Quantitative Precipitation Forecast
Issued by NWS
Issued by NWS
543 FOUS11 KWBC 041937 QPFHSD Probabilistic Heavy Snow and Icing Discussion NWS Weather Prediction Center College Park MD 237 PM EST Sat Jan 4 2025 Valid 00Z Sun Jan 05 2025 - 00Z Wed Jan 08 2025 ...Central Plains through the Mid-Atlantic... Days 1-3... ...Major winter storm begins tonight across the Central Plains and then shifts east to the Mid-Atlantic on Monday... The first major storm of 2025 develops tonight as an amplifying mid-level trough ejects from the Four Corners/Central Rockies and closes off over Kansas by Sunday morning. This closed low will then continue to deepen as it pivots eastward, reflected by NAEFS 500mb-700mb height anomalies falling to as low as the bottom 2.5th percentile of the CFSR climatology. This closed feature will continue to deepen gradually as it moves into the OH/TN Valleys Monday, before slowly opening into a trough across the Mid-Atlantic Tuesday morning. Through this evolution, a strengthening jet streak will pivot around the base of the trough, reaching as high as 150kts, and overlapping effectively with the greatest height falls/PVA to cause intense deep layer ascent. Beneath this synoptic lift, a surface cyclone will develop in the lee of the Rockies and then move nearly due east with subtle deepening until it exits into the Atlantic on Tuesday. As this surface low deepens and move east, impressive moisture will be drawn northward from the Gulf of Mexico within a corridor of intensifying isentropic ascent, especially within the 290-295K surfaces. Here, mixing ratios climb to 4-6 g/kg, reflective of the impressive moist driven by the warm advection, further evidenced by PW anomalies surging to above the 97th percentile according to NAEFS. The accompanying theta-e ridge is then progged to lift cyclonically into a TROWAL surrounding this deepening low, and pivot back into KS/MO on Sunday. This is likely to cause an expanding area of precipitation, with the accompanying elevated instability driving more intense precipitation rates through D1. The pattern conceptually matches one that will support both an intense laterally-translating band of heavy precipitation east and downstream of the surface low, with a secondary, likely more intense, pivoting deformation band to the NW of the low. Locations that receive both of these bands, and stay all snow, will receive the heaviest accumulations. As far as snowfall amounts, they are likely to be quite impressive, especially across the Central Plains and into the Ohio Valley. Across the Plains, the lead WAA band will support snowfall rates of 1-2"/hr, and these types of bands can cause long duration of snow in narrow corridors. While the guidance has come into much better agreement with the placement of this band, there is still some uncertainty as to the exact location, especially due to latitudinal variations in the warm nose placement which will wreak havoc on amounts due to mixing with sleet and freezing rain, as well as much lower SLR (heavy-wet snow). As the low begins to push east, an intense deformation axis will develop across central/eastern KS and into NW MO. The guidance is quite aggressive with this axis, and it appears probable that a pivoting band with convective snow rates of 2-3"/hr is likely as folded theta-e and -EPV overlap in cross- sections suggesting upright (CI) convection potential. During this time the column cools significantly, DGZ depth increases, and winds intensify, so blizzard and near blizzard conditions are also possible. It is this region that will likely experience the most significant snowfall, reflected by WPC probabilities that are high (70-90%) for 12+ inches from N-Central KS through far NW Missouri. A broader swath of 6+ inches is likely (50-70%) encompassing this region and spreading as far east as near Indianapolis on D1. North of this developing system, some interaction of a northern stream shortwave diving out of the High Plains will become absorbed into the larger and more amplified developing system. This will result in a swath of mostly light to moderate snow from SD into NE on the periphery of the more impressive theta-e axis. While snowfall across this region won`t be as intense or heavy as points to the south/east, several inches of light fluffy snow is likely within a cold and increasingly windy column. WPC probabilities are moderate (30-50%) for 4+ inches from the SD/NE border and points south across central NE. Farther downstream, the system begins to move more quickly across the OH VLY and into the Mid-Atlantic, which will limit the duration of heavy snow moreso than in points west. Additionally, the weakening upper low will cause the deformation axis to weaken resulting in less intense snowfall rates. However, impressive rates that will still exceed 1"/hr are expected within the band from Illinois through Ohio, and then continue across portions of the Mid-Atlantic where more uncertainty still exists. Additionally, guidance has become more excited about a secondary shortwave digging through the opening longwave trough, leading to an inverted trough NW of the departing low Monday, with secondary low development also possible east of the DelMarVa. This will, at the very