Tornadoes · United States · Kansas · 2002

F0 tornado, Englewood, Kansas, August 12, 2002

This F0 tornado ran 0.2 miles across Clark County on August 12, 2002, touching down at 9:07 PM CDT and reaching 30 yards wide. 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
August 12, 2002
Touchdown
9:07 PM CDT (02:07 UTC)
Path length
0.2 miles (0.3 km)
Path width
30 yards (27 m)
Deaths
0
Injuries
0
County
Clark County
Touchdown point
37.030, -100.000
Lift-off point
37.030, -100.000
Record number
837

What the Weather Service recorded

A brief tornado lasted a little less than a minute but did not hit anything.

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

The warnings

20 minutes of warning. NWS DDC issued a tornado warning for this county at 01:47 UTC, 20 minutes before the tornado touched down, in force until 02:15 UTC.

Issued (UTC)ExpiredProductOffice
01:00 UTC02:00 UTCSevere Thunderstorm WarningDDC
01:47 UTC02:15 UTCTornado WarningDDC

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 Moderate Risk, with a 0.05 chance of a tornado within 25 miles. The outlook in force was issued at 01:07 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.

What forecasters said that day

The local office's own words before the tornado touched down, as it sent them, from the Iowa Environmental Mesonet's archive of National Weather Service text.

NWS Dodge City, KS wrote its last area forecast discussion before the tornado touched down at Aug 12, 2:40 PM CDT, 6 hours 27 minutes earlier.

Area forecast discussion, Aug 12, 2:40 PM CDT, 6 hours 27 minutes before
AREA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE DODGE CITY KS
240 PM CDT MON AUG 12 2002

DAYS 1-2...
U/A ANALYSIS TODAY STILL SHOWING A 90KT 2H JET ON THE WEST SIDE OF
OUR UPPER TROF NOW MOVING INTO SRN MT/NRN WY. SFC COLD FRONT AT 12Z
EXTENDED FROM SE CO INTO NW KS AND AS OF 18Z JUST BEGAN MOVING INTO
EXTREME WRN KS. MODELS ALREADY AT 18Z MOVING OUR SFC FRONT TOO FAST
TODAY AND BELIEVE UNTIL OUR WAVE COMES OUT LATER TONIGHT THE FRONT
WILL MAKE LITTLE PROGRESS E/SE. AHEAD OF THIS BOUNDARY IN SW KS DWPTS
ARE IN THE 60S AND 7-5H LAPSE RATES AS NOTED BY SPCDY1 AROUND 8 C/KM.
MODIFIED KDDC SOUNDING INDICATING CAPES AROUND 3000 J/KG IF TEMPS
WARM TO AROUND 90 TODAY HOWEVER THERE WAS ALSO A WARM MID LAYER WHICH
WILL HAVE TO BE OVERCOME. STILL WITH THIS IN MIND GIVEN MULTIPLE
BOUNDARIES IN OUR CWA, AND STRONG CONVERGENCE ALONG OUR COLD FRONT
(PER SWOMCD DISCUSSION) DO NOT SEE WHY SCATTERED CONVECTION WILL NOT
DEVELOP, AT LEAST ALONG OUR FRONT LATE THIS AFTERNOON AND EARLY THIS
EVENING. THIS SHOULD THEN BE FOLLOWED BY ANOTHER SHOT OF PCPN,
MAINLY AFTER MIDNIGHT AS OUR VORT LOBE ENTERS ERN CO AND THEN
CROSSES WESTERN KS EARLY TUESDAY MORNING. THIS WILL PUSH OUR COLD
FRONT SOUTH INTO OKLAHOMA WHICH WILL ALLOW THE COOLER AIR LOCATED IN
NEBRASKA TO INVADE THE AREA. THE CURRENT FORECAST HAS A GOOD HANDLE
WITH THIS EVENT AND SEE NO REASON TO LOWER POPS TONIGHT OR TUESDAY
GIVEN THE TIMING OF OUR VORT LOBE. WILL HOWEVER BUMP POPS UP
SLIGHTLY IN THE WEST FOR TUESDAY MORNING.

ALL MODELS CONTINUE TO AGREE WITH THIS WAVE EXITING WESTERN KS BY 18Z
TUESDAY WITH SKIES CLEARING FROM WEST TO EAST. HIGH PRESSURE WILL
THEN BUILD INTO WESTERN KS THROUGH TUESDAY NIGHT WHICH SHOULD
PROVIDE FOR A CLEAR NIGHT AND FAIRLY LIGHT WINDS. HAVING SAID THIS
TEMPS SHOULD FALL OFF INTO AT LEAST THE LOW TO MID 50S AS ADVERTISED
BY FWC/MAV IN MOST AREAS. THE NORTHWEST COULD EVEN SEE SOME UPPER
40S WHICH IS CURRENTLY COVERED BY CURRENT FORECAST. COOLEST DAYTIME
READINGS WILL BE ON TUESDAY AND HOW COOL TO GO WILL DEPEND ON HOW
MUCH SUN WE WILL/WILL NOT SEE. AT THIS TIME APPEARS THE WEST WILL
SEE THE MOST AND EAST THE LEAST SO HAVE OPTED TO STAY CLOSE TO
GUIDANCE IN THE WEST AND UNDERCUT GUIDANCE A FEW DEGREES IN THE EAST.

