


Area Forecast Discussion
Issued by NWS Kansas City/Pleasant Hill, MO
Issued by NWS Kansas City/Pleasant Hill, MO
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024 FXUS63 KEAX 071119 AFDEAX Area Forecast Discussion National Weather Service Kansas City/Pleasant Hill MO 619 AM CDT Mon Jul 7 2025 ...Updated 12z Aviation... .KEY MESSAGES... - Storms Possible Monday Afternoon; Low Confidence In Evolution - Strong Thunderstorm Complex Over Nebraska May Move Across The Area Late Monday Night; Showers Likely, Severe Threat Uncertain - Additional Shower/Storms Much of This Week; Tuesday Activity and Strength Heavily Dependent on Monday Night Activity && .DISCUSSION... Issued at 326 AM CDT Mon Jul 7 2025 Clear skies and weak winds has led to the development of fog across portions of eastern Kansas and Missouri, especially along river valleys, creeks, and other low lying areas. This should mix out by sunrise. Multiple mid-level vort maxima continue to travel across the Central CONUS in a generally westerly to northwesterly flow regime, driven by strong anti-cyclone over the desert southwest. This will continue a cycle of mid-level lift, followed by subsidence. Near surface layer remains fairly moist, with dewpoints holding steady in the upper 60s to lower 70s across most of the forecast area. A transient thermal boundary has stalled along the Interstate 70 corridor overnight, likely a result from the stronger convection that occurred Sunday evening across the Ozarks. A few observations prior to 06z showed some stronger moisture pooling, but as the overnight hours have progressed, the temperature gradient has largely eroded. Surface and 925mb theta-e analysis indicates that something is still there. However, the overnight hours saw a subtle H5 ridge move through, which clearer skies quite a bit on both sides of this thermal boundary. This is making the mesoscale setup for Monday afternoon quite uncertain, and is one of two main factors contributing to low confidence in precipitation chances for the first 24-30 hours of this forecast period. Without well defined cloud cover on either side of this thermal boundary, its hard to see substantial differential heating reestablish its strength today, thinking most of the area should see temperatures in the upper 80s to lower 90s, with dewpoints holding steady in the upper 60s to lower 70s. A few of the 00z CAMs have depicted storm initiation along this remnant thermal boundary, some starting in far northwestern Missouri, and some right over the Kansas City metro. Most of this appears to be tied to peak heating, and would expect destabilization throughout the afternoon given current satellite trends. Will have to keep an eye on cirrus advection from the cloud cover over the High Plains. Diurnal heating of a moist boundary layer should generate a cumulus field by the mid to late afternoon hours. With respect to showers or storms developing will depend on the timing of the mid-level vort maxima moving through. If this lines up with the nearly 2000 J/kg SBCAPE, as depicted in the 00z HREF, a cluster of multicells likely develop. The favorable spot would seem to be along the MO-KS state line, though the instability axis could extend pretty far eastward into Central Missouri. With higher instability, a few stronger storms certainly cannot be ruled out as a the mid-level wave moves through, but RAP and HRRR soundings are not showing as robust of an inverted-v sounding and evaporational cooling potential as we had seen last week. Therefore, if the cumulus field is able to initiate deep convection, would expect the severe threat to be relatively limited, wind gusts perhaps around 40 to 50 MPH. The stronger deep layer shear remains progged over the Central Kansas and Central Nebraska, thus that is where better storm organization likely occurs Monday late afternoon. Once we are past peak heating this evening, CAMs remain relatively dry, and would expect a break from isolated convection if it develops. Attention then turns activity over Nebraska, where stronger H5 height falls, better surface convergence and stronger dCVA aligns with a strong instability axis, along with a greater deep layer shear. By evening, storms over Nebraska congeal, and CAMs along with other ensemble suites are favoring development of an MCS. CAMs so far have been favoring an area of expansive showers moving into northwest Missouri around 06z this evening, then moving east- southeast overnight into Tuesday morning. The HRRR specifically decays the stronger convection by the time it reaches most of the forecast area. And based on the background environment, would make sense as the wind shear drastically decreases as this MCS would exit the Central Plains. Therefore, would anticipate decaying shower activity overnight. The big question, how healthy would the cold pool of the system be as gets to our area. If the MCS maintains itself for longer, there is the potential to see severe wind gusts across portions eastern Kansas to central Missouri, and this morning`s SPC SWODY1 marginal risk highlights this. From analysis this morning, this is a lower probability outcome. And the antecedent mesoscale parameters from the Monday morning remnant boundary and any daytime convection will also play a role. For now, will maintain likely POPs (55-60%) in our northwest with decaying convection, with slight chance POPs further south and southeast. We may not have overly high confidence in showers/storms overnight until we see how convection over Nebraska evolves. Tuesday, another mid-level short-wave moves through, and likely will see another day of stronger destabilization as this lift moves through. However, the early morning convection throws a big question mark on how the boundary layer recovers. With decaying convection, odds are favorable for an outflow boundary, perhaps multiple, to be present across eastern Kansas to Central Missouri. These will probably provide most of the focus for redevelopment on Tuesday. Strong differential heating along these boundaries would likely be the main driver of any kind of severe wind threat. 06z CAMs that have started to come in are indicating stronger storm development for across Central Missouri after 22z on Tuesday. If Tuesday morning convection pushes southeast and stabilizes the boundary layer, the storms and severe threat could push eastward out of our area on Tuesday. Beyond Tuesday, we will continue to see short-waves traverse the region that will bring additional shower and thunderstorm opportunities. Mid to upper-level flow will still remain fairly weak, limiting deep layer shear. Storm strength will largely be tied to the degree of destabilization and what kind of lapse rates can be achieved. Ensembles are likely spreading out low end precipitation chances over too broad of a time period, but given the varying propagation speeds of any of these waves, makes it hard to be certain. Friday into Saturday will finally bring a large scale pattern change to the area, as a strong PV anomaly sends a more robust long wave trough toward the Central CONUS and breaks down the desert southwest ridge. This will provide more moisture transport back to the area, while destabilization could still be robust, but provide better deep layer shear. && .AVIATION /12Z TAFS THROUGH 12Z TUESDAY/... Issued at 616 AM CDT Mon Jul 7 2025 Expecting fog for another hour or so along the Missouri River Valley. This will keep visibility under 1SM at STJ through at least 13z, perhaps goes until 14z. VFR cloud bases expected for most of the afternoon, cumulus field likely develops this afternoon. Potential for isolated shower/storm activity from eastern Kansas into Central Missouri, will place PROB30 in TAF sites for this potential. Late tonight, organized system out of Nebraska will move southeast and begin to decay, bringing shower activity to far northwest Missouri. At this time, uncertain if this will reach STJ and the KC Metro terminals, thus will not place in the 12z TAFs. Will continue to watch high resolution model trends through the day. && .EAX WATCHES/WARNINGS/ADVISORIES... MO...None. KS...None. && $$ DISCUSSION...Krull AVIATION...Krull