Trousdale, KS EF3 Wedge Tornado of May 4, 2007

The Forecast

**Figure 1.** Storm Prediction Center’s (SPC) 1630Z Day 1 convective outlook on May 4, 2007. Top left panel showing moderate risk of severe thunderstorms, top right panel showing tornado probability, bottom left panel showing damaging wind probability and bottom right panel showing large hail probability (SPC, 2007).

Figure 1 depicts the Storm Prediction Center’s (SPC) day 1 convective outlook, showing a moderate risk of severe thunderstorms with a 15% hatched probability of tornadoes on May 4, 2007. Figure 2 depicts a close-up of the tornado probability at 1630Z. In Figure 2, we see a a 15% hatched probability from southwestern Kansas into extreme eastern Colorado.

**Figure 2.** SPC Day 1 tornado probability issued at 1626Z on May 4, 2007. Graphic depicts probability of tornado within 25 miles of a point within the outlined area. Hatched area depicts 10% or greater probability of EF2-EF5 tornadoes within 25 miles of any given point within hatched area (SPC, 2007).

The synoptic pattern on the morning of May 4th was typical of spring in the southern Plains of the United States. Figure 3 depicts an upper-level trough ejecting in the Pacific Northwest. According to the SPC (2007) at 1651Z:

“A POWERFUL UPPER TROUGH IS DEVELOPING OVER THE INTERIOR PORTIONS OF THE WESTERN U.S. THIS SYSTEM IS FORECAST TO MOVE EASTWARD AND BEGIN AFFECTING THE CENTRAL AND NORTHERN PLAINS BY THIS AFTERNOON AND EVENING. STRONG WESTERLY WINDS ALOFT WILL SPREAD ACROSS THE SOUTHERN ROCKIES TODAY…WHILE A SURFACE LOW DEEPENS VICINITY OF THE SOUTHEAST COLORADO/SOUTHWESTERN KANSAS AREA. INCREASINGLY STRONG AND GUSTY SOUTHERLY LOW LEVEL WINDS ACROSS THE HIGH PLAINS WILL TRANSPORT RICH GULF MOISTURE NORTHWARD…WITH DEWPOINTS IN THE MID TO UPPER 60S EXPECTED AS FAR NORTH AS WESTERN KANSAS. STRONG DAYTIME HEATING AND RATHER COOL TEMPERATURES ALOFT WILL RESULT IN AN EXTREMELY UNSTABLE AIR MASS FROM PARTS OF NEBRASKA INTO WESTERN OKLAHOMA AND THE EASTERN TEXAS PANHANDLE. THUNDERSTORMS ARE EXPECTED TO DEVELOP OVER EASTERN COLORADO AND WESTERN KANSAS BY LATE AFTERNOON…SPREADING NORTHEASTWARD INTO PARTS OF NEBRASKA DURING THE EVENING”.

**Figure 3.** 500mb chart at 1200Z on May 4, 2007 showing geopotential height contours, pressure center and observations (SPC, 2019 modified by Francis Lavigne-Theriault, 2019).

The situation at the surface was also typical of the southern Plains in spring. A dryline was seen advancing east-northeastward throughout the day. Figure 4 depicts the dryline at 1:00 pm CDT on May 4th in the Texas panhandle and western Texas.

**Figure 4.** Surface analysis at 1800Z on May 4, 2007 depicting a dryline (in orange), surface station plots, mean sea-level pressure (MSLP) contours and pressure centers (WPC, 2017).

By 4:00 pm CDT, the dryline was extending into southwestern Kansas and sitting just west of Greensburg, KS (Figure 5).

**Figure 5.** Surface analysis at 2100Z on May 4, 2007 depicting a dryline (in orange), surface station plots, mean sea-level pressure (MSLP) contours, pressure centers and location of Greensburg (WPC, 2017, modified by Francis Lavigne-Theriault, 2019).

Below are vertical profiles of the atmospheric conditions at Dodge City, KS, which is roughly 45 minutes west of Greensburg. The sounding on the left (12Z), shows that the atmosphere had a substantial “lid” or “cap” at 850mb with southerly winds at the surface. The sounding on the right at 7:00 pm CDT (00Z) shows a completely different story with an uncapped atmosphere around Greensburg.

