Prognostic Discussion for Monthly Outlook NWS Climate Prediction Center College Park MD 830 AM EST Thu Nov 17 2022 30-DAY OUTLOOK DISCUSSION FOR DECEMBER 2022 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. An updated monthly outlook... for Dec will be issued on Wed November 30 2022 These outlooks are based on departures from the 1991-2020 base period. $$