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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
July 18, 2019 4:00 PM * |
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This is a multi-part message in MIME format... ------------=_1563465642-2024-935 Content-Type: text/plain FOUS30 KWBC 181600 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 1159 AM EDT Thu Jul 18 2019 Day 1 Valid 16Z Thu Jul 18 2019 - 12Z Fri Jul 19 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE NORTHERN MID-ATLANTIC AND THE UPPER MISSISSIPPI VALLEY INTO THE GREAT LAKES... ...16Z update... Changes to the previous outlook include adding a Slight Risk from northern MD into southern CT. Moisture tied to the remnants of T.D. Barry was reflected in the morning precipitable water analysis with values ranging between 2.1 and 2.4 inches. A 700 mb trough axis was located from near ALB to IAD to just west of RNK in 12Z RAOB data. Visible imagery showed clear to scattered cloud cover ahead of a mesoscale circulation over northern MD at 15Z with showers already developing near and ahead of it. Thicker cloud cover was in place farther north. However, broad scale lift will be in place over the northern Mid-Atlantic to far southern New England until about 00Z which may allow for breaks in cloud cover and increased instability to develop across northern locations of the Slight Risk later this afternoon. Given wet antecedent conditions skies and a signal from the 12Z hi-res models for 1-3", locally higher, a Slight Risk was added for the 16Z update. Changes elsewhere across the U.S. were minor, based on the 12Z guidance. Otto ...previous discussion follows... ...Upper Mississippi Valley into the Great Lakes... The early Thursday morning convection across portions of the Upper Mississippi Valley will likely undergo post 1200 utc weakening as it pushes east across southern Wisconsin/northern Illinois. This will be followed by another round of potentially organized convection beginning late Thursday afternoon and continuing into Thursday night/early hours of Friday in the vicinity of the west to east oriented frontal boundary expected to stretch across northern Iowa/southern Minnesota into southern Wisconsin. Instability will increase significantly Thursday afternoon in the vicinity of this frontal boundary...with a large region of mu-cape values 3000 j/kg+ as per the arw...nssl wrf and nam and li values -8 to -12. Moist west southwesterly low level flow...With pw values 2 to 2.5+ standard deviations above the mean....may support a period of training of cells in a west to east direction along and to the north of this front. There continues to be some latitude differences with the axis of the heaviest precip this period. The Ukmet...Canadian global and regional are farther north...while the hi res arw...nmmb and nam nest farther to the south along with the href mean. The 0000 UTC EC did trend farther to the south with its heavy totals over the L.P. of MI and is closer to the farther south hi res models and href mean. At the moment...the farther south axis was preferred. Changes to the previous outlook for this period were to orient the marginal and slight risk areas farther to the south and west into far southern MN into southern WI and the southern portion of the L.P. of MI. ...Mid to Upper TN Valley... A marginal risk area was added from far northeast MS...northern AL into central to eastern TN for locally heavy rainfall Thursday afternoon. Neighborhood probabilities from the arw...nmmb and nam nest show probabilities of 10 to 40% of exceeding 1 and 3 hour ffg values across these areas. In addition href probabilities of 1"+ amounts in the 6 hour period ending 0000 utc Fri July 19 are generally in the 40%+ range for 1 inch of precipitation. Not a lot of confidence with details of convection...but with ffg values relatively low across this area from recent heavy rains...additional isolated runoff issues possible. ...Northern Mid Atlantic... Additional convection possible across portions of the Mid Atlantic from far northern VA...across much of MD into eastern PA and NJ. HREF probabilities for the 6 hour period ending 0000 utc for 1" precip are high across this area...mostly 50-90%...with a smaller area of 2"+ amounts in the 50%+ range from north central MD...southeast PA into central to southern NJ. Similar geographical distributions of neighborhood probabilities exceeding 1 and 3 hour ffg values seen in the arw...nmmb and nam nest. Locally heavy rains possible again in the urban corridor stretching from DC to PHL and NYC...with isolated runoff issues possible across these regions. Oravec Day 2 Valid 12Z Fri Jul 19 2019 - 12Z Sat Jul 20 2019 ...THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL FROM THE NORTHERN PLAINS INTO THE CENTRAL GREAT LAKES... ...Northern Plains into the Upper Midwest... Exiting shortwave will be well east into south-central Canada at the start of the forecast period with an unseasonably strong 250mb 130kt jet to the northwest of the frontal zone allowing for deep unidirectional flow in the vicinity of the boundary. Low level moisture flux throughout the day will support steady increase of total PWats along the boundary, but given the strong ridge and deep EML with 30C 85H temps there providing strong capping. Strong insolation and lapse rates with building low level moisture will support extreme instability values over 5000 J/kg, but will need significant upper-level support or deep moisture convergence to break the cap. Toward over night, LLJ is expected to increase to 30-35kts and with weak late evening cooling should