Freezing Rain and Sleet
Both freezing rain and sleet occur by the same general process:
liquid raindrops in a layer of warm air well above the surface fall into a layer of freezing air
hugging the ground. The difference between these two wintry precipitation types depends on the
thickness of the layer of freezing air.
Freezing rain occurs when the layer of freezing air is so thin that
the raindrops do not have enough time to freeze before reaching the ground. Instead, the water
freezes on contact with the surface, creating a coating of ice on whatever the raindrops
Sleet is simply frozen raindrops and occurs when the layer of
freezing air along the surface is thicker. This causes the raindrops to freeze before reaching
Why are Freezing Rain and Sleet Dangerous?
Both of these wintry precipitation types are hazardous for
travelers. With either type, the ice can create slick spots on roadways, causing motorists to
lose control of their automobiles with little to no warning. Bridges, overpasses and elevated
roadways are especially suseptible to icing as they are surrounded on all sides by the cold air and
freeze more quickly.
In addition, ice caused by freezing rain can rapidly add weight to
tree branches and power lines, causing them to snap or break. In addition to these fallen
branches causing damage to whatever they land on, power outages may also occur.
How is Icing Caused by Freezing Rain Measured?
Ice accumulation from freezing rain does not coat the surface of
objects evenly. Gravity will usually cause the rain water to run to the underside of an object
before it freezes. Wind can create the same effect. In either case, the result would be
a thicker coating of ice on one side of the object compared to the opposite side.
You can accurately estimate the thickness of the ice with the method
below. You will need a ruler and possibly a piece of paper and pencil.
1. Locate an ice-covered object that is out in the open. A small tree branch in the middle of
the yard or clothesline is usually easiest to handle.
2. Move to a position where you can see both the thickest and thinnest portions of ice coating the
object from one side to the other.
3. Using the ruler, measure the thickest part of the ice, from the edge of the object to the edge
of the ice. Record that value on your paper.
4. Similarly, measure the thinest part of the ice, from the edge of the object to the edge of the
ice. Record that value on your paper.
5. Add the two values together and then divide by two. The resulting value is your ice
How is Sleet Measured?
Sleet is measured much the same way snow depth is
measured. You will need a ruler, and possibly a piece of paper and a pen.
1. Locate a surface that is solid, level and in the
open. Avoid measuring sleet depth under trees or directly next to buildings.
2. Slide the ruler directly downward into the sleet until it reaches the ground.
3. Read the value on the ruler to the nearest tenth of an inch, if possible.
4. Record this value on your piece of paper.
How Do I Report Freezing Rain and Sleet to the National Weather Service (NWS)?
Complete our storm report form at http://www.erh.noaa.gov/rnk/LSR
When making your report, please remember to include
the following information, if known:
The time you measured the sleet or
Your location, as specifically as
The time the sleet or icing began.
Hazardous road conditions.
Any damage caused by the icing, including downed tree
branches or powerlines.