Tornadoes · United States · Wisconsin · 2000

F0 tornado, Evansville, Wisconsin, August 5, 2000

This F0 tornado ran 0.1 miles across Rock County on August 5, 2000, touching down at 3:43 PM CDT and reaching 20 yards wide. It killed nobody, and did $10,000 of property damage.

The rating scale

Tracks are drawn in the color of the rating. The Fujita scale rates the damage rather than measuring the wind: the speeds are what that damage is taken to imply.

  1. F040 to 72 mphthis tornado

    Light damage. Surface peeled off some roofs, gutters and siding damaged, branches broken, shallow-rooted trees pushed over.

  2. F173 to 112 mph

    Moderate damage. Roofs badly stripped, mobile homes overturned or badly damaged, exterior doors lost, windows broken.

  3. F2113 to 157 mph

    Considerable damage. Roofs torn off well-built houses, frame homes shifted on their foundations, mobile homes destroyed, large trees snapped or uprooted, cars lifted off the ground.

  4. F3158 to 206 mph

    Severe damage. Whole stories of well-built houses destroyed, large buildings badly damaged, trains overturned, trees debarked, heavy cars lifted and thrown.

  5. F4207 to 260 mph

    Devastating damage. Well-built houses leveled, structures with weak foundations moved some distance, cars thrown and large missiles generated.

  6. F5261 to 318 mph

    Incredible damage. Strong frame houses swept off their foundations, car-sized missiles thrown more than 100 meters, steel-reinforced concrete badly damaged, high-rise buildings deformed.

  7. Unrated

    The survey recorded a tornado but could not put a number on it, most often because it crossed open country and damaged nothing a rating can be read from.

The record

Rating
F0
Date
August 5, 2000
Touchdown
3:43 PM CDT (20:43 UTC)
Path length
0.1 miles (0.2 km)
Path width
20 yards (18 m)
Deaths
0
Injuries
0
Property damage
$10,000
County
Rock County
Touchdown point
42.770, -89.330
Lift-off point
42.770, -89.330
Record number
464

