Overview
During the afternoon and evening of May 16th, a system tracked near our forecast area, producing large-scale lift and a convective environment supportive of severe convection across much of Southern Appalachia and places nearby. All modes of severe weather occurred in our forecast area, including multiple EF-1 tornadoes in southwest Virginia. A total of 31 Local Storm Reports (LSRs) were received for the day, including 5 reports of 1" hail, 24 reports of straight line wind damage, and 2 confirmed tornadoes. There were no injuries or fatalities reported in the forecast area, but there were 2 injuries and 1 fatality that occurred from this event as a whole. At the time of this page being published, the confirmed tornadoes are still preliminary and are subject to change as additional information is gathered.
Tornadoes:
Tornado - Near Stickleyville, VA
Track Map Downloadable KMZ File |
Tornado - Duffield, VA
Track Map Downloadable KMZ File |
Tornado - 3 WSW Pennington Gap, VA
Track Map Downloadable KMZ File |
The Enhanced Fujita (EF) Scale classifies tornadoes into the following categories:
EF0 Weak 65-85 mph |
EF1 Moderate 86-110 mph |
EF2 Significant 111-135 mph |
EF3 Severe 136-165 mph |
EF4 Extreme 166-200 mph |
EF5 Catastrophic 200+ mph |
Photos
Panoramic View of Shelf Cloud from the Morristown NWS Office (Courtesy: NWS Employee) |
Shelf Cloud Viewed from Downtown Sevierville
(Courtesy: Jennifer Reimschuessel)
|
Damage to Pennington Gap Plaza, Pennington Gap, VA (Courtesy: WJHL-TV) |
Tree Damage in Pennington Gap, VA (Courtesy: Kim Carter) |
Tree Down on Route 58 in Hilltons, VA (Courtesy: Pam Murray) |
Quarter-Sized Hail in Boyd's Creek, TN (Courtesy: WATE-TV) |
Radar
Figure 1: Base Reflectivity and Base Velocity near Pennington Gap, VA from the Jackson, KY Radar |
This image shows the reflectivity (left) and base velocity (right) from the Jackson, Kentucky radar. The reflectivity image shows the leading edge of the storm “bowing” out, which is a signature of high winds surging forward. The velocity image shows a maximum velocity of 71 mph (bright pink colors). Keep in mind that at this distance from the radar, the radar is intersecting the storm about 4,000 feet above ground level. This pocket of high winds aloft was likely a rear-flank downdraft that descended to the ground a few minutes later, and produced the extensive wind damage south of Pennington Gap (near the red square). A damage survey estimated wind speeds at the ground of 70 to 90 mph. The velocity image also shows rotation just south of Pennington Gap (green beside red), which prompted the issuance of a tornado warning, but a tornado had not yet reached the ground at this time. Eyewitnesses near Pennington Gap reported that a funnel cloud was spotted. The descent of the rear-flank downdraft can sometimes be a precursor to a tornado touchdown. About 15 minutes later, a tornado touched down near Stickleyville, Virginia.
Figure 2: Base Reflectivity and Storm Relative Velocity near Stickleyville, VA from the Morristown, TN Radar |
This is an image taken from the radar in Morristown, Tennessee near the time that a tornado touched down near Stickleyville. The approximate location of the surveyed tornado is at the red square. The radar is viewing the storm about 3,200 feet above the ground, well above the tornado. This storm is showing some broad rotation aloft, as seen in the storm-relative velocity image on the right. This is a mesocyclone - a rotating updraft in the midlevels of a storm.
Figure 3: Base Reflectivity and Storm Relative Velocity near Duffield, VA from the Morristown, TN Radar |
A tornado touched down south of Duffield, VIrginia, near the red square in the image. The storm-relative velocity image on the right shows rotation in the midlevels of the storms (about 3,600 feet above the ground), which is the mesocyclone and not the tornado. The radar beam is too high to detect the tornado on the ground.
