Link to comment Share on other sites More sharing options...
vortex95 Posted 3 hours ago Share Posted 3 hours ago 3 hours ago, SnowenOutThere said: I think we may be in the best severe setup of the year. We’re over 5000 CAPE, have 40 kt 0-6km shear, and okay enough ML lapse rates. There’s even 100+ surface helicity according to mesoanalysis! The smoke seems to also be inhibiting storm crowding by keeping or LL lapse rates down too. The storms now popping up on radar all have the bean look of supercellular development. We may be in for a memorable day. @vortex95 @high risk@WxUSAF@wxmeddler would love to hear your updated thoughts as storms begin firing! Also, just checked and our composite indices are crazy! We’re at 8 in Nova for supercells and 1 for sig tor (2 east of Baltimore) Storm coverage was better than fcst than either the HRRR or RRFS had ydy. Some supercell structures as well, but they had tough time sustaining for very long. Looking at the radar loop, things got messy very quickly w/ storms moving in various directions due to outflow and rotation, colliding w/ each other. This probably limited the svr wx b/c no one storm could sustain for long, so we got a lot of pulse svr storms, despite the decent wind shear and a lot of CAPE. Maybe if the smoke hung around thicker longer, that would have meant less storms, but any storm would have had a better chance to sustain and rotate? The balance when it comes to the mesoscale is tricky. Small differences can be huge as to storm mode, coverage, and severity, often you don't know it until it is happening. This unknown factor has it appeal. We are still "surprised" at times (June 5, 2024 being among the best recent example), and things can look exactly alike on paper for a setup on two days, but what actually happens as to sensible wx can be a lot different. You still get tstms and svr wx, but it goes far beyond that. Will the storms train/backbuild? How intense (frequency) will the CGs be? (that varies a lot it seems). Discrete cells, a SQLN, or clusters? And who exactly will get crushed? So localized in many cases! 1 Link to comment Share on other sites More sharing options...
CAPE Posted 3 hours ago Share Posted 3 hours ago Getting crushed here now. Frequent lightning, wind is picking up bigtime. Pouring. Hope it stays below severe criteria. I just want the rain. 5 Link to comment Share on other sites More sharing options...
wxmeddler Posted 2 hours ago Share Posted 2 hours ago For the record here is the 18z LWX Balloon. Really impressive thermodynamically. Not so impressive kinematically. Shear is lackluster for anything organized. 1 Link to comment Share on other sites More sharing options...
vortex95 Posted 2 hours ago Share Posted 2 hours ago 3 hours ago, SnowenOutThere said: I suppose memorable is a sliding scale. I didn’t mean to imply we’ll see a widespread tornado or severe outbreak, but I think it might be a day where we reference it by date in the future when discussing upcoming severe systems. And memorable is relative and location specific. Short distances when it comes to tstms can be huge. Ever happen to get a storm that just maxes out over your location w/ crazy CGs so close and relentless for like 5 min, and you are ducking for cover even indoors b/c the thunder so atypically loud and you are literally hearing electrical click/pops before or during every strike? And then after it is like, "whoa, best ever!" But is a very localized experience, esp. when it comes to close lightning strikes and how loud the thunder is. Still, when it happens, it is awesome! Gets the adrenaline pumping! I can never get enough of such experiences. Give me tons of LTG! 1 Link to comment Share on other sites More sharing options...