What the Weather Service recorded

This summer's most powerful downburst wind event to affect south-central and southeast Wisconsin pummeled portions of Dane, Green, and Rock counties with damaging hurricane-force winds, large hail, and urban-flood rains. As the 35 mile long line of thunderstorms moved southeast through Dane, northern Green, and Rock Counties, it increased in strength, ultimately producing straight-line winds estimated up to 100 knots (115 mph), heavy rains at a rate of 1 to 3 inches per hour, and hail stones 1 inch in diameter. Due to downed power lines and poles, ultimately about 18,000 customers had electrical power disrupted for 1 to 2 days. Descriptions of weather-related events follow in a county-by-county breakdown.Dane County:Powerful thunderstorm winds, estimated at 56 knots (65 mph), toppled several large trees in and near the city of Belleville. There were no reports of injuries or deaths. Minor urban-type flooding was noted due to intense rain accompanying the storm.Green County:The squall-line intensified as it clipped the northeast quarter of Green County. Based on inflicted damage, winds gusts were estimated to be 74 knots (85 mph). The worst-hit area extended from a subdivision west of the village of Dayton (Town of Exeter), east/southeast to the county line. About 50 homes sustained varying amounts of damage caused by felled trees, tree branches, or the wind outright. Damage to home siding and roofs was also noted. Hundreds of trees were toppled, about 2 dozen farm buildings were damaged or destroyed, several silos were damaged, and two semi-tractor trailers were overturned. Many power lines were either blown over or knocked down by tree debris.Rock County:This county bore the brunt of the storm as its straight-line winds intensified to an estimated 100 knots (115 mph). The macroburst damage path was 3 to 6 miles wide, extending from southwest of Evansville in the Town of Magnolia (Highway 59 and A) east/southeast through the city of Janesville to southeast of Avalon near Caver Roehl Park. A newspaper headline nicely stated the effects: Rain! Wind! Wow! The powerful winds leveled thousands of trees (some 200 years old); tore roofs off homes; businesses, and farm buildings; blew tops of silos off, flipped over vehicles; blew in windows; damaged or peeled off home siding; knocked over billboards and road signs; closed many roads due to debris, and flattened corn and soybean fields. Based on newspaper photographs and eyewitness accounts, maximum wind gusts were estimated to be in the 87 to 100 knots range (100 -115 mph). The worst of the damage appeared to be equivalent to that caused by tornado winds of about 115 mph, or at the bottom of the F2 category. Many people noted that the sky grew very dark as the storm blew in with a wall of white rain mixed with tree leaves and branches. The city of Janesville was at ground zero, as a 3.7 square mile looked like a bomb had hit its downtown area and the near east and west sides. A roof was torn off one business, and bricks were pealed off another business. It took at least 2 weeks to remove the tree debris from city streets, sidewalks, and backyards. Dozens of vehicles were damaged by felled trees and branches. It is estimated that 400 to 500 city homes sustained some degree of damage (6 destroyed). Traxler and Bond Parks looked like disaster areas and were closed. About 50 electrical poles were snapped by tree debris or the winds. One person in the city was injured when a tree fell on their pickup truck. Just north of Janesville on Interstate-90, another person was injured when their SUV was flipped over by the winds. In addition, 5 semi-tractor trailers were overturned on I-90 in the same vicinity. A new sub-division 3 miles south of Janesville experienced extensive roof or siding damage due to the winds or tree debris. Several vehicles were damaged as well. Just to the south of the city, the wastewater treatment plant recorded 1.48 inches of rain as the storms moved through, resulting in urban flooding. There were other unofficial reports of 2 to 3 inches in the city area.The civil Town of Magnolia, in the western part of the county, was also hard hit by the macroburst, especially near and along Highway 59 and County Trunk Highway A. About 40 power poles in this Town were toppled by the winds or tree debris.A little further north on Croft Road, just southwest of Evansville, a local resident noted this sequence of events: the initial, powerful winds and blinding rains lasted for about 5 minutes and were followed by hailstones up to 1 inch in diameter. Then the rain and hail stopped. After a couple minutes he noticed across the road in a field a ground-based vortex pulling corn stalks up to about 200 feet above the ground, while above it at cloud base was a funnel cloud. This weak vortex then hit a barn and caused slight damage before dissipating. Shortly thereafter, another round of rain, and gusty, but much weaker winds occurred. Based on this resident's account, and their prior experiences with tornadoes while living in Texas, this vortex was classified as a tornado. The macroburst continued to inflict wind damage to a point about 3 miles east/southeast of the Janesville city limits along Highway 14, at which point it weakened. However, the thunderstorms briefly intensified once again southeast of the village of Avalon near Carver Roehl Park. At this location, a barn's roof was lifted and dropped by powerful winds, resulting in a collapsed structure which trapped 40 steer. Fifteen of the steer died from injuries, and some of the hay bales were destroyed. Collectively across Rock County, about 4500 acres of corn and soybean crops were badly damaged or destroyed. Thirty-five farm buildings had minor damage, 8 had major damage, and 19 were destroyed by the winds. Walworth County:The remains of the squall-line generated downburst winds which leveled large trees in and near the city of East Troy.Racine County:The remains of the squall-line generated downburst winds which leveled large trees west of Waterford.Kenosha County:The remains of the squall-line generated downburst winds which leveled large trees southwest of the village of Twin Lakes.Milwaukee County:The remains of the thunderstorms dumped rain amounts of 2.25 to 3.1 inches across Milwaukee County based on Ham reports. Moderate urban flooding resulted. A West Allis motorist was rescued from their stalled vehicle due to water depths of 1.5 to 3 feet in low spots on roads. Similar water depths on strees were noted elsewhere in the county, especially in the southern half. No damage was reported. Synoptically, an upper level trough was moving across Wisconsin on August 5th, with a weak vorticity maxima over the southern part of the state moving east/southeast. The south winds of a low-level jet fed the storms as west-northwest flow at 18,000 feet intensified to 60 knots based on profiler data. Thunderstorm echo tops were 40 to 42,000 feet.

Narrative is incorporated in discussion of August 5th storms below.

From NOAA NCEI's Storm Events Database, the narrative the local forecast office wrote for Storm Data.

The warnings

No tornado warning for this county appears in the archive as in force at the moment the tornado touched down.

Issued (UTC)ExpiredProductOffice
20:38 UTC21:30 UTCSevere Thunderstorm WarningMKX

Every warning and watch covering the touchdown point that day, from the Iowa Environmental Mesonet's archive of National Weather Service products. Lead time is measured from the issue of the warning in force to the touchdown time in the database, both of which were recorded to the minute by different people.

The forecast that day

The Storm Prediction Center had this point in a General Thunderstorms Risk. The outlook in force was issued at 20:15 UTC.

SPC's Day 1 convective outlook as it stood when the tornado began, read at the touchdown point. The same archive is on the radar archive.

The air that afternoon

The radiosonde launches on either side of the tornado, from the nearest station that was launching then, drawn and analyzed the way Storm Lab does: the same diagram, the same parcel and shear definitions SPC's mesoanalysis uses.

Davenport, (KDVN), 12:00Z

8.7 hours before the tornado, 160 km from the path. August 5, 2000.

