Tornadoes · United States · Kansas · 2002

F1 tornado, Dodge City, Kansas, August 11, 2002

This F1 tornado ran 6.5 miles across Ford County on August 11, 2002, touching down at 10:44 PM CDT and reaching 50 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 mph

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

  2. F173 to 112 mphthis tornado

    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
F1
Date
August 11, 2002
Touchdown
10:44 PM CDT (03:44 UTC)
Path length
6.5 miles (10.5 km)
Path width
50 yards (46 m)
Deaths
0
Injuries
0
County
Ford County
Touchdown point
37.800, -100.020
Lift-off point
37.780, -99.920
Record number
834

What the Weather Service recorded

This tornado became wrapped in rain and hit three homes causing significant roof damage. On one house, parts of the roof blew through an adjacent garage causing heavy damage.

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
03:47 UTC04:30 UTCSevere Thunderstorm WarningDDC
04:33 UTC05:15 UTCSevere Thunderstorm WarningDDC
05:13 UTC05:45 UTCSevere Thunderstorm WarningDDC
05:50 UTC08:45 UTCFlash Flood WarningDDC
05:53 UTC08:45 UTCFlash Flood WarningDDC
06:10 UTC07:00 UTCSevere Thunderstorm 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 Slight Risk. The outlook in force was issued at 00:47 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 11, 2:45 PM CDT, 7 hours 59 minutes earlier.

Area forecast discussion, Aug 11, 2:45 PM CDT, 7 hours 59 minutes before
AREA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE DODGE CITY KS
245 PM CDT SUN AUG 11 2002

MAIN FORECAST CHALLENGE IS HOW MUCH OF A COOL DOWN WILL BE FELT
ACROSS SOUTHWEST KS BY TUESDAY.

DAYS 1-2...
KGLD RADAR AND SAT LOOP EARLIER TODAY SHOWING AN OUTFLOW BOUNDARY
MOVING INTO OUR NORTHERN CWA. LEE TROF/DEVELOPING DRY LINE EXTENDED
SOUTH ACROSS ERN COLORADO. BEST MOISTURE AND WEAKEST CAP HOWEVER WAS
PLACE OVER OUR EASTERN CWA WHICH IS WHERE BEST AFTERNOON CU HAVE
BEEN DEVELOPING THIS AFTERNOON AS CONVECTIVE TEMPERATURE BEGINS TO
GET EXCEEDED. MODELS CONTINUE TO PROG A WEAK VORT LOBE TO CROSS
WESTERN KS LATER THIS EVENING SO WITH COOLER 7H TEMPS AND BETTER
MOISTURE PRESENT IN OUR EAST CAN NOT RULE OUT SOME CONVECTION
DEVELOPING HERE. ALSO HARD TO IGNORE OUR BOUNDARIES TO OUR WEST AND
NORTH, ESPECIALLY OUR NORTH. CURRENT FORECAST ALREADY HAS SMALL POPS
GOING IN THE EAST AND WILL KEEP THIS GOING BUT WILL ALSO NOW MENTION
SMALL POPS IN THE WEST.

MAJOR CHANGES BEGIN TO SHAPE ON MONDAY AS OUR COLD FRONT ENTERS NW
KS BY 12Z MON AND OUR NEXT MAJOR UPPER WAVE DROPS SOUTH INTO WY.
AVN/ETA/NGM STILL PLACES FROPAS AT GCK, HYS AND EHA AROUND 18Z, DDC
AROUND 21Z AND P28 AROUND 00Z. WILL THEREFORE CONTINUE TO FOLLOW
THIS TIMING. MODELS ALSO SHOWING BETTER MOIST CONV DEVELOP DURING
THE AFTERNOON AS OUR FRONT MOVES SOUTH/SOUTHEAST OF DDC WITH LIS
DECREASING TO -4 TO -6C/KM. ALTHOUGH COULD STILL SEE SOME CONVECTION
EARLIER IN THE DAY WITH THIS FRONT AS IT CROSSES THE CWA, IT APPEARS
THE BETTER DYNAMICS WILL BE LOCATED IN OUR S/SE CWA IN THE
AFTERNOON. WILL THEREFORE PLACE HIGH CHC POPS IN THE SE AND ONLY SLT
CHC POPS IN THE NW.

