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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
August 1, 2019 8:18 AM * |
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This is a multi-part message in MIME format... ------------=_1564647510-118394-3230 Content-Type: text/plain FOUS30 KWBC 010818 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 417 AM EDT Thu Aug 01 2019 Day 1 Valid 01Z Thu Aug 01 2019 - 12Z Thu Aug 01 2019 ...THERE IS A MODERATE RISK OF EXCESSIVE RAINFALL OVER PORTIONS OF EASTERN KANSAS, WESTERN MISSOURI, AND FAR NORTHEAST OKLAHOMA... ...Central Plains... Short wave energy tracking over the ridge into the eastern portion of the Central Plains interacts with deepening moisture on the nose of a strengthening low level jet and instability to form an MCS that tracks across eastern KS into western MO, mainly after 02/06z. While there is generally good model agreement with the overall synoptic setup, there continues to be some west/east differences with respect to the placement of the highest rainfall axis, which certainly could lead to large repercussions in terms of the greatest flash flood risk. In an attempt to mitigate these differences, both the WPC QPF and Excessive Rainfall Outlook were again based on a multi model blend. Remnants of an MCS crossing eastern KS into western MO early in the period could produce locally heavy rainfall, though will be on the wane as the low level jet weakens and the elevated instability become exhausted. As the morning debris cloudiness exits, an axis of 2000-3000 J/KG of MLCAPE is expected to develop along and north of the front extending across KS into far eastern OK. The instability should be sufficient to support scattered convection in the instability axis before 02/00z, generally on the edge of the mid level capping. The storms are expected to be scattered enough to pose a low end flash flood threat. As short wave energy tracking from MT and the western Dakotas drops southeast, the low level jet backs and strengthens over eastern NE into eastern KS. The 30-40 knot low level southerly flow injects 2.00+ inch precipitable water air (pre-convective environment) into the instability axis. In the presence of synoptic scale lift associated with the short wave energy, an MCS is expected to form over eastern NE between 02/00z and 02/06z, which moves southeast along the edge of the cap. On the southwest side of the MCS, where the propagation vectors align with the 850/400 mb flow, resulting in training. Hourly rainfall rates aoa 2.00 inches are expected where training occurs, before the MCS tracks more southerly and picks up more forward momentum (becomes more outflow dominated). Now fully within the window of the high-res CAMs, there is a multi-model signal for localized 3-6+ inches of rainfall during the day 1 period (which includes residual rain from early today). Based on the most recent MCS, three hour flash flood guidance values have now come down considerably across portions of eastern KS into far western MO -- with a large area below 2.00" and a narrow stripe of 1.00" or less. Based on the antecedent wet conditions with additional heavy rainfall forecast, per collaboration with affected WFOs a Moderate Risk was hoisted over this area. ...Southwest/4 Corners Region/Rockies/Central High Plains... There are two areas of concern for flash flooding across the Southwest into Rockies and central-northern High Plains during Day 1. The first is across portions of AZ/southeast NV into UT and far western CO. The best synoptic scale forcing will exit this region early, however deeper moisture and instability will linger behind the short wave energy. Cloudiness early could affect how quickly instability rebounds across the area, but differential heating would suggest that the terrain could support convective initiation first during the late morning into early afternoon. Between 500-1500 J/KG of MLCAPE is expected along the terrain from central AZ across UT into western CO, peaking between 01/18z and 02/00z. Storms developing in the axis of instability tap the 1.00-1.25 inch precipitable water air in place, which could support hourly rainfall rates nearing an inch (per the 00z high-res CAMS) over the terrain. These rates are high enough to support an isolated to widely scattered flash flood threat in these areas, mainly through 02/06z. Based on the above, a Marginal Risk was stretched from central AZ and portions of western NM up through western and central CO. The second area of concern is across eastern CO-WY into the high plains of western NE-SD. As a frontal boundary becomes banked up along the Front Range in CO, the low level east to northeast flow transports 1.00-1.25 inch precipitable water air (which is about two standard deviations above the mean) across eastern CO-WY into far western NE-SD. Model soundings showed a ribbon of 1000-2000 J/KG of MLCAPE from the Front Range into the High Plains, as convective initiation is expected after 01/18z. The upslope flow could result in slow cell motions with the storms in the terrain, which track across the plains after cold pools become established. Before that occurs, the deepening moisture could support hourly rainfall rates nearing 1.00" (which is depicted by most of the 00z high resolution guidance), especially across eastern CO and western NE. Considering that three hour flash flood guidance is as low as 1.00-1.50 inches over portions of northeast CO, eastern WY, and western NE-SD, an enhanced (Slight) flash flood risk exists over this area. ...Lower Mississippi Valley/Southeast/Mid Atlantic... Deep moisture and instability pool along a frontal boundary across the Mid Atlantic states during Day 2. As the best mid level support for the frontal shears out to the north across New England, the front is expected to slow, and could become quasi stationary across portions of NC into after 01/18z. The moisture and instability should be sufficient to support at least scattered storms along and south of the front, where MLCAPE values are expected to range between 1500/2500 J/KG. Increasing warm cloud depths could allow storms to be fairly efficient rainfall makers, and given the 1.75-2.00+ inch precipitable water axis along the front should support storms capable of producing hourly rainfall rates near 2.00 inches from the mid Atlantic, much of the Southeast, and toward the central Gulf Coast ahead of the stationary surface front. Storm motions could be less than 10 knots, especially across western VA/western NC, which may foster an environment for short term training and cell mergers. There continues to be multi-model support for local 3.00+ inch rainfall amounts, particularly where training occurs. Three hour flash flood guidance values are generally between 2.50/3.50 inches, and training in the higher moisture airmass could allow some locations to approach these values. Based on this, a Marginal Risk was placed across these areas. Hurley Day 2 The Day 2 outlook will be updated by 0830Z. Day 3 The Day 3 outlook will be updated by 0830Z. Day 1 threat area: https://www.wpc.ncep.noaa.gov/qpf/94epoints.t... Day 2 threat area: https://www.wpc.ncep.noaa.gov/qpf/98epoints.t... Day 3 threat area: https://www.wpc.ncep.noaa.gov/qpf/99epoints.t... $$ ------------=_1564647510-118394-3230 Content-Type: text/plain; charset="US-ASCII" Content-Disposition: inline Content-Transfer-Encoding: 7BIT = = = To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM. ------------=_1564647510-118394-3230-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) SEEN-BY: 104/57 106/201 116/18 120/302 331 124/5013 5014 5015 5016 5017 5018 SEEN-BY: 130/803 15/0 153/7715 19/33 35 36 38 75 218/700 222/2 229/426 230/150 SEEN-BY: 152 2320/105 107 240/1120 250/1 261/100 38 266/512 267/155 275/100 SEEN-BY: 282/1031 1056 291/1 111 320/119 219 34/999 340/400 342/13 3634/12 SEEN-BY: 387/21 396/45 5020/1042 712/848 801/189 90/1 |
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