Skew-T log-pSkew-T log-p diagram, Davenport, at 12:00Z on 2000-08-05Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 0 joules per kilogram, CIN -69256, lifted condensation level 1330 meters above ground. Wind barbs in knots down the right edge.LCL10008507005003002001001 km2 km3 km6 km9 km12 km15 km-30°-20°-10°10°20°30°40°
Temperature in red, dew point in green, the mixed-layer parcel dashed. The warm shading is its CAPE, the cool shading the inhibition it has to break through.
HodographHodograph, Davenport, at 12:00Z on 2000-08-05The wind through the lowest 10 kilometers as a curve, rings every 10 meters per second labeled in knots. Zero to 1 km storm-relative helicity 148 square meters per square second, 0 to 6 km bulk shear 33 knots.193958Sfc1 km3 km6 km9 kmRMLM
The wind turning with height, colored by layer: ground to 1 km, 1 to 3 km, 3 to 6 km, 6 to 10 km. RM and LM are the right and left moving storms Bunkers' method gives; the shaded area is the 0 to 1 km storm-relative helicity.
Mixed-layer CAPE
0 J/kg
Mixed-layer CIN
-69256 J/kg
Surface CAPE
0 J/kg
Mixed-layer LCL
1330 m above ground
0-6 km bulk shear
33 kt
0-1 km bulk shear
13 kt
0-1 km storm-relative helicity
148 m²/s²
0-3 km storm-relative helicity
231 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.0
0-3 km lapse rate
3.5 K/km

Open this sounding in Storm Lab

Davenport, (KDVN), 00:00Z

3.3 hours after it, 160 km from the path. August 6, 2000.

Skew-T log-pSkew-T log-p diagram, Davenport, at 00:00Z on 2000-08-06Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 1252 joules per kilogram, CIN -143, lifted condensation level 758 meters above ground. Wind barbs in knots down the right edge.LCLLFCEL10008507005003002001001 km2 km3 km6 km9 km12 km15 km-30°-20°-10°10°20°30°40°
Temperature in red, dew point in green, the mixed-layer parcel dashed. The warm shading is its CAPE, the cool shading the inhibition it has to break through.
HodographHodograph, Davenport, at 00:00Z on 2000-08-06The wind through the lowest 10 kilometers as a curve, rings every 10 meters per second labeled in knots. Zero to 1 km storm-relative helicity 241 square meters per square second, 0 to 6 km bulk shear 51 knots.19395878Sfc1 km3 km6 km9 kmRMLM
The wind turning with height, colored by layer: ground to 1 km, 1 to 3 km, 3 to 6 km, 6 to 10 km. RM and LM are the right and left moving storms Bunkers' method gives; the shaded area is the 0 to 1 km storm-relative helicity.
Mixed-layer CAPE
1252 J/kg
Mixed-layer CIN
-143 J/kg
Surface CAPE
1143 J/kg
Mixed-layer LCL
758 m above ground
0-6 km bulk shear
51 kt
0-1 km bulk shear
27 kt
0-1 km storm-relative helicity
241 m²/s²
0-3 km storm-relative helicity
300 m²/s²
Significant tornado parameter
0.7
Supercell composite
7.2
0-3 km lapse rate
4.2 K/km

Open this sounding in Storm Lab

The surface observations

Monroe (EFT), 27 km from the path, in the two hours either side.

Time (UTC)Temp (°F)Dew point (°F)WindGust (kt)Pressure (mb)Weather
18:43 UTC66.262.6150° 8 kt161010.5-RA
18:56 UTC66.262.6140° 10 kt191009.8HZ
19:16 UTC66.262.6160° 9 kt171009.5HZ
19:36 UTC6862.6170° 12 kt221008.8
19:56 UTC6862.6180° 14 kt231008.1
20:16 UTC6862.6180° 14 kt201007.8
20:36 UTC6862.6320° 8 kt171010.5
20:59 UTC6862.60° 0 kt1009.8
21:16 UTC6862.6160° 3 kt1009.5
21:36 UTC69.864.4170° 3 kt1009.1HZ
21:56 UTC69.864.4180° 7 kt1008.8HZ
22:21 UTC69.864.4180° 6 kt1008.5HZ
22:36 UTC69.864.4180° 6 kt1008.5HZ

From the Iowa Environmental Mesonet's archive of airport observations.

This ground now

The live radar over the trackEvery 2000 tornado in WisconsinEvery tornado in Wisconsin since 1950Warnings in force in Wisconsin nowThe forecast where you are

The other tornadoes of August 5, 2000

1 more were confirmed in the United States that day.

DateTimeRatingWherePath (mi)Width (yd)DeathsInjuriesDamage
August 52:00 AM CDTF1Davison, SD0.2100$100,000

What this means

Ratings are the survey's, read off the damage rather than measured; the rating scale is above. Tornado counts rise through the record as reporting improved, so a year in the 1950s is not comparable with one today except for the strongest tornadoes, which were always noticed.

Sources

NOAA Storm Prediction Center tornado database, 1950-2025, the official record kept by NOAA's Storm Prediction Center.