Prognostic Meteorological Discussion
Issued by NWS
Issued by NWS
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956 FXUS21 KWNC 061726 PMDTHR US Hazards Outlook NWS Climate Prediction Center College Park MD 300 PM EDT September 06 2026 SYNOPSIS: Model ensembles continue to favor anomalous mid-level high pressure across the southern and central Contiguous U.S. (CONUS) and above-normal temperatures across most of the Lower 48, although the risk of extreme heat appears to be diminishing as we move into the second half of September. A potential surge of moisture from the Gulf of California may result in heavy precipitation over portions of the Desert Southwest and Great Basin. Antecedent dryness, combined with little precipitation favored over the next two weeks supports a Rapid Onset Drought (ROD) risk for portions of the Central and Southern Plains, Lower and Middle Mississippi, Ohio and Tennessee Valleys. HAZARDS Slight risk of heavy precipitation for portions of the Desert Southwest and Great Basin, Mon-Fri, Sep 14-18. Flooding possible for portions of the Desert Southwest and Great Basin. Rapid Onset Drought (ROD) risk for portions of the Central and Southern Plains and the Middle and Lower Mississippi, Tennessee, and Ohio Valleys. DETAILED SUMMARY FOR WEDNESDAY SEPTEMBER 09 - SUNDAY SEPTEMBER 13: https://www.wpc.ncep.noaa.gov/threats/threats.php FOR MONDAY SEPTEMBER 14 - SUNDAY SEPTEMBER 20: Dynamical model guidance remains in good agreement regarding elevated chances for subtropical ridging persisting over the south-central U.S. into week-2, with the 0z ECMWF, GEFS, and Canadian ensembles depicting positive 500-hPa height anomalies early in week-2 across the central and eastern CONUS. This lends itself to continued elevated chances for above-normal temperatures during much of the week-2 period. However, over the last several days model consensus has been gradually moving away from support for extreme heat hazards. The Probabilistic Extremes Tools (PETs) show very little potential for maximum temperatures to exceed the 95th climatological percentile (the favored threshold during shoulder seasons) at any point in the forecast period, and daily ensemble calculated heat indices no longer show much signal above 105F. Therefore the slight risk of extreme heat from previous outlooks has been discontinued. However, temperatures are likely to remain well above-normal for much of the southeastern quarter of the CONUS, and those sensitive to heat should continue to exercise caution. Model ensembles indicate a mid-level trough off the West Coast early in week-2. This may combine with enhanced moisture from the Gulf of California due to tropical activity over the Eastern Pacific to generate heavy precipitation over the North American monsoon region. Uncalibrated probabilities from the GEFS and ECMWF both indicate at least a 20% chance of 3-day precipitation totals to exceed half an inch over the region through the middle of the forecast period. Similarly, both PETs indicate at least a 20% chance of 3-day precipitation to exceed the 85th climatological percentile for much of week-2. Therefore, a slight risk of heavy precipitation is posted for Sep 14-18. Additionally, given the continued and increasing indications of potential heavy precipitation, a flooding possible hazard is posted for portions of the Four Corners region during the week-2 period. This region is prone to flash flooding and caution should be exercised near canyons and creek beds, and additional rainfall may hamper recovery efforts from recent flooding in the Grand Canyon. A Rapid Onset Drought (ROD) risk remains designated for parts of the Southern Plains and Lower Mississippi Valley and adjacent portions of the Central Plains, Ohio, Tennessee and Middle Mississippi Valleys, and Southeast U.S. This area has seen 20% to 40% of normal precipitation and deficits of 1 to 2 inches over the past 30 days. Near to below normal precipitation and above normal temperatures remain forecast for this region over the next two weeks increasing evapotranspiration rates into the middle of September. FORECASTER: Danny Barandiaran $$