<?xml version="1.0" encoding="UTF-8" standalone="no"?>
<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">
  <metaDataProperty>
    <MetaData>
      <dateTimeReport>2022-02-04T16:00:00.003Z</dateTimeReport>
      <srcRef>
        <Operation>
          <name>Avalanche.report</name>
        </Operation>
      </srcRef>
    </MetaData>
  </metaDataProperty>
  <observations>
    <Bulletin gml:id="4a82a3e8-3661-4a6f-981c-3940707fe93f" xml:lang="en">
      <metaDataProperty>
        <MetaData>
          <dateTimeReport>2022-02-04T16:00:00.003Z</dateTimeReport>
          <srcRef>
            <Operation>
              <name>Avalanche.report</name>
            </Operation>
          </srcRef>
        </MetaData>
      </metaDataProperty>
      <validTime>
        <TimePeriod>
          <beginPosition>2022-02-04T23:00:00Z</beginPosition>
          <endPosition>2022-02-05T23:00:00Z</endPosition>
        </TimePeriod>
      </validTime>
      <srcRef>
        <Operation>
          <name>Avalanche.report</name>
        </Operation>
      </srcRef>
      <locRef xlink:href="ES-CT-L-02"/>
      <locRef xlink:href="ES-CT-L-03"/>
      <locRef xlink:href="ES-CT-L-01"/>
      <bulletinResultsOf>
        <BulletinMeasurements>
          <dangerRatings>
            <DangerRating>
              <validElevation xlink:href="ElevationRange_2000Hi"/>
              <mainValue>1</mainValue>
            </DangerRating>
            <DangerRating>
              <validElevation xlink:href="ElevationRange_2000Lw"/>
              <mainValue>1</mainValue>
            </DangerRating>
          </dangerRatings>
          <avProblems>
            <AvProblem>
              <type>new snow</type>
              <validAspect xlink:href="AspectRange_n"/>
              <validAspect xlink:href="AspectRange_nw"/>
              <validAspect xlink:href="AspectRange_w"/>
              <validAspect xlink:href="AspectRange_sw"/>
              <validAspect xlink:href="AspectRange_ne"/>
              <validAspect xlink:href="AspectRange_e"/>
              <validAspect xlink:href="AspectRange_se"/>
              <validAspect xlink:href="AspectRange_s"/>
              <validElevation xlink:href="ElevationRange_2000Hi"/>
            </AvProblem>
            <AvProblem>
              <type>gliding snow</type>
              <validAspect xlink:href="AspectRange_w"/>
              <validAspect xlink:href="AspectRange_sw"/>
              <validAspect xlink:href="AspectRange_e"/>
              <validAspect xlink:href="AspectRange_se"/>
              <validAspect xlink:href="AspectRange_s"/>
              <validElevation xlink:href="ElevationRange_1800Hi"/>
            </AvProblem>
          </avProblems>
          <tendency>
            <type>steady</type>
            <validTime>
              <TimePeriod>
                <beginPosition>2022-02-05T23:00:00Z</beginPosition>
                <endPosition>2022-02-06T23:00:00Z</endPosition>
              </TimePeriod>
            </validTime>
          </tendency>
          <avActivityHighlights>Dry snow slides and gliding avalanches are possible in isolated cases.</avActivityHighlights>
          <avActivityComment>As the temperature drops a generally favourable avalanche situation will prevail. In particular very steep shady slopes as well as near-ridge sunny slopes: As a consequence of the new snow only isolated small dry snow slides are possible. In addition very occasional small and, in isolated cases, medium-sized gliding avalanches are possible.</avActivityComment>
          <snowpackStructureComment>Saturday: Over a wide area 2 to 5 cm of snow, and even more in some localities, will fall until the early morning above approximately 2000 m. The new snow will be deposited on a crust in all aspects. This snow is bonding poorly with the old snowpack in particular on shady slopes. Sunny slopes: The surface of the snowpack has frozen to form a strong crust and will hardly soften at all. Shady slopes: In many places there is a danger of falling on the hard snow surface. Faceted weak layers exist in the centre of the old snowpack in particular in places that are protected from the wind. &lt;br/&gt; Above approximately 2000 m there are 100 to 200 cm of snow, and even more in some localities. Snow depths vary greatly at elevated altitudes, depending on the infuence of the wind.</snowpackStructureComment>
          <tendencyComment>Sunday: Slight increase in danger of moist avalanches as a consequence of warming during the day and solar radiation.</tendencyComment>
        </BulletinMeasurements>
      </bulletinResultsOf>
    </Bulletin>
  </observations>
</ObsCollection>