vortex95 Posted 2 hours ago Share Posted 2 hours ago 3 hours ago, AlexD1990 said: So, mesocyclones but staying aloft? Is there any way to tell this apart on radar, maybe a certain tilt level? More days than not when svr wx occurs and it is favorable for supercells, deep layer (0-6 km) shear is good/great, but low-level (0-1 km) is weak. So you can get intense supercells w/ a nasty mesocyclone at mid-levels, but no real signature for rotation or a TDS at low-levels, and thus no tors. I've seen storms like this before in the Plains, You'd think there would be at least be an organized wall cloud for such an intense mesocyclone aloft, but just ragged, disorganized scud. Yet the storm is dumping giant hail and has incredible structure! A rule of thumb I look at for a basic start for a decent tor day is winds at least 30 kt at 925 mb. That gets you you low-level speed shear, which is important. Next, is there any veering of the winds sfc to 850? Low-level directional shear is paramount, esp.for sig tors. Is there a warm front involved? We are taught the cold fronts are the big tstm producers, and they are, but some of best intense tornadic supercells are those that form on or very close to a warm front, and ride along it. Winds locally are backed at the sfc just ahead of a warm front, but veer quicky aloft, so localized shear/helicity can be much higher than the environmental shear/helicity. Typically in most supercells, the mesocyclone (lowest pressure), is at mid-levels, the if conditions are right, the low-levels can organize for solid rotation. The exception is for TC environments. Supercells are often very low-topped, (might not even be 15,000 ft!), and deep layer shear (0-6 km) is not that great, but low-level shear (0-1 km) is excellent,owing to the strongest winds in a TC often found 925 mb to just a few 100 ft above the sfc. So you can get tors in swarms (look at what the remains of Ivan did in VA in Sep 2004), but most are weak, even a higher percentage from their continental counterparts b/c you don't have much CAPE in a TC environment, so updraft acceleration typically can't support strong/intense tors. 2 1 Link to comment Share on other sites More sharing options...
ThePhotoGuy Posted 2 hours ago Share Posted 2 hours ago Extensive damage throughout my neighborhood. Over 20 separate homes with trees laying on them. Trees down everywhere. Telephone poles snapped in half. Neighbors keep saying a tornado went through the area. Luckily no damage at the house but no power. 1 Link to comment Share on other sites More sharing options...
vortex95 Posted 2 hours ago Share Posted 2 hours ago You had this left mover (anticyclonic supercell) near Manassas earlier. You do not even have to look at the velocity to know this. The storm is deviating to the left of the mean flow and it has the flared NW to SE structure w/ the anvil streaming to the SE despite the storm moving NE! When storms rotate, it becomes complex as to the total motion vectors acting on the storm. Anticyclonic supercells rarely produce tors (in the NHEMI), but giant hail and microbursts are just as likely as w/ cyclonic supercells 1 Link to comment Share on other sites More sharing options...
high risk Posted 2 hours ago Share Posted 2 hours ago 1 hour ago, vortex95 said: I attached the VIS image at 1716z (13:15 EDT on the image is 1:15pm EDT, right?) Was this CG verified? Sometimes isolated strikes are misplotted when there is a lot of activity. No anvil overhead or close to Damascus, but +CGs has been known shoot out laterally up to 10 mi from a CB. And when a storm, esp. a supercell, has a thick anvil streaming well downwind (can be well over 100 mi when winds aloft are strong), you can get CGs out of the anvil 50+ miles away. Farthest I have seen reported and verified is 90 mi from the parent cell core out of the anvil (storms near Enid OK and in strikes far NW OKC)! All of what you said is legit, but I'm leaning now towards the idea that this was an artifact. As you said, getting a strike super far away from the core is possible, but I think you need a much more powerful setup than we had today. Link to comment Share on other sites More sharing options...
vortex95 Posted 1 hour ago Share Posted 1 hour ago 53 minutes ago, wxmeddler said: For the record here is the 18z LWX Balloon. Really impressive thermodynamically. Not so impressive kinematically. Shear is lackluster for anything organized. That is an exceptional amount of CAPE (nearly 6000) for a location on the East Coast. I am surprised there were not more svr hail reports. Low-level shear is weak. 0-6 km shear 37 kt so there is your supercell support. I think the storm coverage was a bit too much and that is what precluded more sig svr wx overall. A bit stronger capping probably would gone a long way. 1 Link to comment Share on other sites More sharing options...
AlexD1990 Posted 1 hour ago Share Posted 1 hour ago Right when the two storm complexes merged, tornado warning Link to comment Share on other sites More sharing options...
ThePhotoGuy Posted 55 minutes ago Share Posted 55 minutes ago Was there a severe thunderstorm warning for Anne Arundel when the storm hit? Link to comment Share on other sites More sharing options...
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