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    <publicationTime>2021-03-05T16:00:00Z</publicationTime>
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      <startTime>2021-03-05T23:00:00Z</startTime>
      <endTime>2021-03-06T23:00:00Z</endTime>
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    <source>
      <operation>
        <name>Avalanche.report</name>
        <website>http://conselharan2.cyberneticos.net/</website>
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    <region id="ES-CT-L-02">
      <name>Southern limit of Aran</name>
    </region>
    <region id="ES-CT-L-03">
      <name>South slope of Aran</name>
    </region>
    <region id="ES-CT-L-01">
      <name>North and center of Aran</name>
    </region>
    <dangerRating>
      <mainValue>low</mainValue>
      <artificialDangerRating>no_rating</artificialDangerRating>
      <naturalDangerRating>no_rating</naturalDangerRating>
    </dangerRating>
    <tendency>
      <type>increasing</type>
      <validTime>
        <startTime>2021-03-06T23:00:00Z</startTime>
        <endTime>2021-03-07T23:00:00Z</endTime>
      </validTime>
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    <avalancheActivityHighlights>The avalanche conditions are mostly favourable.</avalancheActivityHighlights>
    <avalancheActivityComment>The old snowpack remains generally well bonded. &lt;br/&gt; &lt;br/&gt; Weak layers in the old snowpack can be released in isolated cases and mostly by large additional loads also on extremely steep shady slopes. Areas where the snow cover is rather shallow where hard layers are lying on a weakly bonded old snowpack are especially unfavourable. In very isolated cases the avalanches in these loacations are large.</avalancheActivityComment>
    <snowpackStructureComment>The weather will be very cloudy. 2 to 5 cm of snow will fall above approximately 2000 m. The light wind will transport only a little snow. &lt;br/&gt; High altitudes: The snowpack is favourably layered; its surface consists of loosely bonded snow. &lt;br/&gt; Intermediate altitudes: The surface of the snowpack will freeze very little. &lt;br/&gt; At low altitude from a snow sport perspective, in most cases insufficient snow is lying.</snowpackStructureComment>
    <tendencyComment>Slight increase in danger of dry avalanches as a consequence of the new snow.</tendencyComment>
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