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Severe thunderstorms are expected to develop this afternoon and evening from the southern and central Plains into the lower to mid Missouri Valley, and upper Mississippi Valley. Tornadoes, large hail and severe wind gusts will be possible.
← back to overviewSPC AC 230502
Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 1202 AM CDT Thu Apr 23 2026
Valid 231200Z - 241200Z
THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS PARTS OF EASTERN KANSAS
### SUMMARY
Severe thunderstorms are expected to develop this afternoon and evening from the southern and central Plains into the lower to mid Missouri Valley, and upper Mississippi Valley. Tornadoes, large hail and severe wind gusts will be possible.
Southern and Central Plains/Lower to Mid Missouri Valley/Upper Mississippi Valley
An upper-level trough will move through the central Rockies this morning, and into the High Plains this afternoon as a 50 to 60 knot mid-level jet moves into the Great Plains. At the surface, a cold front will advance southeastward into the mid Missouri Valley and central Plains. Moisture advection ahead of the front will increase surface dewpoints into the mid 60s F by afternoon. This will contribute to moderate destabilization as surface temperatures warm along the moist axis. Thunderstorms are first expected to develop ahead of the front over the mid Missouri and upper Mississippi Valleys in the early to mid afternoon. Convective coverage will rapidly expand southward into eastern Kansas by late afternoon, and into far northern Oklahoma during the early to mid evening. MCS development appears likely to take place along and ahead of the front.
The best environment for severe storms will be in eastern Kansas. In this area, RAP forecast soundings late this afternoon ahead of the front have MLCAPE peaking just above 3000 J/kg, with 700-500 mb lapse rates in the 7.5 to 8 C/km range. 0-6 km shear is forecast to be in the 35 to 40 knot range. This environment will support supercells with large hail. Hailstones greater than 2 inches in diameter will be possible with the more intense supercells. In addition, 0-3 km storm-relative helicity is forecast to increase into the 300 to 400 m2/s2 range by 00Z, as at 40 to 50 knot low-level jet strengthens. This will support tornadoes with supercells. Supercells will initially be discrete but a line is expected to form by early evening. As the line forms, rotating cells within the line should also be capable of producing tornadoes. A strong tornado or two will be possible late this afternoon and early this evening. A wind-damage threat is also expected to develop. The southern edge of the line will impact far northern Oklahoma in the early to mid evening. Convective coverage should be isolated further south across the rest of Oklahoma.
Further north-northeast into Iowa and southern Minnesota, instability will not be as strong. RAP forecast soundings by late afternoon have MLCAPE peaking in the 1500 to 2000 J/kg range. This, combined with 30 to 35 knots of deep-layer shear and 700-500 mb lapse rates of 7 to 7.5 C/km should support large hail with supercells. Supercells and developing line segments should also be capable of producing wind damage, hail and a tornado or two.
..Broyles/Chalmers.. 04/23/2026
CLICK TO GET WUUS01 PTSDY1 PRODUCT
NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 1300Z
Scatteed severe thunderstorms are possible Friday from the Southern Plains into the Lower Mississippi Valley. Large hail and damaging winds will be the main hazards, with a brief tornado also possible. Isolated strong wind gusts may occur across portions of the lower Ohio Valley as well.
← back to overviewSPC AC 230600
Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 0100 AM CDT Thu Apr 23 2026
Valid 241200Z - 251200Z
THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS PARTS OF THE SOUTHERN PLAINS INTO THE LOWER MISSISSIPPI VALLEY
### SUMMARY
Scatteed severe thunderstorms are possible Friday from the Southern Plains into the Lower Mississippi Valley. Large hail and damaging winds will be the main hazards, with a brief tornado also possible. Isolated strong wind gusts may occur across portions of the lower Ohio Valley as well.
Synopsis
Broad cyclonic flow will persist across much of the central and western US as a longwave trough remains anchored over the northern states. In the absences of stronger large-scale ascent across the southern US, convective evolution will be driven primarily by remnant boundaries and subtle perturbations within the broader cyclonic flow.
