Winter Precipitation

Snow is probably the most well known type of winter precipitation.  There are, however, several other forms in which precipitation can fall during the cold winter months.  It all depends on the temperature profile of the lower atmosphere.

All precipitation starts out as snow up in the clouds.  But, as it falls toward the Earth, it can pass through one or more layers of air with different temperatures.  When the snow passes through a thick layer of warm air – above 32°F – it melts into rain.  If the warm air layer extends all the way to the ground, rain will fall at the surface.  However, if there is a thin layer of cold air – below 32°F – near the ground, the rain becomes super-cooled and freezes upon impact with anything that has a temperature of at or below freezing.  This is known as freezing rain.  It is one of the most dangerous types of winter precipitation, as it forms a glaze of ice on almost everything it comes in contact with, including roads, tree branches, and power lines.

Sleet is different than freezing rain – it is a frozen precipitation.  It falls at ground level in the form of ice-pellets. Passing through a thick layer of sub-freezing air near the surface, liquid raindrops are given enough time to re-freeze before reaching the ground. Sleet often bounces when it hits a surface, but does not stick to any objects.  It can, however, accumulate.

Snow is another type of frozen precipitation.  It takes the shape of multi-sided ice crystals, often called flakes.  Snow will fall at the surface when air temperatures are below freezing all the way from the cloud-level down to the ground.  In order for the snow to stick and accumulate, surface temperatures must also be at or below freezing.

When all of these precipitation types fall during a single storm, it is called a wintry mix.

Precipitation type depends on the temperature profile of the atmosphere.

Precipitation type depends on the temperature profile of the atmosphere.

Image Credit: NOAA