Prognostic Discussion for Monthly Outlook NWS Climate Prediction Center College Park MD 300 PM EST Wed Nov 30 2022 30-DAY OUTLOOK DISCUSSION FOR DECEMBER 2022 The updated monthly temperature and precipitation outlooks for December 2022 are based on the latest dynamical model guidance, WPC temperature and precipitation forecasts during the first week of the month, the CPC 6-10/8-14 day temperature and precipitation outlooks, and the likelihood of a negative Arctic Oscillation (AO) and North Atlantic Oscillation (NAO) through at least mid-December. The Madden-Julian Oscillation (MJO) strengthened during mid-November with an eastward propagation to the West Pacific. The MJO continues to shift eastward over the Western Hemisphere. The GEFS depicts a reemergence of the MJO across the Indian Ocean later in December, while the ECMWF weakens it. If the GEFS solution verifies, then a transition to a warmer pattern for the northern and eastern contiguous United States (CONUS) may occur late in December. However, large uncertainty exists given the MJO weakening favored by the ECMWF model and strong high latitude blocking likely through at least mid-December. Arctic high pressure is forecast to shift southward to the western and north-central CONUS at the beginning of December. Ensemble means remain in excellent agreement that high latitude blocking develops over the Northern Hemisphere early in December, consistent with a negative phase of the AO. In addition, a very strong blocking ridge is forecast to shift westward to Greenland and the Davis Strait with a west-based negative NAO. Given the excellent model agreement and consistency on this high latitude blocking and anomalous cold during the first two weeks of the month, below-normal temperatures are favored for the north-central CONUS along with parts of the West. The largest probabilities (50 to 70 percent, or more) extend from the Pacific Northwest east to the northern Great Plains and upper Mississippi Valley where the negative temperature anomalies are greatest early in the month and is also consistent with La Niña composites. Following a mild start to the month across the eastern CONUS, colder temperatures are forecast for these areas by the second week of December. Therefore, equal chances (EC) of below, near, or above-normal temperatures are forecast for this region. Despite some tools leaning warmer, the likelihood of a -NAO through mid-December resulted in EC for parts of the Southeast. Although above-normal temperatures are slightly favored for the southern tier of the CONUS, forecast confidence is low given the strong high latitude blocking and potential for modified Arctic air to shift southward at times during December. Ensemble means are in good agreement that anomalous 500-hPa ridging persists over the north-central Pacific through at least the first two weeks of the month. Downstream of this longwave ridge axis, a persistent trough of varying amplitude is forecast near or offshore of the West Coast during early to mid-December. This trough is likely to enhance onshore flow and lead to a relatively wet pattern for much of the West through mid-December. The week 3-4 model solutions (valid Dec 14 to 27) favor a continuation of this wet pattern into the latter half of the month. Therefore, increased probabilities for above-normal precipitation are forecast for much of the West. EC is forecast for southern California and the desert Southwest where precipitation signals are weaker. A dry start to December along with good consistency among recent daily CFS model runs supports elevated probabilities for below-normal precipitation from eastern New Mexico and the southern high Plains northeastward to parts of the Midwest. Northwest flow, associated with cold air advection, early in the month is another reason for this dryness across the Midwest. Heavy precipitation (1 to 3 inches, or more) during the first week of the month along with the expectation for a mean surface front and additional precipitation during the remainder of December increases chances for above normal precipitation across the Ohio and Tennessee Valleys. A dry start to the month and recent daily runs of the CFS model favor below normal precipitation across much of the Coastal Plain of the Southeast and Florida. This wet to dry dipole from the Ohio River southward to the Gulf Coast is typical during La Niña. EC is forecast for the lower Mississippi Valley, Mid-Atlantic, and Northeast due to weaker precipitation signals at various time scales throughout December. Model guidance remains steady as anomalous 500-hPa ridging is likely to persist over the north-central Pacific and Aleutians. Above-normal temperatures are favored for the Aleutians along with western and northern Mainland Alaska. Below-normal temperatures are most likely for the Alaska Panhandle, based on colder-than-normal temperatures during early to mid-December and also consistent with recent