Southern Plains into the Lower Mississippi Valley
Convection is expected to be ongoing from portions of Oklahoma into Arkansas and Missouri at the start of the forecast period, largely tied to a convectively augmented cold front. This activity may still be capable of producing isolated strong wind gusts early in the period, but should gradually weaken through the morning as the low-level jet dissipates and the parent shortwave trough moves away from the region.
The primary severe threat is expected to develop from afternoon into the evening along the effective frontal zone and any residual outflow or differential heating boundaries. Current guidance suggests the boundary will settle near or south of the I-40 corridor, though some uncertainty in the exact location remains. Notably, the HRRR is an outlier in maintaining a farther north and west boundary as compared to other members of the 20260423/00Z HREF.
By afternoon, strong heating south of the boundary will support a moderately to strongly unstable airmass (SBCAPE values in the 2000-3000 J/kg range) from central/east Texas northward toward the boundary, with instability gradually decreasing with eastward extent into Mississippi and Alabama. Deep-layer shear will remain modest across the region (generally 30-35 knots), supporting organized multicells and occasional transient supercells.
Thunderstorms should develop/intensify from eastern Oklahoma into Arkansas along one or more of boundaries across the region. Initial storms may pose a threat for large hail and localized damaging wind gusts as low-level shear will generally remain weak. However, localized enhancements along boundaries or any MCV could support a brief tornado risk.
With time, storm interactions and consolidating outflows should support upscale growth into one or more clusters or linear MCS structures. These systems should move east-southeast into northern Louisiana and central Mississippi through the afternoon and evening hours. While the modest deep-layer shear may temper the overall wind threat somewhat, sufficient organization should still support a corridor of damaging wind gusts.
Farther west into central and eastern Texas, isolated convection may occur along a dryline as diurnal heating weakens inhibition to the east. Storm coverage is expected to remain sparse given weak ascent, but any sustained updrafts in this strongly unstable environment could produce large hail.
Portions of the Ohio Valley
A separate corridor of thunderstorms may develop during the afternoon across portions of the eastern Indiana and western Ohio in the wake of earlier convection. Modest destabilization should occur with perhaps up to 1000 J/kg of SBCAPE. Although the low-level jet will be weakening through the day, residual flow and modest deep-layer shear may support loosely organized convection capable of producing damaging wind gusts.
..Marsh.. 04/23/2026
CLICK TO GET WUUS02 PTSDY2 PRODUCT
NOTE: THE NEXT DAY 2 OUTLOOK IS SCHEDULED BY 1730Z
Severe thunderstorms will likely develop across portions of Oklahoma and Kansas during the evening. These storms will pose a risk of very large hail, damaging winds, and a couple of tornadoes. Isolated severe thunderstorms may also develop across portions of North Texas during the afternoon.
← back to overviewSPC AC 230727
Day 3 Convective Outlook NWS Storm Prediction Center Norman OK 0227 AM CDT Thu Apr 23 2026
Valid 251200Z - 261200Z
THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS PORTIONS OF SOUTH-CENTRAL KANSAS INTO CENTRAL AND EASTERN OKLAHOMA AND FAR NORTHWEST ARKANSAS
### SUMMARY
Severe thunderstorms will likely develop across portions of Oklahoma and Kansas during the evening. These storms will pose a risk of very large hail, damaging winds, and a couple of tornadoes. Isolated severe thunderstorms may also develop across portions of North Texas during the afternoon.
Synopsis
Increasingly diffluent southwest flow will overspread the Southern and Central Plains on Saturday as the midlevel pattern responds to a strong shortwave trough/vorticity maximum moving into the Southwest. This will induce strong southerly winds across the Plains, helping to quickly draw an old frontal boundary northward. This boundary should be oriented from northwest to southeast across portions of Oklahoma by late Saturday.
Portions of Kansas, Oklahoma, and western Arkansas
Most of the day should be devoid of thunderstorms as mid-level heights rise downstream of a digging trough across the Southwest. At the same time, strong southerly winds will transport Gulf moisture northward from the far Southern Plains into the Central Plains. Diurnal heating of this airmass will result in the development of strong instability across much of the area, as maximum SBCAPE values approach 4000 J/kg across portions of north Texas into central Oklahoma.