spark an overnight MCS that will progress across the frontal zone into MN/N WI. Still, the later start, weaker angle of convergence from the LLJ may limit overall coverage with time. Additionally, given proximity to the core of the mid-level speed max, convection is likely to be fast moving limiting overall duration of heavy rainfall cores in one given location. Still, given the strength of updrafts and depth of available moisture over 1.75" TPWs, increasing through the late period, the sheer rain-rates may be impressive enough to yield short-duration exceedance of FFG values. Additionally, given orientation of LLJ, additional upstream redevelopment that has the chance for repeating suggests isolated areas that may even exceed 3hr FFG values that may have been reduced from Day 1 period. While model guidance has seen a better overall agreement in the placement of the frontal boundary, and therefore corridor of heavy rainfall, areal averages of 1-2" and isolated 2-3" remain spotted across a corridor from central SD into N WI/UP of MI through the remainder of the overnight period into day 3, and the WPC QPF forecast is generally a blend of the global guidance supporting a broad Marginal Risk of Excessive Rainfall across the stationary frontal zone. ...Central Great Lakes Hi-Res CAMs driven by the ARW and NAM-NEST support lingering ongoing convection at the end of day 1 to support outflow as the some shortwave energy anticylconically rounds the NE side of the ridge to drop south across the LP of MI into NW OH/NE PA/W NY. Quick rebuild of instability with early morning insolation will support enhanced redevelopment by midday that will progress southeast with sufficient rainfall rates capable of pressing 1 hourly FFG values (1-1.25"...as such have expanded the Marginal Risk to incorporate the 1-3" totals and isolated flash flooding possible in this area. Gallina Day 3 Valid 12Z Sat Jul 20 2019 - 12Z Sun Jul 21 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE MIDWEST CENTERED ON IOWA... ...Midwest into Michigan... At the start of the forecast period (20.12z), ongoing isentropic ascent across the stationary boundary will be growing upscale to a solid MCS with and MCV crossing the North Central Great Lakes. Unseasonably strong 250mb jet will shifting northeast centered into Ontario, this will provide solid left entrance region dynamics across the Upper Midwest and support height-falls and tail end of shortwave energy to amplify and press eastward across the Dakotas by 21.00z. This will enhance strong post-frontal northerly flow across the Northern Plains and Upper Mississippi River Valley, sharpening the frontal zone both north-south but also vertically. Deep moisture will remain pooled along the lagging frontal zone across SE SD, but with pressing height-falls will quickly back the LLJ more southerly, weakly at 10-20kts near the inflection surface to 850mb trof extending out of the Colorado High Plains. Moisture/instability will build at this intersection/SE into warm sector reaching 3000-3500 J/kg by 21z. By mid-day winds will increase and given nearly 180 degrees of convergence across a steepened boundary, should spark strong/deep convection. Given exiting shortwave/jet energy, the resulting convective complex will be slower moving eastward along the boundary before the frontal zone as a whole drives south. Very strong updrafts, deep moisture should result in strong rain rates and given slightly veered 850mb flow, supporting some weak backbuilding upstream, cross-track/short-term training should exist across SE NEB into S IA and result in areal averages of 2-4" with hourly rates of 2-2.5"/hr yielding a solid potential for scattered flash flooding to result. This is, generally, in line with the 00z GFS/NAM and to account for some variation in timing, a slightly northern ECMWF blend was implemented for WPC QPF. All in all, a broad Slight Risk of Excessive Rainfall was placed from the surface to 850mb inflection point eastward across IA and downstream into S WI and NW IL. A Marginal Risk extends into Central MI, where sandy soil conditions and slightly reduced instability/moisture flux intersecting with the frontal boundary should limit overall coverage for flash flooding, but still remains a non-zero threat given the environment. ...Front Range of Colorado/High Plains of NW Kansas... Global guidance, in particular the GFS continues to suggest as the front drops south across the High Plains, while reduced to further east, remaining moisture banked up along the Range, day-time heating supporting upslope flow has the potential for scattered heavy rainfall producing thunderstorms, with some suggestion of initially slow development moving off terrain with chaotic cell motions and intersections of outflow boundaries that may pose short-term stalled downdrafts capable of isolated rainfall totals of 2-3". The 00z ECWMF trended this direction as well but with a more consolidated complex (likely due to slower timing and allowance for stronger/broader overall development than the earlier developing GFS/NAM). While confidence is not particularly high in one given location, the environment is supportive of this flooding threat and so a Marginal Risk was extended west to incorporate this threat, particularly along the Front Range of CO and SE WY. Gallina 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... $$ ------------=_1563465642-2024-935 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. ------------=_1563465642-2024-935-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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