Figure 4: Base Reflectivity in Anderson County, TN |
This storm produced quarter sized hail between Oak Ridge and Clinton around 4:30 pm EDT. The left image is reflectivity at about 7,500 feet above the ground, and the right image is reflectivity about 15,000 feet above the ground. This core of high reflectivity (pink area) in the midlevels of the storm is a hail core. The storm’s updraft is lofting the hail high into the storm, where temperatures are well below freezing, allowing hailstones to grow. Another interesting feature in this image is the area of low reflectivity extending out of the west side of the storm (gray and dark blue colors). This is called a three body scatter spike, or hail spike. It is a radar artifact that occurs when a portion of energy from the radar beam hits hail, is reflected off the hail to the ground, is reflected again from the ground to the hail, then is reflected back to the radar. Because of the extra time it takes for this energy to be reflected three times and returned to the radar (only a fraction of a millisecond), the radar displays this energy down radial of the storm’s hail core.
Figure 5: Base Reflectivity and Base Velocity in Grainger/Hamblen Counties |
The close proximity of this storm to the KMRX radar (red dot near Talbott), allows for good detection of high winds close to the ground. The velocity image on the right is showing an area of high winds moving directly toward the radar, with a maximum speed of 63 mph. Trees and power lines were blown down by this storm near Joppa and Rutledge in Grainger County, and in Hamblen County near Alpha. The reflectivity image on the left shows the forward surge of outflow winds on the leading edge of the storm. A photo of this storm was taken from our office at 6:23 pm EDT, about the same time as this radar image.
Storm Reports
W - Wind
H - Hail
T - Tornado
Public Information Statement National Weather Service Morristown TN 725 PM EDT Wed May 17 2023 ...NWS Damage Survey for May 16, 2023 Thunderstorm Wind Event in Pennington Gap, Virginia... A NWS survey team investigated damage in Pennington Gap, Virginia. A 2.5 mile wide swath of damage was found on the south side of town. Wind speeds were estimated between 70 and 90 mph. && NOTE: The information in this statement is preliminary and subject to change pending final review of the event and publication in NWS Storm Data.
PRELIMINARY LOCAL STORM REPORT...SUMMARY NATIONAL WEATHER SERVICE MORRISTOWN TN 1041 AM EDT WED MAY 17 2023 ..TIME... ...EVENT... ...CITY LOCATION... ...LAT.LON... ..DATE... ....MAG.... ..COUNTY LOCATION..ST.. ...SOURCE.... ..REMARKS.. 0350 PM HAIL MALONEYVILLE 36.09N 83.84W 05/16/2023 M1.00 INCH KNOX TN PUBLIC REPORT FROM MPING: QUARTER (1.00 IN.). 0350 PM HAIL MALONEYVILLE 36.09N 83.84W 05/16/2023 U1.00 INCH KNOX TN PUBLIC REPORT FROM MPING: QUARTER (1.00 IN.). 0403 PM HAIL 15 NE KNOXVILLE 36.13N 83.76W 05/16/2023 M1.00 INCH KNOX TN PUBLIC 1 INCH HAIL IN CORRYTON, TN. TIME ESTIMATED FROM RADAR. 