Understanding and Assessing Impacts
An ice storm is formed under a particular set of atmospheric conditions in which a layer of warm is sandwiched between two layers of cold air. Snow forms in the upper cold layer and passes through the warm air on its way towards the ground, melting into rain as it does so. This rain then passes through the lower layer of cold air but instead of freezing, it becomes supercooled. That is to say, the temperature of a drop of water will be below the freezing point (0°C) but will not have sufficient time to turn to ice. When this supercooled rain lands on a surface, it almost immediately freezes, coating the surface it landed on in a film of ice. These kinds of events are common in Canada. The reforestation program in Brampton was initiated in the wake of a major ice storm in 1998 and the city was again struck by another major ice storm only 15 years later in 2013. It is also likely that freezing rain and ice storms are going to be more common in the Winter months in Southern Ontario and Quebec, with some reports indicating the potential for a 40% increase in such incidents.