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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
July 15, 2019 8:08 PM * |
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This is a multi-part message in MIME format... ------------=_1563221610-51656-11344 Content-Type: text/plain FOUS30 KWBC 152008 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 407 PM EDT Mon Jul 15 2019 Day 1 Valid 1822Z Mon Jul 15 2019 - 12Z Tue Jul 16 2019 ...THERE IS A MODERATE RISK OF EXCESSIVE RAINFALL FOR FAR SOUTHEAST TEXAS & SOUTHWEST ARKANSAS... ...Flash Flood risk associated with Barry... Slowly decreasing low-level convergence should result in the activity continuing to lose organization while shifting west into southeast TX where heavy rain occurred earlier this morning. central LA into far southwest MS...and will carry a Moderate risk to account for this threat. Elsewhere across the Lower MS Valley instability is expected to be a mitigating factor for heavy rainfall rates. Think most of the high res models are likely overdoing QPF amounts this morning from northern MS into AR,MO,TN,KY. By this afternoon some instability may be able to wrap into the system, but the general model consensus keeps convective activity rather localized in nature by this time. All in all, when combined with recent heavy rainfall, maintained a slight risk. One area to watch closely tonight will be southwest AR, possibly into far southeast OK. The 0-12z high res models are all quite aggressive in developing a training axis of convection here overnight, with a signal for local 5-10" totals towards 12z/7 am CDT Tuesday. This fits well with the conceptual model of heavy rainfall to the south southwest of an MCV or tropical low within a convergent moisture field where enough effective bulk shear exists to develop a curved, training band. The nocturnal low level jet increases helping enhance convergence and moisture transport. A look at RAP model fields does indeed show this evolution tonight, and would fit what the various high res models are depicting as well. Given this, think confidence is probably a bit above average that we will see some type of training convective axis setup tonight over this area...and given the PWs in place, significant flash flooding is certainly a possibility. Coordination with Little Rock AR (LZK) and Shreveport LA (SHV) led to the introduction and extent of the moderate risk area. ...Northern Plains into the Upper MS Valley and Great Lakes... Low confidence forecast across this region as models have handled convection the pasty few days very poorly; a look at the 700 hPa temperatures shows why, with no strong mid-level capping inversion particularly near this area. There do appear to be enough ingredients in place, however, to suggest the potential for a more organized flash flood risk later today into tonight across portions of MN and WI. A look at the 850mb moisture transport field shows a nice increase in both the magnitude and convergence of 850mb moisture transport over this region during the afternoon and overnight. This signal, along with the persistence of the signal for several hours, can typically be a good indicator for organized backbuilding/training convection. PWs and instability would both be high enough to support a flash flood risk should convection evolve in this way. There is some signal that outflow from the overnight MCS could be one focus for development this afternoon, with additional development along a front dropping south late in the day. Overall the consensus of solutions suggests the area around west-central WI has the highest chance of seeing an organized threat, and thus will maintain a Slight Risk across these areas. Some of the mesoscale guidance shows high amounts in this area -- recent HRRR, WRF NSSL, and NAM CONEST runs show a signal for local 4-7" amounts, but placement is a large issue, enough to preclude a moderate risk at this time. Certainly some chance the better focus ends up south or north of this, and will extend a Marginal risk to account for this. Convection is also likely this afternoon over MT and off the High Plains. The High Plains activity may try to organized into at least small scale clusters as they move into NE and SD. Will carry a Marginal risk to account for this given decent PWs in place. ...Upper Ohio Valley... Thunderstorms are developing over areas of lower flash flood guidance values across portions of the upper Ohio Valley. Cells in KY are showing relatively little motion and hourly rain totals of 1.5" as of late per radar imagery. Local amounts of 2-3" appear possible in this area, so extended the marginal risk area eastward to account for the KY and WV convection. Roth/Chenard Day 2 Valid 12Z Tue Jul 16 2019 - 12Z Wed Jul 17 2019 ...THERE IS A MODERATE RISK OF EXCESSIVE RAINFALL ACROSS SOUTHERN AND CENTRAL ARKANSAS WITH A SLIGHT RISK EXTENDING INTO THE OHIO VALLEY... ...Lower Mississippi Valley into the Southern Great Lakes... The remaining circulation of T.D. Barry will gradually lift northward through the MS VLY before becoming absorbed into the westerlies and opening late on day 2 and shearing off to the northeast. South and east of this circulation, the moisture plume will continue to channel from the Gulf Coast evidenced by higher PWATs of 1.5-2.5 standard deviations above the climo mean lifting from AR into MI. The channel will be tightened with the strengthening/impinging Subtropical ridge pressing west across the Southeast US, drawing additional moisture, but in a sense is drier relative to the deeper moisture closer to Barry. This channel will also be favoring the higher instability axis to the south, and an evolution similar to today across LA/TX is expected in AR/TN Tuesday. The combination of elevated MUCape and mid-level confluence to drive ascent will drive convective development with the potential for excessive rain rates through the afternoon. The strong convective elements are likely across AR where the greatest overlap of instability and PWAT combine, and HREF probabilities are high for 2"/hr through 18Z along with EC probabilities for 5". Guidance does differ in the exact location of the heaviest rainfall due to minor perturbations in the confluence band, but these types of rain rates on