During the late evening a subtle perturbation within the southwest flow is forecast to approach Oklahoma. In response to this, the low-level jet is forecast to increase to between 30 and 40 knots. As it crosses the northward moving warm front, this warm-air advection/isentropic ascent will combine with modest large-scale ascent from the approaching midlevel perturbation to support scattered thunderstorm develop on the north side of the moisture gradient. Although differences exist between the various models, the generic depiction of forecast soundings show long hodographs with varying degrees of low-level curvature in the presence of 2000-3000 J/kg of MUCAPE. Thus, any storm that develops within the environment will be capable of producing all hazards initially. With time, thunderstorms should grow upscale into one or more southeast moving bowing segments capable of producing damaging winds with perhaps a QLCS tornado threat.
North Texas into Southern Oklahoma
Diurnal heating of a moist airmass to the east of a dryline will result in an extremely unstable airmass developing by the afternoon. Although the region will be devoid of large-scale forcing for ascent, temperatures in the 90Fs to the west of the dryline may be sufficient to induce dryline circulations capable of initiating isolated thunderstorms. Any thunderstorm that develops will be capable of producing very large hail.
..Marsh.. 04/23/2026
CLICK TO GET WUUS03 PTSDY3 PRODUCT
NOTE: THE NEXT DAY 3 OUTLOOK IS SCHEDULED BY 1930Z
You are looking at an outlook that is part of the medium range forecast (the outlook for days 4-8). The most important thing to note is that lack of a risk does not mean zero risk. Generally speaking, confidence has to be pretty high for the Storm Prediction Center to have an outlook area this far into the future.
When no specific risk areas are shown, you might see one of these phrases:
If you bookmark this page, it will continue to update with each new outlook that is issued.
| Day 4 | Saturday, April 25 | low / uncertain |
| Day 5 | Sunday, April 26 | 30% |
| Day 6 | Monday, April 27 | 15% |
| Day 7 | Tuesday, April 28 | predictability too low |
| Day 8 | Wednesday, April 29 | predictability too low |
← back to overviewZCZC SPCSWOD48 ALL ACUS48 KWNS 220900 SPC AC 220900
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0400 AM CDT Wed Apr 22 2026
Valid 251200Z - 301200Z
DISCUSSION
An active severe weather pattern will continue through early next week.
On Saturday/Day-4, model guidance continues to show thunderstorms developing during the late afternoon and early evening hours along a lifting warm front across the Southern Plains. Along and south of this boundary, the environment will be strongly unstable with MUCAPE values between 2000-3000 J/kg as a low-level jet continually advects mid 60Fs dewpoints north across the boundary. Effective layer shear around 40 knots would support an initial supercell threat that should grow upscale into bowing segments overnight. A 30% area is introduced across southwest Kansas into east-central Oklahoma for the expectation is for strong bowing segments to move east-southeast overnight into a strong low-level jet. These storms will be capable of producing strong winds, large hail, and QLCS tornadoes.
On Sunday/Day-5, ongoing convection across southeast Kansas and western Missouri at the start of the period may pose a continued risk of hail and damaging winds, and this convection may persist into mid morning. To the west, continued moist low-level advection will allow for surface dewpoints to rise into the upper 60Fs to low 70Fs across central Oklahoma to the east of a sharp dryline. At the same time, a low-amplitude shortwave should approach the Southern Plains during the late afternoon and evening hours, with a mid-990-millibar surface low developing across northwest Oklahoma along the dryline. The result of this setup will be a volatile atmosphere where MLCAPE values around 4000 J/kg exist within a strongly shear environment (vertical shear nearly 50 knots). Should thunderstorms initiate, a high-end severe weather threat could materialize during the late afternoon and evening hours across central and eastern Oklahoma and southern Kansas. However, global models continue to struggle to develop convection within this environment despite model guidance having modest upward vertical velocities overspreading the dryline. Pattern recognition suggests the need for a 30% severe area for this potential despite the lack of a QPF signal in the global models, and have opted to add one with this forecast. The location of this 30% will likely need to be refined in subsequent outlooks.
