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      <name>Schober Mountains</name>
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    <avalancheActivityHighlights>Gliding avalanches require caution. Fresh wind slabs require caution.</avalancheActivityHighlights>
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      <name>Durreck Range</name>
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      <name>Western Rieserferner Mountains</name>
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      <name>Val Müstair Alps</name>
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      <naturalAvalancheReleaseProbability>1</naturalAvalancheReleaseProbability>
      <naturalHazardSiteDistribution>2</naturalHazardSiteDistribution>
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      <type>dp2</type>
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    <dangerPattern>
      <type>dp6</type>
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      <dangerRating>
        <aspect>SW</aspect>
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        <aspect>E</aspect>
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        <aspect>N</aspect>
        <aspect>W</aspect>
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      <dangerRating>
        <aspect>NW</aspect>
        <aspect>NE</aspect>
        <aspect>N</aspect>
        <elevation uom="m">
          <lowerBound>2200</lowerBound>
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    <avalancheActivityHighlights>Gliding avalanches require caution. Fresh wind slabs require caution.</avalancheActivityHighlights>
    <avalancheActivityComment>An appreciable danger of gliding avalanches exists, in particular in the regions with a lot of snow on steep grassy slopes below approximately 2600 m. Areas with glide cracks are to be avoided as far as possible. As a consequence of a strong to storm force northerly wind, sometimes avalanche prone wind slabs will form in all aspects. They are clearly recognisable to the trained eye. Weakly bonded old snow: Dry avalanches can in some places be released in the old snowpack by large loads, especially in little used backcountry terrain. This applies especially on steep shady slopes in particular above approximately 2000 m in areas where the snow cover is rather shallow. The avalanche prone locations are rather rare but are barely recognisable, even to the trained eye. Slight increase in avalanche danger as a consequence of warming during the day and solar radiation. In steep terrain there is a danger of falling on the icy crust.</avalancheActivityComment>
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    <tendencyComment>Increase in avalanche danger as a consequence of warming during the day and solar radiation. Moderate, level 2.</tendencyComment>
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    <region id="AT-07-20">
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      <name>Western Verwall Mountains</name>
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      <name>Gurgler Range</name>
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      <name>Eastern Verwall Mountains</name>
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      <name>Northern Zillertal Alps</name>
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      <name>Eastern Lechtal Alps - Ammergau Alps</name>
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      <name>Northern Oetz and Stubai Alps</name>
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      <name>Mieming Mountains</name>
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      <name>Western Tuxer Alps</name>
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      <name>Karwendel Mountains</name>
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      <name>Brandenberg Alps</name>
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      <name>Western Kitzbühel Alps</name>
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    <region id="AT-07-18">
      <name>Eastern Kitzbühel Alps</name>
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      <name>Western Lechtal Alps</name>
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      <name>Central Lechtal Alps</name>
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      <name>Glockturm Range</name>
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    <region id="AT-07-09">
      <name>Grieskogel Mountains</name>
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      <mainValue>moderate</mainValue>
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      <naturalDangerRating>moderate</naturalDangerRating>
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      <naturalHazardSiteDistribution>1</naturalHazardSiteDistribution>
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      <type>dp6</type>
