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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
July 27, 2019 8:29 PM * |
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This is a multi-part message in MIME format... ------------=_1564259390-118394-1235 Content-Type: text/plain FOUS30 KWBC 272029 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 428 PM EDT Sat Jul 27 2019 Day 1 Valid 16Z Sat Jul 27 2019 - 12Z Sun Jul 28 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL OVER PORTIONS OF THE NORTHERN PLAINS AS WELL AS PARTS OF THE CENTRAL AND SOUTHERN ROCKIES... ...Southern Louisiana and Far Southeast Texas... Daytime heating, in addition to deepening moisture along a weak northward moving surface boundary will likely support increasing shower and thunderstorm coverage across the region this afternoon. Although flash flood guidance values are relatively high across the region (greater than 3-inches for 1-hr), weak steering flow through the low to mid levels is expected to support slow moving cells, raising the potential for locally heavy amounts producing runoff concerns. Within the Marginal Risk area, HREF 40km neighborhood probabilities for the 12-hr period ending at 06Z are generally 50 percent or greater for amounts exceeding 2-inches. ...Northern Plains... The upper ridge over the northern-central Rockies will flatten somewhat today, in response to the shortwave trough skirting the northwest U.S./southwest Canadian border along with a convectively-aided vort lobe that will drop into the high plains during the evening. Strengthening s-se low-level flow ahead of the aforementioned vort and associated surface low will help draw a more moist and unstable airmass farther northwest and into eastern WY and southeast MT. MUCAPES climb between 1500-2500 j/kg during peak daytime heating hours this afternoon, then are expected to drop below 1000 j/kg overnight. PWs climbing to 1.25" across the high plains and to 1.50+ farther east are modestly anomalous for late July (around 2 standard deviations above normal). Relatively high-based convection with DCAPEs ~500 j/kg or greater, along with the degree of vertical wind shear, will promote fairly swift cell progression. However, the high-res CAMs show the potential for renewed convection along/ahead of the surface warm/stationary front, as the compact area of difluent upper flow pushes rather slowly eastward overnight. The Slight Risk area delineates areas of lower FFG -- i.e. 1" or less within one hour and 1-1.5" within 3 hours. The latest HREF and experimental HREF both depict the highest exceedance probabilities across a portion of southwest SD between 21-00Z -- with 50-60% or greater probabilities that 3 hourly QPF will exceed the current FFG. ...Central and Southern Rockies/Intermountain West... Moisture from the Central Plains and instability over much of the terrain and plains of CO and NM combine to produce storms with heavy to excessive rainfall Saturday. There was generally good model agreement with respect to the synoptic setup and placement of the highest rainfall amounts, so the WPC QPF and Excessive Rainfall Outlook were based on a multi model blend of 00Z guidance. A low-level east to southeast flow continues to transport 1.00-1.25 inch PWs across the plains of CO and NM into the terrain from the Front Range in CO into the Sangre de Cristo Mountains of CO into northern NM. Underneath a flattening mid-level ridge, modest instability will be present, as the models continue to advertise MUCAPES between 1000-1500 j/kg along the terrain, and model soundings show the cap breaking in the afternoon. After the convection develops, it will shift slowly southward along the terrain into the plains, as the mid-level flow is fairly weak under the ridge. Slow moving storms along the terrain fosters an environment favoring cell mergers and short term training, which in turn results in hourly rainfall totals in excess of an inch. Seven day rainfall totals over portions of eastern CO have been 300+ percent of normal, with three hour flash flood guidance values as low as 1.00/1.50 inches. Given the moist antecedent conditions, and the potential for high rainfall rates with slow moving cells, the Slight Risk was maintained over portions of eastern NM into central NM. Pereira/Hurley/Jackson Day 2 Valid 12Z Sun Jul 28 2019 - 12Z Mon Jul 29 2019 ......THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM A PORTION OF THE NORTHERN PLAINS TO LAKE SUPERIOR... ...Northern Plains to Upper Great Lakes... Deepening moisture and increasing instability ahead of a short wave trough moving from SD into MN before merging into a long wave trough crossing the Canadian Prairies feeds convection capable of producing excessive rainfall Sunday into Sunday night. There remained good model agreement with the large scale pattern, though time and position differences with the surface low made for differences with the QPF. WPC QPF and the Excessive Rainfall Outlook were based mainly on a compromise between the 12Z ECMWF and 12Z NAM Nest. The 12Z GFS remained faster a weaker with the surface low compared to consensus. Convection is expected to be ongoing as it tracks from SD into MN Sunday morning. This activity will be reinvigorated as the low deepens through Sunday as it tracks toward Lake Superior. The developing convection is fed 1.75 to 2 inch precipitable water air (which is 2.5 standard deviations above the mean) on a 30 to 40 knot low level southwest flow. 