The severe threat should continue into Monday/Day-6 across portions of the Lower Mississippi Valley. Strong storms should develop along and ahead of an eastward moving cold front. MUCAPE of 2000-3000 J/kg and 40-knots of deep-layer shear will support supercell thunderstorms capable of all severe hazards. The location, number, and intensity of these supercells will likely be modulated by the events of Sunday. Specifically, if widespread convection does not occur Sunday across the Southern Plains, a more robust reservoir of CAPE/lapse-rates will be available to thunderstorms across the Lower Mississippi Valley on Monday and a higher-end severe potential may develop. This will be monitored in subsequent forecasts.
By Tuesday/Day-7 into Wednesday/Day-8, uncertainty in the severe potential across the southeast increases too much to have confidence in identifying specific locations. Although, as the mesoscale details become cleared in the preceding days, areas may need to be added in subsequent forecasts.
..Marsh.. 04/22/2026
CLICK TO GET WUUS48 PTSD48 PRODUCT
You are looking at an outlook that is part of the medium range forecast (the outlook for days 4-8). The most important thing to note is that lack of a risk does not mean zero risk. Generally speaking, confidence has to be pretty high for the Storm Prediction Center to have an outlook area this far into the future.
When no specific risk areas are shown, you might see one of these phrases:
If you bookmark this page, it will continue to update with each new outlook that is issued.
| Day 4 | Saturday, April 25 | low / uncertain |
| Day 5 | Sunday, April 26 | 30% |
| Day 6 | Monday, April 27 | 15% |
| Day 7 | Tuesday, April 28 | predictability too low |
| Day 8 | Wednesday, April 29 | predictability too low |
← back to overviewZCZC SPCSWOD48 ALL ACUS48 KWNS 220900 SPC AC 220900
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0400 AM CDT Wed Apr 22 2026
Valid 251200Z - 301200Z
DISCUSSION
An active severe weather pattern will continue through early next week.
On Saturday/Day-4, model guidance continues to show thunderstorms developing during the late afternoon and early evening hours along a lifting warm front across the Southern Plains. Along and south of this boundary, the environment will be strongly unstable with MUCAPE values between 2000-3000 J/kg as a low-level jet continually advects mid 60Fs dewpoints north across the boundary. Effective layer shear around 40 knots would support an initial supercell threat that should grow upscale into bowing segments overnight. A 30% area is introduced across southwest Kansas into east-central Oklahoma for the expectation is for strong bowing segments to move east-southeast overnight into a strong low-level jet. These storms will be capable of producing strong winds, large hail, and QLCS tornadoes.
On Sunday/Day-5, ongoing convection across southeast Kansas and western Missouri at the start of the period may pose a continued risk of hail and damaging winds, and this convection may persist into mid morning. To the west, continued moist low-level advection will allow for surface dewpoints to rise into the upper 60Fs to low 70Fs across central Oklahoma to the east of a sharp dryline. At the same time, a low-amplitude shortwave should approach the Southern Plains during the late afternoon and evening hours, with a mid-990-millibar surface low developing across northwest Oklahoma along the dryline. The result of this setup will be a volatile atmosphere where MLCAPE values around 4000 J/kg exist within a strongly shear environment (vertical shear nearly 50 knots). Should thunderstorms initiate, a high-end severe weather threat could materialize during the late afternoon and evening hours across central and eastern Oklahoma and southern Kansas. However, global models continue to struggle to develop convection within this environment despite model guidance having modest upward vertical velocities overspreading the dryline. Pattern recognition suggests the need for a 30% severe area for this potential despite the lack of a QPF signal in the global models, and have opted to add one with this forecast. The location of this 30% will likely need to be refined in subsequent outlooks.