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        <aspect>SW</aspect>
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        <aspect>SE</aspect>
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        <elevation uom="m">
          <upperBound>2600</upperBound>
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        <aspect>NW</aspect>
        <aspect>NE</aspect>
        <aspect>N</aspect>
        <elevation uom="m">
          <lowerBound>2400</lowerBound>
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    <avalancheActivityHighlights>Gliding snow represents the main danger. Fresh wind slabs require caution.</avalancheActivityHighlights>
    <avalancheActivityComment>A latent danger of gliding avalanches exists. This applies on steep grassy slopes. The avalanche prone locations are to be found in all aspects below approximately 2000 m and on steep sunny slopes below approximately 2600 m. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches and moist snow slides being released will increase a little. During the night as well, individual gliding avalanches are possible. In their paths avalanches can entrain large quantities of snow. These can in isolated cases reach very large size. Areas with glide cracks are to be avoided. The strong wind has transported the fresh and old snow significantly. This applies at high altitudes and in high Alpine regions. The fresh wind slabs can be released by a single winter sport participant in some cases in particular on northwest to north to northeast facing aspects above approximately 2400 m. Such avalanche prone locations are rather rare and are clearly recognisable to the trained eye. Mostly avalanches are only small. At elevated altitudes the avalanche prone locations will become more prevalent. The backcountry and freeriding conditions are generally favourable.</avalancheActivityComment>
    <snowpackStructureComment>Fresh wind slabs are lying on soft layers on northwest to north to northeast facing aspects above the tree line. Outgoing longwave radiation during the night will be good. The surface of the snowpack will soften during the day. This applies at low altitude as well as on very steep sunny slopes below approximately 2400 m. The old snowpack will be moist at low altitude. The old snowpack will be in most cases favourable.</snowpackStructureComment>
    <tendencyComment>Gliding snow represents the main danger. Slight increase in danger as a consequence of warming during the day and solar radiation.</tendencyComment>
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      </extFile>
      <extFile>
        <type>website</type>
        <description>Link to region on the website</description>
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    <publicationTime>2019-02-23T16:00:00Z</publicationTime>
    <validTime>
      <startTime>2019-02-23T23:00:00Z</startTime>
      <endTime>2019-02-24T23:00:00Z</endTime>
    </validTime>
    <source>
      <operation>
        <name>Avalanche.report</name>
        <website>https://avalanche.report</website>
      </operation>
    </source>
    <region id="AT-07-29">
      <name>Lienzer Dolomites</name>
    </region>
    <dangerRating>
      <mainValue>moderate</mainValue>
      <artificialDangerRating>moderate</artificialDangerRating>
      <artificialAvalancheSize>2</artificialAvalancheSize>
      <artificialAvalancheReleaseProbability>2</artificialAvalancheReleaseProbability>
      <artificialHazardSiteDistribution>2</artificialHazardSiteDistribution>
      <naturalDangerRating>low</naturalDangerRating>
      <naturalAvalancheReleaseProbability>1</naturalAvalancheReleaseProbability>
      <naturalHazardSiteDistribution>1</naturalHazardSiteDistribution>
    </dangerRating>
    <dangerPattern>
      <type>dp1</type>
    </dangerPattern>
    <avalancheProblem>
      <type>persistent_weak_layers</type>
      <dangerRating>
        <aspect>NE</aspect>
        <aspect>NW</aspect>
        <aspect>N</aspect>
        <elevation uom="m">
          <lowerBound>2000</lowerBound>
        </elevation>
      </dangerRating>
    </avalancheProblem>
    <tendency>
      <type>decreasing</type>
      <validTime>
        <startTime>2019-02-24T23:00:00Z</startTime>
        <endTime>2019-02-25T23:00:00Z</endTime>
      </validTime>
    </tendency>
    <avalancheActivityHighlights>Weakly bonded old snow requires caution.</avalancheActivityHighlights>
    <avalancheActivityComment>Dry avalanches can in some places be released in the old snowpack by large loads. This applies especially on very steep shady slopes in particular above approximately 2000 m in areas where the snow cover is rather shallow. Mostly the avalanches in these loacations are medium-sized. The avalanche prone locations are rather rare but are barely recognisable, even to the trained eye. Slight increase in avalanche danger as a consequence of warming during the day and solar radiation. In steep terrain there is a danger of falling on the icy crust.</avalancheActivityComment>