BY MONDAY NIGHT OUR WY (THE MORE SIG VORT LOBE) WILL DROP SOUTH INTO
EAST CENTRAL CO BY 12Z TUE. RIGHT ENTRANCE REGION OF 25H JET ALSO
WILL BE PLACED NEAR WESTERN KS BY 12Z TUES. WITH LIFT PRESENT AND
MOISTURE POOLING BEHIND OF COLD FRONT WILL THEREFORE GO WITH HIGH
CHC/LIKELY POPS LATE MONDAY NIGHT ACROSS ALL THE CWA. WILL ALSO
CONTINUE HIGH CHC/LIKELY POPS INTO TUESDAY AS THIS WAVE MOVES EAST
ACROSS THE STATE ON TUESDAY. CLOUDS, PCPN AND CURRENT OBS IN SRN
CANADA IN THIS AIR MASS LOOKS AS IF TEMPS WILL REMAIN WELL BELOW
NORMAL ON TUESDAY. THE 12Z FWC/MAV NOT LOOKING TO BAD ON FORECAST
HIGHS. GUIDANCE MAY EVEN BE A BIT TOO WARM IN THE SOUTH WHERE PCPN
AND CLOUDS MORE LIKELY TO HOLD ON ALL DAY. WILL THEREFORE FOLLOW THE
GUIDANCE TREND BUT WILL TRIM A FEW MORE DEGREES OFF ACROSS THE
SOUTH. WILL TAPER OFF PCPN AND EVEN TRY TO BRING A CLEARING TREND
BEHIND OUR S/W TROF WHICH WILL BE CROSSING THE CWA EARLY IN THE DAY.

THANKS FOR THE CORD...ICT, OUN.

DAYS 3-7...

SIGNIFICANT REGIME TRANSITION, ESPECIALLY ACROSS THE EAST ASIAN/
PACIFIC/NORTH AMERICAN SECTOR, IS WELL UNDERWAY AT THIS TIME.  THIS
CHANGE MAY BE LINKED TO THE RELATIVELY PERSISTENT (ABOUT 2-3 WEEKS)
AND VERY LARGE AREA OF DEEP MOIST TROPICAL CONVECTION FROM ROUGHLY
160 DEG W TO 60 DEG E, FROM ABOUT 10 DEG SOUTH OF THE EQUATOR TO
ROUGHLY 25 DEG N.

THIS AREA OF THUNDERSTORMS IS GENERALLY BEING FORCED BY
ANOMALOUSLY WARM SEA SURFACE TEMPERATURES, ESPECIALLY FOR THOSE
AROUND THE DATELINE, AND ALSO THE INDIAN MONSOON SYSTEM.  THERE IS
NOT MUCH EVIDENCE (YET) OF A MADDEN-JULIAN OSCILLATION (MJO).
FOR SOME ADDITIONAL DETAIL ABOUT THE PLANETARY-SCALE CIRCULATION,
PLEASE REFER TO THE FORECAST REASONING SECTION OF
HTTP://WWW.CRH.NOAA.GOV/DDC/WEEK2HTML.

THIS TRANSITION IS LEADING TO THE ESTABLISHMENT OF ROUGHLY A
MIDDLE/UPPER TROPOSPHERIC DATELINE TROUGH/140 DEG W RIDGE/100 DEG W
TROUGH, NORTH OF ABOUT 30 DEG.  IN ADDITION, THE EXTRATROPICAL
WESTERLIES ARE MIGRATING SOUTHWARD INTO THE LOWER 48 STATES, AT
LEAST FOR THIS UPCOMING WEEK.  UNDERSTANDING THE SUMMER BASE STATE,
THE ABOVE MENTIONED WAVE TRAIN CAN BE VIEWED AS A VERSION OF THE
PACIFIC/NORTH AMERICAN TELECONNECTION (WEAKLY NEGATIVE PHASE).  THIS
SITUATION WILL ALLOW PERHAPS SEVERAL SYNOPTIC-SCALE COLD FRONTS TO
MIGRATE ACROSS THE PLAINS DURING MY FORECAST PERIOD.  OF COURSE,
TIMING WILL BE DIFFICULT, AS WELL AS POSITIONING.

A FINAL POINT TO MAKE IS THAT THIS REGIME WILL BE SLOWLY
RETROGRESSIVE, SUCH THAT ABOUT A WEEK FROM NOW THE MID/UPPER
TROPOSPHERIC TROUGH AXIS INITIALLY AROUND 100 DEG W SHOULD BE ALONG
THE WEST COAST OF NORTH AMERICA, WITH HEIGHT RISES FIRST OVER THE
SOUTHEAST US, AND THEN EVENTUALLY THE CENTRAL PLAINS (AGAIN -- WHAT
HAS BEEN OBSERVED MUCH OF THIS SUMMER).

ALL OF THE OPERATIONAL GLOBAL NWP ARE CONVERGING TO THIS SCENARIO,
AFTER A PERIOD OF LOW SKILL.  THE LATTER IS OFTEN THE CASE DURING A
REGIME TRANSITION.  UNDERSTANDING THEIR BIASES, ETC., I HAVE NO REAL
NWP PREFERENCE.  HOWEVER, I THINK THE DETERMINISTIC ECMWF FROM 1200
UTC 10 AUGUST INITIAL CONDITIONS AND THE 1200 UTC 11 AUGUST AVN ARE
THE CLOSEST TO THE REAL ATMOSPHERE.