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. The amount of instability is uncertain with at least 500 to 1000 J/Kg MUCAPE expected. This airmass could support hourly rainfall totals near 1.5 inches and there is a multi model signal for 2 to 2.5 inches of rainfall over central MN to the Lake Superior shore. Three hour flash flood guidance values are generally 1.5 to 2.5 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 maintained over much of southern and central MN into northern WI and the western UP along with some more of eastern SD to cover the ongoing storms in the morning. ...Central Plains... A cold front trailing the shortwave trough crossing the northern plains will push into IA/MO Sunday night. Southwesterly low level flow ahead of the trough will bring PWs up to 1.75 to 2 inches Sunday night from eastern KS to eastern IA. Scattered convection developing late Sunday afternoon over eastern NE/western IA could organize and track east while propagating south given westerly mean flow and northerly propagation vectors. Despite 3hr FFG of 2.5 to 3 inches, localized repeating cells could raise flash flood concerns and a Marginal Risk was raised that extends to across IA to southwest MO. ...New Mexico... The mid-level ridge eases to the west Sunday 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 near an inch 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 maintained over the eastern slopes of central NM mountains. ...Northeast... Moisture and instability south of a frontal boundary extending from southern Ontario into northern ME could feed convection capable of producing heavy rainfall Sunday afternoon and evening. 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 during peak heating. 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. No excessive area was assigned again, but given some ingredients, a Marginal Risk could be needed here eventually. Hayes/Jackson Day 3 Valid 12Z Mon Jul 29 2019 - 12Z Tue Jul 30 2019 ...THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL OVER PORTIONS OF THE SOUTHERN ROCKIES AND SOUTHWEST AS WELL AS THE LOWER MISSISSIPPI VALLEY... ...Southern Rockies/Southwest... As the mid-level ridge reasserts itself over the Southwest states, the monsoonal flow starts to become reestablished over the Southwest and Southern Rockies Monday. While the best thrust of moisture is expected across southern AZ (where precipitable water values rebound to near 1.75 inches Monday night), the best instability is expected across the Southern Rockies into the Sangre de Cristo Mountains. An axis of 500/1000 J/KG of MLCAPE is expected to develop from the Front Range of the Rockies in CO into northern and southwest NM, peaking Monday evening. The developing storms will tap 1.00 inch precipitable water air on a 10/15 knot low level southeast flow to produce local 1.00 inch rainfall amounts over the higher terrain, where the storms will be almost stationary against the upslope flow. Once maximum heating occurs, the storms will begin to move slowly west northwest with the weak mid-level flow, retaining the potential to produce hourly rainfall rates between 0.50/1.00 inches away from the terrain. Three hour flash flood guidance values are as low as 1.50 inches in these areas, so a low end flash flood threat is expected. Based on the above, a Marginal risk was placed over the higher terrain and adjacent locations. Further west across southeast AZ, the moisture plume from northern Mexico possesses more moisture than CO/NM, but instability could end up being the limiting factor for a more organized flash flood threat. Scattered storms could produce local 1.00 inch rainfall amounts over the higher terrain before moving out into lower terrain, but the general lack of forcing would suggest that the storms should be short lived. Slow cell motions under the ridge position could allow for cell mergers and short training. Based on the above, the Marginal Risk was maintained from the San Juans to much of the higher terrain in NM to the southeast corner of AZ. ...Lower Mississippi Valley... Moisture and instability extending ahead of a slowing cold front are expected to feed convection that could produce locally heavy rainfall from the Lower MS Valley into the OH Valley Monday into Monday night. The best moisture feed ahead of the front is expected across MO into AR/OK and LA during and just after peak heating. Model soundings showed an axis of 1500/2500 J/KG of MLCAPE coincident with the deepest moisture, and developing storms are expected to drop southeast with the mid-level flow. There is a model signal that a cold pool could form with storms over AR, resulting in the storms dropping south into northern LA as they weaken. Three hour flash flood guidance values are generally above 2.50 inches from MO into northeast OK, and above 3.50 inches over much of the Lower MS Valley. Given the organized thunderstorm threat, raised a Marginal Risk for southern MO/much of AR and the lower MS Valley with an understanding that this threat area should become more focused in the future. Hayes/Jackson 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... $$ ------------=_1564259390-118394-1235 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. ------------=_1564259390-118394-1235-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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