12/08/2017
The most recent run of the GFS (American Computer Model) brings Saturday's coastal low pressure system significantly closer to the coast, meaning the chances for some snow in Maryland have risen significantly. This won't be a tremendous snow event by any means, as temperatures will be right around freezing, which doesn't promote a significant moisture to snow ratio. Likewise, the amount of moisture necessary for major snowfall accumulations simply won't be present this time around.
The Eastern Shore and Southern Maryland (Anne Arundel, Calvert, St. Mary's, Prince George's Counties) face the highest chances of seeing accumulating snow. The US-50 corridor between Cambridge and Salisbury will likely see the greatest accumulations. The snow may mix with rain at times, especially during the midday hours, as temperatures will be fluctuating above and below the freezing line. Snowfall totals will likely remain in the one to three inch range, but four inches of snow will be possible locally. This has the potential to make untreated roadways slippery and hazardous.
The Baltimore area will also see some accumulations, with up to two inches of snow possible for areas immediately surrounding Baltimore City. Southern suburbs, such as Glen Burnie and Laurel, may see higher amounts of snowfall thanks to a richer stream of moisture passing through those areas.
Keep in mind that temperatures are forecasted to hover around the freezing mark for the majority of the day on Saturday. This means that accumulation forecasts are particularly difficult to pinpoint simply because a slight local change in temperature could lead to heavier snowfall or a changeover to rain. Additionally, the snow that does fall will be a slushy, wet snow, particularly in areas significantly south of the Mason-Dixon Line.
Folks in Baltimore should expect the onset of snowfall to arrive sometime between 6am and 8am on Saturday morning. Snow will persist throughout the day, before tapering off between 8pm and 10pm Saturday evening.
I'll provide more updates as more information comes in. Model trends over the next twenty-four hours will be more crucial than ever in predicting this system's fate.
For you weather nerds out there, this is a classic example of snowfall being produced from a baroclinic leaf associated with a wintertime coastal low pressure system, or 'Nor'easter'. This phenomenon expels moisture behind the location of a cold front, allowing it to mix with significantly colder temperatures and produce snow rather than rain. This is a rather low-grade example, but the majority of the major snowstorms we see in Maryland are produced thanks to these kinds of systems.
(Image: 00z NAM Model run for ~1pm on Saturday)