The large temperature difference within a few centimetres in the snow cover promotes the build-up transformation. As a result, thin, angular layers can form, which are predominantly present over large areas. The incipient weak layer can form in all exposures, but is increasingly found in sun-exposed terrain, as was the case in the winter of 2018-2019.
Furthermore, the angular crystals do not form immediately during or after the snowfall, but only in the following days. When and to what extent the weak layer forms becomes apparent over time.
In combination with the gm. 4, a melting hard layer usually also forms. Either a relatively warm snow surface is hardened by a drop in temperature, or a cold snow surface is moistened by the onset of warming (e.g. during wet snowfall or rain), which can also lead to the formation of a thin layer of melted snow.