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      "wxSynopsisComment": null,
      "snowpackStructureComment": "In early morning the snowpack at intermediate altitudes has a melt-freeze crust capable of bearing loads, on sunny slopes it is icy. In the core of the snowpack, compact melt-freeze forms dominate, without weak layers except at ground level where there is moistness. During the course of the day, solar radiation and higher temperatures make the snowpack quite wet, thereby making it forfeit its firmness. At high altitudes, strong SW winds on Sunday night generated small snowdrift accumulations, they were deposited atop melt-freeze crusts and are prone to triggering. On shady slopes and in wind-protected terrain there is still powder to be found. On sunny slopes, the slopes below 1400 m are becoming increasingly bare. Springtime conditions reign. A daytime cycle of danger prevails. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Increasing danger of wet-snow avalanches due to solar radiation and springlike temperatures",
      "avalancheActivityComment": "In early morning, avalanche danger in the Bavarian Alps is low. As a result of springlike temperatures and solar radiation, danger levels increase to moderate during the daytime. Main problem: wet snow. As a result of the uppermost snowpack layers becoming thoroughly wet, small, in isolated cases also medium-sized wet-snow avalanches can be expected to release on sunny steep slopes. At intermediate altitudes on steep, smooth grass-covered slopes and in sparsely wooded zones, the entire snowpack can glide over the ground. Slopes with glide cracks should be circumvented / avoided. Apart from that, older snowdrift accumulations at high altitudes have persisted. These can be triggered by large additional loading, e.g. going on foot or groups not maintaining distances. Isolated avalanche prone locations occur in extremely steep terrain in NW-N-E aspects.",
      "bulletinID": "BYCAAMLGenID3637-BYCHG_PM",
      "predecessor_id": "BYCAAMLGenID3637-BYCHG"
    },
    {
      "regions": [
        {
          "regionID": "BYBGD"
        }
      ],
      "validTime": {
        "startTime": "2021-02-23T12:00:00+01:00",
        "endTime": "2021-02-23T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "W",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-02-22T17:47:56+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "In early morning the snowpack at intermediate altitudes has a melt-freeze crust capable of bearing loads, on sunny slopes it is icy. In the core of the snowpack, compact melt-freeze forms dominate, without weak layers except at ground level where there is moistness. During the course of the day, solar radiation and higher temperatures make the snowpack quite wet, thereby making it forfeit its firmness. At high altitudes, strong SW winds on Sunday night generated small snowdrift accumulations, they were deposited atop melt-freeze crusts and are prone to triggering. On shady slopes and in wind-protected terrain there is still powder to be found. On sunny slopes, the slopes below 1400 m are becoming increasingly bare. Springtime conditions reign. A daytime cycle of danger prevails. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Increasing danger of wet-snow avalanches due to solar radiation and springlike temperatures",
      "avalancheActivityComment": "In early morning, avalanche danger in the Bavarian Alps is low. As a result of springlike temperatures and solar radiation, danger levels increase to moderate during the daytime. Main problem: wet snow. As a result of the uppermost snowpack layers becoming thoroughly wet, small, in isolated cases also medium-sized wet-snow avalanches can be expected to release on sunny steep slopes. At intermediate altitudes on steep, smooth grass-covered slopes and in sparsely wooded zones, the entire snowpack can glide over the ground. Slopes with glide cracks should be circumvented / avoided. Apart from that, older snowdrift accumulations at high altitudes have persisted. These can be triggered by large additional loading, e.g. going on foot or groups not maintaining distances. Isolated avalanche prone locations occur in extremely steep terrain in NW-N-E aspects.",
      "bulletinID": "BYCAAMLGenID3637-BYBGD_PM",
      "predecessor_id": "BYCAAMLGenID3637-BYBGD"
    }
  ]
}