0403 PM HAIL 15 NE KNOXVILLE 36.13N 83.76W 05/16/2023 M1.00 INCH KNOX TN PUBLIC 1 INCH HAIL IN CORRYTON, TN. TIME ESTIMATED FROM RADAR. 0420 PM TSTM WND DMG 2 NNW ALPHA 36.20N 83.40W 05/16/2023 HAMBLEN TN NWS EMPLOYEE TREES AND LARGE TREE LIMBS DOWN IN AND NEAR SEVEN OAKS SUBDIVISION. 0425 PM HAIL 5 SW CLINTON 36.04N 84.20W 05/16/2023 E1.00 INCH ANDERSON TN PUBLIC 0428 PM HAIL 6 NE OAK RIDGE 36.03N 84.22W 05/16/2023 M1.00 INCH ANDERSON TN PUBLIC SOCIAL MEDIA PICTURE OF QUARTER SIZE HAIL. EXACT LOCATION IN OAK RIDGE NOT PROVIDED. 0432 PM HAIL 6 NE OAK RIDGE 36.03N 84.22W 05/16/2023 U0.70 INCH ANDERSON TN PUBLIC REPORTED BY TRAINED SPOTTER. 0432 PM HAIL 6 NE OAK RIDGE 36.03N 84.22W 05/16/2023 M0.70 INCH ANDERSON TN PUBLIC REPORTED BY TRAINED SPOTTER. 0449 PM HAIL 1 NW DANDRIDGE 36.04N 83.43W 05/16/2023 E0.70 INCH JEFFERSON TN PUBLIC REPORTED BY TRAINED SPOTTER. 0449 PM HAIL 1 NW DANDRIDGE 36.04N 83.43W 05/16/2023 E0.70 INCH JEFFERSON TN PUBLIC REPORTED BY TRAINED SPOTTER. 0455 PM HAIL KARNS 35.98N 84.12W 05/16/2023 M0.88 INCH KNOX TN BROADCAST MEDIA 0500 PM TSTM WND DMG 2 WNW KNOXVILLE 35.98N 83.98W 05/16/2023 KNOX TN 911 CALL CENTER 3 TREES DOWN. ONE TREE ON TOP OF CAR. 0501 PM TSTM WND DMG ENGLEWOOD 35.42N 84.49W 05/16/2023 MCMINN TN BROADCAST MEDIA ROOF DAMAGE TO BARN AND TREES DOWN. TIME ESTIMATED FROM RADAR. 0503 PM HAIL 3 SW POWELL 35.99N 84.05W 05/16/2023 E0.70 INCH KNOX TN PUBLIC . 0503 PM HAIL 3 SW POWELL 35.99N 84.05W 05/16/2023 E0.70 INCH KNOX TN PUBLIC 0515 PM TSTM WND DMG WISE 36.98N 82.58W 05/16/2023 WISE VA 911 CALL CENTER TREES DOWN. 0525 PM TSTM WND DMG PENNINGTON GAP 36.76N 83.03W 05/16/2023 LEE VA PUBLIC MULTIPLE TREES DOWN. 0530 PM HAIL 3 NNE KNOXVILLE 36.02N 83.92W 05/16/2023 E1.00 INCH KNOX TN TRAINED SPOTTER 0530 PM TSTM WND DMG DUFFIELD 36.72N 82.80W 05/16/2023 SCOTT VA PUBLIC TREES DOWN. 0535 PM TSTM WND DMG FINCASTLE 36.41N 84.05W 05/16/2023 CAMPBELL TN 911 CALL CENTER TREES DOWN. 0545 PM TSTM WND DMG SEVIERVILLE 35.89N 83.58W 05/16/2023 SEVIER TN 911 CALL CENTER NUMEROUS TREES DOWN. 0550 PM TSTM WND DMG 5 W HONAKER 37.02N 82.06W 05/16/2023 RUSSELL VA 911 CALL CENTER MULTIPLE TREES DOWN. 0600 PM TSTM WND DMG 4 ENE CLINCHPORT 36.70N 82.67W 05/16/2023 SCOTT VA PUBLIC SEVERAL TREES DOWN ACROSS THE COUNTY. 0615 PM TSTM WND DMG RUTLEDGE 36.27N 83.52W 05/16/2023 GRAINGER TN 911 CALL CENTER TREE DEWON IN RUTLEDGE. 0615 PM TSTM WND DMG 1 ENE JOPPA 36.24N 83.60W 05/16/2023 GRAINGER TN PUBLIC REPORT FROM MPING: 3-INCH TREE LIMBS BROKEN; POWER POLES BROKEN. 0635 PM TSTM WND DMG OAK RIDGE 35.96N 84.30W 05/16/2023 ANDERSON TN 911 CALL CENTER FEW TREES DOWN. 0635 PM TSTM WND DMG SHADY VALLEY 36.52N 81.93W 05/16/2023 JOHNSON TN PUBLIC MULTIPLE TREES DOWN. 0640 PM TSTM WND DMG 2 NNW ALPHA 36.20N 83.39W 05/16/2023 HAMBLEN TN AMATEUR RADIO FEW TREES DOWN. 0643 PM HAIL 2 SE HOPEWELL 35.21N 84.87W 05/16/2023 U0.75 INCH BRADLEY TN PUBLIC REPORT FROM MPING: DIME (0.75 IN.). 