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<ObsCollection xmlns="http://caaml.org/Schemas/V5.0/Profiles/BulletinEAWS" xmlns:gml="http://www.opengis.net/gml" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="en" xsi:schemaLocation="http://caaml.org/Schemas/V5.0/Profiles/BulletinEAWS http://caaml.org/Schemas/V5.0/Profiles/BulletinEAWS/CAAMLv5_BulletinEAWS.xsd">
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    <Bulletin gml:id="84224997-1be6-4b06-9efb-170b998bfbf1" xml:lang="en">
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        <Operation>
          <name>Avalanche.report</name>
        </Operation>
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      <locRef xlink:href="AT-08-05-01"/>
      <locRef xlink:href="AT-08-05-02"/>
      <locRef xlink:href="AT-08-06"/>
      <locRef xlink:href="AT-08-01"/>
      <locRef xlink:href="AT-08-03-02"/>
      <locRef xlink:href="AT-08-02"/>
      <locRef xlink:href="AT-08-03-01"/>
      <locRef xlink:href="AT-08-04"/>
      <bulletinResultsOf>
        <BulletinMeasurements>
          <dangerRatings>
            <DangerRating>
              <validElevation xlink:href="ElevationRange_2200Hi"/>
              <mainValue>2</mainValue>
            </DangerRating>
            <DangerRating>
              <validElevation xlink:href="ElevationRange_2200Lw"/>
              <mainValue>2</mainValue>
            </DangerRating>
          </dangerRatings>
          <avProblems>
            <AvProblem>
              <type>old snow</type>
              <validAspect xlink:href="AspectRange_nw"/>
              <validAspect xlink:href="AspectRange_w"/>
              <validAspect xlink:href="AspectRange_e"/>
              <validAspect xlink:href="AspectRange_ne"/>
              <validAspect xlink:href="AspectRange_n"/>
              <validElevation xlink:href="ElevationRange_2200Hi"/>
            </AvProblem>
            <AvProblem>
              <type>wet snow</type>
              <validAspect xlink:href="AspectRange_nw"/>
              <validAspect xlink:href="AspectRange_ne"/>
              <validAspect xlink:href="AspectRange_n"/>
              <validElevation>
                <elevationRange uom="m">
                  <beginPosition>1800</beginPosition>
                  <endPosition>2200</endPosition>
                </elevationRange>
              </validElevation>
            </AvProblem>
          </avProblems>
          <tendency>
            <type>steady</type>
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              <TimePeriod>
                <beginPosition>2026-04-09T15:00:00Z</beginPosition>
                <endPosition>2026-04-10T15:00:00Z</endPosition>
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            </validTime>
          </tendency>
          <wxSynopsisComment>On Thursday, no longer brilliant sunshine, but good mountain weather. It will remain dry, quite sunny and mild. During the course of the day, high-altitude clouds will move in high above the summits. They will hamper the sunlight, bring about diffuse light conditions. Temperature at 2000m: 6 degrees; at 3000m: -1 degree. Brisk northwesterly winds at high altitudes.</wxSynopsisComment>
          <avActivityHighlights>Swiftly rising daytime avalanche danger. Near-surface weak layers can often be triggered by winter sports enthusiasts.</avActivityHighlights>
          <avActivityComment>Following a night of clear skies, generally favorable backcountry touring conditions in early morning. However, avalanche danger, particularly on very steep north-facing slopes, increases rapidly at 1800-2200m due to solar radiation and daytime warming in all aspects, particularly below 2400m, also above that altitude on very steep sun-exposed slopes. Naturally triggered avalanches can be expected; persons can trigger wet-snow slab avalanches. If near-surface avalanches fracture down to deeper layers of the snowpack they can, in isolated cases, grow to large size. In addition, winter sports enthusiasts can trigger near-surface weak layers on high-altitude shady slopes. Danger zone are impossible to recognize. Attention: danger of taking a fall on hardened snowpack surfaces on steep slopes.</avActivityComment>
          <snowpackStructureComment>Good nocturnal outgoing longwave radiation will generate a gradually thicker melt-freeze crust which, however, will swiftly soften up during the course of the day. At altitudes between 1800 and 2200m the snowpack (also on north-facing slopes) is thoroughly wet and the ground-level rotten snow is extremely prone to triggering already in early morning. On high-altitude shady steep slopes there are unfavorable intermediate layers in the uppermost metre of the snowpack which in places can be triggered. A solid mid-section of compact layers inside the snowpack blankets a fundament of buried hoar and faceted crystals.</snowpackStructureComment>
          <tendencyComment>Due to reduced nocturnal longwave outgoing radiation on Thursday night, wet-snow problem will predominate already in early morning on Friday.</tendencyComment>
          <generalHeadlineComment>Swiftly rising daytime avalanche danger</generalHeadlineComment>
        </BulletinMeasurements>
