I told you I’d save it for a sunny day, so while we enjoy a rare weather phenomena today (yes, for northeast Ohio, I’m talking about the sun) I’d like to write about a topic that gets a lot of attention: the meteorology behind the different types of winter precipitation.
As I have said many times before, meteorology not only deals with conditions at earth’s surface, but also since the atmosphere is three-dimensional, deals with conditions all the way up through the troposphere. The types of precipitation: rain, snow, sleet, and freezing rain, all depend on the “thermal profile” of the troposphere. The diagram below shows the exact meaning of this.

Photo Courtesy Steve Cross
Okay, so what does this all mean? As you can tell, cold air needs to be present in the atmosphere for moisture to be present. Most precipitation occurs from a clash of a warm and cool (sometimes even cold) air mass. From the diagram, you can see at the top of the troposphere it is all snow. (There is another process which uses rain without the development of snow first [called the supercooled warm rain process] which I’m not going to go into for simplicity’s sake). This is because as you ascend in the troposphere, the temperature decreases. However, when a temperature inversion occurs, a layer of warm air invades the lower atmosphere. This inversion can be caused by a warm front, but in general this means that while you ascend in the troposphere it gets warmer before it gets colder. This is the area in red shading in our diagram. The type of precipitation which forms depends on exactly how thick this layer of warm air is, and is why it is extremely difficult to forecast some winter storms.
Rain occurs when the thermal profile is all warm air in the lower atmosphere. This is depicted in the farthest right part of the diagram.
Moving left, our next type of precip is freezing rain. Freezing rain is snow which falls through the temperature inversion and melts the snow to become rain. However, since right at the surface temperatures are 32 degrees F or below, these rain particles freeze on contact and is known of as freezing rain. You can see now why this is very difficult to predict. Meteorologists have a map which helps attempt to predict ice events. It is the 850 millibar temperature map, which gives the temperature in the lower levels of the atmosphere. However, as you can expect, one degree makes a lot of difference as to what type of precipitation occurs, so forecasters are walking a fine-line with this type of weather.
Sleet then, occurs with a larger pocket of cold air at the surface and doesn’t spend as much time in the warm air. This means that, as the snow falls into the warm air it starts melting. However, since it goes back into the cold air more quickly than the freezing rain did, it isn’t entirely melted. It re-freezes when it comes back into the cold air and often bounces off the ground. This then, doesn’t freeze on contact and is less threatening than freezing rain.
Snow, of course, is when the entire region in the lower troposphere is cold and no melting takes place. The snowflake remains a snowflake when reaching the surface.
No matter what type of wintry precipitation falls, driving is always hazardous when the temperature drops. When we forecast any type of precipitation, you should take extra caution while outdoors. Freezing rain is the most dangerous, as when it accumulates the ice can cause extreme problems. Sleet and snow accumulations, as you well know, can do the same as can rain. I can go into greater science behind the types of precipitation, but this I believe will help the common person understand the basic science behind the different types of precipitation. If you have any questions, please let me know!