All About Freezing Rain | Earth - EarthSky

Freezing rain

Freezing rain is simply rain that falls through a shallow layer of cold temperatures at or below 32 degrees Fahrenheit (0 degrees Celsius) near the surface. When this rain becomes super-cooled, it can freeze on contact with roads, bridges, trees, power lines and vehicles. It can look beautiful on the limbs of trees. But when freezing rain accumulates, it can add a lot of weight on trees – a quarter of an inch of ice can add 500 pounds (225 kg) of weight – which can bring trees down and result in numerous power outages and damage to homes.

Freezing rain is typically the weather threat that creates the most car accidents, injuries and deaths in winter storms. Many people can drive in the rain and snow, but when the roads become icy, it is almost impossible to drive. Severe ice storms can shut down large cities, result in thousands of power outages, and the most severe ones can also become billion-dollar disasters (rare).

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Different types of winter precipitation

It is important to know the difference between snow, sleet and freezing rain.

1) Snow forms when the entire layer of air is sub-freezing. Snow consists of ice crystals and is white and fluffy.

2) Sleet forms when the layer of sub-freezing air is fairly deep at 3,000 to 4,000 feet (900-1200 meters). This allows time for the water droplet to freeze into a tiny piece of ice and become sleet as it falls to the surface. Precipitation in the wintertime that falls as tiny ice pellets is sleet. Hail is only associated with strong thunderstorms and are larger in size and can cause damage.

3) Freezing rain forms when the sub-freezing layer is very shallow. At 2,000 feet (600 m) from the surface, temperatures are above freezing, so any precipitation that falls is liquid. Once rain hits that shallow cold air near the surface, it freezes on contact with any object.

Shallow cold air at the surface can sometimes occur thanks to cold air damming. Cold air damming, abbreviated as CAD, is where a low-level cold air mass becomes trapped topographically. These events can be very common near or around mountain regions, and is known to occur across the eastern United States thanks to the Appalachian Mountains. Some of the worst ice storms to form were thanks to this CAD effect that is also known as the “wedge.” This term is used because shallow cold air is wedged down the Appalachian Mountains thanks to a ridge of high pressure typically located across New England, eastern Canada, or the Mid-Atlantic.

Freezing rain causes major problems

When it comes to freezing rain, it is the weight of the ice on the trees that causes problems. They can fall over and crush cars, houses and power lines. According to Steve Nix, brittle tree species typically take the brunt of heavy icing. Trees such as poplars, silver maples, birches, willows and hackberries are more likely to break and fall over due to the weight of the ice. One of the big reasons these trees break and fall over first is because they are fast growers. They also develop weak, V-shaped crotches that can easily split apart under the added weight of ice.

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Bottom line: Freezing rain is simply rain that falls into a shallow layer of below-freezing temperatures. When a super-cooled droplet hits an object, it freezes and becomes ice. Ice from freezing rain can down power lines, paralyze cities, bring down trees and cause serious accidents.

Read more: Too cold to snow? Is that possible?

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