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Tornado outbreak of April 9–11, 1947

1947 windstorm through the U.S. states of Texas, Oklahoma, and Kansas

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Through Great Plains, Tornado and Fog

Background

Early on April 9, the United States Weather Bureau in Amarillo, Texas, forecast late-afternoon temperatures of about 60 °F (16 °C) over the Texas panhandle. At the time, dense, low-lying stratus and a layer of fog were present, with temperatures ranging from the upper 40s to low 50s °F. However, an approaching warm front—then extended from Sherman, Texas, to Raton, New Mexico—would later combine with a robust trough aloft to enhance conditions for severe weather. In tandem with this, a low-pressure area over northeastern New Mexico, along with an attendant dry line, would gradually eject, leading to stronger low-level wind shear and more pronounced lapse rates. Around 2:00 p.m. CST (18:00 UTC), helicity was near 135 m2/s2, but would decline afterward. As it did so, however, an unexpected decrease in cloud cover allowed for greater-than-expected diurnal heating, leading to a substantial rise in atmospheric instability and associated buoyancy. By 6:30 p.m. CST (00:30 UTC), the low-pressure center was situated over southern Colorado, and a 53-to-61-mile-per-hour (85 to 98 km/h) jet stream existed 4,000 to 7,000 ft (1,200 to 2,100 m; 1.2 to 2.1 km) above sea level. Surface-based temperatures quickly reached the upper 60s °F. In the mixed layer, the convective available potential energy (CAPE) rose above 1,100 j/kg, and the lifted condensation level (LCL) was just 752 m (0.752 km) above ground level, along with a level of free convection (LFC) of 1,410 m (1.41 km). Mixed-layer convective inhibition by then had decreased, offsetting the loss of helicity, and the presence of the warm front acted in concert with the aforementioned factors to favor supercells capable of generating strong tornadoes. Gusts of 30 to 40 mph (48 to 64 km/h) attended the passage of a cold front overnight.

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