Weather Guides

Winter Weather Explained: Snow, Sleet & Freezing Rain

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Winter storms are some of the hardest storms to forecast and some of the most disruptive. A difference of one or two degrees, sometimes thousands of feet above the ground, decides whether a storm brings a beautiful snowfall, a slushy mess, or an ice storm that knocks out power for a week. This guide explains what controls precipitation type, how to read the alerts, and what to watch for on the map.

Snow, sleet, and freezing rain: it's all about the layers

Most precipitation in the mid-latitudes, even in summer, starts as snow high in the cloud. What reaches the ground depends on the temperature of the layers it falls through on the way down:

TypeTemperature profileWhat happens
SnowBelow freezing all the way down (or only a very shallow warm layer near the ground)Snowflakes reach the ground intact.
SleetA warm layer aloft, then a deep freezing layer near the groundSnow melts into rain in the warm layer, then refreezes into small ice pellets before landing. Sleet bounces and sounds like rice hitting a window.
Freezing rainA warm layer aloft, then a shallow freezing layer at the groundSnow melts into rain, but the cold layer is too thin to refreeze it in the air. The rain is supercooled and freezes on contact with anything below freezing, coating it in a glaze of ice.
RainAbove freezing near the groundSnow melts and stays liquid.

These layers are often arranged geographically along a storm's path. In a typical winter storm moving across the eastern U.S., you might find rain to the south and east, then a band of freezing rain, then sleet, then snow to the north and west, sometimes within 50 miles. As warm air pushes in aloft during the storm, the bands shift, so a location can change from snow to sleet to freezing rain in a few hours. That's why winter forecasts so often say "a wintry mix," and why snow totals can bust when warm air arrives sooner or later than expected.

Why ice storms are so destructive

Freezing rain is the most damaging winter precipitation because ice is heavy and accumulates on everything: trees, power lines, cars, and roads. A rough guide to ice accumulation:

Many of the costliest winter storms in U.S. history have been ice storms rather than snowstorms, with power out for days or weeks across entire regions.

Winter weather alerts

Criteria vary by region, because six inches of snow is routine in Buffalo and paralyzing in Atlanta. In general:

On the RadarBug map, Winter Storm Watches are blue, Winter Weather Advisories are green, and every warning, including Winter Storm, Ice Storm, and Blizzard Warnings, is red.

Wind chill and frostbite

Wind chill describes how cold it feels on exposed skin, because wind strips away the thin layer of warm air next to your body. At an air temperature of 0 °F with a 15 mph wind, the wind chill is about −19 °F, and exposed skin can get frostbite in about 30 minutes. At wind chills around −35 °F, that time falls to roughly 10 minutes.

Wind chill doesn't make objects colder than the air temperature: a car radiator or pipes won't drop below the actual temperature. It describes how fast your body loses heat.

Winter weather on radar

Radar shows snow, but it reads it differently from rain, and it helps to know the quirks:

Staying safe in winter weather

Winter forecasts can change quickly as a storm approaches, especially near the rain-snow line. Check the latest forecast and alerts from your local National Weather Service office before traveling, and see the Severe Weather Preparedness Checklist for preparing for multi-day power outages.

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