top of pre-conditioned soils due to antecedent heavy rain has prompted a MDT risk across portions of southern and central AR. Further north and east, the moisture axis will shift into the lower Great Lakes, but instability and PWAT anomalies will be somewhat lower. Still, this tropical airmass will support bands of convection with heavy rainfall from the TN VLY northward into the western OH VLY, and there is good model consensus for 1-3" of rainfall, with rates above 1"/hr likely at times. Flash flooding will be possible despite relatively drier antecedent conditions, and the SLGT risk has been extended NE towards Lake Erie due to pockets of FFG as low as 1.5"/3hr. ...Northern Plains... A slow moving frontal zone will drift in the vicinity Tuesday and Tuesday night, along which ripples of mid-level energy will waver the positioning due to subtle waves of low pressure developing in response. At the same time, ascent will be driven through at least weak jet coupling of the RRQ of a jet streak moving across northern MN, and the LFQ of a secondary jet streak lifting into the Central Rockies. Beneath these features, surface wave development in response to pressure falls will allow low-level winds to back, driving robust moist advection into the Plains on 25-40 kts of 850mb LLJ, especially after 17/00Z. PWATs climb to 1-2 standard deviations above the climatological normal, which in conjunction with MUCape rising above 2000 J/kg supports a highly favorable thermodynamic environment for convection and heavy rainfall. While the environment seems favorable for heavy rainfall, some guidance discrepancies still prevent enough confidence for a SLGT risk. The available HREF members vary considerably the first half of day 2 with heavy rainfall placement with convectively enhanced s/w MCSs moving atop the mid-level ridge. Additionally, some uncertainty persists as to the placement of the front itself, which will be the focus for the best rainfall/training potential. Despite high 14-day rainfall departures, and low FFG across SD, will maintain the inherited MRGL risk until better confidence can be achieved in where the highest rainfall and/or rainfall rates will locate. Gallina/Weiss Day 3 Valid 12Z Wed Jul 17 2019 - 12Z Thu Jul 18 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM TENNESSEE THROUGH THE CENTRAL OHIO VALLEY AND INTO UPSTATE NEW YORK... ...Tennessee Valley northeast into Upstate New York... Moisture streaming ahead of what was once Tropical Storm Barry will lift into the Ohio Valley and northeast as the remnant center shears increasingly into the westerlies. Instability will be continue to be limited with only 500-1000 J/kg expected by 00z across much of the Ohio Valley, remaining south across TN/KY where values will be in the 2000-3000 J/kg range, slightly higher west where the moisture axis will separate from the instability axis by midday. Deep moisture will still be present with PWATs of 2" or more through the afternoon, before banking up against the terrain of the Appalachians and reducing below 1.5" early overnight Thursday. As such, any confluence is likely to produce isolated to scattered convection further north across E OH/W WV becoming more numerous in Central/Eastern KY and TN. Still, the ideal unidirectional steering flow will break toward a greater western component by evening supporting faster eastward propagation/cell motions and reducing extreme rainfall totals. Still, rates of 2"/hr are possible producing 1-3" of rainfall with locally higher amounts possible. FFG in TN is reasonable high, 2-3"/3hrs, but the potential for excessive rain rates in the tropical air mass supports the SLGT risk. Further north into Ohio and New York state, some enhanced ascent will be likely in the RRQ of a departing upper jet as tropical moisture streams northward on an 850mb LLJ of 25-35 kts. Instability will be limited as noted above, so convective initiation is is likely to be scattered, but mean steering flow along a residual front will support training of any convective cells. As such there is an increasing signal for a west to east QPF swath across the Great Lakes into the Hudson River Valley. The guidance is converging on this axis of heavier rainfall, and note an increase in ECENS probabilities for 6-h and 12-h rainfall. For these reasons and higher than normal recent rainfall across the area, especially in Ohio, have extended the SLGT risk northeast into New York state. ...Upper Midwest... Ascent through a weakly coupled jet structure and low-level convergence along a front will likely produce thunderstorm development on day 3. Weak mid-level impulses rotating atop a strengthening upper ridge to the south will further drive convective strength, with clusters of thunderstorms or MCSs possible, especially late in the evening and at night. These MCSs will be fueled by an intensifying 850mb southerly LLJ to 30+ kts which will veer cyclonically into MN/WI and drive anomalous PWATs reaching 2.5 standard deviations above the climo mean into those states. Intense moisture flux during this time will combine with ample instability noted by forecast MUCape of over 3000 J/kg to persist and intensify convection along the stationary front. Despite what may be rapid motion of this feature, some training combined with high likelihood for excessive rain rates of 2"/hr support an enhanced flash flood risk, especially if the heaviest rainfall can occur across regions with relatively lower FFG of 1.5"/3hr. While the dynamics and environment would support a SLGT risk, there remains considerably placement uncertainty into where the best overlap of forcing, and MCS track, will occur. The trend this afternoon has been for a subtle northward push of the max axis in the guidance, but there is still enough spread, including the 12Z/ECMWF which keeps the heaviest rainfall as far south as the MN/IA border, to prevent a SLGT risk at this time. However, it is likely that a SLGT risk will be needed as guidance converges onto a distinct solution closer in time to the forecast period. Gallina/Weiss 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... $$ ------------=_1563221610-51656-11344 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. 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