| MadSci Network: Earth Sciences |
Precipitation is funny business - depending on the temperature gradient between where the precipitation originates and ground level, rain or snow will fall unchanged, or one will transform itself into the other. And then there's freezing rain... The simplest answer is that precipitation is rain above 0 degrees C and snow below 0 degrees C. If you allow a few degrees either way to compensate for marginally warmer or marginally cooler air between you and the altitude where the precipitation is formed, this is a good rule of thumb. It is also possible for snow to fall through a particularly warm layer of atmosphere to become rain or graupel (snow pellets), and conversely, for rain to fall through a cooler layer of atmosphere to become freezing rain or ice pellets. There is a common belief that snow will not fall below a certain temperature. While there is some element of fact to this myth, it is generally untrue. If the temperature is very low, and falls off at a normal rate with altitude, it is not likely to snow; since the phase change of water (ie, the point[s] where ice becomes water or water becomes vapor) is dependent on temperature), even minute amounts of water will condense out as ice fog at low temperatures. (You kind of have to be Canadian to appreciate ice fog. If you're from Florida, the only place you'll ever see ice fog is in a movie.) Snow can, however, fall at temperatures considerably (-20 to -30 degrees C) below zero, if the temperatures at the upper levels are relatively warm. An upper cold low, for instance, can kick humidity high into the atmosphere, and can also usher in very cold temperatures behind its cold front. Since snow will not get any snowier as it falls through cold air, in Canada, we often see snow accompanying bitterly cold temperatures. And, of course, should strong winds also be present, we have classical blizzard conditions. Thank goodness it's a dry cold...
Try the links in the MadSci Library for more information on Earth Sciences.