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          <snowpackStructureComment>Somewhat older wind slabs are lying on the unfavourable surface of an old snowpack, especially on very steep northwest, north and northeast facing slopes above approximately 2200 m, also on very steep west and east facing slopes above approximately 2500 m, as well as on very steep southeast, south and southwest facing slopes in high Alpine regions. &lt;br/&gt; &lt;br/&gt; Towards its base, the snowpack is faceted and weak, especially on shady slopes above approximately 2200 m. &lt;br/&gt; &lt;br/&gt; Steep sunny slopes: Sunshine and high temperatures will give rise to moistening of the snowpack.</snowpackStructureComment>
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          <snowpackStructureComment>As a consequence of a sometimes strong wind from variable directions, sometimes avalanche prone wind slabs formed in the last few days. The fresh and somewhat older wind slabs are lying on the unfavourable surface of an old snowpack. &lt;br/&gt; Distinct weak layers exist in the bottom section of the snowpack in particular on steep shady slopes. This applies especially above approximately 2000 m.</snowpackStructureComment>
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          <snowpackStructureComment>Somewhat older wind slabs are lying on the unfavourable surface of an old snowpack, especially on very steep northwest, north and northeast facing slopes above approximately 2200 m, also on very steep west and east facing slopes above approximately 2500 m, as well as on very steep southeast, south and southwest facing slopes in high Alpine regions. &lt;br/&gt; &lt;br/&gt; Avalanche prone weak layers exist in the bottom section of the snowpack in particular in shady places that are protected from the wind, especially above approximately 2200 m. &lt;br/&gt; &lt;br/&gt; Steep sunny slopes: Sunshine and high temperatures will give rise to moistening of the snowpack.</snowpackStructureComment>
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          <avActivityHighlights>Wind slabs and weakly bonded old snow require caution.</avActivityHighlights>
          <avActivityComment>Weakly bonded old snow is to be evaluated with care and prudence. These avalanche prone locations are to be found in particular on steep northwest to north to northeast facing slopes, especially on very steep slopes above the tree line, as well as at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. &lt;br/&gt; The wind slabs can be released, especially by large additional loads, in particular on west to north to east facing aspects above the tree line. Avalanches can also release deeper layers of the snowpack and reach quite a large size. &lt;br/&gt; As a consequence of warming during the day and solar radiation individual mostly small moist loose snow slides are possible. This applies on very steep slopes at the base of rock walls.</avActivityComment>
          <snowpackStructureComment>As a consequence of a sometimes strong wind from variable directions, sometimes avalanche prone wind slabs formed in the last few days. The fresh and somewhat older wind slabs are lying on the unfavourable surface of an old snowpack. &lt;br/&gt; Distinct weak layers exist in the bottom section of the snowpack in particular on steep shady slopes. This applies especially above approximately 2000 m.</snowpackStructureComment>
          <tendencyComment>The avalanche danger will persist.</tendencyComment>
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          <avActivityHighlights>Wind slabs require caution.</avActivityHighlights>
          <avActivityComment>The somewhat older wind slabs can be released in isolated cases, especially on very steep shady slopes at elevated altitudes. The avalanche prone locations are to be found especially adjacent to ridgelines and in gullies and bowls. These places are rather rare clearly recognisable to the trained eye. Mostly avalanches are only small. The wind slabs are to be avoided in particular in terrain where there is a danger of falling.</avActivityComment>
          <snowpackStructureComment>The fresh and somewhat older wind slabs have bonded well with the old snowpack. They are now only very rarely prone to triggering. &lt;br/&gt; &lt;br/&gt; In very isolated cases weak layers exist in the bottom section of the snowpack on west, north and east facing slopes. This applies above approximately 2200 m.</snowpackStructureComment>
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                <endPosition>2026-03-26T16:00:00Z</endPosition>
              </TimePeriod>
            </validTime>
          </tendency>
          <avActivityHighlights>Low avalanche danger will prevail.</avActivityHighlights>
          <avActivityComment>Dry avalanches can be released, in particular by large loads, but they will be small in most cases. Individual avalanche prone locations are to be found on steep shady slopes at high altitude. &lt;br/&gt; As a consequence of warming during the day only isolated moist snow slides and avalanches are possible, but they will be mostly small, in the event of solar radiation in particular on extremely steep slopes.</avActivityComment>
          <snowpackStructureComment>Shady slopes: Isolated avalanche prone weak layers exist in the old snowpack in particular on northwest, north and northeast facing slopes. &lt;br/&gt; &lt;br/&gt; Sunny slopes: The old snowpack will be moist. The weather conditions will give rise to thorough wetting of the snowpack at intermediate and high altitudes.</snowpackStructureComment>
          <tendencyComment>Low avalanche danger will prevail.</tendencyComment>
        </BulletinMeasurements>
      </bulletinResultsOf>
    </Bulletin>
  </observations>
</ObsCollection>
