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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
July 20, 2019 8:18 AM * |
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This is a multi-part message in MIME format... ------------=_1563610737-2024-1928 Content-Type: text/plain FOUS30 KWBC 200818 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 417 AM EDT Sat Jul 20 2019 Day 1 Valid 01Z Sat Jul 20 2019 - 12Z Sat Jul 20 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS THE UPPER GREAT LAKES...PORTIONS OF NEW YORK AND PENNSYLVANIA...AS WELL AS SOUTH DAKOTA... ...Upper Great Lakes... The main focus for flash flooding is tied to the MCS growing CROSSING WI this evening. Ahead of the MCS, the low level flow is transporting 2.00+ inch precipitable water from southern MN (which is between two and three standard deviations above the mean) into southern and central WI. The deep moisture is supporting hourly rainfall rates in excess of 2.00 inches with the activity, though dry air in the mid levels (per the 00z GRB sounding) suggest that hail could be contaminating these values. The MCS maintain itself for at least the next 2-4 hours in the presence of the very strong instability (with MLCAPE values in excess of 5000 J/KG just upstream over southern WI (where surface dew points are in the upper 70s to lower 80s). While hail and wind will continue to be threats with the growing system, there is a window for a flash flood threat (generally before about 20/03z) on the southern edge of the MCS, where a training west to east band of convection could allow for short term training and/or backbuilding. This scenario is supported by the most recent HRRR run, which showed the potential hourly rainfall rates in excess of 2.00 inches over portions of central WI. These amounts appear plausible where training occurs, as the deep warm cloud layer could support efficient rainfall makers before 20/03z. Three hour flash flood guidance is as low as 1.50 inches over central WI, and these amounts could be exceeded, especially where training occurs. Once the MCS matures, it is expected to to become more outflow dominated, and the flash flood threat will diminish once this occurs. Before that time, flash flooding is considered possible. ...Lower Great Lakes... Convective clusters across southeast MI and northwest PA are following axes instability (where MLCAPE values are still between 2000/3000 J/KG) early this evening, spreading out along outflow boundaries. While mid level forcing is not strong in the flat ridge position, the instability is strong enough to support following the outflow boundaries into the late evening hours. The storms are also embedded in an axis of 1.75/2.00 inch precipitable water air, which could support hourly rainfall rates near 2.00 inches. Three hour flash flood guidance values are as low as 1.50/2.00 inches in these areas, and given the deep moisture and place, and the potential for training on outflow boundaries, the threat of flash flooding is expected to continue through through about 20/03z. After that time, the instability is expected to be exhausted, or become more elevated, probably resulting in the activity becoming less organized. This would effectively end the flash flood threat. ...Northern Plains... Convection developing north of a frontal boundary becomes focused on a axis of instability and increasing moisture oriented west to east across portions of SD into far southwest MN, mainly between 20/06z. A subtle short wave over west central WY is expected to cross SD after 20/03z. strengthening the low level flow ahead of it. The low level flow is expected to transports 1.25/1.50 inch precipitable water air in a ribbon of of 2500/3500 J/KG of MUCAPE tracking north over the warm front. After convective initiation, the activity is expected to spread out in a west to east long extending across north central SD into far southwest MN. As the 850-300 mb mean wind becomes better aligned with the propagation vectors, training becomes more likely, especially after 20/06z across western into central SD. The deepening moisture plume (resulting in rising warm cloud heights) could support hourly rainfall rates near 1.50 inches over central SD. Through 20/12z, a few pieces of high resolution guidance (most notably the most recent HRRR) indicated the potential for local 3.00+ inch rainfall amounts, which could occur in areas of training. Three hour flash flood guidance values are generally between 1.00/1.50 inches across much of SD, due to heavy rainfall in the past seven days (where 7 day totals have been as much as 400+ percent above normal). While there is some spread in the high resolution guidance in the placement of the highest rainfall axis (north versus south, due primarily to how they resolve the mid level capping), the ingredients for flash flooding, superimposed over wet soils, necessitated an upgrade to a Slight Risk over much of central SD. The upgraded was collaborated with WFOs UNR/ABR/FSD. Hayes Day 2 Valid 12Z Sun Jul 21 2019 - 12Z Mon Jul 22 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM THE CENTRAL PLAINS EAST INTO THE OHIO VALLEY... ...Central Plains, Mid-MS Valley, OH Valley... A front will continue to slowly move into the Central Plains, Mid-MS Valley into the OH Valley Sunday into early Monday. Models are coming into slightly better agreement on the orientation and timing of the front, especially across the OH Valley. The GFS and now CMC are showing signs, however, of more organized convection as mid-level energy moves atop the aforementioned front. The rest of the model guidance remains weaker with the impulses and the position of the jet axis a bit farther removed to the north and east. Thus the GFS and CMC have higher QPF amounts across eastern KS into northern MO as an organized complex moves from SE NE into MO Sunday evening/night. Given the GFS has shown run to run continuity, the CMC is now showing similar features and GEFS probabilities support the higher QPF amounts, felt it should be incorporated into the model blend. With respect to the ingredients in place, moisture and instability will continues to pool right along and south of the boundary, with precipitable water around 2 inches and MUCAPE values over 3500 J/kg. As previously mentioned, there continues to be uncertainty with respect to the interaction between the mid-level energy and the surface features, thus resulting in questionable organized convection in the central CONUS. At this time, forecasting weak to modest mid-level impulse atop this surface boundary which should promote convection along the front from the Central Plains/Mid-MS Valley across the OH/TN Valley. Areal average QPF generally ranges between 1-2+ inches with locally higher amounts associated with convection. The two main areas of concern are across east KS/northern MO with the potential for organized convection and portions of the OH Valley where FFG are lower. Rain rates could climb over 1.5 inches/hour. The propagation of the convection along the front should limit the flash flood potential as it sinks south. However, if a complex forms as depicted by the GFS, some training could occur. There is enough signal to support isolated to potentially more widespread flash flooding concerns, therefore a Slight Risk was introduced to encompass these regions. ...Southern Rockies... As a front continues to dive south through the Northern Plains, settling into the Central Plains, Mid-MS Valley and OH Valley, a trailing boundary along the Front Range will act as a catalyst for convection during the afternoon into the overnight hours Sunday into Monday. Mid-level high pressure will build overhead with impulses rounding this feature which too will promote vertical motion. At the surface, as the Canadian high builds south into the Northern Plains, easterly flow will enhance upslope flow during the afternoon. Moisture that pooled south of the aforementioned front will bank up against the high terrain with instability of over 2000 J/kg available during the afternoon/evening hours. These factors should promote convective initiation along the windward slopes of the Rockies in CO and NM. Given fairly weak flow, convective cells should have fairly slow storm motion along the slopes with more erratic propagation as they grow upscale. Regardless, expect heavy rainfall is given decent moisture transport across this region. Hourly rain rates may approach 1 inch/hour which is just shy of the one hour FFG (1.5 inches) across this region. Again, given the uncertainty with respect to the evolution and storm motion, feel there could be some locations that see 2+ inches when all is said and done. Models have trended down with QPF for the 00Z forecast suite and thus have trimmed amounts slightly. Though ensemble probabilities, albeit somewhat low, still highlight this region as exceeding 2 inches. Models tend to do poorly within this flow regime/pattern and thus will maintain the Marginal Risk across this area with some refinements made based on WPC QPF. Pagano 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... $$ ------------=_1563610737-2024-1928 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. ------------=_1563610737-2024-1928-- --- 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 130/803 SEEN-BY: 15/0 153/7715 19/33 35 36 38 75 218/700 222/2 229/426 230/150 152 SEEN-BY: 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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