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1971 Inverness tornado

1971 tornado across the Mississippi Delta

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Meteorological synopsis

Multiple days before the event, upper-level analysis displayed conditions that were "close to ideal" for a significant tornado outbreak. A large upper-level trough situated across the Rockies, with a substantial eastward motion toward the Great Plains, leading to significant divergence over the prefrontal warm sector. This divergence caused a significant lifting mechanism that storms could take advantage of, but surface-based shortwave meteorology was still very new, and subsequently, it was unknown how the system would behave further in the week.

On February 21, 1971, a procedural surface weather analysis failed to indicate either a well-developed low-pressure area, or a defined frontal boundary near the Mississippi Delta region; signs that would normally indicate a severe weather outbreak. At the time, an amorphous warm front extended eastward from East Texas to portions of Mississippi, and a relating cold front extended southward over east Texas. Temperatures across the region rose to 60–70 F, with signs of significant instability and dew points.

By 3:00 AM CDT, the NSSFC released a severe weather outlook. The outlook stated that "a few severe thunderstorms were expected" during the afternoon across eastern Texas to western Alabama. Again at 9:00AM CDT, a severe weather outlook was released further establishing the possibility of severe thunderstorms around Texas, Louisiana, Arkansas, Mississippi, Tennessee, and Alabama.

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