0645 PM TSTM WND DMG 1 NNW LOWLAND 36.16N 83.21W 05/16/2023 HAMBLEN TN LAW ENFORCEMENT A FEW TREES DOWN. 0650 PM TSTM WND DMG CLEVELAND 35.18N 84.87W 05/16/2023 BRADLEY TN 911 CALL CENTER FEW TREES AND POWER LINES DOWN. 0656 PM HAIL 2 S POWELL 36.00N 84.02W 05/16/2023 E0.25 INCH KNOX TN PUBLIC 0656 PM HAIL 1 NW KARNS 35.98N 84.13W 05/16/2023 M0.70 INCH KNOX TN PUBLIC . 0656 PM HAIL 1 NW KARNS 35.98N 84.13W 05/16/2023 M0.70 INCH KNOX TN PUBLIC 0703 PM TSTM WND DMG 1 W BENTON 35.18N 84.67W 05/16/2023 POLK TN TRAINED SPOTTER MULTIPLE TREES DOWN. 0704 PM HAIL 3 NW BEARDEN 35.97N 84.04W 05/16/2023 E0.25 INCH KNOX TN PUBLIC REPORTED BY TRAINED SPOTTER. 0710 PM TSTM WND DMG 2 WSW BENTON 35.17N 84.68W 05/16/2023 POLK TN TRAINED SPOTTER TREES DOWN ACROSS ROADWAY. 0725 PM TSTM WND DMG 4 NW EMBREEVILLE 36.23N 82.51W 05/16/2023 WASHINGTON TN DEPT OF HIGHWAYS CORRECTS PREVIOUS TSTM WND DMG REPORT FROM 4 NW EMBREEVILLE. A FEW TREES DOWN. 0725 PM TSTM WND DMG 3 NE KNOXVILLE 36.00N 83.90W 05/16/2023 KNOX TN 911 CALL CENTER SEVERAL TREES DOWN. 0728 PM FLASH FLOOD 3 NE KNOXVILLE 36.01N 83.91W 05/16/2023 KNOX TN 911 CALL CENTER FLOODING OF ROADWAYS. 0730 PM HAIL 3 SW KARNS 35.94N 84.13W 05/16/2023 E0.25 INCH KNOX TN PUBLIC REPORTED BY TRAINED SPOTTER. 0730 PM FLASH FLOOD 1 SSE KNOXVILLE 35.96N 83.93W 05/16/2023 KNOX TN PUBLIC REPORT FROM MPING: STREET/ROAD FLOODING; STREET/ROAD CLOSED; VEHICLES STRANDED. 0730 PM FLOOD MALONEYVILLE 36.09N 83.84W 05/16/2023 KNOX TN PUBLIC REPORT FROM MPING: RIVER/CREEK OVERFLOWING; CROPLAND/YARD/BASEMENT FLOODING. 0740 PM TSTM WND DMG 3 NW EMBREEVILLE 36.22N 82.50W 05/16/2023 WASHINGTON TN DEPT OF HIGHWAYS CORRECTS PREVIOUS TSTM WND DMG REPORT FROM 3 NW EMBREEVILLE. A FEW TREES DOWN. 0830 PM TSTM WND DMG TUSQUITEE 35.08N 83.77W 05/16/2023 CLAY NC LAW ENFORCEMENT TREE DOWN. EXACT LOCATION UNKNOWN.
Environment
Figure 1: 300mb Heights, Divergence, and Winds at 2200 UTC, 16 May 2023 | Figure 2: 500mb Heights, Temperature, and Winds at 2200 UTC, 16 May 2023 | Figure 3: 850mb Heights, Temperature, and Winds at 2200 UTC, 16 May 2023 |
An upper level jet across the lower Ohio Valley into the mid-Atlantic states produced large-scale forcing over the central and southern Appalachians into the eastern Tennessee valley. The 300mb analysis showed divergence aloft over southeast Kentucky, southwest Virginia and northeast Tennessee which aided in the development of storms.
The upper forcing enhanced the boundary layer jet over the eastern Tennessee valley and southern Appalachians with southwest winds of 30 kts. This low level jet pulled abundant moisture and instability into the central and southern Appalachians.
Figure 4: Surface Station Plot at 2200 UTC, 16 May 2023 | Figure 5: Surface Moisture Convergence and Mixing Ratio at 2100 UTC, 16 May 2023 |
The surface analysis at 2200Z, May 16th 2023 showed an area of low pressure across southwest Virginia with a cold front extending west across northern Tennessee with a near stationary boundary east to northeast of the low over western Virginia.
