


Area Forecast Discussion
Issued by NWS Kansas City/Pleasant Hill, MO
Issued by NWS Kansas City/Pleasant Hill, MO
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724 FXUS63 KEAX 111123 AFDEAX Area Forecast Discussion National Weather Service Kansas City/Pleasant Hill MO 623 AM CDT Tue Mar 11 2025 ...Updated 12z Aviation... .KEY MESSAGES... - Slightly Cooler Today, But Still Warm - Above Normal Temperatures Through Friday - Strong System Moves Through Friday and Saturday - Conditional Severe Thunderstorm Threat Friday; Potential For Dry Air To Quickly Erode Thunderstorm Chances With This System && .DISCUSSION... Issued at 350 AM CDT Tue Mar 11 2025 Split flow regime still ongoing across North America with polar jet streak across the Canadian Prairie Provinces and Northern Great Lakes Region, with stronger subtropical jet streak over the Gulf into the eastern Pacific. Subtle H5 height falls over the past 12 hours have moved southward with the northern system, but no substantial forcing has made it close to our area. In general perspective, the mid-level flow while brisk is still mostly zonal. Strong PV anomaly off the southwest coast of the CONUS will provide a few troughs and strong vorticity maxima over the next couple of days through this mostly zonal flow regime. For today though, the system in the Northern Great Lakes region is dragging a cold front across much of the upper Midwest, and this is slowly moving southward across Iowa. This is expected to provide a few hours of northerly flow, especially for our northern Missouri Counties. Areas south of Interstate 70 may still hold onto a southerly wind component. Surface anticyclone over the Gulf continues to prevent any notable moisture transport into our region, so despite the cool thermal boundary, cloud development will be very limited if anything develops at all. Temperatures across northern Missouri today will be in the lower 60s as this boundary moves southward, with a gradual increase into the mid and upper 70s for areas south of Interstate 70. NBM inner-quartile spread for any particular location is only about 4F, therefore indicating higher confidence in the placement of this boundary. Greatest variability is between Hwy. 36 and Interstate 70, but in general most points are expected be in the upper 60s to perhaps lower 70s. With clear skies allowing for insolation most of the afternoon, expecting another day of strong boundary layer mixing, which will again reduce dewpoints into the lower and mid 30s across the area. This yields relative humidity values in the lower 30s through the afternoon. Winds today will not be as gusty as Monday, therefore fire weather related concerns are not as high as they were yesterday. Fuels are still dry though, so there is still some limited fire weather risks for this afternoon. Through the evening, first localized vorticity maxima moves through the flow, and provides weaker dCVA across the Central Plains that will prompt some lift to lower surface pressure. The mid-level support is not broad enough to develop a robust surface cyclone, but it should be enough to prompt a flow response to southwesterly, enhancing a WAA regime heading into the evening and prevents further southward movement of the thermal boundary that will keep Northern Missouri cooler this afternoon. Expecting some nighttime cooling with clear skies, but not expecting temperatures to drop much below 45 degrees given the change to WAA. Wednesday and Thursday, more notable H5 trough is progged to eject across the Central Plains ahead of the strong PV anomaly moving closer to the southwest California coast. The dCVA into the Plains will deepen the weak surface cyclone and strengthen southwesterly flow across our area, as well as creating modest mid-level ridge axis that passes across the lower Missouri River Valley. This is expected to boost temperatures back into the 70s for most of the area. During this time, the flow remains more southwesterly than southerly, meaning we are still missing out on stronger moisture transport from the Gulf. As this system progresses, the better CVA tracks toward the eastern portions of the southern Plains into the lower Mississippi River Valley. The H5 height falls and enhanced kinematics only make it as far north as the Ozarks region, not climbing much further north than Interstate 44. Eventually by Thursday, modest H5 height falls start, but again the better forcing and moisture supply remains well south of the area. Therefore, will maintain a dry forecast for our area. GEFS and other ensemble suites limit probabilities for any measurable precipitation in our southeast to under 15 percent. Given the dry boundary layer and very dry antecedent conditions over the several days, hard to see any activity developing unless this short-wave makes a dramatic shift northward. Attention than turns to Friday and Saturday, as the main PV anomaly finally moves into the CONUS and brings a deep trough across the Intermountain West. Over the past several days, had noted output from NAEFS and other systems that provide context to extreme values of various parameters were showing higher potential for extreme H5 height minima as well MSLP with this system, and current medium range deterministic guidance still depicts an overall synoptic pattern that supports this. During the very early Friday morning period, 100+kt H5 jet streak starts to move around the trough axis, allowing this deep trough to acquire a negative tilt. This setup will favor robust dCVA into the Front Range, providing plenty of lift for surface cyclogenesis. Surface pressure falls will