{
  "bulletins": [
    {
      "regions": [
        {
          "regionID": "DE-BY-41"
        },
        {
          "regionID": "DE-BY-42"
        },
        {
          "regionID": "DE-BY-43"
        },
        {
          "regionID": "DE-BY-20"
        },
        {
          "regionID": "DE-BY-51"
        }
      ],
      "validTime": {
        "startTime": "2022-01-07T23:00:00+00:00",
        "endTime": "2022-01-08T23:00:00+00:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "Treeline"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "Treeline"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S"
            ]
          },
          "problemType": "wind_drifted_snow",
          "comment": null
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Depending on amounts of new snow and wind, avalanche danger could rise."
      },
      "bulletinID": "RID1322RGR1",
      "publicationTime": "2022-01-07T17:00:00+00:00",
      "avalancheActivityHighlights": "Snowdrift accumulations prone to triggering. Risk of falling on icy snowpack surface.",
      "avalancheActivityComment": "Avalanche danger above the treeline is moderate, below that altitude danger is low. Fresh snowdrifts are the main problem. Slab avalanches of small-to-medium size can be triggered even by minimum additional loading in places, i.e. from one sole skier. Avalanche prone locations are found above the treeline in steep ridgeline terrain in N/E/S aspects, in freshly wind-loaded gullies and bowls and behind/below protruberances.",
      "snowpackStructureComment": "Winds from westerly directions intensified at high altitude, small snowdrift accumulations were generated. These were deposited atop loose-snow layers and are thus very prone to triggering. Beneath the new snow of recent days is a melt-freeze encrusted largely stable old snowpack. At lower altitudes the loose snow blankets wet ground."
    },
    {
      "regions": [
        {
          "regionID": "DE-BY-11"
        },
        {
          "regionID": "DE-BY-12"
        },
        {
          "regionID": "DE-BY-30"
        }
      ],
      "validTime": {
        "startTime": "2022-01-07T23:00:00+00:00",
        "endTime": "2022-01-08T23:00:00+00:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "Treeline"
          },
          "customData": [],
          "mainValue": "considerable"
        },
        {
          "elevation": {
            "upperBound": "Treeline"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S"
            ]
          },
          "problemType": "wind_drifted_snow",
          "comment": null
        },
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "gliding_snow",
          "comment": null
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "bulletinID": "RID1322RGR2",
      "publicationTime": "2022-01-07T17:00:00+00:00",
      "avalancheActivityHighlights": "Fresh snowdrifts very prone to triggering",
      "wxSynopsisComment": "Avalanche danger\nabove the timberline is expected to remain tense.",
      "avalancheActivityComment": "Avalanche danger above the treeline is considerable, below that altitude danger is low. Fresh snowdrifts are the main problem. Slab avalanches of small-to-medium size can be triggered even by minimum additional loading in places, i.e. from one sole skier. Avalanche prone locations are found above the treeline in steep ridgeline terrain in N/E/S aspects, in freshly wind-loaded gullies and bowls and behind/below protruberances.\r\nIn the Allg\u00e4u on steep grass-covered slopes which have not yet discharged and in forest clearances, isolated mall-to-medium sized glide-snow avalanches can trigger.",
      "snowpackStructureComment": "Precipitation will set in, westerly winds will intensify, new snowdrift accumulations will be generated extensively. They will be deposited atop loose layers with some surface hoar and thus, be quite prone to triggering. Beneath the loose snow is a melt-freeze encrusted old snowpack. At high altitudes a thin layer of faceted crystals has formed beneath the melt-freeze crust. At intermediate altitudes the old snowpack fundament is largely stable. At low altitudes the loose snow blankets wet ground."
    },
    {
      "regions": [
        {
          "regionID": "DE-BY-52"
        },
        {
          "regionID": "DE-BY-60"
        }
      ],
      "validTime": {
        "startTime": "2022-01-07T23:00:00+00:00",
        "endTime": "2022-01-08T11:00:00+00:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "Treeline"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "Treeline"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S"
            ]
          },
          "problemType": "wind_drifted_snow",
          "comment": null
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "The avalanche situation will initially remain tense above the timberline."
      },
      "bulletinID": "RID1322RGR3",
      "publicationTime": "2022-01-07T17:00:00+00:00",
      "avalancheActivityHighlights": "Fresh snowdrifts very prone to triggering",
      "wxSynopsisComment": "Precipitation will set in, westerly winds will intensify, fresh snowdrift accumulations will be generateed which will grow further during the course of the day. They will be deposited atop loose snow layers, sometimes atop surface hoar, and be very prone to triggering. Beneath the loose snow is a melt-freeze crusted old snowpack. At high altitudes in some places, a thin layer of faceted crystals has formed beneath the melt-freeze crust. At intermediate altitudes the old snowpack fundament is largely stable. At lower altitudes, loose snow blankets the wet ground.",
      "avalancheActivityComment": "Avalanche danger above the treeline will increase from moderate to considerable during the day. Fresh snowdrifts are the main problem. Slab avalanches of small-to-medium size can be triggered even by minimum additional loading in places, i.e. from one sole skier. Avalanche prone locations are found above the treeline in steep ridgeline terrain in N/E/S aspects, in freshly wind-loaded gullies and bowls and behind/below protruberances. With ascending altitude, danger zones tend to increase and thus, avalanches can be larger."
    },
    {
      "regions": [
        {
          "regionID": "DE-BY-52"
        },
        {
          "regionID": "DE-BY-60"
        }
      ],
      "validTime": {
        "startTime": "2022-01-08T11:00:00+00:00",
        "endTime": "2022-01-08T23:00:00+00:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "Treeline"
          },
          "customData": [],
          "mainValue": "considerable"
        },
        {
          "elevation": {
            "upperBound": "Treeline"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S"
            ]
          },
          "problemType": "wind_drifted_snow",
          "comment": null
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "The avalanche situation will initially remain tense above the timberline."
      },
      "bulletinID": "RID1322RGR3_PM",
      "publicationTime": "2022-01-07T17:00:00+00:00",
      "avalancheActivityHighlights": "Fresh snowdrifts very prone to triggering",
      "wxSynopsisComment": "Precipitation will set in, westerly winds will intensify, fresh snowdrift accumulations will be generateed which will grow further during the course of the day. They will be deposited atop loose snow layers, sometimes atop surface hoar, and be very prone to triggering. Beneath the loose snow is a melt-freeze crusted old snowpack. At high altitudes in some places, a thin layer of faceted crystals has formed beneath the melt-freeze crust. At intermediate altitudes the old snowpack fundament is largely stable. At lower altitudes, loose snow blankets the wet ground.",
      "avalancheActivityComment": "Avalanche danger above the treeline will increase from moderate to considerable during the day. Fresh snowdrifts are the main problem. Slab avalanches of small-to-medium size can be triggered even by minimum additional loading in places, i.e. from one sole skier. Avalanche prone locations are found above the treeline in steep ridgeline terrain in N/E/S aspects, in freshly wind-loaded gullies and bowls and behind/below protruberances. With ascending altitude, danger zones tend to increase and thus, avalanches can be larger.",
      "predecessor_id": "RID1322RGR3"
    }
  ]
}