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      <name>Sexten Dolomites</name>
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    <region id="IT-32-TN-09">
      <name>Latemar</name>
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      <name>Southern Adamello</name>
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    <region id="IT-32-TN-01">
      <name>Adamello - Presanella</name>
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      <name>Northern Brenta - Peller</name>
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      <name>Southern Brenta</name>
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      <name>Southern Lagorai</name>
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      <name>Northern Lagorai</name>
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    <region id="AT-07-01">
      <name>Allgäu Alps</name>
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      <name>Eastern Lechtal Alps - Ammergau Alps</name>
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      <name>Val Müstair Alps</name>
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      <name>Western Verwall Mountains</name>
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      <name>Southern Stubai Alps</name>
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    <region id="IT-32-BZ-05">
      <name>Southern Zillertal Alps and High Tauern</name>
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    <region id="AT-07-14">
      <name>Northern Oetz and Stubai Alps</name>
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    <region id="IT-32-BZ-06">
      <name>Saldurn-Mastaun Ridge</name>
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      <name>Western Tuxer Alps</name>
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      <name>Texel Mountains</name>
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      <name>Eastern Tuxer Alps</name>
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      <name>Sarntal Alps</name>
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      <name>Western Pfunderer Mountains</name>
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      <name>Glockturm Range</name>
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      <name>Maddalene</name>
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      <name>Pine' - Mocheni Valley</name>
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      <name>Eastern Pfunderer Mountains</name>
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      <name>Durreck Range</name>
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      <name>Weißkugel Range</name>
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    <region id="IT-32-BZ-12">
      <name>Western Rieserferner Mountains</name>
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    <region id="AT-07-21">
      <name>Gurgler Range</name>
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    <region id="IT-32-BZ-13">
      <name>Western Deferegger Alps</name>
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    <region id="AT-07-22">
      <name>Central Stubai Alps</name>
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    <region id="IT-32-BZ-14">
      <name>Ortler Range</name>
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      <name>Northern Zillertal Alps</name>
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      <name>Ulten Valley</name>
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    <region id="AT-07-24">
      <name>Venediger Range</name>
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    <region id="IT-32-BZ-16">
      <name>Eastern Nonsberger Alps</name>
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    <region id="AT-07-25">
      <name>Eastern Rieserferner Mountains</name>
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      <name>Northern Dolomites of Fiemme</name>
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      <name>Glockner Range</name>
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      <name>Primiero - Pale di S. Martino</name>
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      <name>Eastern Deferegger Alps</name>
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      <name>Prags Dolomites</name>
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    <region id="AT-07-28">
      <name>Schober Mountains</name>
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      <name>Cembra Valley</name>
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    <region id="AT-07-29">
      <name>Lienzer Dolomites</name>
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      <name>Western Nonsberg Alps</name>
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      <name>Sole, Pejo and Rabbi</name>
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      <name>Paganella</name>
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    <region id="IT-32-TN-10">
      <name>Marzola - Valsugana</name>
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      <mainValue>low</mainValue>
      <elevation uom="m">
        <lowerBound>2400</lowerBound>
      </elevation>
      <artificialDangerRating>no_rating</artificialDangerRating>
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        <upperBound>2400</upperBound>
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      <artificialDangerRating>no_rating</artificialDangerRating>
      <naturalDangerRating>no_rating</naturalDangerRating>
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      <type>dp6</type>
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      <type>wind_drifted_snow</type>
      <dangerRating>
        <aspect>NW</aspect>
        <aspect>NE</aspect>
        <aspect>N</aspect>
        <elevation uom="m">
          <lowerBound>2400</lowerBound>
        </elevation>
        <mainValue>low</mainValue>
        <artificialDangerRating>low</artificialDangerRating>
        <artificialAvalancheSize>2</artificialAvalancheSize>
        <artificialAvalancheReleaseProbability>2</artificialAvalancheReleaseProbability>
        <artificialHazardSiteDistribution>1</artificialHazardSiteDistribution>
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      <type>increasing</type>
      <validTime>
        <startTime>2022-01-04T23:00:00Z</startTime>
        <endTime>2022-01-05T23:00:00Z</endTime>
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    <avalancheActivityComment>A favourable avalanche situation will prevail. Wind slabs represent the main danger. Avalanche prone locations for dry avalanches are to be found in particular adjacent to ridgelines above approximately 2400 m and in the vicinity of peaks. &lt;br/&gt; Dry avalanches can additionally in very isolated cases be released in deep layers by large loads. This applies in particular on extremely steep shady slopes above approximately 2400 m in areas where the snow cover is rather shallow. The number and size of avalanche prone locations will increase with altitude. &lt;br/&gt; In isolated cases avalanches are medium-sized. &lt;br/&gt; In steep terrain there is a danger of falling on the hard snow surface.</avalancheActivityComment>
    <snowpackStructureComment>As a consequence of the occasionally strong westerly wind, fresh snow drift accumulations will form. These are mostly small and in some cases prone to triggering. &lt;br/&gt; The snowpack will be subject to considerable local variations. In very isolated cases weak layers exist in the centre of the old snowpack in particular on shady slopes. This applies in particular above approximately 2400 m. Above the tree line snow depths vary greatly, depending on the infuence of the wind. On sunny slopes below approximately 2200 m only a little snow is now lying. &lt;br/&gt; The old snowpack is moist and its surface has a melt-freeze crust. This applies in particular on sunny slopes and at low and intermediate altitudes.</snowpackStructureComment>
    <tendencyComment>Increase in avalanche danger as a consequence of new snow and wind.</tendencyComment>
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    <region id="AT-07-05">
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      <name>Western Kitzbühel Alps</name>
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      <name>Wilder Kaiser Mountains - Waidring Alps</name>
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    <region id="AT-07-18">
      <name>Eastern Kitzbühel Alps</name>
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    <dangerRating>
      <mainValue>low</mainValue>
      <artificialDangerRating>no_rating</artificialDangerRating>
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    <tendency>
      <type>steady</type>
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        <startTime>2022-01-04T23:00:00Z</startTime>
        <endTime>2022-01-05T23:00:00Z</endTime>
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    <avalancheActivityHighlights>A favourable avalanche situation will prevail.</avalancheActivityHighlights>
    <avalancheActivityComment>A low (level 1) danger of gliding avalanches and snow slides exists. This applies on very steep grassy slopes.</avalancheActivityComment>
    <snowpackStructureComment>The snowpack will be stable. The old snowpack is moist and its surface has a melt-freeze crust. This applies in particular on sunny slopes, as well as at low and intermediate altitudes. &lt;br/&gt; At low and intermediate altitudes a little snow is lying. Above the tree line snow depths vary greatly, depending on the infuence of the wind.</snowpackStructureComment>
    <tendencyComment>A favourable avalanche situation will prevail.</tendencyComment>
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