The Tornado

At 2:53 pm CDT, the SPC issued a mesoscale discussion reading:

“TRENDS ARE BEING CLOSELY MONITORED FOR SIGNS OF CONVECTIVE INITIATION. ALTHOUGH TIMING IS STILL A BIT UNCERTAIN…ONE OR MORE TORNADO WATCHES WILL PROBABLY BE REQUIRED LATE THIS AFTERNOON”.

**Figure 6.** Mesoscale discussion #0685 issued at 2:53 pm CDT showing area of potential supercell development, low pressure center, cold front and dryline (SPC, 2007).

At the time of this mesoscale discussion, the SPC (2007) mentioned that the mixed-layer convective available potential energy (MLCAPE) was in the 3000-4000 J/kg range, which indicates a very unstable air mass.

**Figure 7.** Tornado watch #227 issued by the Storm Prediction Center at 6:15 pm CDT on May 4, 2007 (SPC, 2007).

At 6:15 pm CDT, the SPC in Norman, OK issued tornado watch 227 for western and central Kansas, western and northern Oklahoma and the eastern Texas panhandle and northwest Texas (Figure7). The tornado watch read:

“WIDELY SCATTERED STORMS/SUPERCELLS POSSIBLE IN VERY UNSTABLE AIR MASS ALONG SLOWLY RETREATING DRY LINE THIS EVENING. STRENGTHENING ASCENT/WIND FIELD ASSOCIATED WITH APPROACHING FOUR CORNERS UPPER TROUGH MAY ENHANCE TORNADO POTENTIAL AFTER DARK AS LLJ INCREASES TO AROUND 50 KTS” (SPC, 2007).

According to Bluestein (2009), left-splitting cells were the dominant mode of convection for the day until around 0030-0100 UTC (7:30 pm – 8:00 pm CDT), after which cell splitting was no longer observed. It took about one hour for the Greensburg storm to become tornadic and at 0127 UTC (8:27 pm CDT), a weak cyclonic signature was observed on Doppler radar, which can be associated with the first tornado observed on this storm. Figure 8 depicts all the associated tornadoes generated by this supercell storm.

**Figure 8.** Storm damage tracks from five tornadoes in Kansas on May 4, 2007. Beginning and end times are estimated in CDT from Dodge City, KS WSR-88D radar signatures and correlation with damage paths. Tornado “5” being the Greensburg EF5 tornado (Bluestein, 2009).

After a 30 minute interval of cyclic tornado production (Figure 8), the Greensburg EF5 tornado formed at 9:03 pm CDT (NOAA’s NCEI, 2019) and struck Greensburg roughly 50 minutes later (Bluestein, 2009). Below is a Doppler radar loop of the supercell that produced the Greensburg EF5 tornado.

Doppler radar loop of Greensburg Storm on May 4, 2007 (SPC, 2019).

Scientific Breakthrough from “Greensburg Storm”

**Figure 9.** The Greensburg tornado of May 4, 2007 from 29 km southwest of Greensburg looking north-northeastward at 0234 UTC, when damage path was at least 1.5 km wide (Tanamachi & al., 2012).

According to Tanamachi, Bluestein, Houser, Frasier and Hardwick (2012), data were collected in the “Greensburg storm” by the University of Massachusetts X-band, mobile, polarimetric Doppler radar for an astounding 70 minutes, where 10 tornadoes were detected. This mobile Doppler radar data set is one of only a few documenting an EF5 tornado and the supercell’s transition from short-track, cyclic tornado production to long-track tornado production.

**Figure 10.** UMass X-Pol (a) uncalibrated equivalent reflectivity (in dBZ_e), (b) aliased velocity (in m s⁻¹), (c) dealiased and edited velocity (in m s⁻¹), (d) differential reflectivity (in dB), and (e) copolar cross-correlation coefficient (unitless) at 0229 UTC. All data are from an elevation angle of 3.1° except for (e), where 4.1° data are shown because 3.1° data were contaminated by beam blockage. The scans intersect the tornado at an altitude of 1.9 km AGL [2.5 km AGL in (e)]. At this time, the damage track of the mature Greensburg tornado was 2.5 km wide, and (c) shows the same Doppler velocity data after manual dealiasing and some editing. Range rings are 15 km apart; spokes are 30° apart (Tanamachi et al., 2012).

