Tornadoes · United States · Kansas · 2002

F0 tornado, Jetmore, Kansas, August 26, 2002

This F0 tornado ran 0.2 miles across Hodgeman County on August 26, 2002, touching down at 9:05 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 26, 2002
Touchdown
9:05 PM CDT (02:05 UTC)
Path length
0.2 miles (0.3 km)
Path width
30 yards (27 m)
Deaths
0
Injuries
0
County
Hodgeman County
Touchdown point
37.900, -100.130
Lift-off point
37.900, -100.130
Record number
282

What the Weather Service recorded

This brief tornado was filmed by the spotter, but it did not last long and did not hit anything.

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
02:54 UTC03:45 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, with a 0.02 chance of a tornado within 25 miles. The outlook in force was issued at 01:12 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 26, 3:18 PM CDT, 5 hours 47 minutes earlier.

Area forecast discussion, Aug 26, 3:18 PM CDT, 5 hours 47 minutes before
AREA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE DODGE CITY KS
318 PM CDT MON AUG 26 2002

DAYS 1-2...

SEVERAL FEATURES TO INFLUENCE THIS FORECAST PACKAGE.  FOR THE
IMMEDIATE FUTURE, OUTFLOW BOUNDARY SAGGING SOUTHWEST FROM EARLY
MORNING MCS IN CENTRAL NEBRASKA HAS PUSHED INTO THE FAR NORTHERN
CWA.  NEW TSRA DEVELOPMENT MAY FIRE SOUTH FROM SOUTHWEST NEBRASKA
ALONG THIS OUTFLOW BOUNDARY THROUGH EARLY EVENING.  ELSEWHERE,
ATMOSPHERE HAS BECOME INCREASINGLY UNSTABLE AS SFC TEMPS HAVE WARMED
WELL INTO THE 80S TO AROUND 90 AND SURFACE DEW POINTS HAVE REMAINED
IN THE 60S.  MORNING U/A ANALYSIS INDICATING AND WATER VAPOR IMAGERY
SHOWING SIGNIFICANT DIFLUENT FLOW ACROSS THE WESTERN HIGH PLAINS IN
THE MID/UPPER LEVELS WITH 90 KT SOUTHERN BRANCH JET NOSING INTO THE
CENTRAL ROCKIES.

THINK THAT 30KM MM5, 12Z RUN, HAD THE BEST SOLUTION IN FORMING
RATHER STOUT MCS IN NORTHEAST COLORADO, SOUTHWEST NEBRASKA AND
NORTHWEST KANSAS, AND DROPPING THIS FEATURE SOUTH/SOUTHEAST ALONG
THE MID LEVEL BAROCLINIC ZONE.  THUS, WILL BASE POPS HIGHLY ON THIS
SOLUTION WITH LIKELY NORTH AND NORTHWEST TO SLIGHT CHANCE SOUTHEAST
CWA.

ON TUESDAY THE ATMOSPHERE WILL LIKELY BE IN RECOVERY MODE FROM
OVERNIGHT CONVECTION WITH ANOTHER ROUND POSSIBLE TOMORROW NIGHT AS
ANOTHER S/WV TROUGH APPROACHES IN THE SOUTHERN BRANCH OF THE
WESTERLIES AND THE SURFACE BOUNDARY STRENGTHENS WITH DAYTIME HEATING.

DAYS 3-7...

MID TO LATTER PART OF THIS WEEK STILL LOOKING FAIRLY ACTIVE WITH THE
SOUTHERN BRANCH OF THE WESTERLIES CONTINUING FOR A FEW MORE DAYS.
CLOSED LOW FORECAST TO ESTABLISH ITSELF OVER THE NORTHERN ROCKIES ON
TUESDAY IS FORECAST TO OPEN UP AND LIFT OUT INTO THE NORTHERN PLAINS
BY FRIDAY AFTER WHICH AN UPPER LEVEL RIDGE OF HIGH PRESSURE BUILDS
NORTHEAST INTO THE CENTRAL PLAINS.  UNTIL THAT TIME, THE LOW LEVEL
BAROCLINIC ZONE WILL LIKELY STAY IN PLACE WHERE IT HAS BEEN ACROSS
THE CENTRAL PLAINS.  WITH THIS IN MIND, WILL CONTINUE TO HOLD ON TO
THE LATE AFTERNOON AND NIGHTTIME THUNDERSTORM FORECAST.  THE WEATHER
SHOULD QUIET DOWN A BIT FOR THE PERIOD FROM SATURDAY THROUGH MOST OF
MONDAY AS THE UPPER LEVEL RIDGE DOMINATES THE WEATHER FOR A FEW
DAYS.  EARLY NEXT WEEK, THE MAIN BELT OF UPPER LEVEL WESTERLY FLOW
SAGS BACK DOWN ACROSS THE U.S./CANADIAN BORDER WITH A COUPLE OF
SHORTWAVE TROUGHS MOVING EAST ACROSS THE NORTHERN U.S. EARLY NEXT
WEEK.  THINK THAT THE NEXT CHANCE FOR THUNDERSTORMS WOULD BE AROUND
MONDAY NIGHT ALONG A SURFACE BOUNDARY THAT SHOULD GET PUSHED SOUTH
INTO THE CENTRAL HIGH PLAINS.  WILL KEEP THE 8-10 DAY OUTLOOK THE
SAME WITH NEAR NORMAL ON BOTH THE TEMPS AND PRECIP.

