How sun and aspect change the snow
Two slopes on the same mountain, on the same day, can hold completely different snow. The biggest reason is which way they face.
Snow explained
Short explainers on the processes behind Snowvy's modelled conditions: sun and aspect, wind, buried frost, crusts and facets, and what a model can and cannot tell you.
Two slopes on the same mountain, on the same day, can hold completely different snow. The biggest reason is which way they face.
Snowvy shows modelled snow conditions. Here is what that means, why it can be wrong, and why it never replaces the avalanche bulletin.
Surface hoar is beautiful to ski through and notorious once it is buried. It is one of the persistent weak layers avalanche forecasters watch most closely.
Wind moves more snow around a mountain than most people expect. Where it drops that snow, it can build a slab.
A crust feels solid underfoot. The trouble is often what grows next to it.
Most snow bonds and strengthens within days of falling. Some layers don't, and can stay weak for most of a season.
Water changes snow faster than anything else. A slope can go from firm to slushy in a few hours.
A storm is what skiers wait for. It is also when the snowpack changes most quickly.
Snowvy aims to cover every snowy mountain on Earth. Not every place gets the same detail, so every place says what it has.
The snowpack layers explain what is inside the snow. The surface layer, now being built, answers a simpler question: what will my skis meet here at 11:00, and why?
Modelled, not an avalanche forecast. Snowvy explains the snowpack; it never says a slope is safe. Read your regional avalanche bulletin and make your own decisions.