Snow has a strong affinity for itself, meaning snowflakes naturally tend to bond together with a strength that varies depending on temperature and humidity. It can be said that the lower the temperature, the more the flakes tend to crystallize, turning into ice. An example of this is the so-called “powder snow,” typical of cold and dry Arctic climates. It consists of frozen flakes that, once on the ground, tend to remain separated from each other. Conversely, the so-called “wet snow” occurs in winter in temperate regions when the temperature…
Read More“RideMax Frost” tires by Bkt: the snowball effect