daily CFS model runs. Along with the favored below-normal temperatures, elevated probabilities for below-normal precipitation are forecast for the Panhandle. Predicted southwest flow and excellent agreement among precipitation tools support increased probabilities for above-normal precipitation across much of western and northern Mainland Alaska. *********** Previous discussion, released on November 17, is below *********** The December 2022 temperature and precipitation outlooks are based on the Weeks 3-4 model solutions (valid for early to mid-December), dynamical model output for December, La Niña composites, consideration on the forecasted state of the Madden Julian Oscillation (MJO), and decadal trends. Below-average sea surface temperatures continue across the central and eastern equatorial Pacific, while suppressed convection was observed near and west of the Date Line this past month. The oceanic and atmospheric observations reflect La Niña conditions which are likely to persist through the winter. The MJO is forecast to strengthen and propagate eastward to the West Pacific during late November. Although the GEFS and ECMWF models are in good agreement on this MJO evolution, large ensemble spread exists on the strength of the MJO with many GFS ensemble members depicting a higher amplitude MJO event compared to the majority of ECMWF ensemble members. Lagged composites, based on phase 5 of the MJO RMM index, would favor below-normal temperatures overspreading the central and eastern contiguous U.S. (CONUS) during early to mid-December. Given the expected mild start to the month for most areas east of the Rockies, this would translate to a highly variable temperature pattern during December which lowers forecast confidence in the monthly temperature outlook for the central and eastern CONUS. Therefore, a large coverage of equal chances (EC) of below, near, or above-normal temperatures is necessary. Below-normal temperatures are favored for the northern Great Plains where the week 3-4 ECMWF model along with La Niña composites feature a cold signal. Above-normal temperatures are only slightly favored along the East Coast, consistent with the week 3-4 model solutions and the North American Multi-Model Ensemble (NMME). The dynamical model output along with La Niña composites support increased probabilities for above-normal temperatures throughout the southern tier of the CONUS. Although there is support for larger probabilities of above-normal temperatures across the Southeast, the GFS ensemble mean depicts a negative NAO heading into December which limits forecast confidence for this region. The highest forecast confidence in the temperature outlook exists across the Southwest where week 3-4 solutions along with dynamical and statistical tools are in good agreement. La Niña composites for November-December-January (NDJ) are the major guidance relied upon for the December precipitation outlook along with the NMME. Above-normal precipitation is most likely across the Pacific Northwest, northern to central Rockies, and northern high Plains. Conversely, below-normal precipitation is favored for parts of the Southwest, central to southern Great Plains, Gulf Coast, and Southeast. Although statistical tools support a drier outcome for California, EC is forecast for the state due to a lack of support from monthly dynamical models and a robust wet signal evident in the week 3-4 ECMWF model solution. Also, the ensemble means are in good agreement on an amplified 500-hPa trough centered near the West Coast during the final week of November. EC is also forecast for the Great Lakes and Ohio Valley where the wet signal, associated with La Niña, typically occurs later in the winter season. The dynamical and statistical tools are in good agreement and depict elevated probabilities for below (above)-normal temperatures for the Alaska Panhandle (western Mainland Alaska). Despite the NMME favoring above-normal temperatures across the Aleutians, EC was forecast for this region due to negative sea surface temperature anomalies nearby and a strong cold signal in the week 3-4 ECMWF model. The NMME and decadal trends support increased probabilities for above-normal precipitation for northwestern Alaska. Although La Niña typically favors dryness for the Alaska Panhandle during the winter, EC was forecast due to a weak signal among the dynamical model output. FORECASTER: Brad Pugh The climatic normals are based on conditions between 1991 and 2020, following the World Meteorological Organization convention of using the most recent 3 complete decades as the climate reference period. The probability anomalies for temperature and precipitation based on these new normals better represent shorter term climatic anomalies than the forecasts based on older normals. The next monthly outlook...for Jan ... will be issued on Thu Dec 15 2022 These outlooks are based on departures from the 1991-2020 base period. $$