While we all remember the events like July 1989, June 1995 or June 2011 severe weather events like the one yesterday on June 22nd are far more common. Marginal/modest factors came together to produce sporadic reports of large hail and wind damage. No significant severe weather was reported but we had an impressive cluster of storms nonetheless.
At the end of a 3-day heat wave, an approaching shortwave and weak cold front was the impetus for convective initiation. Don’t get too excited about this 00z June 23 500mb analysis! Weak height falls and DCVA created broad synoptic scale lift over southern New England – and was enough to break the cap that had stifled convection the previous two days.
Temperatures in the low 90s and dew points between 65 and 70 were enough to overcome the eroding cap and convection fired across the state after 1:00 p.m. Sea breeze boundaries, differential heating boundaries (thanks to advancing mid level cloud deck), and eventually outflow boundaries created a mish mash of thunderstorms across Connecticut. While it was easy to get overwhelmed by the shear (no pun intended) of storms the ones that produced severe weather were easy to pick out on radar. Everything behaved well!
Mid level winds remained weak (500mb flow about 30 knots) with 0-6km bulk shear values between 25 and 30 knots during the event. Even with only modest 500-700mb lapse rates MLCAPE values ranged from 1500-2000 j/kg – certainly enough to support severe convection. While most storms were of the ordinary cell variety there were two supercells that developed and several multi cell clusters that lead to a number of borderline severe wind and hail reports.
No surprise the majority of the reported damage (and likely all the severe criteria hail and wind reports) came from supercells even though the environment looked somewhat meh for sueprcells. The first developed in the Catskills and tracked through Dutchess County, NY. As should be expected given unidirectional wind profile and straight hodographs the supercell split shortly after moving into Connecticut.
While it wasn’t clear given marginal deep layer shear that supercells would develop the straight hodograph indicates that splitting supercells are favored with neither right or left favored from there (thanks Shabbs). Here is a 3d radar cross section of the supercell shortly it split over Sharon.
You can see a hook echo to the south associated with a low level mesocylcone and rear flank downdraft. The core of this storm was dropping some pretty significant hail as well near Cornwall Bridge with 70dbz up to 26,000ft and impressive three body scatter spikes (hail spikes) on ENX radar (not shown). Wind damage was reported in Kent south of the storm and that was likely due to 40-50 knot winds in the storm’s rear flank downdraft. In fact damage was widespread enough that Macedonia State Park and Kent Falls State Park were closed due to tree damage.
The right moving supercell died a quick death shortly after its RFD developed as low level shear was insufficient to keep the RFD from choking the storms updraft. The left moving supercell strengthened a bit as it moved toward Torrington.
Damage was widespread in Goshen, Torrington, and Harwinton and was likely due to RFD winds in some locations (particularly south) and a macroburst in other locations (particularly north) as the core of the supercell began to collapse.
The second supercell of the day developed in Manchester and quickly split like the Litchfield County storm. The left mover produced a macroburst in Tolland that was easy to see on radar as the core collapsed, while the right mover hung on for a while doing damage in Willimantic and Scotland before falling apart.
The storm split occurred between 4:20 p.m. and 4:30 p.m. and by 4:42 p.m. you can see above two distinct updrafts both producing hail and wind damage. It appears that downbursts/macrobursts occurred in both storms moving in very different directions.
Every severe weather event is different but many around here have similarities. Weak mid level lapse rates and moisture-laden sounding (nothing says siggy severe like moist adiabatic, right?) gave us marginal CAPE and there was just enough deep layer shear to develop 2 supercells. It still amazes me how powerful doppler radar is and how we can analyze these storms so easily. During our severe weather coverage yesterday we were able to point out specific areas vulnerable for severe wind/hail damage and we nailed every single one (Kent, Sharon, Goshen, Torrington, Harwinton, Tolland, Windham, Scotland) with good lead time. Let’s hope the next one is so easy 🙂