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          <snowpackStructureComment>Outgoing longwave radiation during the night will be severely restricted over a wide area. The surface of the snowpack has frozen to form a strong crust only at high altitudes. In some regions rain to 2200 m. The rain will give rise to a loss of strength within the snowpack. &lt;br/&gt; &lt;br/&gt; Isolated avalanche prone weak layers exist in the top section of the snowpack in all aspects. Large-grained weak layers exist in the bottom section of the snowpack on very steep shady slopes, especially below approximately 2400 m, as well as adjacent to ridgelines at high altitudes and in high Alpine regions. &lt;br/&gt; &lt;br/&gt; At low altitude only a little snow is lying, especially on sunny slopes.</snowpackStructureComment>
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          <snowpackStructureComment>Outgoing longwave radiation during the night will be severely restricted over a wide area. The surface of the snowpack has frozen to form a strong crust only at high altitudes. In some regions rain to 2200 m. The rain will give rise to a loss of strength within the snowpack. &lt;br/&gt; &lt;br/&gt; Isolated avalanche prone weak layers exist in the top section of the snowpack in all aspects. Large-grained weak layers exist in the bottom section of the snowpack on very steep shady slopes, especially below approximately 2400 m, as well as adjacent to ridgelines at high altitudes and in high Alpine regions. &lt;br/&gt; &lt;br/&gt; At low altitude only a little snow is lying, especially on sunny slopes.</snowpackStructureComment>
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          <avActivityHighlights>In some localities increase in danger of wet avalanches as a consequence of the rain.</avActivityHighlights>
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          <snowpackStructureComment>Outgoing longwave radiation during the night will be severely restricted over a wide area. The surface of the snowpack has frozen to form a strong crust only at high altitudes. In some regions rain to 2300 m. Here the danger of wet avalanches will increase appreciably. The rain will give rise to a loss of strength within the snowpack. &lt;br/&gt; &lt;br/&gt; At high altitudes and in high Alpine regions 5 to 15 cm of snow will fall over a wide area. The new snow and wind slabs will be deposited on a weakly bonded old snowpack in particular on extremely steep shady slopes above approximately 2400 m. Large-grained weak layers exist in the bottom section of the snowpack on shady slopes. &lt;br/&gt; &lt;br/&gt; At low altitude only a little snow is lying, especially on sunny slopes.</snowpackStructureComment>
          <tendencyComment>The danger of moist and wet avalanches will already be elevated in the early morning. High altitudes and the high Alpine regions: Fresh wind slabs require caution.</tendencyComment>
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          <snowpackStructureComment>Outgoing longwave radiation during the night will be reduced in some places. In steep terrain there is a danger of falling on the hard snow surface. The surface of the snowpack will already soften in the late morning. Sunshine and high temperatures will give rise to a loss of strength within the snowpack. The snowpack will become increasingly wet all the way through. &lt;br/&gt; &lt;br/&gt; Isolated avalanche prone weak layers exist in the top section of the snowpack in all aspects. Large-grained weak layers exist in the bottom section of the snowpack on shady slopes. &lt;br/&gt; &lt;br/&gt; At low altitude only a little snow is lying, especially on sunny slopes.</snowpackStructureComment>
          <tendencyComment>Outgoing longwave radiation during the night will be reduced.</tendencyComment>
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          <avActivityHighlights>In some localities increase in danger of wet avalanches as a consequence of the rain.</avActivityHighlights>
          <avActivityComment>The danger of wet avalanches will already be elevated in the early morning. As a consequence of the rain there will be an increase in the danger of wet avalanches. Wet avalanches can in some places be released in near-surface layers by a single winter sport participant. As the penetration by moisture increases natural wet avalanches are possible, even medium-sized ones. In the regions exposed to rain caution is to be exercised in particular on very steep shady slopes and. &lt;br/&gt; &lt;br/&gt; Individual avalanche prone locations for dry avalanches are to be found in particular on near-ridge shady slopes and in areas where the snow cover is rather shallow above approximately 2600 m. Avalanches can be released, mostly by large loads. Apart from the danger of being buried, restraint should be exercised as well in view of the danger of avalanches sweeping people along and giving rise to falls.</avActivityComment>
          <snowpackStructureComment>Outgoing longwave radiation during the night will be severely restricted over a wide area. The surface of the snowpack has frozen to form a strong crust only at high altitudes. In some regions rain to 2200 m. The rain will give rise to a loss of strength within the snowpack. &lt;br/&gt; &lt;br/&gt; Isolated avalanche prone weak layers exist in the top section of the snowpack. Large-grained weak layers exist in the bottom section of the snowpack on very steep shady slopes, especially above approximately 2600 m. &lt;br/&gt; &lt;br/&gt; At low altitude only a little snow is lying, especially on sunny slopes.</snowpackStructureComment>
          <tendencyComment>The danger of wet avalanches will already be elevated in the early morning. In high Alpine regions the danger of dry avalanches will increase a little.</tendencyComment>
        </BulletinMeasurements>
      </bulletinResultsOf>
      <locRef xlink:href="IT-32-BZ-20"/>
      <locRef xlink:href="IT-32-BZ-10"/>
      <locRef xlink:href="IT-32-BZ-11"/>
      <locRef xlink:href="IT-32-BZ-12"/>
      <locRef xlink:href="IT-32-BZ-01"/>
      <locRef xlink:href="IT-32-BZ-13"/>
      <locRef xlink:href="IT-32-BZ-02"/>
      <locRef xlink:href="IT-32-BZ-14"/>
      <locRef xlink:href="IT-32-BZ-03"/>
      <locRef xlink:href="IT-32-BZ-04"/>
      <locRef xlink:href="AT-07-24"/>
      <locRef xlink:href="IT-32-BZ-05"/>
      <locRef xlink:href="AT-07-25"/>
      <locRef xlink:href="IT-32-BZ-06"/>
      <locRef xlink:href="AT-07-26"/>
      <locRef xlink:href="IT-32-BZ-07"/>
      <locRef xlink:href="AT-07-27"/>
      <locRef xlink:href="IT-32-BZ-08"/>
      <locRef xlink:href="AT-07-28"/>
      <locRef xlink:href="IT-32-BZ-09"/>
      <locRef xlink:href="AT-07-29"/>
    </Bulletin>
  </observations>
</ObsCollection>