DAYS 3-7...
TODAYS DIAGNOSTIC DATA SHOWS NO CLEAR INDICATION OF AN MJO EITHER
MOIST OR DRY. CONSIDERABLE TROPICAL CONVECTION SHOWS ON DAILY
SATELLITE LOOPS WITH TWO REGIONS WHERE ROSSBY WAVE DISPERSION MAY BE
INFLUENCING THE CONVECTIVE MODES. THE FIRST IS THE PERSISTENT
CONVECTIVE COMPLEXES SEEN OVER THE INDIAN OCEAN, AND THE OTHER IS
THE RELATIVELY ACTIVE REGION ALONG THE EQUATOR FROM AROUND 140E TO
JUST EAST OF THE DATE LINE. THE WARM EPISODE EL NINO MAY BE
CONTRIBUTING TO THE LATTER. AVERAGE ANGULAR MOMENTUM ANOMALIES FOR
THE NORTHERN HEMISPHERE WESTERLIES IS NOW AT A RELATIVE MINIMUM BUT
APPEARS ABOUT TO INCREASE SO NO CLEAR SIGNAL IS PRESENT IN THESE
DATA EITHER. THE GENERAL CIRCULATION STATE OF THE NORTHERN
HEMISPHERE WESTERLIES CONTINUES TO BE A LOWER LATITUDE HYBRID WAVE 5
WITH THE UPPER LATITUDES OSCILLATING AROUND A WAVE ONE SOLUTION WITH
THE POLAR VORTEX.

FOR THE BULK OF THIS FORECAST CYCLE, THE MOST SIGNIFICANT FEATURE
APPEARS TO BE A DEVELOPING AREA OF UPPER LEVEL CROSS POLAR FLOW FROM
THE KARA SEA EASTWARD ALONG THE NORTH COAST OF SIBERIA INTO ALASKA.
WITH TIME, THE MODELS ARE MOSTLY IN AGREEMENT IN DEVELOPING A BROAD
CYCLONIC CIRCULATION ALOFT ENCOMPASSING MOST OF THE ARCTIC OCEAN,
CANADA, GREENLAND AND ICELAND. THE RESULT SHOULD BE A NUMBER OF COLD
AIR SURGES CROSSING THE POLAR REGION BEFORE DIVING SOUTH ALONG THE
WEST COAST OF CANADA INTO THE WESTERN CONUS. THIS BECOMES THE
DOMINATE NORTHERN HEMISPHERE CIRCULATION FEATURE AS IT CUTS OFF
MINOR UPPER CYCLONES OVER THE NORTH PACIFIC, WESTERN EUROPE AND THE
EASTERN ATLANTIC. MEANWHILE, THE UPPER LEVEL TROUGH OVER THE EASTERN
CONUS ON DAY 3 SHOULD RETROGRADE IN RESPONSE TO THESE IMPULSES SO
THAT BY THE WEEKEND WE SEE A MEAN WEST COAST UPPER TROUGH AND A
BUILDING UPPER RIDGE OVER THE CONUS.

THE ABOVE SCENARIO ARGUES FOR A SERIES OF UPPER LEVEL SHORT WAVE
TROUGHS ROTATING ACROSS THE NORTHERN CONUS DURING THIS FORECAST
PERIOD. THERE IS LITTLE AGREEMENT BETWEEN THE MODELS IN THE TIMING
OF EACH OF THESE FEATURES. EACH OF THESE WILL BRING A CANADIAN COLD
FRONT SOUTH INTO THE NORTHERN CONUS BUT THERE IS CONSIDERABLE
QUESTION WHETHER ANY OF THESE FRONTS COULD GET AS FAR SOUTH AS THE
FORECAST AREA. THE GOING FORECAST APPEARS TO HAVE PLAYED ONE OF
THESE FRONTS INTO THE FORECAST AREA ON SATURDAY. WHILE THERE IS
SERIOUS DOUBT OF THIS OCCURRING AT THIS TIME PER THE MODELS, IT ALSO
CANNOT BE RULED OUT DUE TO THE ABOVE REASONING AND WILL CONTINUE
THIS TREND RATHER THAN MAKING CHANGES BASED UPON WHAT MAY LARGELY BE
MODEL NOISE.

