Calgary winters don’t stay frozen. A chinook strips the snow off your roof in January, the melt runs for the eaves, and whatever doesn’t drain refreezes after dark. A trough with proper slope and clear downspouts moves that water while it’s still liquid. A trough holding standing water freezes into a solid bar, and ice builds on ice from there. That’s why we set slope with a level instead of eyeballing it, and place downspouts where melt can actually leave, not where they’re easiest to hang.
The other half of the ice problem starts inside the attic. Warm air leaking up from the house heats the roof deck, snow melts from underneath, and the runoff refreezes over the cold overhang no matter how well the trough below drains. If you fight thick ice at the eaves every winter, the lasting fix usually starts with attic airflow. Our soffit & fascia page explains how that ventilation works.