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      "snowpackStructureComment": "At intermediate altitudes a thin melt-freeze crust forms during the night which softens swiftly during the day. The sink-in depths increase significantly in all aspects late in the morning, moistness penetrates the snowpack which looses its firmness. In particular in forests and on sun-exposed slopes the water reaches the ground-level layers which promotes gliding of the snow masses. On steep shady high altitude slopes weak intermediate layers have persisted locally in the uppermost meter of the snowpack. Elsewhere the snowpack has clearly settled and the snowpack base is mostly stable. Up to about 1400 m south-facing slopes are becoming increasingly bare of snow.  Springlike conditions are set to continue. Backcountry ski, snowshoe or snowboard tours should be started early and be terminated early. Please note: public ski areas are currently not supervised and not secured from avalanche danger.",
      "avalancheActivityHighlights": "Wet-snow avalanches in all aspects during the course of the day!",
      "avalancheActivityComment": "Avalanche danger in the Bavarian Alps will increase from low to moderate during the course of the day. Main problem: wet snow. Wet loose-snow avalanches can be expected up to the summits in steep rocky terrain. On smooth grass-covered slopes at intermediate altitude that have not yet discharged and in wooded zones the wet snow masses can also start gliding over the ground. Avalanches can attain medium size with an increased probability of triggering in the second half of the day. In addition, slab avalanches can be triggered on isolated extremely steep shady high altitude slopes in the uppermost meter of the old snowpack. This is in general now only possible by large additional loading in places where snow is shallow. The slabs that release are mostly small.",
      "bulletinID": "BYCAAMLGenID3711-BYCHG_PM",
      "predecessor_id": "BYCAAMLGenID3711-BYCHG"
    },
    {
      "regions": [
        {
          "regionID": "BYBGD"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T12:00:00+01:00",
        "endTime": "2021-03-30T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "W",
              "NW",
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-03-29T18:11:39+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "At intermediate altitudes a thin melt-freeze crust forms during the night which softens swiftly during the day. The sink-in depths increase significantly in all aspects late in the morning, moistness penetrates the snowpack which looses its firmness. In particular in forests and on sun-exposed slopes the water reaches the ground-level layers which promotes gliding of the snow masses. On steep shady high altitude slopes weak intermediate layers have persisted locally in the uppermost meter of the snowpack. Elsewhere the snowpack has clearly settled and the snowpack base is mostly stable. Up to about 1400 m south-facing slopes are becoming increasingly bare of snow.  Springlike conditions are set to continue. Backcountry ski, snowshoe or snowboard tours should be started early and be terminated early. Please note: public ski areas are currently not supervised and not secured from avalanche danger.",
      "avalancheActivityHighlights": "Wet-snow avalanches in all aspects during the course of the day!",
      "avalancheActivityComment": "Avalanche danger in the Bavarian Alps will increase from low to moderate during the course of the day. Main problem: wet snow. Wet loose-snow avalanches can be expected up to the summits in steep rocky terrain. On smooth grass-covered slopes at intermediate altitude that have not yet discharged and in wooded zones the wet snow masses can also start gliding over the ground. Avalanches can attain medium size with an increased probability of triggering in the second half of the day. In addition, slab avalanches can be triggered on isolated extremely steep shady high altitude slopes in the uppermost meter of the old snowpack. This is in general now only possible by large additional loading in places where snow is shallow. The slabs that release are mostly small.",
      "bulletinID": "BYCAAMLGenID3711-BYBGD_PM",
      "predecessor_id": "BYCAAMLGenID3711-BYBGD"
    }
  ]
}