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Ask FLYING: What Kind of Precip Will Fall First?

It's frozen, but is it snow? [Credit: Adobe Stock]
Gemini Sparkle

Key Takeaways:

  • Precipitation type (snow, ice pellets, rain) is determined by the vertical temperature profile, with subtle temperature differences and the presence of above-freezing layers (warm nose) aloft being crucial.
  • In the Midwest, a common sequence with a warm front involves snow transitioning to ice pellets, then to rain or freezing rain, as warm air overruns cold air, creating and deepening a "warm nose."
  • Lake-effect snow, however, typically remains snow as it occurs within a consistent cold air mass where cold air flows over warmer lake waters, lacking the changing air mass dynamics that produce temperature inversions and other precipitation types.
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Q: Is it possible to identify the typical sequence during which snow will fall in the Midwest versus an area prone to receiving lake effect snow? It seems snow pellets or sleet/ice pellets appear before flakes in some circumstances.

A: Outside of large hailstones, the precipitation type that gets reported at the surface depends entirely on the vertical temperature profile. A winter weather system that lays down a few inches of snow, and one that produces ice pellets or rain may hinge on a degree or two of difference in the temperature aloft. This kind of uncertainty is what drives meteorologists crazy during the cold season. While the weather can unfold in countless ways, there are a few common themes to consider.  

For snow to reach the surface, a couple of things need to occur. First, the temperature close to the surface and aloft needs to be sufficiently cold. Even so, the entire temperature profile below the base of the snow-producing cloud doesn’t have to be below 0 degrees Celsius but cannot be too warm or snowflakes will melt as they fall into the above-freezing air near the surface. Nevertheless, it is possible to get wet snow on grassy surfaces with a surface temperature as warm as +4 degrees C. But at that temperature, it usually melts on contact if it survives at all. 

Scott Dennstaedt, Ph.D

Scott resides in Charlotte, North Carolina, and flies regularly throughout the Mid-Atlantic and Southeast U.S. He is a CFI and former NWS meteorologist. Scott is the author of "The Skew-T log (p) and Me: A Primer for Pilots" and the founder of EZWxBrief.

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