    <snowpackStructureComment>Outgoing longwave radiation during the night will be good. The surface of the snowpack will soften during the day. This applies at low altitude as well as on very steep sunny slopes. Isolated avalanche prone weak layers exist in the bottom section of the snowpack, in particular on shady slopes above approximately 2000 m.</snowpackStructureComment>
    <tendencyComment>The avalanche danger will decrease gradually.</tendencyComment>
  </bulletin>
  <bulletin id="c8ff2621-6694-4746-8405-72489b0e4c91" lang="en">
    <metaData>
      <extFile>
        <type>dangerRatingMap</type>
        <description>Simplified danger rating map of the region</description>
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      </extFile>
      <extFile>
        <type>website</type>
        <description>Link to region on the website</description>
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    <publicationTime>2019-02-23T16:00:00Z</publicationTime>
    <validTime>
      <startTime>2019-02-23T23:00:00Z</startTime>
      <endTime>2019-02-24T23:00:00Z</endTime>
    </validTime>
    <source>
      <operation>
        <name>Avalanche.report</name>
        <website>https://avalanche.report</website>
      </operation>
    </source>
    <region id="IT-32-BZ-18">
      <name>Gröden Dolomites</name>
    </region>
    <region id="IT-32-BZ-07">
      <name>Texel Mountains</name>
    </region>
    <region id="IT-32-BZ-19">
      <name>Prags Dolomites</name>
    </region>
    <region id="IT-32-BZ-08">
      <name>Sarntal Alps</name>
    </region>
    <region id="IT-32-BZ-20">
      <name>Sexten Dolomites</name>
    </region>
    <region id="IT-32-BZ-14">
      <name>Ortler Range</name>
    </region>
    <region id="IT-32-BZ-03">
      <name>Schnals Ridge</name>
    </region>
    <region id="IT-32-BZ-15">
      <name>Ulten Valley</name>
    </region>
    <region id="IT-32-BZ-06">
      <name>Saldurn-Mastaun Ridge</name>
    </region>
    <dangerRating>
      <mainValue>moderate</mainValue>
      <artificialDangerRating>moderate</artificialDangerRating>
      <artificialAvalancheSize>3</artificialAvalancheSize>
      <artificialAvalancheReleaseProbability>2</artificialAvalancheReleaseProbability>
      <artificialHazardSiteDistribution>2</artificialHazardSiteDistribution>
      <naturalDangerRating>low</naturalDangerRating>
      <naturalAvalancheReleaseProbability>1</naturalAvalancheReleaseProbability>
      <naturalHazardSiteDistribution>1</naturalHazardSiteDistribution>
    </dangerRating>
    <dangerPattern>
      <type>dp1</type>
    </dangerPattern>
    <dangerPattern>
      <type>dp6</type>
    </dangerPattern>
    <avalancheProblem>
      <type>persistent_weak_layers</type>
      <dangerRating>
        <aspect>NE</aspect>
        <aspect>NW</aspect>
        <aspect>N</aspect>
        <elevation uom="m">
          <lowerBound>2000</lowerBound>
        </elevation>
      </dangerRating>
    </avalancheProblem>
    <avalancheProblem>
      <type>wind_drifted_snow</type>
      <dangerRating>
        <aspect>NW</aspect>
        <aspect>NE</aspect>
        <aspect>N</aspect>
        <elevation uom="m">
          <lowerBound>2200</lowerBound>
        </elevation>
      </dangerRating>
    </avalancheProblem>
    <tendency>
      <type>steady</type>
      <validTime>
        <startTime>2019-02-24T23:00:00Z</startTime>
        <endTime>2019-02-25T23:00:00Z</endTime>
      </validTime>
    </tendency>
    <avalancheActivityHighlights>Wind slabs and weakly bonded old snow require caution.</avalancheActivityHighlights>
    <avalancheActivityComment>Dry avalanches can in some places be released in the old snowpack by large loads. This applies especially on very steep shady slopes in particular above approximately 2000 m in areas where the snow cover is rather shallow. Mostly the avalanches in these loacations are medium-sized. The avalanche prone locations are rather rare but are barely recognisable, even to the trained eye. The strong wind has transported the old snow. The fresh wind slabs in steep terrain are to be bypassed. Slight increase in avalanche danger as a consequence of warming during the day and solar radiation. In steep terrain there is a danger of falling on the icy crust.</avalancheActivityComment>
    <snowpackStructureComment>The surface of the snowpack has frozen to form a strong crust only at high altitudes, in particular on steep sunny slopes. Isolated avalanche prone weak layers exist in the bottom section of the snowpack, in particular on shady slopes above approximately 2000 m. The fresh wind slabs are easy for the trained eye to recognise and can in some cases be released easily especially at their margins.</snowpackStructureComment>