GOING EXTENDED FORECAST IS REASONABLE.  ONE OF THE SOURCE REGIONS OF
THE UPCOMING COOL AIR INTRUSION, WHICH AFFECTS MY CWA DAYS 1 AND 2,
IS COMING FROM THE ARCTIC LATITUDES OF NORTHWESTERN CANADA.  THUS I
WILL LIKELY LOWER MINIMUM TEMPERATURES INTO THE 50S FOR WEDNESDAY
MORNING (SHOULD NOT BE ANY RECORD LOWS), AND CORRESPONDINGLY LOWER
THE MAX TEMPERATURES FOR THAT DAY.  I WILL LEAVE IN THE MENTION OF
THUNDERSTORMS FOR THE OVERNIGHT HOURS OF WEDNESDAY INTO THURSDAY.
TEMPERATURES SHOULD WARM TO AT LEAST NORMAL FROM THURSDAY ONWARD.
FINALLY, ALL FACTORS CONSIDERED, I WILL INTRODUCE ANOTHER
OPPORTUNITY OF THUNDERSTORMS FOR MY CWA ON DAY 6.  OUR LOCAL 8-10
DAY (8/19-21) FORECAST WILL READ ABOVE NORMAL TEMPERATURES AND BELOW
NORMAL PRECIPITATION (BACK TO THE RIDGE).

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

DDC   67  82  58  72 /  30  20  50  30
GCK   65  80  58  72 /  30  20  50  40
EHA   65  81  58  70 /  20  30  70  70
LBL   67  86  61  69 /  20  50  70  70
HYS   68  83  58  71 /  30  30  50  30
P28   70  90  63  69 /  20  50  70  70

.DDC...NONE.

FCSTID =18/23

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

3.7 hours before the tornado, 7 km from the path. August 12, 2002.

Skew-T log-pSkew-T log-p diagram, Dodge City, at 00:00Z on 2002-08-12Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 2276 joules per kilogram, CIN -26, lifted condensation level 2144 meters above ground. Wind barbs in knots down the right edge.LCLLFCEL10008507005003002001001 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 00:00Z on 2002-08-12The 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 -5 square meters per square second, 0 to 6 km bulk shear 30 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
2276 J/kg
Mixed-layer CIN
-26 J/kg
Surface CAPE
3413 J/kg
Mixed-layer LCL
2144 m above ground
0-6 km bulk shear
30 kt
0-1 km bulk shear
10 kt
0-1 km storm-relative helicity
-5 m²/s²
0-3 km storm-relative helicity
140 m²/s²
Significant tornado parameter
0.0
Supercell composite
8.6
0-3 km lapse rate
8.2 K/km

Open this sounding in Storm Lab

Dodge City, (KDDC), 12:00Z

8.3 hours after it, 7 km from the path. August 12, 2002.

Skew-T log-pSkew-T log-p diagram, Dodge City, at 12:00Z on 2002-08-12Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 770 joules per kilogram, CIN -469, lifted condensation level 1255 meters above ground. Wind barbs in knots down the right edge.LCLLFCEL10008507005003002001001 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 2002-08-12The 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 504 square meters per square second, 0 to 6 km bulk shear 45 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
770 J/kg
Mixed-layer CIN
-469 J/kg
Surface CAPE
373 J/kg
Mixed-layer LCL
1255 m above ground
0-6 km bulk shear
45 kt
0-1 km bulk shear
33 kt
0-1 km storm-relative helicity
504 m²/s²
0-3 km storm-relative helicity
619 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.3
0-3 km lapse rate
3.9 K/km

Open this sounding in Storm Lab

The surface observations

Dodge City (DDC), 3 km from the path, in the two hours either side.

Time (UTC)Temp (°F)Dew point (°F)WindGust (kt)Pressure (mb)Weather
01:56 UTC8663170° 12 kt1010.8
02:56 UTC8462150° 11 kt1010.8
03:47 UTC73.466.2340° 32 kt461014.6HZ SQ
03:56 UTC5959340° 43 kt651012.9-RA BR
04:03 UTC60.860.8360° 34 kt571013.2FG
04:08 UTC62.662.620° 19 kt501014.2BR
04:11 UTC62.662.610° 15 kt421014.2+RA BR
04:14 UTC66.262.630° 21 kt421014.2TSRA BR
04:31 UTC66.262.6240° 16 kt271016.3+TSRA
04:35 UTC66.262.6170° 20 kt271013.5+TSRA BR
04:43 UTC64.460.8 6 kt1015.2+TSRA BR
04:56 UTC6361 3 kt1015.6+RA BR
05:09 UTC64.462.60° 0 kt1016.3+TSRA

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 11, 2002

7 more were confirmed in the United States that day.

DateTimeRatingWherePath (mi)Width (yd)DeathsInjuriesDamage
August 114:00 PM CDTF4Stutsman, ND1.0300$650,000
August 118:05 PM CDTF0Mahnomen, MN0.225$10,000
August 118:20 PM CDTF0Logan, KS0.125
August 118:40 PM CDTF0Red Willow, NE0.125
August 118:45 PM CDTF0Clearwater, MN0.225
August 118:55 PM CDTF0Clearwater, MN0.225
August 1111:00 PM CDTF1Hodgeman, KS0.250

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.