Tornadoes · United States · Iowa · 1999

F0 tornado, Goldfield, Iowa, June 8, 1999

This F0 tornado ran 0.2 miles across Wright County on June 8, 1999, touching down at 6:09 PM CDT. It killed nobody.

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
June 8, 1999
Touchdown
6:09 PM CDT (23:09 UTC)
Path length
0.2 miles (0.3 km)
Path width
0 yards (0 m)
Deaths
0
Injuries
0
County
Wright County
Touchdown point
42.850, -93.920
Lift-off point
42.850, -93.920
Record number
992

What the Weather Service recorded

A strong upper level disturbance moved north-northeast into Iowa during the afternoon hours. A very unstable airmass was in place over the state with lifted indices near -10 degrees C. Surface dew points were in the low 70s as high temperatures soared into the upper 80s and 90s. This combined to produce CAPE values near 5000 J/kg. Thunderstorms erupted initially developed in more or less an east to west line. That line lifted north and as it did produced very heavy rain and some hail of three quarters of an inch to an inch in diameter. A second line formed in a more north to south orientation and moved east across the state. There were also some reports of dime size or larger hail from that line as well. Serious crop damage occurred in Hancock County southeast of Kanawha due to the hail. Crops needed to be replanted in the area. The main problem was with the intersection of the two lines. At the intersection of the two outflow boundaries from the lines a few brief tornadoes occurred. These were more like spin up tornadoes and were very short lived, causing no significant damage. One was in Wright County north of Goldfield, another Humboldt County southwest of Renwick, with yet another in Hancock County southeast of the Kanawha area. As the storms moved through the Lake Mills area in Winnebago County, high winds downed trees and caused vehicle damage. As the evening progressed, the upper level vorticity maximum was evident in the radar signature. The comma head of the precipitation passes over Black Hawk and Grundy Counties. Reports southeast of Waterloo indicated 3.76 inches of rainfall in a 90 minute period. Meanwhile, the area between Reinbeck and Wellsburg received in excess of 5 inches of rain in a 3 hour period. Normally, this amount of rain would not be all that serious, however soil conditions in that part of the state were very saturated resulting in significant runoff. Flash flooding occurred in the two counties. Numerous gravel roads were washed out over the northwest part of Butler County with widespread flooding reported between Reinbeck and Wellsburg.

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

The warnings

5 minutes of warning. NWS DMX issued a tornado warning for this county at 23:04 UTC, 5 minutes before the tornado touched down, in force until 23:35 UTC.

Issued (UTC)ExpiredProductOffice
23:04 UTC23:35 UTCTornado WarningDMX
23:28 UTC00:00 UTCSevere Thunderstorm WarningDMX

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 Slight Risk. The outlook in force was issued at 19:46 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.

Minneapolis, MN (KMPX), 12:00Z

11.2 hours before the tornado, 224 km from the path. June 8, 1999.

Skew-T log-pSkew-T log-p diagram, Minneapolis, MN at 12:00Z on 1999-06-08Temperature 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 -431, lifted condensation level 1727 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, Minneapolis, MN at 12:00Z on 1999-06-08The 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 -160 square meters per square second, 0 to 6 km bulk shear 47 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
-431 J/kg
Surface CAPE
147 J/kg
Mixed-layer LCL
1727 m above ground
0-6 km bulk shear
47 kt
0-1 km bulk shear
36 kt
0-1 km storm-relative helicity
-160 m²/s²
0-3 km storm-relative helicity
-132 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.0
0-3 km lapse rate
4.9 K/km

Open this sounding in Storm Lab

Minneapolis, MN (KMPX), 00:00Z

0.8 hours after it, 224 km from the path. June 9, 1999.

Skew-T log-pSkew-T log-p diagram, Minneapolis, MN at 00:00Z on 1999-06-09Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 1002 joules per kilogram, CIN -159, lifted condensation level 1650 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, Minneapolis, MN at 00:00Z on 1999-06-09The 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 245 square meters per square second, 0 to 6 km bulk shear 22 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
1002 J/kg
Mixed-layer CIN
-159 J/kg
Surface CAPE
756 J/kg
Mixed-layer LCL
1650 m above ground
0-6 km bulk shear
22 kt
0-1 km bulk shear
33 kt
0-1 km storm-relative helicity
245 m²/s²
0-3 km storm-relative helicity
309 m²/s²
Significant tornado parameter
0.0
Supercell composite
1.4
0-3 km lapse rate
6.5 K/km

Open this sounding in Storm Lab

The surface observations

Clarion (CAV), 18 km from the path, in the two hours either side.

Time (UTC)Temp (°F)Dew point (°F)WindGust (kt)Pressure (mb)Weather
21:25 UTC91.459180° 18 kt211011.5
21:45 UTC8666.2170° 14 kt181011.5
22:05 UTC91.468170° 15 kt181011.2
22:25 UTC87.871.6140° 14 kt171011.5
22:45 UTC8669.8120° 13 kt171011.2
23:05 UTC75.268190° 18 kt231011.9
23:25 UTC69.866.210° 8 kt1013.5
23:45 UTC6864.410° 15 kt331013.5
00:05 UTC71.666.230° 12 kt1012.9
00:25 UTC73.464.490° 19 kt271011.5
00:45 UTC73.466.2120° 17 kt231011.5
01:05 UTC71.664.4120° 14 kt231011.5

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

This ground now

The live radar over the trackEvery 1999 tornado in IowaEvery tornado in Iowa since 1950Warnings in force in Iowa nowThe forecast where you are

The other tornadoes of June 8, 1999

6 more were confirmed in the United States that day.

DateTimeRatingWherePath (mi)Width (yd)DeathsInjuriesDamage
June 812:15 PM CDTF0Harris, TX0.550$30,000
June 85:59 PM CDTF0Humboldt, IA0.10
June 86:15 PM CDTF0Hancock, IA0.20
June 86:55 PM CDTF0Mountrail, ND0.510
June 87:45 PM CDTF0Renville, ND0.510
June 86:50 PM MDTF0Corson, SD2.020

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.