According to Tanamachi et al. (2012), the structure of the Greensburg supercell’s hook changed considerably throughout the UMass X-Pol deployment. Figure 11 depicts the evolution of the “hook echo” of the Greensburg storm.

**Figure 11.** Evolution of hook echo of Greensburg storm in UMass X-Pol (left) uncalibrated equivalent reflectivity (in dBZ) and dealiased Doppler velocity (in ms^-1) on the right on May 4, 2007. (a)–(d) indicates early tornado production stage with numerous small, short-lived vortices, (c),(d) the transition to a single, long-track tornado production phase, (e),(f) the developing phase of the Greensburg tornado, and (g)–(j) the mature Greensburg tornado with two satellite tornadoes, one of which is anticyclonic (Tanamachi et al., 2012).

At 0139 UTC (8:39 pm CDT), a maximum of four simultaneous radar velocity signatures were detected by the UMass X-Pol (Figure 11. c,d), representing several different tornadoes at varying stages of their life-cycle (Tanamachi et al., 2012).

Recap

According to Bluestein (2009), during the evening of May 4, 2007, the “Greensburg Storm” cyclically produced tornadoes for about 30 minutes before producing a large, long-lived tornado. According to NOAA’s NCEI’s storm event database (2019), an EF3 tornado developed at 10:31 pm CDT seven miles south-southwest of Trousdale, KS in Edwards County. The tornado travelled northward for 13.2 miles with a maximum width of 3872 yards (2.2 miles wide). The tornado caused no fatalities, but caused one injury and $1.5 million dollars in property damage. The wedge tornado ended at 11:08 pm CDT three miles south-southwest of Belpre, KS in Edwards County.

**Figure 12.** Sister tornadoes east of Greensburg, KS on May 4, 2007 (C. Dan Robinson, n.d.).

Sources

NOAA’s National Centers for Environmental Information. (2019). Storm Events Database. Retrieved from: https://www.ncdc.noaa.gov/stormevents/eventdetails.jsp?id=35937

NOAA’s National Weather Service Storm Prediction Center. (2007). Severe Weather Event: May 04, 2007. Retrieved from: https://www.spc.noaa.gov/exper/archive/event.php?date=20070504

NOAA’s National Weather Service Storm Prediction Center. (2019). Surface and Upper Air Maps. Retrieved from: https://www.spc.noaa.gov/obswx/maps/

NWS Weather Prediction Center. (2017). WPC’s Surface Analysis Archive. Retrieved from: https://www.wpc.ncep.noaa.gov/archives/web_pages/sfc/sfc_archive.php

National Weather Service Dodge City, Kansas. (2012). Greensburg – Five years after EF-5 tornado. Retrieved from: https://www.weather.gov/ddc/greensburgfiveyear

NOAA’s Storm Prediciton Center. (2019). U.S. Tornado Outbreak Interface. Retrieved from: https://www.spc.noaa.gov/exper/outbreaks/#

Tanamachi, R.L., H.B. Bluestein, J.B. Houser, S.J. Frasier, and K.M. Hardwick, 2012: Mobile, X-band, Polarimetric Doppler Radar Observations of the 4 May 2007 Greensburg, Kansas, Tornadic Supercell.Mon. Wea. Rev.,140, 2103–2125, https://doi.org/10.1175/MWR-D-11-00142.1

Bluestein, H.B., 2009: The Formation and Early Evolution of the Greensburg, Kansas, Tornadic Supercell on 4 May 2007.Wea. Forecasting,24, 899–920, https://doi.org/10.1175/2009WAF2222206.1

National Weather Service Dodge City, Kansas. (2008). The Rebuilding of Greensburg – one year later [PDF]. Retrieved from: https://www.weather.gov/media/ddc/Greensburg_1year_later.pdf

Stormtrack. (n.d.). May 4, 2007: Greensburg, Kansas and Arnett, Oklahoma tornadoes. Retrieved from: https://stormtrack.org/weather-library/storm-chasing-event-archive/2007-events/may-4-2007-greensburg-kansas-and-arnett-oklahoma-tornadoes/