Summary
Showers and thunderstorms ahead of an approaching cold front and associated surface low brought rain and thunderstorms to the Tennessee Valley just before daybreak through the morning hours on the 25th. As the morning and early afternoon progressed, this activity pushed east into Georgia around 1 pm. This activity produced some heavier rainfall over much of northern Alabama, but no severe weather.
As the afternoon progressed some surface heating occurred as the clouds thinned. As a result, instability increased in over northern Alabama. This can be seen in the surface analysis below, as surface temperatures climbed into the mid 60s. Marginal low level moisture was present with dewpoints in the mid to upper 50s. Locations south of the red line had dewpoints in the 50s, while the purple line depicts where dewpoints were above 60 degrees.
At the same time, shear (a wind parameter needed for supercell and tornadic storm development) increased. This increase in shear aided by a 90 knot (103 mph) jet streak pushing east from eastern Texas and Lousiana at 500 mb (around 19,000 feet) and into northern Alabama along and ahead of the cold front. This wind maximum can be seen in the 500 mb analysis chart below, outlined in purple.
Shear through the late afternoon and early evening hours remained high enough for an isolated tornado threat. Wet-bulb temperatures were at an ideal level for large hail (between 7000 and 9000 feet) throughout the day and into the early evening hours. This set the stage for the development of severe thunderstorms producing large hail and isolated tornadoes.
Below are loops of radar images around the time the tornado touched down in Morgan County. The loop on the left shows storm relative velocity between 5:35 pm and 5:58 pm. During this window, the tornado developed and moved across extreme southeastern portions of Morgan County, just northwest of the Joppa community. The image on the right is a base storm reflectivity product and shows precipitation. Click on the image to initiate a larger loop in a new window.

Morgan County Tornado Survey Summary
| Rating |
EF-1 |
Peak Wind |
100 mph |
| Path Length |
3 miles |
Peak Path Width |
50 yards |
Below are some pictures of the damage along the path of this tornado.
Damage Reports for Entire Severe Weather Event:
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