High daytime freezing levels and mild overnight temperatures will stress the snowpack, with the greatest concern for thin snowpack areas where buried crusts and weak layers may become reactive.
Stick to conservative, low-angle, and supported terrain features. Avoid overhead hazard during peak warming and sunshine.
Multiple crusts exist throughout the snowpack that may form ideal sliding layers for avalanche activity as warm temperatures weaken the snowpack.
Avoid slopes that have moist or wet surface snow in the afternoon when warming is expected to be most intense. Warming will be amplified on steep, sun-affected slopes around rocky outcrops.
Stick to shaded slopes earlier in the day if you choose to venture out, and head out of the backcountry before peak warming.
The base of the snowpack remains very weak. Deep persistent slab avalanches continue to be reported adjacent forecast areas with similar snowpack structures.
This is a low-probability/high-consequence avalanche problem as this layer is deeply buried near the ground. Avoid thin, rocky start zones and shallow areas with variable snowpack depths.
Uncertainty is high about how this layer will react to this warm weather and when it will reach the tipping point for large avalanche activity.
Observations are limited at this point in the season. If you have any observations, let us know what you are seeing through the Mountain Information Network.
Loose snow avalanches have been observed throughout the week as the sun weakens the surface snow.
Recent avalanche activity in adjacent forecast areas highlights the need to avoid rocky and thin snowpack areas for the remainder of the season. A fatal size 3 was reported from near Lake Louise on April 22nd, in a particularly thin and rocky area with a 50 cm deep snowpack. All information can be found here.
Warm temperatures will weaken the surface snow as freezing levels rise on Tuesday, breaking down surface crusts and moistening any previously dry snow to around 2500 m on all aspects. Sun-affected terrain will see the most intense warming, likely creating wet and slushy snow to mountain top.
Around 20-40 cm deep, a thick melt-freeze crust is found up to 2200 m. As temperatures increase this will become a concern for avalanche activity.
The mid snowpack is generally settled and strong at treeline and above. The exception is areas where snow depths measure less than 150 cm. In these thin areas, the mid-pack is likely weaker and more faceted. These areas will respond more rapidly to warming temperatures, becoming unstable.
A weak layer of large, sugary crystals persists at the base of the snowpack. This layer is a concern as warming affects the snowpack - particularly in thin and rocky snowpack areas.
Monday Night
Mostly cloudy. Light westerly wind. Freezing levels drop to 1700 m. Flurries possible.
Tuesday
Mostly sunny with freezing levels rising to 2500 m. Treeline temperatures around +7 °C. Moderate westerly winds. No snowfall.
Wednesday
Mostly sunny with freezing levels rising to 2800 m. Treeline temperatures of +10 °C. Moderate westerly winds.
Thursday
Full sun with freezing levels heading towards 3000 m. Treeline temperatures above +10 °C. Light westerly winds.
More details can be found in the Mountain Weather Forecast.