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

DDC   65  82  64  85 /  40  20  30  20
GCK   65  83  64  87 /  40  20  40  20
EHA   66  84  65  88 /  40  30  40  20
LBL   65  83  64  87 /  40  20  40  20
HYS   65  82  64  85 /  60  10  30  20
P28   67  82  66  86 /  20   0  20  20

.DDC...NONE.

FCSTID = 07/02

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, 25 km from the path. August 27, 2002.

Skew-T log-pSkew-T log-p diagram, Dodge City, at 00:00Z on 2002-08-27Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 882 joules per kilogram, CIN -128, lifted condensation level 1721 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 2002-08-27The 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 15 square meters per square second, 0 to 6 km bulk shear 42 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
882 J/kg
Mixed-layer CIN
-128 J/kg
Surface CAPE
3488 J/kg
Mixed-layer LCL
1721 m above ground
0-6 km bulk shear
42 kt
0-1 km bulk shear
7 kt
0-1 km storm-relative helicity
15 m²/s²
0-3 km storm-relative helicity
204 m²/s²
Significant tornado parameter
0.1
Supercell composite
13.2
0-3 km lapse rate
6.9 K/km

Open this sounding in Storm Lab

Dodge City, (KDDC), 12:00Z

9.9 hours after it, 25 km from the path. August 27, 2002.

Skew-T log-pSkew-T log-p diagram, Dodge City, at 12:00Z on 2002-08-27Temperature and dew point through the depth of the atmosphere, with the mixed-layer parcel lifted from the surface. Mixed-layer CAPE 29 joules per kilogram, CIN -673, lifted condensation level 1762 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 2002-08-27The 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 97 square meters per square second, 0 to 6 km bulk shear 48 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
29 J/kg
Mixed-layer CIN
-673 J/kg
Surface CAPE
0 J/kg
Mixed-layer LCL
1762 m above ground
0-6 km bulk shear
48 kt
0-1 km bulk shear
16 kt
0-1 km storm-relative helicity
97 m²/s²
0-3 km storm-relative helicity
138 m²/s²
Significant tornado parameter
0.0
Supercell composite
0.0
0-3 km lapse rate
3.7 K/km

Open this sounding in Storm Lab

The surface observations

Dodge City (DDC), 21 km from the path, in the two hours either side.

Time (UTC)Temp (°F)Dew point (°F)WindGust (kt)Pressure (mb)Weather
00:56 UTC7764110° 15 kt1015.2
01:56 UTC7664110° 17 kt1015.6
02:12 UTC75.264.4120° 17 kt231015.9TS
02:56 UTC7365340° 17 kt251020-TSRA
03:04 UTC64.462.6340° 40 kt581020.3+TSRA BR SQ
03:08 UTC62.660.8330° 37 kt631020.3-TSRA BR SQ
03:26 UTC62.660.830° 22 kt401022+TSRA BR
03:36 UTC62.660.860° 16 kt1021TSRA BR
03:43 UTC62.660.890° 16 kt1020.7-TSRA
03:56 UTC6461100° 18 kt1019.3-TSRA

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

The radar

The Dodge City radar (KDDC), 21 km away, was scanning. The volume nearest the touchdown began at 02:07 UTC.

Open the radar archive at this moment, over the track

Reflectivity and velocity, decoded from the Level II archive in the browser. Volumes take a few seconds to open the first time.

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 26, 2002

9 more were confirmed in the United States that day.

DateTimeRatingWherePath (mi)Width (yd)DeathsInjuriesDamage
August 269:05 AM EDTF0Dare, NC0.150$10,000
August 262:05 PM MDTF0Dundy, NE0.325
August 263:08 PM CDTF0Hancock, IA0.120
August 264:00 PM CDTF0Polk, MN3.025
August 263:10 PM MDTF0Sheridan, NE0.510$1,000
August 264:35 PM CDTF0Cheyenne, KS0.325
August 265:00 PM CDTF0Red Lake, MN0.225
August 265:15 PM CDTF0Polk, MN1.025
August 268:15 PM CDTF0Becker, MN0.225

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.