AS THE UPPER TROUGH BECOMES ANCHORED OVER THE WESTERN CONUS THIS
WEEKEND WITH COOLER CANADIAN AIR DIGGING INTO IT FROM THE CROSS
POLAR FLOW, THE SOUTHEASTERN CONUS UPPER RIDGE SHOULD BUILD BACK
INTO THE PLAINS. THIS WILL PROVIDE ABOVE NORMAL TEMPERATURES AND
BELOW NORMAL PRECIPITATION FOR MONDAY AND THE OUTLOOK PERIODS. THIS
IS ALSO CONSISTENT WITH THE GOING FORECAST.

PRELIMINARY GUIDANCE FOR COORDINATION ONLY. OFFICIAL FORECASTS ARE
CONTAINED WITHIN THE DODGE CITY ZONE FORECAST.

DDC   57  74  52  86 /  60  30   0   0
GCK   55  77  50  86 /  60  20   0   0
EHA   54  75  51  85 /  60  20   0   0
LBL   57  73  52  86 /  70  40   0   0
HYS   55  76  50  86 /  50  20   0   0
P28   63  71  56  86 /  70  60   0   0

.DDC...NONE.

FCSTID =BURGERT/JOHNSON

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.

Dodge City, (KDDC), 00:00Z

2.1 hours before the tornado, 83 km from the path. August 13, 2002.

Skew-T log-pSkew-T log-p diagram, Dodge City, at 00:00Z on 2002-08-13Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 2080 joules per kilogram, CIN -70, lifted condensation level 1516 meters above ground. Wind barbs in knots down the right edge.LCLLFCEL10008507005003002001001 km2 km3 km6 km9 km-30°-20°-10°0°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, Dodge City, at 00:00Z on 2002-08-13The 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 158 square meters per square second, 0 to 6 km bulk shear 46 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
2080 J/kg
Mixed-layer CIN
-70 J/kg
Surface CAPE
3532 J/kg
Mixed-layer LCL
1516 m above ground
0-6 km bulk shear
46 kt
0-1 km bulk shear
28 kt
0-1 km storm-relative helicity
158 m²/s²
0-3 km storm-relative helicity
339 m²/s²
Significant tornado parameter
1.3
Supercell composite
23.8
0-3 km lapse rate
7.0 K/km

Open this sounding in Storm Lab

Dodge City, (KDDC), 12:00Z

9.9 hours after it, 83 km from the path. August 13, 2002.

Skew-T log-pSkew-T log-p diagram, Dodge City, at 12:00Z on 2002-08-13Temperature 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 -70233, lifted condensation level 1269 meters above ground. Wind barbs in knots down the right edge.LCL10008507005003002001001 km2 km3 km6 km9 km12 km15 km-30°-20°-10°0°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, Dodge City, at 12:00Z on 2002-08-13The 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 -239 square meters per square second, 0 to 6 km bulk shear 56 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
0 J/kg
Mixed-layer CIN
-70233 J/kg
Surface CAPE
4 J/kg
Mixed-layer LCL
1269 m above ground
0-6 km bulk shear
56 kt
0-1 km bulk shear
24 kt
0-1 km storm-relative helicity
-239 m²/s²
0-3 km storm-relative helicity
-18 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.4
0-3 km lapse rate
2.7 K/km

Open this sounding in Storm Lab

The surface observations

West Woodward (WWR), 78 km from the path, in the two hours either side.

Time (UTC)Temp (°F)Dew point (°F)WindGust (kt)Pressure (mb)Weather
00:09 UTC93.260.8170° 20 kt251009.5
00:29 UTC91.460.8160° 16 kt231009.1
00:53 UTC89.660.8160° 16 kt201008.8
01:10 UTC89.659150° 13 kt201009.1
01:31 UTC89.659160° 14 kt201009.1
01:49 UTC87.859150° 13 kt181009.1
02:09 UTC87.859160° 13 kt191009.8
02:29 UTC87.859150° 13 kt1009.8
02:51 UTC87.859150° 11 kt161010.5
03:09 UTC87.860.8140° 10 kt171010.8VCTS
03:28 UTC87.860.8150° 11 kt151011.5TS
03:50 UTC87.862.6180° 8 kt141012.2VCTS

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

This ground now

The live radar over the trackEvery 2002 tornado in KansasEvery tornado in Kansas since 1950Warnings in force in Kansas nowThe forecast where you are

The other tornadoes of August 12, 2002

4 more were confirmed in the United States that day.

DateTimeRatingWherePath (mi)Width (yd)DeathsInjuriesDamage
August 127:36 PM CDTF0Clark, KS0.130
August 127:52 PM CDTF0Meade, KS0.330
August 1210:20 PM CDTF0Douglas, MO0.1100
August 1210:35 PM CDTF1Ozark, MO8.0200$50,000

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.