A strong ridge of high pressure setting up along the B.C. coastline will become the main weather-maker for the west – including in southern Alberta.
In a classic adiabatic pattern, snow will fall on the B.C. side of the Rockies on Wednesday leaving dry air to descend along the leeward side – the Alberta side – of the mountains.
As that dry air flows toward the foothills, it will gain in temperature faster than it lost in temperature on its ascent on the windward side of the range.
The result will be a persistent westerly pattern with elevated temperatures and enhanced evaporation – or snow melt across southern Alberta.
Daytime highs are expected to remain above freezing in Calgary starting Tuesday, and overnight lows will be warmer than the average daytime highs at times.
Since January is typically one of the coldest months across the region, any precipitation that does …