Summary of the January 5-6, 2025 Winter Storm Impact

A significant winter storm impacted the Wakefield area from January 5 to 6, 2025, as a “Miller B” low-pressure system traversed through the region, resulting in three phases of precipitation including snow, sleet, and freezing rain, with numerous reports of power outages and substantial snow accumulation in various counties.

From January 5 to January 6, 2025, a significant “Miller B” low-pressure system moved from Kentucky and Tennessee to northern North Carolina, evolving into a second low off the Virginia/North Carolina coast. The weather event had three distinct phases affecting the Wakefield area.

Phase 1 occurred late on January 5, with temperatures in central and southeastern Virginia ranging from the upper 30s to lower 40s. Despite a dry air mass, isentropic ascent caused steady light to moderate snow in southern Virginia. This phase produced 2-3.5 inches of snow in a few hours before transitioning to sleet and freezing rain.

Phase 2, early January 6, saw improved mid-level ascent and resulted in a mix of precipitation types, prominently freezing rain in the central Virginia Piedmont. This caused significant power outages, with ice accumulations reaching 0.25 inches in some areas. Northern regions recorded 4 to 8 inches of snow, while sleet fell in southern regions.

Phase 3 began in the evening of January 6, post a lull in precipitation during the afternoon. Fresh snowfall of up to 2 inches occurred as temperatures fell into the upper 20s. This phase concluded the storm’s impact on the region.

This weather event has been noted as the most significant winter storm in the Wakefield area since January 2022, with total snow amounts nearing 10 inches in northern Dorchester County and widespread totals of 3 to 5 inches throughout the Richmond Metro area, albeit limited snow depth due to rain during Phase 2.

The January 5-6 winter storm was characterized as a “Miller B” type, which plays a crucial role in winter weather patterns across the southeastern United States. These systems are known for their capacity to bring varying forms of precipitation, influenced by temperature and moisture levels. Understanding these systems is essential for forecasting and preparing for severe winter weather impacts, as was observed during this notable storm.

In summary, the January 5-6, 2025 winter storm exemplified the complexities of a “Miller B” low-pressure system, resulting in a prolonged and impactful weather event for the Wakefield area. Observations noted significant snowfall and ice accumulation, which led to power outages and travel disruptions. This storm has been recognized as a major weather event for the region, emphasizing the importance of monitoring such systems.

Original Source: www.weather.gov