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From | To | Subject | Date/Time | |||
Mike Powell | All | HVYRAIN: Excessive Rainfa |
May 22, 2024 7:51 AM * |
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FOUS30 KWBC 220809 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 409 AM EDT Wed May 22 2024 Day 1 Valid 12Z Wed May 22 2024 - 12Z Thu May 23 2024 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM NORTHEAST TEXAS/SOUTHEAST OKLAHOMA, INTO SOUTHERN ARKANSAS AND NORTHERN LOUISIANA... The southern portion of the frontal boundary emanating from the low moving from the Upper Mississippi Valley into southern Ontario this morning will slow significantly from the Southern Plains into the Lower Arkansas and Mid Mississippi Valley during the upcoming day 1 period, becoming aligned more parallel to the southwest flow aloft. Additional convection likely to form in the axis of PW values 2+ standard deviations above the mean as shortwave energy moves east northeastward across the Southern Plains and along this slowing frontal zone. There has been a significant southward shift in nearly all of the models with the forecast axis of heaviest precip along this front. The individual hi res runs and the HREF mean are the farthest south now, with global models to the north of the HREF mean, closer to the 18Z axis of the RRFS and 06Z May 21 axis of the RRFSMEAN. The 00Z EC is the farthest south global model, closer to the hi res and HREF mean axis. WPC has followed the southward trend in our latest qpf and we will also trend farther to the south with the Excessive Rainfall probabilities. Training of cells parallel to the boundary is a concern for heavy to locally excessive rainfall totals day 1, although confidence is not great with placement given the spread and significant changes run to run. With respect to the previous outlook for this period, there has been approximately a 60-80 mile southward adjustment to the marginal and slight risk areas, extending them farther south into northeast Texas and northern Louisiana and reducing the risk from the OH/MS river confluence into northern Arkansas. Day 2 Valid 12Z Thu May 23 2024 - 12Z Fri May 24 2024 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM FAR NORTHEAST TEXAS/ FAR SOUTHEAST OKLAHOMA, ACROSS SOUTHERN ARKANSAS INTO NORTHERN MISSISSIPPI... Similar to the day 1 time period, a stationary frontal boundary expected to remain stretched in a west southwest to east northeasterly direction across northeast Texas/southeast Oklahoma into Arkansas, although this front will be weakening with time. PW values expected to remain 1.5 to 2 standard deviations above the mean along this weakening front during day 2. Additional shortwave energy moving west to east across the Southern Plains will support additional convection in this high PW axis and potential for additional heavy rains from northeast Texas/southeast Oklahoma, east across the Lower Arkansas Valley into the Lower Mississippi Valley. Given the low confidence with how convection will develop day 1 and whether there will be an outflow boundary still in tact for the day 2 convection, confidence does remain low on qpf placement. Models do seem to support a farther northward axis day 2 compared to day 1 as the stationary front weakens and southerly low level flow pushes the high PW values farther to the north. There still is potential for overlap of day 1 heavy rains with day 2, but with low confidence in the day 1 axis, confidence is low as to where this overlap will be. The new day 2 Excessive Rainfall Outlook did trend southward from the previous issuance for this period by approximately 50 miles to better match the latest WPC and model qpf consensus. ...Eastern portions of the Northern to Central Plains into the Upper Mississippi Valley... No significant changes made to the marginal risk area across eastern portions of the Northern to Central Plains into the Upper Mississippi Valley. Additional convection likely ahead of the next strong area of height falls rotating from the Northern Rockies into the Northern and Central Plains day 2. This region has seen heavy rainfall amounts over the past 24 hours, keeping stream flows high prior to the potential day 2 mounts. There is a lot of spread with qpf details, leading to low confidence in any one solution. However, with the strong upper trof, and associated strengthening low level southerly flow and increasing PW values, there will be potential for localized heavy rainfall amounts that may fall across areas that received heavy totals over the past 24 hours. Oravec Day 3 Valid 12Z Fri May 24 2024 - 12Z Sat May 25 2024 ...THERE IS A MARGINAL RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE UPPER MISSISSIPPI VALLEY INTO THE UPPER GREAT LAKES AND FROM THE LOWER ARKANSAS/LOWER MISSISSIPPI VALLEYS INTO THE TENNESSEE VALLEY AND SOUTHERN TO CENTRAL APPALACHIANS... ...Upper Mississippi Valley into the Upper Great Lakes... The next strong area of height falls moving into the Northern High Plains at the end of day 2 will continue to push eastward through the Northern Plains and into the Upper Mississippi Valley during day 3. The overall favorable large scale conditions ahead of these height falls day 2 will continue into day 3 along the associated front where strong frontal convergence in an axis of PW values 1 to 1.5 standard deviations above the mean will support potential for moderate to locally heavy rainfall totals. This front does look very progressive day 3, which may limit very heavy amounts. The marginal risk was drawn to where there may be overlap of locally heavy rains day 3 with heavy rains that have fallen over the past 24 hours. ...Lower Arkansas/Lower Mississippi Valley, Tennessee Valley into the Southern to Central Appalachians... A broad marginal risk area was maintained from the Lower Arkansas/Lower Mississippi Valley region, east northeast across the Tennessee Valley and into the Southern to Central Appalachians. PW values across these regions will remain above average for the day 3 period, with additional shortwave energy moving west to east supporting scattered convection and locally heavy rainfall amounts. Not a lot of confidence in where the scattered convection will become more organized, with a fairly large spread in model qpf details. Oravec = = = --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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