Overview
On September 13th, 2025, a highly amplified trough would push across the four corners region in the early afternoon. This trough was producing supercells across Utah and western Colorado early in the day, some of which were tornadic, and as it traversed eastward, would continue to spawn supercell thunderstorms across central Colorado. One of these supercells would go on to intensify along the northern fringes of the La Garita Mountains. As this storm tracked into the WFO Pueblo County Warning Area, it quickly developed an intense mesocyclone thanks to the 50-60 knots of bulk shear in place, and as it passed over Sawtooth Mountain, would then go on to produce a brief tornado along the northern slopes of the mountain.Tornadoes
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Tornado - Sawtooth Mountain Tornado
Track Map
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The Enhanced Fujita (EF) Scale classifies tornadoes into the following categories:
| EF0 Weak 65-85 mph |
EF1 Moderate 86-110 mph |
EF2 Significant 111-135 mph |
EF3 Severe 136-165 mph |
EF4 Extreme 166-200 mph |
EF5 Catastrophic 200+ mph |
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Photos & Video
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| Image of the tornado scar via Copernicus Satellite data |
Radar
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| Loop of radar reflectivity and velocity of the Sawtooth Mountain Tornado. | Image of radar reflectivity and velocity of the Sawtooth Mountain Tornado. |
Environment
Synoptic Environment:
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| Figure 1: 300mb pattern at 12 PM MDT September 13th. | Figure 2: 500mb pattern at 12 PM MDT September 13th. | Figure 3: 700mb pattern at 12 PM MDT September 13th. |
Near-storm Environment:
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| Figure 4: Surface pattern at 12 PM MDT September 13th. | Figure 5: 0-6km Bulk Shear at 12 PM MDT September 13th. | Figure 6: Effective SRH at 12 PM MDT September 13th. |
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| Figure 7: Mixed Layer CAPE at 12 PM MDT September 13th. | Figure 8: Supercell Composite (SCP) at 12 PM MDT September 13th. | Figure 9: Significant Tornado Parameter (STP) at 12 PM MDT September 13th. |
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| Figure 10: RAP sounding of environment for the Sawtooth Mountain Tornado |
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