
MY TAKEAWAY
Option 1 (Top Scenario):
- Storm Track: The low-pressure system takes a more northerly route, bringing warm Gulf air farther north ahead of the system.
- Impact: This leads to a predominant rain event across much of the Southeast, with a narrow band of mixed precipitation (sleet/freezing rain) to the north of the rain zone. Snowfall is confined to areas farther north, where the cold air remains entrenched.
- Cause: This setup typically results from a weaker ridge in the Midwest and a more zonal flow, which limits how far south the cold air can push. The warm air overruns the majority of the storm track, reducing the chances of significant snow in the southern regions.
Option 2 (Bottom Scenario):
- Storm Track: The low-pressure system tracks farther south, allowing cold air to dive deeper into the South and interact with Gulf moisture.
- Impact: Snowfall becomes the dominant precipitation type for a much larger area, especially in the Tennessee Valley, Mid-South, and into the Carolinas. A more widespread snow/mix zone appears, with less rain compared to Option 1. The transition zone shifts farther south, making this a colder and snowier outcome for many areas.
- Cause: This is driven by stronger Midwest ridging, which amplifies the jet stream and allows Arctic air to penetrate farther south. The storm track is forced to stay south, creating better conditions for snow.
Key Takeaways:
- Option 1 favors warmer conditions with limited snow, especially for southern regions.
- Option 2 is a more favorable setup for widespread snow and wintry weather, thanks to a colder, more suppressed storm track.
- The eventual outcome will depend on the strength of the Midwest ridge and how far south the cold air can push before the storm arrives.