{
  "bulletins": [
    {
      "regions": [
        {
          "regionID": "AT-08-01"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T07:30:00+02:00",
        "endTime": "2021-03-30T12:00:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R1"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-02"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T07:30:00+02:00",
        "endTime": "2021-03-30T12:00:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "2200"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "2200"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R2"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-03"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T07:30:00+02:00",
        "endTime": "2021-03-30T12:00:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "2200"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "2200"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R3"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-04"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T07:30:00+02:00",
        "endTime": "2021-03-30T12:00:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "2200"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "2200"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R4"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-05"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T07:30:00+02:00",
        "endTime": "2021-03-30T12:00:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "2200"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "2200"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R5"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-06"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T07:30:00+02:00",
        "endTime": "2021-03-30T12:00:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "2200"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "2200"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R6"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-01"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T12:00:00+02:00",
        "endTime": "2021-03-31T07:30:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "considerable"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R1_PM",
      "predecessor_id": "DibosBulletinDeID6033-AT8R1"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-02"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T12:00:00+02:00",
        "endTime": "2021-03-31T07:30:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "considerable"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R2_PM",
      "predecessor_id": "DibosBulletinDeID6033-AT8R2"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-03"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T12:00:00+02:00",
        "endTime": "2021-03-31T07:30:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "considerable"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R3_PM",
      "predecessor_id": "DibosBulletinDeID6033-AT8R3"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-04"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T12:00:00+02:00",
        "endTime": "2021-03-31T07:30:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "considerable"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R4_PM",
      "predecessor_id": "DibosBulletinDeID6033-AT8R4"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-05"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T12:00:00+02:00",
        "endTime": "2021-03-31T07:30:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "considerable"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R5_PM",
      "predecessor_id": "DibosBulletinDeID6033-AT8R5"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-06"
        }
      ],
      "validTime": {
        "startTime": "2021-03-30T12:00:00+02:00",
        "endTime": "2021-03-31T07:30:00+02:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "considerable"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "NW"
            ]
          },
          "problemType": "persistent_weak_layers"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "3000"
            },
            "customData": [],
            "aspect": [
              "E",
              "SE",
              "S",
              "SW",
              "W"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "Nocturnal skies will be clear. Wednesday will be sunny and very mild. The danger of dry-snow avalanches is not expected to change significantly. The danger of wet-snow avalanches will increase noticeably during the course of the day. Glide-snow avalanches continue to be possible.\r\nAndreas Pecl\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-03-30T07:30:00+02:00",
      "avalancheActivityHighlights": "Mostly favourable conditions in morning. General danger + wet-snow avalanches then increase with daytime warmth and solar radiation.",
      "wxSynopsisComment": "Sunny weather, outstanding visibility, intermittent cirrus clouds demonstrate the rising temperature also at high altitudes. The zero-degree level will ascend to 3300m. Temperature at 2000 m: 9 degrees. Mostly light winds.",
      "snowpackStructureComment": "Following a night of adequate outgoing longwave radiation, the snowpack on sunny slopes and in general at low and intermediate altitudes has formed a melt-freeze crust capable of bearing loads and is stable. On high-altitude shady slopes the near-to-surface layers of old snow are still powdery, often lie deposited atop soft layers of older drifts which are still triggerable with ascending altitude on extremely steep slopes. Bonding to the old snowpack and between intermediate layers is generally good, but only moderate in high alpine regions. The embedded Sahara dust has been a weak (gliding) layer over the last few days in small releases.",
      "avalancheActivityComment": "Mostly low avalanche danger prevails in the morning, moderate danger at high altitudes. Isolated dry-snow avalanche prone locations are found particularly in very steep shady terrain and in extremely steep terrain in general. Older snowdrift accumulations can be triggered primarily by large additional loading. When an avalanche fractures in more deeply embedded weak layers, in isolated cases it can grow to medium size. Danger of naturally triggered wet-snow avalanches increases to considerable due to daytime warming and solar radiation, especially on sunny slopes. Wet-snow avalanches can also be triggered by backcountry skiers. On steep grassy slopes up to intermediate altitude, small-to-medium glide-snow avalanches are possible.",
      "bulletinID": "DibosBulletinDeID6033-AT8R6_PM",
      "predecessor_id": "DibosBulletinDeID6033-AT8R6"
    }
  ]
}