    <tendencyComment>The avalanche danger will persist. Moderate, level 2.</tendencyComment>
  </bulletin>
  <bulletin id="79e8fa9b-3cca-473e-92a1-2f0b8e40688c" lang="en">
    <metaData>
      <extFile>
        <type>dangerRatingMap</type>
        <description>Simplified danger rating map of the region</description>
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      </extFile>
      <extFile>
        <type>website</type>
        <description>Link to region on the website</description>
        <fileReferenceURI>https://avalanche.report/bulletin/2019-02-24?region=79e8fa9b-3cca-473e-92a1-2f0b8e40688c</fileReferenceURI>
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    <publicationTime>2019-02-23T16:00:00Z</publicationTime>
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      <startTime>2019-02-23T23:00:00Z</startTime>
      <endTime>2019-02-24T23:00:00Z</endTime>
    </validTime>
    <source>
      <operation>
        <name>Avalanche.report</name>
        <website>https://avalanche.report</website>
      </operation>
    </source>
    <region id="IT-32-TN-02">
      <name>Southern Adamello</name>
    </region>
    <region id="IT-32-TN-13">
      <name>Primiero - Pale di S. Martino</name>
    </region>
    <region id="IT-32-TN-01">
      <name>Adamello - Presanella</name>
    </region>
    <region id="IT-32-TN-04">
      <name>Northern Brenta - Peller</name>
    </region>
    <region id="IT-32-TN-05">
      <name>Southern Brenta</name>
    </region>
    <region id="IT-32-TN-16">
      <name>Fassa Valley</name>
    </region>
    <region id="IT-32-TN-19">
      <name>Sole, Pejo and Rabbi</name>
    </region>
    <region id="IT-32-TN-08">
      <name>Southern Lagorai</name>
    </region>
    <region id="IT-32-TN-07">
      <name>Northern Lagorai</name>
    </region>
    <region id="IT-32-TN-09">
      <name>Latemar</name>
    </region>
    <region id="IT-32-TN-20">
      <name>Maddalene</name>
    </region>
    <region id="IT-32-TN-21">
      <name>Pine' - Mocheni Valley</name>
    </region>
    <dangerRating>
      <mainValue>moderate</mainValue>
      <artificialDangerRating>low</artificialDangerRating>
      <artificialAvalancheSize>2</artificialAvalancheSize>
      <artificialAvalancheReleaseProbability>1</artificialAvalancheReleaseProbability>
      <artificialHazardSiteDistribution>1</artificialHazardSiteDistribution>
      <naturalDangerRating>moderate</naturalDangerRating>
      <naturalAvalancheReleaseProbability>1</naturalAvalancheReleaseProbability>
      <naturalHazardSiteDistribution>2</naturalHazardSiteDistribution>
    </dangerRating>
    <dangerPattern>
      <type>dp10</type>
    </dangerPattern>
    <avalancheProblem>
      <type>persistent_weak_layers</type>
      <dangerRating>
        <aspect>NE</aspect>
        <aspect>E</aspect>
        <aspect>NW</aspect>
        <aspect>N</aspect>
        <aspect>W</aspect>
        <elevation uom="m">
          <lowerBound>treeline</lowerBound>
        </elevation>
      </dangerRating>
    </avalancheProblem>
    <avalancheProblem>
      <type>wet_snow</type>
      <dangerRating>
        <aspect>SW</aspect>
        <aspect>E</aspect>
        <aspect>SE</aspect>
        <aspect>S</aspect>
        <aspect>W</aspect>
      </dangerRating>
    </avalancheProblem>
    <tendency>
      <type>steady</type>
      <validTime>
        <startTime>2019-02-24T23:00:00Z</startTime>
        <endTime>2019-02-25T23:00:00Z</endTime>
      </validTime>
    </tendency>
    <avalancheActivityHighlights>Weak layers in the lower part of the snowpack necessitate caution and restraint. As a consequence of warming during the day and solar radiation the prevalence of avalanche prone locations will increase in the afternoon.</avalancheActivityHighlights>
    <avalancheActivityComment>The wind slabs have bonded quite well with the old snowpack in particular on steep sunny slopes. These can be released, especially by large additional loads,. Faceted weak layers exist in the bottom section of the old snowpack especially on steep west, north and east facing slopes. The avalanche prone locations are to be found in particular at transitions from a shallow to a deep snowpack and in gullies and bowls, and behind abrupt changes in the terrain. A clear night will be followed in the early morning by quite favourable conditions generally, but the avalanche danger will increase later. Moist avalanches can in isolated cases penetrate near-ground layers of the snowpack and reach large size in particular on sunny slopes. Backcountry tours and off-piste skiing should be started very early and concluded timely.</avalancheActivityComment>
