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EF2 tornado in Pike County, Indiana

Tornado March 15, 2025 · Pike County, Indiana

EF2

Rating

33.1 mi

Whole path

400 yd

Path width

$3.5M

Damage as recorded

NOAA records this tornado county by county. Its path ran through Gibson County → Pike County; the totals above are for the whole tornado.

EF0EF1EF2EF3EF4EF5Unrated

The path drawn at its surveyed width of 400 yards (0.23 mi) — zoom in and the swath grows to true scale. Other tornadoes recorded nearby that day are shown faint.

What EF2 means. On the Enhanced Fujita scale, EF2 is considerable damage: roofs torn off well-built houses, mobile homes destroyed, large trees snapped or uprooted, consistent with estimated gusts of 111–135 mph. The rating comes from a survey of the worst damage after the storm, not from a wind measurement, so it says as much about what the tornado hit as about how strong it was.

What the National Weather Service wrote

An EF-2 tornado developed just northeast of Haubstadt in Gibson County and moved northeast through Oakland City and into Pike County. It continued northeast through mostly rural areas, damaging trees, power poles and outbuildings, and eventually crossed the White River into Daviess County just east of County Road 257. The most significant damage occurred along County Road 356 east of Algiers, where several metal truss high transmission towers were crumpled. The estimated peak wind was 120 mph. The total length of the tornado was just shy of 58 miles.

The wider storm

A significant severe weather episode unfolded across southwest Indiana in the early morning hours of the 15th, as a line of severe storms produced a tornado, damaging winds, and large hail. A strong negative-tilt 500mb trough moved northeast from Kansas to the Upper Midwest through the day and into the evening on the 14th. The associated 978mb surface low followed a similar track, and led to a rapid increase in low-level moisture just ahead of a trailing dry line that moved eastward across southwest Indiana on the morning of the 15th. The moisture return was sufficient for 1000-2000J/kg of CAPE to develop. Wind fields were extremely strong, with storm relative helicity in the 0-1km layer of 300m2/s2 and above, and 600m2/s2 in the 0-3km layer. The significant tornado parameter was over 6 which supported strong and long-track tornadoes. In addition, steep mid-level lapse rates around 8C/km supported very large hail. One EF-2 tornado developed near Haubstadt and moved northeast through Oakland City and on through northern Pike County and then into Daviess County. Oakland City took the brunt of the damage as a church and a few homes suffered roof damage and a mobile home was severely damaged. Otherwise, the tornado impacted trees, power poles, and farm buildings all along its path. In addition, 60-70 mph straight line winds were reported to the north and east of Evansville, and large hail was reported in several locations. The largest hail was up to golf ball size in Princeton.

Began near Dongola (38.3602, -87.3157).

Source: NOAA Storm Events Database, event 1242167. Narratives are written by the National Weather Service forecast office that issued the report.

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