      </bulletinResultsOf>
    </Bulletin>
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        <Operation>
          <name>Avalanche.report</name>
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      <locRef xlink:href="AT-08-05-01"/>
      <locRef xlink:href="AT-08-05-02"/>
      <locRef xlink:href="AT-08-06"/>
      <locRef xlink:href="AT-08-01"/>
      <locRef xlink:href="AT-08-03-02"/>
      <locRef xlink:href="AT-08-02"/>
      <locRef xlink:href="AT-08-03-01"/>
      <locRef xlink:href="AT-08-04"/>
      <bulletinResultsOf>
        <BulletinMeasurements>
          <dangerRatings>
            <DangerRating>
              <validElevation xlink:href="ElevationRange_2800Hi"/>
              <mainValue>2</mainValue>
            </DangerRating>
            <DangerRating>
              <validElevation xlink:href="ElevationRange_2800Lw"/>
              <mainValue>3</mainValue>
            </DangerRating>
          </dangerRatings>
          <avProblems>
            <AvProblem>
              <type>wet snow</type>
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              <validAspect xlink:href="AspectRange_e"/>
              <validAspect xlink:href="AspectRange_se"/>
              <validAspect xlink:href="AspectRange_s"/>
              <validAspect xlink:href="AspectRange_sw"/>
              <validAspect xlink:href="AspectRange_w"/>
              <validAspect xlink:href="AspectRange_ne"/>
              <validAspect xlink:href="AspectRange_n"/>
              <validElevation xlink:href="ElevationRange_2800Lw"/>
            </AvProblem>
            <AvProblem>
              <type>old snow</type>
              <validAspect xlink:href="AspectRange_nw"/>
              <validAspect xlink:href="AspectRange_e"/>
              <validAspect xlink:href="AspectRange_w"/>
              <validAspect xlink:href="AspectRange_ne"/>
              <validAspect xlink:href="AspectRange_n"/>
              <validElevation xlink:href="ElevationRange_2200Hi"/>
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          </avProblems>
          <tendency>
            <type>steady</type>
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                <beginPosition>2026-04-09T15:00:00Z</beginPosition>
                <endPosition>2026-04-10T15:00:00Z</endPosition>
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            </validTime>
          </tendency>
          <wxSynopsisComment>On Thursday, no longer brilliant sunshine, but good mountain weather. It will remain dry, quite sunny and mild. During the course of the day, high-altitude clouds will move in high above the summits. They will hamper the sunlight, bring about diffuse light conditions. Temperature at 2000m: 6 degrees; at 3000m: -1 degree. Brisk northwesterly winds at high altitudes.</wxSynopsisComment>
          <avActivityHighlights>Swiftly rising daytime avalanche danger. Near-surface weak layers can often be triggered by winter sports enthusiasts.</avActivityHighlights>
          <avActivityComment>Following a night of clear skies, generally favorable backcountry touring conditions in early morning. However, avalanche danger, particularly on very steep north-facing slopes, increases rapidly at 1800-2200m due to solar radiation and daytime warming in all aspects, particularly below 2400m, also above that altitude on very steep sun-exposed slopes. Naturally triggered avalanches can be expected; persons can trigger wet-snow slab avalanches. If near-surface avalanches fracture down to deeper layers of the snowpack they can, in isolated cases, grow to large size. In addition, winter sports enthusiasts can trigger near-surface weak layers on high-altitude shady slopes. Danger zone are impossible to recognize. Attention: danger of taking a fall on hardened snowpack surfaces on steep slopes.</avActivityComment>
          <snowpackStructureComment>Good nocturnal outgoing longwave radiation will generate a gradually thicker melt-freeze crust which, however, will swiftly soften up during the course of the day. At altitudes between 1800 and 2200m the snowpack (also on north-facing slopes) is thoroughly wet and the ground-level rotten snow is extremely prone to triggering already in early morning. On high-altitude shady steep slopes there are unfavorable intermediate layers in the uppermost metre of the snowpack which in places can be triggered. A solid mid-section of compact layers inside the snowpack blankets a fundament of buried hoar and faceted crystals.</snowpackStructureComment>
          <tendencyComment>Due to reduced nocturnal longwave outgoing radiation on Thursday night, wet-snow problem will predominate already in early morning on Friday.</tendencyComment>
          <generalHeadlineComment>Swiftly rising daytime avalanche danger</generalHeadlineComment>
        </BulletinMeasurements>
      </bulletinResultsOf>
    </Bulletin>
    <Bulletin gml:id="6b176b71-f841-4c03-91ed-fbfb621e9eb5" xml:lang="en">
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          <name>Avalanche.report</name>
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      <locRef xlink:href="AT-08-07"/>
      <bulletinResultsOf>
        <BulletinMeasurements>
