


Prognostic Meteorological Discussion
Issued by NWS
Issued by NWS
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902 FXUS06 KWBC 011907 PMDMRD Prognostic Discussion for 6 to 10 and 8 to 14 day outlooks NWS Climate Prediction Center College Park, MD 300 PM EDT Mon September 01 2025 6-10 DAY OUTLOOK FOR SEP 07 - 11 2025 The ECMWF, GEFS and Canadian ensemble models broadly agree on the 500-hPa height pattern over North America and surrounding regions during the 6-10 day period, with only minor variations among the models in terms of amplitude and phase of predicted wave features. The manual height blend is based on ensemble means, weighing the ECMWF model greater due to recent model anomaly correlation skill. The manual blend shows a ridge and above normal 500-hPa heights over Alaska, western and central Canada, and the western and central Contiguous U.S. (CONUS), while a trough with below normal 500-hPa heights are predicted over the eastern CONUS. Another trough is forecast along the West Coast. Near to slightly above normal 500-hPa heights are predicted across Hawaii. Above normal temperatures are favored for the Aleutians, the Alaska Panhandle, most of Mainland Alaska, and most of the western CONUS (except for parts of California and Nevada, where below normal temperatures are favored, due to a trough predicted along the West Coast) in association with predicted broad anomalous ridging and above normal 500-hPa heights over these areas. Conversely, the trough forecast across the eastern CONUS, especially early in the period, favors below normal temperatures over most of the eastern and central CONUS, except for the Gulf Coast states where above normal temperatures are favored due to subtropical ridging to the south of a mean frontal boundary, consistent with most of the dynamic temperature forecast tools. Above normal temperatures are favored for Hawaii due to slightly above normal 500-hPa heights and above normal sea surface temperatures in the adjacent Pacific. Above normal precipitation is forecast over most of the western and central CONUS, consistent with the autoblend and consolidated precipitation forecast tools. Influxes of monsoonal moisture across the Southwest combined with a stationary frontal boundary across the southern High Plains are the main drivers for this predicted active period. Conversely, near to below normal precipitation is favored across most of the eastern CONUS (except for the southern Atlantic Coast and the Gulf Coast states where above normal precipitation chances are elevated ahead of the predicted mean trough axis) due to predicted surface high pressure associated with a cool stable Canadian airmass. Below normal precipitation is also favored for Southeast Alaska, associated with anomalous ridging forecast over western Canada. Above normal precipitation is more likely across most of the remainder of Alaska ahead of a trough predicted over the Bering Sea. Above normal precipitation is favored for Hawaii, supported by the consolidation precipitation forecast tool. The official 6-10 day 500-hPa height blend consists of 30% of Today`s 6z GFS Ensemble Mean centered on Day 8, 40% of Today`s 0z European Ensemble Mean centered on Day 8, and 30% of Today`s 0z Canadian Ensemble Mean centered on Day 8 FORECAST CONFIDENCE FOR THE 6-10 DAY PERIOD: Above average, 4 out of 5, due to good agreement among todays ensemble means. 8-14 DAY OUTLOOK FOR SEP 09 - 15 2025 Ensemble mean forecasts for the 500-hPa circulation pattern over North America remain in general agreement and a transition in the 500-hPa pattern is well underway across much of the country during the 8-14 day period. As time progresses, a much more zonal regime takes hold across much of the CONUS. In the manual blend of model forecasts, a weak anomalous trough is predicted over the Aleutians, while a ridge and above normal 500-hPa heights are forecast over Alaska, Canada and north-central and northeastern CONUS throughout the period. An anomalous trough is forecast over the West Coast. Generally near normal heights are forecast for Hawaii throughout the period. Near to above normal temperatures are likely for most of Alaska due to persistent ridging and above normal heights. Enhanced probabilities of above normal temperatures are also forecast across much of the central CONUS, due to predicted ridging and above normal 500-hPa heights. Conversely, below normal temperatures are favored for the northeastern CONUS due to predicted anomalous troughing early in the period. Below normal temperatures are also favored over portions of California, Nevada, Oregon, and Idaho, under a predicted trough over the West Coast, supported by most of the temperature forecast tools. Above normal temperatures are more likely for the southeastern CONUS, to the south of a predicted frontal boundary and consistent with above normal SSTs in the adjacent Atlantic and Gulf waters. Above normal temperatures are likely for Hawaii, due largely to observed above normal SSTs in the adjacent Pacific. A wet pattern is favored for most of the northwestern and north-central CONUS, due to a trough trough