Message Area
Casually read the BBS message area using an easy to use interface. Messages are categorized exactly like they are on the BBS. You may post new messages or reply to existing messages! You are not logged in. Login here for full access privileges. |
Previous Message | Next Message | Back to National Weather Network <-- <--- | Return to Home Page |
|
||||||
From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
July 27, 2019 8:01 AM * |
|||
This is a multi-part message in MIME format... ------------=_1564214490-118394-1123 Content-Type: text/plain FOUS30 KWBC 270801 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 400 AM EDT Sat Jul 27 2019 Day 1 Valid 01Z Sat Jul 27 2019 - 12Z Sat Jul 27 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL NEAR NEW MEXICO & THE WASATCH MOUNTAINS OF UTAH... ...Central and Southern Rockies and Great Basin... Convection over the Colorado/New Mexico Rockies has been able to fire in an area where Precipitable Water values were in the 1.0 to 1.25 inch range owing to the elevated heat source of the terrain and low level upslope/convergent flow. This, combined with moderate instability, will continue to lead to locally heavy rainfall with rates in excess of an inch per hour. will lead to locally heavy rain, perhaps as high as 2" an hour. Areas with prior showers/storms have reduced 3-6 hr flash flood guidance, between 1-1.5 inches on 3 hours, thus the need for a slight risk area in the terrain of southeast CO across NM, including the Sangre de Cristo and Manzano Mountains. A shortwave trough moves east from California into Intermountain West today. As a result, the deep high centered over the four corners region will shift south and west in time. This will send further mid-level impulses around the ridge and help promote widespread shower/thunderstorm development from over NV/UT due to insolation within the disturbance's dry slot, currently shifting northward across central NV and southern UT. Locally heavy rain is possible where cell mergers occur, up to 2" an hour. NAM forecast soundings show low directional shear today, promoting localized training. An upgrade to a slight risk was coordinated this morning with the SLC/Salt Lake City forecast office. ...Central Plains... Convection flared up again from the Western High Plains to the Central Plains along and near a wavy and poorly defined boundary. Until the storms dissipate shortly after sunset, storms will be in an environment where CAPE values early this evening were in excess of 1500 J per kg but forecast to drop to 500 - 750 J per kg by 06Z. Southerly flow at 850 mb will be feeding moisture into the area, allowing for a few cells to produce intense rainfall and isolated flash flooding problems. Once cells begin to move, they should be generally be moving southeasterly paralleling the low level thermal field. The 12C isotherm still seemed to be working as a guide for its movement. Maintained the Marginal Risk area...thinking that the better risk of heavy rainfall was over the Sandhills...and rainfall rates should be tapering off as the cells move out the that area. ...Western Great Lakes to Upper Midwest... Expanded the Marginal Risk area southward to encompass a second area of active convection that was clipping the northern portion of the Twin Cities and areas downstream into Wisconsin. Several rounds of convection have been moving into an area with an unstable atmosphere despite fairly modest moisture. The 00Z sounding from KMPX showed over 4000 J per kg with under 1 inch of Precipitable Water...with the storms being fed moisture on southwesterly flow at the lowest levels. Farther north...little change made to the on-going Marginal Risk area over parts of the Minnesota Arrowhead into parts of the western Great Lakes. A 700 mb shortwave rotating under the upper trough in southern Canada combined with well defined 700 mb convergence and theta-e advection has resulted in convection over parts of the Arrowhead which has produced locally heavy rainfall. That convection will continue eastward southeast across the UP of MI. The high res WRF ARW/ARW2, NAM Conus Nest, and NSSL WRF all forecast local amounts of 1-2" of rain which was near flash flood guidance, though only in a couple random locations. While the storms should be progressive given the deep layer flow around the southern Canadian trough, some brief back-building of storms can't be ruled out which leads to localized flash flooding. Bann Day 2 Valid 12Z Sun Jul 28 2019 - 12Z Mon Jul 29 2019 ......THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM THE UPPER MISSISSIPPI VALLEY INTO THE UPPER GREAT LAKES... ...Northern Plains across the Upper Mississippi Valley into the Upper Great Lakes... Deepening moisture and increasing instability ahead of a long wave trough and associated cold front crossing the Northern Plains into the Upper MS Valley and Upper Great