          <dangerRatings>
            <DangerRating>
              <mainValue>1</mainValue>
            </DangerRating>
          </dangerRatings>
          <avProblems>
            <AvProblem>
              <type>gliding snow</type>
              <validAspect xlink:href="AspectRange_nw"/>
              <validAspect xlink:href="AspectRange_s"/>
              <validAspect xlink:href="AspectRange_sw"/>
              <validAspect xlink:href="AspectRange_n"/>
              <validAspect xlink:href="AspectRange_se"/>
              <validAspect xlink:href="AspectRange_w"/>
              <validAspect xlink:href="AspectRange_ne"/>
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          </avProblems>
          <tendency>
            <type>decreasing</type>
            <validTime>
              <TimePeriod>
                <beginPosition>2026-04-09T15:00:00Z</beginPosition>
                <endPosition>2026-04-10T15:00:00Z</endPosition>
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            </validTime>
          </tendency>
          <wxSynopsisComment>On Thursday, no longer brilliant sunshine, but good mountain weather. It will remain dry, quite sunny and mild. During the course of the day, high-altitude clouds will move in high above the summits. They will hamper the sunlight, bring about diffuse light conditions. Temperature at 2000m: 6 degrees; at 3000m: -1 degree. Brisk northwesterly winds at high altitudes.</wxSynopsisComment>
          <avActivityHighlights>Main danger: wet-snow avalanches</avActivityHighlights>
          <avActivityComment>Avalanche danger is low in the morning and rises to moderate during the course of the day. On steep slopes with lots of snow and a smooth underground which have not yet discharged, glide-snow avalanches can trigger at any time of day or night in all aspects. Zones below glide cracks should be avoided. Due to daytime warming and solar radiation, wet loose-snow avalanches can trigger naturally, particularly on extremely steep slopes. Avalanches can grow to medium size and place exposed hiking trails at risk.</avActivityComment>
          <snowpackStructureComment>South-facing slopes are frequently bare of snow. Where there’s a snowpack on the ground, it’s thoroughly wet.</snowpackStructureComment>
          <tendencyComment>As a result of dropping temperatures, avalanche danger will decrease on Friday.</tendencyComment>
          <generalHeadlineComment>Swiftly rising daytime avalanche danger</generalHeadlineComment>
        </BulletinMeasurements>
      </bulletinResultsOf>
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      <locRef xlink:href="AT-08-07"/>
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          <dangerRatings>
            <DangerRating>
              <mainValue>2</mainValue>
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          <avProblems>
            <AvProblem>
              <type>wet snow</type>
              <validAspect xlink:href="AspectRange_nw"/>
              <validAspect xlink:href="AspectRange_s"/>
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              <validAspect xlink:href="AspectRange_w"/>
              <validAspect xlink:href="AspectRange_ne"/>
              <validAspect xlink:href="AspectRange_e"/>
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            <type>decreasing</type>
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                <endPosition>2026-04-10T15:00:00Z</endPosition>
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            </validTime>
          </tendency>
          <wxSynopsisComment>On Thursday, no longer brilliant sunshine, but good mountain weather. It will remain dry, quite sunny and mild. During the course of the day, high-altitude clouds will move in high above the summits. They will hamper the sunlight, bring about diffuse light conditions. Temperature at 2000m: 6 degrees; at 3000m: -1 degree. Brisk northwesterly winds at high altitudes.</wxSynopsisComment>
          <avActivityHighlights>Main danger: wet-snow avalanches</avActivityHighlights>
          <avActivityComment>Avalanche danger is low in the morning and rises to moderate during the course of the day. On steep slopes with lots of snow and a smooth underground which have not yet discharged, glide-snow avalanches can trigger at any time of day or night in all aspects. Zones below glide cracks should be avoided. Due to daytime warming and solar radiation, wet loose-snow avalanches can trigger naturally, particularly on extremely steep slopes. Avalanches can grow to medium size and place exposed hiking trails at risk.</avActivityComment>
          <snowpackStructureComment>South-facing slopes are frequently bare of snow. Where there’s a snowpack on the ground, it’s thoroughly wet.</snowpackStructureComment>
          <tendencyComment>As a result of dropping temperatures, avalanche danger will decrease on Friday.</tendencyComment>
          <generalHeadlineComment>Swiftly rising daytime avalanche danger</generalHeadlineComment>
        </BulletinMeasurements>
      </bulletinResultsOf>
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  </observations>
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