quickly spread eastward across the Plains into the lower Missouri River Valley with this setup, increasing southerly flow across the area, and begins to increase theta-e advection. Pressure gradient drastically increases, and this will provide very gusty winds throughout much Friday, even in periods without precipitation. Depending on how much moisture transport we realize, there will likely be a period of elevated fire weather concerns with this system. Would imagine that at some point there should be some degree of isentropic ascent. Overall, expecting an expansive warm-sector across the area with respect to temperatures. Inner-quartile spread amongst various ensemble suites are between 78F and 82F degrees for most points in our forecast area. With this highly dynamic system, the backside of this will start to pull in drier air, but with daytime heating, should weaken the thermal gradient as it progresses across the Plains. Current guidance is suggesting this airmass behind the boundary to characterized by dewpoint depressions of over 30F, and in some ensemble members over 40F from the surface up to around 700mb. This will be more a Pacific Cold front type of feature or a psuedo dryline of sorts, given the amount of mixing that appears that could be going on with the robust momentum that is present. This feature is the reason why both the overall thunderstorm threat and severe weather threat remains very conditional. If the dry air wins out, we may just end up with strong winds and a few light showers or sprinkles. As this system gains speed, this boundary is likely to surge east very quickly throughout the day. And as it does, will quickly erode boundary layer moisture, as well as quickly reduce any type of SBCAPE or MLCAPE. Current deterministic GFS and ECMWF depict around 500-700 J/kg of MLCAPE in the warm sector after 18z on Friday. That may not seem like much, but given the strong mid-level support and forcing along the boundary, that will be all you need to get a thunderstorm if we are able to realize it. However, respective ensemble guidance though remains split on how fast this moisture discontinuity boundary pushes through, with some members clearing this before peak heating on Friday, resulting in no destabilization ahead of the most favorable forcing for our CWA. Therefore, ensemble probabilities for CAPE above 1000 J/kg remains very low, while a threshold of 500 J/kg is around 50 to 60 percent, concentrated mainly east of Interstate 35. Areas east of Highway 63 hold onto higher probabilities for severe weather, especially toward the Ohio River Valley as the window for destabilization is much longer. Based on that, if this system does not surge too quickly, deep layer shear of 55+ kts will be capable of organizing storms Friday late afternoon into the early evening if the moisture is there for it. Throughout the open warm sector, could support a period of supercell development, but as the cool/dry boundary moves eastward, deep layer shear becomes more parallel to the overall forcing, which would favor some type of MCS, could even be enough organization for a QLCS. Therefore, all severe weather hazard types right now look to be possible if thunderstorms are realized at all, we will see starting Thursday morning how the CAMs handle the evolution of this system, might there be any kind of differential heating boundary present if cloud cover develops in isentropic upglide. This will make is easier to pinpoint potential mesoscale outcomes. If we do not see enough instability, but moisture transport with isentropic ascent occurs before this moisture discontinuity boundary moves through, could see non- thunderstorm rain shower activity early Friday. Current ensemble members paint about at 30-40 percent chance for rain measurable across most of the area, with above 60 percent closer to Hwy. 63. For a threshold of 0.10 inches of QPF or greater, about 30-40 percent along and east of Hwy. 63, but rapidly decreases as you move westward. A lot of ensemble members keep the KC metro dry with this system. As mentioned in the beginning of this section, gusty non- thunderstorms winds are still expected given how strong this system is. If this dry surge occurs during daylight, we could also see fire weather issues for a few hours, especially with wind gusts above 40 MPH. Finally, there will be a lot of cold air on the northwest side of the system. As for right now, all the stronger lifting mechanisms are progged from northern Nebraska into the northern Plains, and this is where the highest wintry precipitation probabilities are at. Our far northern Missouri Counties may become cold enough Saturday morning to support frozen precipitation, but QPF remains very light by the time temperatures drop below freezing. Thus, not overly concerned about wintry precipitation impacts for our area at this time. Secondary trough axis moves through Sunday into Monday, and could provide some light precipitation activity but moisture content may not be there to actually produce it. Stronger ridge then develops across the Central CONUS through the start of next week and should send temperatures back into the 60s, perhaps 70s across our area. && .AVIATION /12Z TAFS THROUGH 12Z WEDNESDAY/... Issued at 621 AM CDT Tue Mar 11 2025 Clear skies will lead to VFR conditions across the area for most of the day. Winds out of the southwest between 5 and 10 kts. Winds may be more northeasterly in northern Missouri. VFR cloud bases may move in early Wednesday morning. && .EAX WATCHES/WARNINGS/ADVISORIES... MO...None. KS...None. && $$ DISCUSSION...Krull AVIATION...Krull