Lakes feeds convection capable of producing excessive rainfall during Day 2. There was generally good model agreement concerning the overall synoptic setup (outside of the 00z GFS, whose solution continues to be weaker with the frontal passage), so the WPC QPF and Excessive Rainfall Outlook were based on a multi model blend. Convection is expected to be ongoing (and weakening) as it tracks from SD into MN during the first part of Day 2. Cloudiness associated with weakening activity could delay heating across MN into WI during the morning hours. After the clouds break, instability climbs to 2500/3550 J/KG of MLCAPE stretching from eastern NE/IN across southern MN into WI and the northern portion of the LP of MI ahead of the front and long wave trough, peaking between 29/00z and 29/06z. The developing convection is fed 2.00+ inch precipitable water air (which is about two standard deviations above the mean) on a 25/35 knot low level southwest flow during this time frame. Lift ahead of the long wave trough should allow the convection to expand in coverage, and become better organized as it moves over southern and central MN into northern and central WI. Simulated radar imagery from the 00z NAM CONUS Nest indicated that rounds of progressive convection cross MN and WI, which could result in areas with repeating cells. This airmass could support hourly rainfall rates near 1.50 inches (as shown by the 00z NAM CONUS Nest), and there is a multi model signal for 2.00/2.50 inches of rainfall over central MN into northern WI, closest to the best instability gradient. Three hour flash flood guidance values are as low as 1.50 inches over portions of MN into WI (including the Minneapolis metro area), and these numbers could be exceeded where convection trains ahead of the front. Based on this, a Slight Risk was placed over much of southern and central MN into northern WI. ...New Mexico... The mid level ridge eases to the west during Day 2, and the monsoon flow becomes suppressed temporarily. However, deeper moisture and instability across eastern NM could support convection with heavy to locally excessive rainfall, especially in the afternoon and evening hours. Storms developing in an axis of 1000 J/KG of MLCAPE are expected to tap 1.25 inch precipitable water air (which is about two standard deviations above the mean) in place over eastern NM to support convection capable of producing hourly rainfall rates near an inch (in agreement with the 00z NAM CONUS Nest) along and just west of the terrain (as the storms moving slowly to the west with the mid level flow). Three hour flash flood guidance is generally near 1.50 inches, and it is possible that these amounts could occur where storms merge or where short term training occurs. Since there is some spread in coverage of storms during Day 2 (as instability could be a limiting factor for a more organized flash flood threat), a Marginal Risk was placed over a portion of east central NM. ...Northeast... Moisture and instability south of a frontal boundary extending from southern Ontario into northern ME could feed convection capable of producing heavy rainfall during the afternoon and evening hours of Day 2. Weak short wave energy in the mid level flow south of the front is expected to interact with 1.25/1.50 inch precipitable water air and 1000/2000 J/KG of MLCAPE stretching from western NY/western PA across NY state into northern and central New England, mainly in the 28/18z to 29/03z time frame. The weakly difluent flow ahead of the short wave could allow small clusters of storms to move across this area, generally following the best instability axis, but much of the activity is expected to be fairly short lived in nature. For the most part, the mid level flow should be sufficient to keep the convection progressive, limiting an organized flash flood threat. In addition, much of the area has been fairly dry over the past seven days, with three hour flash flood guidance values generally over 2.50 inches. While there could be some locally heavy rainfall, the overall threat of organized flash flood threat seems to be low. With this in mind, no excessive area was assigned, but if later model solutions indicate a better threat, a Marginal Risk could be needed here in later forecast. Hayes 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... $$ ------------=_1564214490-118394-1123 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. ------------=_1564214490-118394-1123-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
||||||
|
Previous Message | Next Message | Back to National Weather Network <-- <--- | Return to Home Page |
Execution Time: 0.1027 seconds If you experience any problems with this website or need help, contact the webmaster. VADV-PHP Copyright © 2002-2024 Steve Winn, Aspect Technologies. All Rights Reserved. Virtual Advanced Copyright © 1995-1997 Roland De Graaf. |