Warm and moist conditions were noted south of the boundary across Tennessee with temperatures in the 80s and dewpoints in the 60s, much cooler air in Kentucky air-mass north of the boundary. A convergent wind field helped to focus the severe storms in this area during the late afternoon and evening hours.
Table 1: K1A6 (Middlesboro KY) surface observations on 16 May 2023
Figure 6: RAP Initialization Sounding at K1A6 (Middlesboro KY) at 2000 UTC, 16 May 2023
Figure 7: RAP Initialization Sounding at K1A6 (Middlesboro KY) at 2100 UTC, 16 May 2023
Figure 8: RAP Initialization Sounding at KTRI (Tri-City Airport TN) at 2100 UTC, 16 May 2023
The K1A6 (Middlesboro, KY) and KTRI (Tri-City Airport) RAP initialization soundings at 20 and 21 UTC, 16 May 2023 were utilized to diagnose the environment near the Lee County, Virginia tornado.
The soundings depicted a marginally unstable environment with CAPES of 1000 J/Kg and low-level CAPE over 100+ J/Kg. Lifting Condensation Level (LCL) of 900-1000 meters. The effective storm scale shear was in the middle and upper 30s knots with the 0-1 km shear of 15 to 20 knots. Overall, a marginal environment for tornadoes across southwest Virginia. The K1A6 (Middlesboro, KY) surface observations depicted a backing of the surface winds ahead of the storm which likely enhanced the low-level shear within this area.
However, the favorable low-level CAPE and close proximity of surface low and stationary boundaries across southwest Virginia likely improved the near storm environment.
Figure 9: MLCAPE and CIN at 2200 UTC, 16 May 2023 | Figure 10: 0-3 km MLCAPE and Surface Vorticity at 2000 UTC, 16 May 2023 | Figure 11: CAPE (-10 to -30 C), Freezing Level, and 0-6 km Shear at 2000 UTC, 16 May 2023 |
Figure 12: Mid-Level Lapse Rates (700-500mb) at 2200 UTC, 16 May 2023 | Figure 13: DCAPE and DCIN Mid-Level Lapse Rates (700-500mb) at 2200 UTC, 16 May 2023 | Figure 14: Effective Shear at 2200 UTC, 16 May 2023 |
Figure 15: 0-1 km Shear at 2200 UTC, 16 May 2023 | Figure 16: 0-1 km Storm Relative Helicity at 2200 UTC, 16 May 2023 | Figure 17: 0-3 km Storm Relative Helicity at 2200 UTC, 16 May 2023 |
Figure 18: Supercell Composite Parameter (SCP) (effective layer with muCIN) and Bunkers Storm Motion at 2000 UTC, 16 May 2023 | Figure 19: Significant Tornado Parameter (effective layer) and MLCIN at 2000 UTC, 16 May 2023 | Figure 20: Derecho Composite Parameter (effective layer) and MLCIN at 2000 UTC, 16 May 2023 |
Figure 21: SHERBE (0-3 km LR, EBWD, and 700-500 mb LR) at 2000 UTC, 16 May 2023 |
The SPC mesoanalysis depicted an unstable environment with MLCAPES of 1000-2000 J/Kg. As noted above the 0-3 km MLCAPE was quite high with values of 100-150.
Even though the mid-level lapse of 6 degree C was at best marginal favorable, Hail CAPES of 500-700 J/Kg and effective storm scale shear in the 30s to near 40 knots produced an environment for favorable hail growth and resident time for severe hail.
Downdraft CAPES of 700-800 J/Kg and a low-level jet up to 30 knots were sufficient to produce damaging straight line winds and/or downbursts with the storms. This was also noted with the Derecho Composite Parameter (DCP) values of 2+.
The Supercell Composite Parameter (SCP) and Significant Tornado Parameter depicted an overall favorable environment for rotating storms across much of the area with the greatest potential of tornadoes over southwest Virginia and far northeast Tennessee. The SHERBE composite parameter also noted this area as the highest concern for low CAPE and high Shear tornadoes.
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