A slow moving storm system over the northern Gulf Coast will continue periods of showers and thunderstorms over much of the Southeast U.S. through this weekend. The risk for heavy to excessive rainfall increases on Sunday as a surge of increased moisture moves over parts of northern Florida into southern Georgia. Read More >
Overview
A seasonably strong cold front approached the area during the afternoon hours of August 20, 2016. Showers with isolated thunderstorms developed ahead of this front and moved through northern Indiana, southwest lower Michigan and northwest Ohio. Although the showers and isolated storms mainly produced gusty sub-severe winds and heavy rainfall, a few storms produced isolated wind damage and two weak tornadoes.
A National Weather Service damage survey team from this office was dispatched to investigate storm damage across southeast Elkhart, northeast Allen County and northwestern Kosciusko County in Indiana. Three EF-0 tornadoes briefly touched down in these locations, and details regarding these tornadoes can be found below. Aside from the tornadoes and isolated wind damage reports in Allen County, IN and Jay County, most of the showers and isolated thunderstorms produced little to no damage. There were several reports of funnel clouds associated with showers in Huntington, Wells, Allen counties in Indiana, and Defiance county in Ohio.
Tornadoes:
Tornado 1: 1 mile NE of Syracuse, IN
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Tornado 2: 8 miles NE of Fort Wayne, IN
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Tornado 3: 5 miles SW of Milford, IN
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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 |
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Radar Loop -Syracuse
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KIWX Radar Loop from 3:15 - 3:22 PM EDT on 8/20/2016 This radar loop contains reflectivity and storm relative velocity. The small red square in the image is the location of the tornado touchdown. The second frame of the loop, roughly 3:17 PM EDT, shows very subtle rotation just west of the touchdown location. The next frame, at approximately 3:20 PM EDT, continues to show a subtle rotational couplet, just as the tornado had lifted. The tornado touched down and lifted within a period of one radar scan. Notice the rotational couplet is in the middle of the highest reflectivity, which would make the tornado rain-wrapped and hard to see. This radar feature is so subtle and shallow that it would likely not have been resolved if it were located further away from the radar, but was visible at only 5.5 miles away from the radar. |
Photos - Syracuse
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Minor shingle and siding damage to a residence | Large healthy tree branch snapped | Tree branches snapped and thrown away from tree grove |
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Tree damage and bent corn | Flattened corn where the tornado lifted | Multiple tops/branches of trees snapped off |
Radar Loop - Fort Wayne
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KIWX Radar Loop from 5:35 - 5:50 PM EDT on 8/20/2016 This radar loop contains reflectivity, storm relative velocity, correlation coefficient (CC) and normalized rotation (NROT). The small yellow square in the image is roughly the location of the tornado touchdown and the small yellow cross is roughly the location where the tornado lifted. Broad rotation noted on the first frame of the image quickly tightened into a stronger gate to gate couplet by the fourth frame, right around the time of touchdown. In the fourth and fifth frames, a noted reduction in the CC values co-located with the velocity couplet indicates debris being lofted into the air. The rotation weakens by the sixth and seventh frames, right around the time that the tornado lifted. Several reports of funnel clouds continued as the storm moved northeast through Grabill, with reports of the funnel nearly reaching the ground. However, no damage was reported northeast of the tornado track. |
Photos - Fort Wayne
Courtesy of WANE-TV - Wooden swing set carried across the yard and tipped over | Courtesy of WANE-TV - Flattened corn | Courtesy of WANE-TV - Power pole slightly bent |
Courtesy of WANE-TV - Tree branches snapped | Courtesy of WANE-TV - Large tree limb snapped | Courtesy of WANE-TV - Scattered small limbs, part of a downed large limb, and damage to an electrical fixture. |
Radar Loop - Milford
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KIWX Radar Loop from 3:15 - 3:22 PM EDT on 8/20/2016 This radar loop contains reflectivity and storm relative velocity. The small red square in the image is the location of the tornado touchdown. The second frame of the loop, roughly 3:17 PM EDT, shows very subtle rotation just west of the touchdown location. The next frame, at approximately 3:20 PM EDT, continues to show a subtle rotational couplet, just as the tornado had lifted. The tornado touched down and lifted within a period of one radar scan. Notice the rotational couplet is in the middle of the highest reflectivity, which would make the tornado rain-wrapped and hard to see. This radar feature is so subtle and shallow that it would likely not have been resolved if it were located further away from the radar, but was visible at only 5.5 miles away from the radar. |
Photo - Milford
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Minor shingle and siding damage to a residence | Large healthy tree branch snapped | Tree branches snapped and thrown away from tree grove |
Environment
A cold front was near the border of Indiana and Illinois at 3pm August 20. Surface temperatures were only in the low to upper 70s, however dewpoint temperatures were near 70 degrees. The environment was only modestly unstable, with SBCAPE values in the 1000-1500 j/kg range. Higher dewpoints and a moist boundary layer yielded LCL's in the 500-750 m range. Although deep layer flow was not all that impressive, with SFC-6 km bulk shear values around 30 knots, low level flow was quite high, with SFC-1 km bulk shear values 20 to 25 knots. 0-1 km SRH values ranged from 150-200 m2/s2 across the area. The combination of modest instability, high 0-1 km shear/helicity, high surface dewpoints and low LCL's supported weak tornado development.
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Figure 1: Surface Temperature, Dewpoint, Pressure 300pm August 20 | Figure 2: Surface Based CAPE 300pm August 20 | Figure 3: Lifting Condensation Levels 300pm August 20 |
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Figure 4: 0-1 km Bulk Shear 300pm August 20 | Figure 5: 0-6 km Bulk Shear 300pm August 20 | Figure 6: 0-1 km Storm Relative Helicity 300pm August 20 |
SPC Products
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Figure 7: SPC Day 1 Convective Outlook 800am August 20 | Figure 8: Mesoscale Discussion #1569 213pm August 20 | Figure 9: Mesoscale Discussion Text 213pm August 20 |
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