predicted over the West Coast. Above normal precipitation chances are elevated along the Gulf and Southeast coasts around the periphery of a predicted anomalous trough early in the period. Modestly enhanced chances of below normal precipitation is forecast for parts of the northeastern CONUS due to predicted surface high pressure early in the period. These enhanced below normal precipitation chances were kept low due to the potential transition to a wetter pattern toward the end of week-2. Above normal precipitation is favored for most of Mainland Alaska and the Alaska Peninsula ahead of troughing forecast over the Aleutians. Above normal precipitation is favored across the Hawaiian islands, consistent with the consolidation precipitation forecast tool. The official 8-14 day 500-hPa height blend consists of: 30% of Today`s 6z GFS Ensemble Mean centered on Day 11, 40% of Today`s 0z European Ensemble Mean centered on Day 11, and 30% of Today`s 0z Canadian Ensemble Mean centered on Day 11 FORECAST CONFIDENCE FOR THE 8-14 DAY PERIOD: Below average, 2 out of 5, due to uncertainties surrounding a predicted transitional 500-hPa flow pattern across much of North America. FORECASTER: Luke H Notes: The notation for the categorical forecast indicated on the maps is the same as that in the tables: A-above N-near normal B-below The temperature map shows regions with > 33% chance of being warmer (orange, "A"), colder (blue, "B"), or close to (unshaded, "N"). Historical average values for the calendar period of the forecast (dashes, "f"). Labels on the shaded lines give the probability (> 33%) of the more likely category (B or A). Probability of N is always < 40%. The precipitation map shows regions with > 33% chance of being wetter (green, "A"), drier (tan, "B"), or close to (unshaded, "n"). Historical median values for the calendar period of the forecast (dashes, "inches"). Labels on the shaded lines give the probability (> 33%) of the more likely category (B or A). Probability of N is always < 40%. In the southwest and other climatologically dry regions - there will be a greater than 33.3% chance of no precipitation and occasionally even a normal (i.e. Median) value of zero - especially during the dry seasons. In such cases a forecast of near normal is effectively a forecast of little or no precipitation. The climate prediction center uses 1991-2020 base period means as reference in the climate outlooks. The next set of long-lead monthly and seasonal outlooks will be released on September 18. Analogs to the 5 day mean observed pattern centered 3 days ago (D-3) for the region from 20N to 70N latitude and 175E to 60W longitude include the 5 day periods centered on the following dates: 19630827 - 19790821 - 19610819 - 19810825 - 19870903 Analogs to the 7 day mean observed pattern centered 4 days ago (D-4) for the region from 20N to 70N latitude and 175E to 60W longitude include the 7 day periods centered on the following dates: 19630827 - 19610818 - 19870903 - 19790820 - 19510822 6-10 DAY OUTLOOK TABLE Outlook for Sep 07 - 11 2025 STATE TEMP PCPN STATE TEMP PCPN STATE TEMP PCPN WASHINGTON A A OREGON A A NRN CALIF N A SRN CALIF B N IDAHO A A NEVADA B A W MONTANA A A E MONTANA A A WYOMING A A UTAH A A ARIZONA A A COLORADO A A NEW MEXICO A A N DAKOTA A A S DAKOTA A A NEBRASKA B A KANSAS B A OKLAHOMA B A N TEXAS B A S TEXAS A A W TEXAS B A MINNESOTA B N IOWA B N MISSOURI B N ARKANSAS B N LOUISIANA A N WISCONSIN B B ILLINOIS B B MISSISSIPPI B N MICHIGAN B B INDIANA B B OHIO B B KENTUCKY B B TENNESSEE B B ALABAMA B N NEW YORK B B VERMONT B B NEW HAMP B B MAINE B B MASS B B CONN B B RHODE IS B N PENN B B NEW JERSEY B B W VIRGINIA B B MARYLAND B B DELAWARE B N VIRGINIA B N N CAROLINA B A S CAROLINA B A GEORGIA B A FL PNHDL A A FL PENIN A A AK N SLOPE A A AK ALEUTIAN A N AK WESTERN A A AK INT BSN A A AK S INT A A AK SO COAST A A AK PNHDL A B 8-14 DAY OUTLOOK TABLE Outlook for Sep 09 - 15 2025 STATE TEMP PCPN STATE TEMP PCPN STATE TEMP PCPN WASHINGTON A A OREGON N A NRN CALIF B A SRN CALIF B N IDAHO B A NEVADA B A W MONTANA N A E MONTANA A A WYOMING A A UTAH A A ARIZONA A N COLORADO A A NEW MEXICO A N N DAKOTA A A S DAKOTA A A NEBRASKA A A KANSAS A A OKLAHOMA A N N TEXAS A N S TEXAS A N W TEXAS A N MINNESOTA A A IOWA A A MISSOURI A N ARKANSAS A N LOUISIANA A N WISCONSIN A N ILLINOIS A N MISSISSIPPI A N MICHIGAN A N INDIANA A N OHIO N N KENTUCKY N N TENNESSEE A N ALABAMA A N NEW YORK B N VERMONT B N NEW HAMP B N MAINE B N MASS B N CONN B N RHODE IS B N PENN B N NEW JERSEY B N W VIRGINIA B N MARYLAND B N DELAWARE B N VIRGINIA B N N CAROLINA B A S CAROLINA N A GEORGIA N A FL PNHDL A A FL PENIN A A AK N SLOPE A A AK ALEUTIAN A A AK WESTERN A A AK INT BSN A A AK S INT A A AK SO COAST A A AK PNHDL A N LEGEND TEMPS WITH RESPECT TO NORMAL PCPN WITH RESPECT TO MEDIAN A - ABOVE N - NEAR NORMAL A - ABOVE N - NEAR MEDIAN B - BELOW B - BELOW THE FORECAST CLASSES REPRESENT AVERAGES FOR EACH STATE. NORMAL VALUES - WHICH MAY VARY WIDELY ACROSS SOME STATES - ARE AVAILABLE FROM YOUR LOCAL WEATHER SERVICE FORECAST OFFICE. FOR ADDITIONAL INFORMATION SEE MESSAGE FXUS06 KWBC - ON AWIPS AS PMDMRD. $$