The severe threat should continue into Monday/Day-6 across portions of the Lower Mississippi Valley. Strong storms should develop along and ahead of an eastward moving cold front. MUCAPE of 2000-3000 J/kg and 40-knots of deep-layer shear will support supercell thunderstorms capable of all severe hazards. The location, number, and intensity of these supercells will likely be modulated by the events of Sunday. Specifically, if widespread convection does not occur Sunday across the Southern Plains, a more robust reservoir of CAPE/lapse-rates will be available to thunderstorms across the Lower Mississippi Valley on Monday and a higher-end severe potential may develop. This will be monitored in subsequent forecasts.
By Tuesday/Day-7 into Wednesday/Day-8, uncertainty in the severe potential across the southeast increases too much to have confidence in identifying specific locations. Although, as the mesoscale details become cleared in the preceding days, areas may need to be added in subsequent forecasts.
..Marsh.. 04/22/2026
CLICK TO GET WUUS48 PTSD48 PRODUCT
You are looking at an outlook that is part of the medium range forecast (the outlook for days 4-8). The most important thing to note is that lack of a risk does not mean zero risk. Generally speaking, confidence has to be pretty high for the Storm Prediction Center to have an outlook area this far into the future.
When no specific risk areas are shown, you might see one of these phrases:
If you bookmark this page, it will continue to update with each new outlook that is issued.
| Day 4 | Saturday, April 25 | low / uncertain |
| Day 5 | Sunday, April 26 | 30% |
| Day 6 | Monday, April 27 | 15% |
| Day 7 | Tuesday, April 28 | predictability too low |
| Day 8 | Wednesday, April 29 | predictability too low |
← back to overviewZCZC SPCSWOD48 ALL ACUS48 KWNS 220900 SPC AC 220900
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0400 AM CDT Wed Apr 22 2026
Valid 251200Z - 301200Z
DISCUSSION
An active severe weather pattern will continue through early next week.
On Saturday/Day-4, model guidance continues to show thunderstorms developing during the late afternoon and early evening hours along a lifting warm front across the Southern Plains. Along and south of this boundary, the environment will be strongly unstable with MUCAPE values between 2000-3000 J/kg as a low-level jet continually advects mid 60Fs dewpoints north across the boundary. Effective layer shear around 40 knots would support an initial supercell threat that should grow upscale into bowing segments overnight. A 30% area is introduced across southwest Kansas into east-central Oklahoma for the expectation is for strong bowing segments to move east-southeast overnight into a strong low-level jet. These storms will be capable of producing strong winds, large hail, and QLCS tornadoes.
On Sunday/Day-5, ongoing convection across southeast Kansas and western Missouri at the start of the period may pose a continued risk of hail and damaging winds, and this convection may persist into mid morning. To the west, continued moist low-level advection will allow for surface dewpoints to rise into the upper 60Fs to low 70Fs across central Oklahoma to the east of a sharp dryline. At the same time, a low-amplitude shortwave should approach the Southern Plains during the late afternoon and evening hours, with a mid-990-millibar surface low developing across northwest Oklahoma along the dryline. The result of this setup will be a volatile atmosphere where MLCAPE values around 4000 J/kg exist within a strongly shear environment (vertical shear nearly 50 knots). Should thunderstorms initiate, a high-end severe weather threat could materialize during the late afternoon and evening hours across central and eastern Oklahoma and southern Kansas. However, global models continue to struggle to develop convection within this environment despite model guidance having modest upward vertical velocities overspreading the dryline. Pattern recognition suggests the need for a 30% severe area for this potential despite the lack of a QPF signal in the global models, and have opted to add one with this forecast. The location of this 30% will likely need to be refined in subsequent outlooks.
The severe threat should continue into Monday/Day-6 across portions of the Lower Mississippi Valley. Strong storms should develop along and ahead of an eastward moving cold front. MUCAPE of 2000-3000 J/kg and 40-knots of deep-layer shear will support supercell thunderstorms capable of all severe hazards. The location, number, and intensity of these supercells will likely be modulated by the events of Sunday. Specifically, if widespread convection does not occur Sunday across the Southern Plains, a more robust reservoir of CAPE/lapse-rates will be available to thunderstorms across the Lower Mississippi Valley on Monday and a higher-end severe potential may develop. This will be monitored in subsequent forecasts.
