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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
July 20, 2019 8:31 AM * |
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This is a multi-part message in MIME format... ------------=_1563611514-2024-1938 Content-Type: text/plain FOUS30 KWBC 200831 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 430 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 PORTIONS OF THE CENTRAL PLAINS INTO THE MIDDLE TO UPPER MISSISSIPPI VALLEY... ...Lee of the Central Rockies across the Central Plains...Mid to Upper Mississippi Valley into the Lower Great Lakes... The surface frontal boundary stretching from the lee of the Central Rockies...east northeastward across the Central Plains and into the Mid to Upper Mississippi Valley and Lower Great Lakes will be a focus for potentially active convection this period. This frontal boundary will remain along the southern edge of the westerlies where upper difluence maxima will accentuate lift in an axis of widespread instability along this front...li values -4 top -12...mu-cape 2000-4000+ j/kg. Strong frontal convergence expected along the length of the front with inflow of pw values 1 to 2.5+ standard deviations above the mean expected through the period. Given the above...there will likely be widespread area of heavy to locally excessive precipitation this period in the vicinity of this front. The slight risk area was drawn to cover the axis of higher href neighborhood probabilities...40 to 60%+ of 2"+ along this front. With respect to the previous outlook for this period...the slight risk was expanded farther to the west southwest across portions of the Central Plains into the lee of the Central Rockies. ...Mid to Upper Tennessee Valley into the Central Gulf Coast... Model consensus is for additional heavy rain potential this period stretching from the Central Gulf coast...northeastward into the Middle to Upper TN Valley/Southern Appalachians in a weak mid to upper level shear axis. PW values expected to remain 1 to 1.5+ standard deviations above the mean and instability is forecast to build to 1000-1500 j/kg by Saturday afternoon. Expect convection to blossom quickly Saturday afternoon and dissipate shortly after sunset. FFG values are relatively high across this region...but there is the likelihood of additional heavy rains falling across areas that received heavy rains in the past 24 hours. This may result in isolated runoff issues. Oravec 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 Valid 12Z Mon Jul 22 2019 - 12Z Tue Jul 23 2019 ...THERE IS A SLIGHT RISK FROM THE TN VALLEY AND SOUTHERN APPALACHIANS NORTH INTO PORTIONS OF NEW ENGLAND... ...TN Valley/Appalachians/Northeast... A front will slowly approach the TN Valley, Appalachians Mountains moving through the Northeast Monday into Monday night as a deep trough digs south across the Great Lakes. Moisture and instability will pool along and just south of this boundary. Precipitable water values will climb to over 2 inches across portions of the TN Valley, banking up against the western slopes of the Appalachians and into the mid-Atlantic region Monday afternoon/evening. This is over 2 standard deviations above the mean. Pockets of instability over 2000 J/kg was noted within the model soundings, especially across the mid-Atlantic region. Within the mid-level, impulses will continues to round the aforementioned trough. Upper level jet axis will pivot to the northeast from Ontario into Quebec positioning the right entrance region across the central Appalachians into the Mid-Atlantic and Northeast by later in the period. All this to say mid/upper level support is plentiful and with such a strong front, this would only suggest widespread and potentially multiple sounds of shower/thunderstorm activity, especially Monday afternoon through the evening hours. The main area of concern with respect to heavy precipitation will be from the expected pre-frontal convection which will impact portions of the TN Valley into the central/northern Appalachians. Areal average precipitation in this area is around 1-2 inches with higher values possible with training as the mean wind becomes better aligned with the corfidi vectors. With sensitive soils across much of this region as evident by FFG as low as 0.75 inches, felt it advantageous to introduce a Slight Risk from the TN Valley/southern Appalachians north into New England. Given such a strong synoptic pattern, especially for this time of year, and the multi-model signal for very heavy precipitation (widespread 2+ inches), feel a Moderate Risk may be warranted if QPF increases and model guidance comes into better agreement on placement. A Marginal Risk extends as far south as the Lower MS Valley who have seen quite a bit of rain with Barry and are still rebounding from flash flooding. Pagano 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... $$ ------------=_1563611514-2024-1938 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. ------------=_1563611514-2024-1938-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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