How Ice Dams Form on GTA Roofs
Southern Ontario winters are unusually hard on roofs because temperatures swing above and below freezing so often. A sunny afternoon at 2°C followed by a night at −12°C is the perfect recipe for ice dams. Warm air leaking from the living space into the attic heats the underside of the roof deck, snow on the upper roof melts, and that meltwater runs down to the overhang. The overhang sits outside the heated envelope of the house, so it is much colder, and the water refreezes there.
Night after night, that refrozen water builds into a ridge of ice along the eaves and inside the eavestrough. Once the ridge is tall enough, new meltwater has nowhere to go. It pools behind the ice and works its way up and under the shingles, which are designed to shed water downhill, not hold back standing water. The result is a leak that shows up as stained ceilings, wet insulation, peeling paint around windows, or water running down interior walls, often in the middle of February when roof repairs are hardest to do.
Homes in Toronto, North York, Etobicoke and older parts of the inner suburbs are especially prone because many were built with modest attic insulation, shallow roof pitches, and limited soffit ventilation. Bungalows and 1.5-storey homes with finished upper floors and knee walls are some of the most common ice dam homes we see across the GTA.








