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          <snowpackStructureComment>Faceted weak layers exist in the old snowpack, especially on shady slopes above approximately 2200 m, as well as on east and west facing slopes above approximately 2400 m. &lt;br/&gt; The wind slabs are in individual cases still prone to triggering above approximately 2600 m. &lt;br/&gt; Sunshine and high temperatures will give rise as the day progresses to increasing moistening of the snowpack. These conditions will bring about a gradual weakening of the snowpack in particular on steep sunny slopes.</snowpackStructureComment>
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          <snowpackStructureComment>Faceted weak layers exist in the old snowpack, especially on shady slopes above approximately 2200 m, as well as on east and west facing slopes above approximately 2400 m. &lt;br/&gt; The wind slabs are in individual cases still prone to triggering above approximately 2600 m. &lt;br/&gt; Sunshine and high temperatures will give rise as the day progresses to increasing moistening of the snowpack. These conditions will bring about a gradual weakening of the snowpack in particular on steep sunny slopes.</snowpackStructureComment>
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          <snowpackStructureComment>The weather conditions facilitated a substantial strengthening of the snowpack. Outgoing longwave radiation during the night was good over a wide area. &lt;br/&gt; Sunshine and high temperatures will give rise as the day progresses to gradual softening of the snowpack especially on sunny slopes. These conditions will bring about a substantial weakening of the snowpack from midday.</snowpackStructureComment>
          <tendencyComment>Saturday: The avalanche danger will increase during the day. Wet snow represents the main danger.</tendencyComment>
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          <snowpackStructureComment>Sunshine and high temperatures will give rise as the day progresses to gradual moistening of the snowpack in particular on sunny slopes. These conditions will bring about a weakening of the snowpack. &lt;br/&gt; In some cases the wind slabs have bonded still only poorly with the old snowpack. In some places wind slabs are lying on a hard crust. &lt;br/&gt; Individual weak layers exist in the old snowpack in particular on shady slopes. This applies above approximately 2200 m. &lt;br/&gt;</snowpackStructureComment>
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          <avActivityHighlights>Wind slabs are to be evaluated with care and prudence. As the day progresses as a consequence of warming there will be a gradual increase in the danger of moist and wet avalanches.</avActivityHighlights>
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          <avActivityHighlights>Wet avalanches as the day progresses.</avActivityHighlights>
          <avActivityComment>Avalanches can in isolated cases be released by people, especially on very steep shady slopes at elevated altitudes. &lt;br/&gt; On sunny slopes mostly small wet avalanches are to be expected as a consequence of warming during the day and solar radiation.</avActivityComment>
          <snowpackStructureComment>Hardly any weak layers exist in the old snowpack. &lt;br/&gt; Sunshine and high temperatures will give rise as the day progresses to increasing moistening of the snowpack. These conditions will bring about a gradual weakening of the snowpack in particular on steep sunny slopes.</snowpackStructureComment>
          <tendencyComment>Significant warming. Increase in danger of wet avalanches in the course of the day.</tendencyComment>
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