By Tuesday/Day-7 into Wednesday/Day-8, uncertainty in the severe potential across the southeast increases too much to have confidence in identifying specific locations. Although, as the mesoscale details become cleared in the preceding days, areas may need to be added in subsequent forecasts.
..Marsh.. 04/22/2026
CLICK TO GET WUUS48 PTSD48 PRODUCT
You are looking at an outlook that is part of the medium range forecast (the outlook for days 4-8). The most important thing to note is that lack of a risk does not mean zero risk. Generally speaking, confidence has to be pretty high for the Storm Prediction Center to have an outlook area this far into the future.
When no specific risk areas are shown, you might see one of these phrases:
If you bookmark this page, it will continue to update with each new outlook that is issued.
| Day 4 | Saturday, April 25 | low / uncertain |
| Day 5 | Sunday, April 26 | 30% |
| Day 6 | Monday, April 27 | 15% |
| Day 7 | Tuesday, April 28 | predictability too low |
| Day 8 | Wednesday, April 29 | predictability too low |
← back to overviewZCZC SPCSWOD48 ALL ACUS48 KWNS 220900 SPC AC 220900
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0400 AM CDT Wed Apr 22 2026
Valid 251200Z - 301200Z
DISCUSSION
An active severe weather pattern will continue through early next week.
On Saturday/Day-4, model guidance continues to show thunderstorms developing during the late afternoon and early evening hours along a lifting warm front across the Southern Plains. Along and south of this boundary, the environment will be strongly unstable with MUCAPE values between 2000-3000 J/kg as a low-level jet continually advects mid 60Fs dewpoints north across the boundary. Effective layer shear around 40 knots would support an initial supercell threat that should grow upscale into bowing segments overnight. A 30% area is introduced across southwest Kansas into east-central Oklahoma for the expectation is for strong bowing segments to move east-southeast overnight into a strong low-level jet. These storms will be capable of producing strong winds, large hail, and QLCS tornadoes.
On Sunday/Day-5, ongoing convection across southeast Kansas and western Missouri at the start of the period may pose a continued risk of hail and damaging winds, and this convection may persist into mid morning. To the west, continued moist low-level advection will allow for surface dewpoints to rise into the upper 60Fs to low 70Fs across central Oklahoma to the east of a sharp dryline. At the same time, a low-amplitude shortwave should approach the Southern Plains during the late afternoon and evening hours, with a mid-990-millibar surface low developing across northwest Oklahoma along the dryline. The result of this setup will be a volatile atmosphere where MLCAPE values around 4000 J/kg exist within a strongly shear environment (vertical shear nearly 50 knots). Should thunderstorms initiate, a high-end severe weather threat could materialize during the late afternoon and evening hours across central and eastern Oklahoma and southern Kansas. However, global models continue to struggle to develop convection within this environment despite model guidance having modest upward vertical velocities overspreading the dryline. Pattern recognition suggests the need for a 30% severe area for this potential despite the lack of a QPF signal in the global models, and have opted to add one with this forecast. The location of this 30% will likely need to be refined in subsequent outlooks.
The severe threat should continue into Monday/Day-6 across portions of the Lower Mississippi Valley. Strong storms should develop along and ahead of an eastward moving cold front. MUCAPE of 2000-3000 J/kg and 40-knots of deep-layer shear will support supercell thunderstorms capable of all severe hazards. The location, number, and intensity of these supercells will likely be modulated by the events of Sunday. Specifically, if widespread convection does not occur Sunday across the Southern Plains, a more robust reservoir of CAPE/lapse-rates will be available to thunderstorms across the Lower Mississippi Valley on Monday and a higher-end severe potential may develop. This will be monitored in subsequent forecasts.
By Tuesday/Day-7 into Wednesday/Day-8, uncertainty in the severe potential across the southeast increases too much to have confidence in identifying specific locations. Although, as the mesoscale details become cleared in the preceding days, areas may need to be added in subsequent forecasts.
..Marsh.. 04/22/2026
CLICK TO GET WUUS48 PTSD48 PRODUCT
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