least, lengthen the duration of light to moderate snow from OH to DE, with potentially a secondary axis of heavy snow along this trough adding to snow totals. At this time, despite latitudinal uncertainty, WPC probabilities are moderate to high for 6+ inches of snow, primarily on D2, from Indianapolis eastward to the Washington, D.C. metro area. Locally as much as 12" of snow is possible across the lower OH Valley, with lesser totals expected across the Mid-Atlantic, although more uncertainty exists there. And, not to be outdone, this system will also pose a significant to damaging ice threat within the warm nose south of the heaviest snow. The models have been trending a bit south/colder since yesterday which pushes the ice axis a little farther south as well, but the intense WAA over-topping the cold surface layer accompanied by persistent E/NE dry-bulb advection is a classic setup for damaging freezing rain. Although there is some uncertainty into how efficiently the ice can accrete at times due to what should be intense precipitation rates, the threat for damaging ice has continued to increase from eastern KS through southern MO and into central KY. Here, WPC probabilities for more than 0.25" of ice are high (70-90%), with even some 10-30% chance for greater than 0.5" of ice. This could result in downed limbs and power lines leading to widespread power outages and impossible travel. Farther east across the Central Appalachians and surrounding foothills, WPC probabilities for 0.25" of ice peak around 50%. Finally, between the heavy snow and heavy icing, the forecast profiles indicate a narrow stripe with cold layer depths greater than 1000m, or above the 90th percentile for freezing rain in the south-central US. This suggests sleet, especially in the presence of a relatively weak warm nose aloft and the aforementioned persistent dry advection at the surface. Heavy accumulations of sleet are difficult to achieve, but in this setup it is possible that 1-2" of sleet will accumulate causing tremendous driving impacts. The greatest risk for the major sleet accumulations are from near St. Louis southeast to extreme southern IN, but fluctuations in placement are still possible. This system has prompted the issuance of key messages which are linked below. ...Western U.S.... Days 1-3... A shortwave trough riding over a ridge axis centered off the Pacific Northwest crosses Washington late tonight before being absorbed into the trough over the Rockies that trails the low developing over Kansas. Moisture streams in ahead of this trough, making for moderate to heavy snow on the WA Cascades tonight with snow levels rising from around 3500ft to 4000ft which means passes will be impacted. Enough moisture reaches inland to bring moderate snows to the Bitterroots and ranges around Glacier NP on Sunday with snow levels rising from 2500ft to 4000ft. Day 1 snow probabilities for >4" are moderate (around 50%) at Cascades pass level and high (over 80%) for >8" in the higher North Cascades terrain. Day 1 snow probabilities for >4" are 50-80% over the greater Bitterroots and western Glacier NP ranges. The next shortwave trough rides over the ridge Sunday night, diving across the OR Coast and becoming very positively-tilted over the the Desert Southwest on Tuesday. High initial snow levels around 7000ft over the OR Cascades only drop to around 6000ft under the trough axis, so only the highest OR Cascades, well above pass level will receive heavy snow. Snow levels will be closer to 5000ft over the Great Basin and 4000ft over the northern Rockies. Day 2 snow probabilities for >4" are generally 30-60% over terrain in eastern OR, much of central/southern ID, northeast NV, and central MT. As light to locally moderate precip shifts south with the trough Monday night, snow levels in Utah will be around 5000ft. However, on Tuesday there is a heavy snow potential on the eastern slopes of the central/southern CO Rockies as strong high pressure (central sfc pressure around 1040mb) shifts south down the Dakotas, aiding an easterly low level flow to the moisture coming in from the west. Day 3 snow probs for >4" are 20-50% for southern portions of the Front Range and much of the Sangre de Cristos. ...Lake Effect Snow - Lake Ontario... Day 1... Low pressure centered over James Bay will weaken tonight into Sunday as a rapidly developing low off Nova Scotia becomes the dominant surface low in a broad gyre over southeast Canada. As a result, the great pressure gradient between James Bay and a 1044mb high over Manitoba will weaken and the strong WNW flow over central Ontario will gradually diminish. Sufficient WNW flow will persist over eastern Lake Superior, northern Lake Huron, southern Georgian Bay, Lake Simcoe, and Lake Ontario to provide maximum moisture fetch for LES single-banding to persist through midday Sunday between the Tug Hill and Syracuse before drifting south and weakening Sunday afternoon. Day 1 snow probabilities for >12" are >80% on an axis from Oswego to Rome with the potential for a local maximum exceeding 2 feet in Oswego County. Weiss/Jackson ...Winter Storm Key Messages are in effect. Please see current Key Messages below... https://www.wpc.ncep.noaa.gov/key_messages/LatestKeyMessage_1.png $$