    <snowpackStructureComment>The snowpack will become in most cases well bonded. The surface of the snowpack has frozen to form a strong crust and will soften during the day. Wind slabs are lying on the unfavourable surface of an old snowpack in particular on extremely steep, rather lightly snow-covered shady slopes. Faceted weak layers exist in the bottom section of the snowpack in particular here.</snowpackStructureComment>
    <tendencyComment>As a consequence of warming during the day and the solar radiation, the likelihood of moist loose snow avalanches being released will increase gradually in particular on rocky sunny slopes below approximately 2500 m.</tendencyComment>
  </bulletin>
  <bulletin id="5aba7fd9-feb6-4712-80ed-cfc6c4b229b7" lang="en">
    <metaData>
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        <type>dangerRatingMap</type>
        <description>Simplified danger rating map of the region</description>
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      <extFile>
        <type>website</type>
        <description>Link to region on the website</description>
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    <publicationTime>2019-02-23T16:00:00Z</publicationTime>
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      <startTime>2019-02-23T23:00:00Z</startTime>
      <endTime>2019-02-24T23:00:00Z</endTime>
    </validTime>
    <source>
      <operation>
        <name>Avalanche.report</name>
        <website>https://avalanche.report</website>
      </operation>
    </source>
    <region id="IT-32-BZ-16">
      <name>Eastern Nonsberger Alps</name>
    </region>
    <region id="IT-32-BZ-17">
      <name>Northern Dolomites of Fiemme</name>
    </region>
    <region id="IT-32-TN-12">
      <name>Prealps</name>
    </region>
    <region id="IT-32-TN-15">
      <name>Cembra Valley</name>
    </region>
    <region id="IT-32-TN-03">
      <name>Bondone and Stivo</name>
    </region>
    <region id="IT-32-TN-14">
      <name>Vallarsa</name>
    </region>
    <region id="IT-32-TN-17">
      <name>Western Nonsberg Alps</name>
    </region>
    <region id="IT-32-TN-06">
      <name>Folgaria - Laverone</name>
    </region>
    <region id="IT-32-TN-18">
      <name>Ledro Valley</name>
    </region>
    <region id="IT-32-TN-11">
      <name>Paganella</name>
    </region>
    <region id="IT-32-TN-10">
      <name>Marzola - Valsugana</name>
    </region>
    <dangerRating>
      <mainValue>low</mainValue>
      <artificialDangerRating>low</artificialDangerRating>
      <artificialAvalancheSize>2</artificialAvalancheSize>
      <artificialAvalancheReleaseProbability>2</artificialAvalancheReleaseProbability>
      <artificialHazardSiteDistribution>1</artificialHazardSiteDistribution>
      <naturalDangerRating>low</naturalDangerRating>
      <naturalAvalancheReleaseProbability>1</naturalAvalancheReleaseProbability>
      <naturalHazardSiteDistribution>1</naturalHazardSiteDistribution>
    </dangerRating>
    <avalancheProblem>
      <type>persistent_weak_layers</type>
      <dangerRating>
        <aspect>NE</aspect>
        <aspect>NW</aspect>
        <aspect>N</aspect>
        <elevation uom="m">
          <lowerBound>treeline</lowerBound>
        </elevation>
      </dangerRating>
    </avalancheProblem>
    <avalancheProblem>
      <type>wet_snow</type>
      <dangerRating>
        <aspect>SW</aspect>
        <aspect>E</aspect>
        <aspect>SE</aspect>
        <aspect>S</aspect>
        <aspect>W</aspect>
        <elevation uom="m">
          <upperBound>2200</upperBound>
        </elevation>
      </dangerRating>
    </avalancheProblem>
    <tendency>
      <type>steady</type>
      <validTime>
        <startTime>2019-02-24T23:00:00Z</startTime>
        <endTime>2019-02-25T23:00:00Z</endTime>
      </validTime>
    </tendency>
    <avalancheActivityHighlights>Slight increase in avalanche danger as a consequence of warming during the day.</avalancheActivityHighlights>
    <avalancheActivityComment>The early morning will see quite favourable conditions generally. As the day progresses as a consequence of warming during the day and solar radiation there will be only a slight increase in the danger of moist avalanches. Avalanches can in isolated cases be released by small loads and reach medium size. The fresh wind slabs must be evaluated with care and prudence in all aspects. &lt;br/&gt; Weakly bonded old snow: Individual avalanche prone locations for dry avalanches are to be found in particular on very steep shady slopes above the tree line. In steep terrain there is a danger of falling on the icy crust.</avalancheActivityComment>
    <snowpackStructureComment>Only a little snow is lying. The surface of the snowpack has frozen to form a strong crust only at high altitudes and will soften during the day, especially on steep sunny slopes. Faceted weak layers exist in the bottom section of the snowpack in particular in shady places that are protected from the wind.</snowpackStructureComment>
    <tendencyComment>Low, level 1.</tendencyComment>
  </bulletin>
</bulletins>
