On March 18, an upper-level
trough was situated across the Western United States. As time progressed, the trough began to progress to the east. By March 20, forecasters at the
National Weather Service's
Storm Prediction Center were calling attention to "some potential for discrete storms" in Mississippi on March 24 ahead of the cold front, their severity contingent on prior destabilization of the atmosphere. On March 22, the
National Weather Service's
Storm Prediction Center (SPC) issued a level 3/enhanced risk of severe weather across portions of
Louisiana,
Arkansas, and
Mississippi for
supercell thunderstorms capable of large hail, damaging winds, and strong tornadoes (EF2+ on the
Enhanced Fujita scale). The enhanced risk was expanded northward the following day, and the original outlined area was upgraded to a level 4/moderate risk.’s Severe Weather Outlook for March 24, 2023|left|218x218pxOn March 24, water vapor imagery showed a potent mid-level
trough. Strong mid-level winds between the trough and strong
high-pressure area across the
Southeastern United States were displaying in models as well. Meanwhile, a quickly deepening
low-pressure area was expected to drag a
warm front northward, leading to a broad, unstable air mass to its south. Although some reduction in moisture was expected across Mississippi due to drier air aloft and warm surface temperatures into the 80s Fahrenheit, continued
advection of moist air from the
Gulf of Mexico seemed supportive of
dewpoints in the upper 60s and lower 70's across
Louisiana,
Arkansas, and
Mississippi by the evening hours. Thus, mixed-layer
convective available potential energy was expected to rise into the 1,500–2,000 J/kg range. Forecasters initially thought that strong forcing of ascent across Arkansas would lead to an organized
squall line capable of both tornadoes and damaging winds, whereas more discrete supercells would be possible farther south, particularly along north–south oriented confluence bands in the open
warm sector. The tornado threat relied on the amount of wind shear in the lower levels, which would aid in sustaining supercells.
Storm development from
Jackson, Mississippi, launched less than an hour before the EF4 tornado began A
tornado watch was issued at 5:15 p.m.
Central Daylight Time (
UTC−5) for portions of eastern
Arkansas, northeastern
Louisiana, central and northern
Mississippi, and western
Tennessee. The watch mentioned the possibility of several strong to intense tornadoes with persistent supercells. Clusters of storms evolved along the confluence bands in conjunction with improving
wind shear profiles. However, given their displacement from the surface low and better forcing, there was some uncertainty as to whether they would become better organized. A strengthening low-level jet and surface moisture increased confidence in the maturation of these cells, but tornadic development had not yet begun in the area as of 00:00 UTC. At their 01:00 UTC outlook, the SPC lowered the probability of tornadoes to a 10% (significant) tornado area, thus downgrading the moderate risk to an enhanced risk. The SPC cited weaker than expected instability in the area, with increased confidence in only limited buoyancy developing. However, the same update noted that "a couple of longer-track supercells" and "a few strong tornadoes" remained possible. while the EF4 tornado was ongoing As the update was being issued, a
strong supercell evolved near the Louisiana-Mississippi border. By 7:57 pm. CDT, a strong
velocity couplet formed at the base of the supercell, which then produced what would become this long-tracked violent EF4 tornado, and at 8:04 pm, as the storm approached the town of
Rolling Fork, a
tornado emergency was placed. Afterwards, the tornado struck
Rolling Fork,
Midnight, and
Silver City, inflicting catastrophic damage and causing over a dozen fatalities. While the violent EF4 tornado was on the ground, Harry Weinman, a forecaster at the SPC, issued a special
meso-gamma mesoscale discussion for the tornado. The discussion concluded by noting that the downstream atmospheric environment would allow the storm producing the violent EF4 tornado to persist for 30 to 60 minutes. ==Tornado summary==