of Texas at 2:00 p.m. CDT on May 27 showing the cold front (solid line with pennants), dry line (dashed line with semicircles), gravity wave (solid line), and low-pressure area (L symbol). The alignment of these features produced the local environmental conditions enabling the tornado outbreak.|alt=A weather map of Texas On the morning of May 27, 1997, an upper-level low-pressure area located over portions of
South Dakota and
Nebraska had moved northward which caused a weak, mid-level flow across
Texas. While this occurred, a
cold front extended southwest of a surface-based low-pressure area from
Fayetteville, Arkansas to the
Dallas–Fort Worth metroplex (DFW) to the
Permian Basin, which also included two decaying
outflow boundaries northeast of the DFW metroplex. A
gravity wave was also noted from the cold front near
Waco, Texas and southward, which would promote initiation of supercells, including the one which produced the Jarrell tornado. The latter two factors were caused by an overnight
mesoscale convective system which had dissipated before the mesoscale setup of the Jarrell tornado. An upper-air balloon sounding was conducted by the
National Weather Service in Fort Worth while the cold front passed directly over the
DFW metroplex, which showed favorable mid-level
lapse rates, a
dewpoint temperature of on the surface, and some
wind shear, though not towards the surface, which suggested non-tornadic supercell activity. However, a sounding launched from
Calvert, Texas a few hours later revealed surface-based CAPE values above 6500
J/kg, up from 3000 J/kg shown by the sounding previously launched over the DFW metroplex. Shortly thereafter, the supercell began to move slightly westward towards Jarrell and
Salado while continuing to show signs of rapid, low-level rotation. This would result in another tornado warning being issued by the National Weather Service in Austin/San Antonio for Williamson County, including Jarrell, at 15:30 CDT (22:30 UTC), in response to the storm's approach to the town. The warning was in effect for a duration of one hour, and local warning sirens in the town went off an estimated 10–12 minutes before the impact. Multiple short-lived, small, and rope-like
funnel clouds preceded the Jarrell tornado; and despite being theorized and commonly accepted as being separate tornadoes, there is a possibility that these were part of it. Additionally, some reports stated an F1 tornado near Prairie Dell as an earlier continuation of this tornado. == Tornado summary ==