{
  "bulletins": [
    {
      "regions": [
        {
          "regionID": "AT-08-01"
        }
      ],
      "validTime": {
        "startTime": "2021-02-18T07:30:00+01:00",
        "endTime": "2021-02-19T07:30:00+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "W",
              "NW"
            ]
          },
          "problemType": "wind_drifted_snow"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "2000"
            },
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "On Friday, heavily overcast to start with, gradually becoming quite sunny during the daytime amid mild temperatures. Saturday will be sunny, the zero-degree level ascending to 3000 m. Avalanche danger will be subject to the classic daytime danger cycle.\r\nBernhard Anwander\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-02-18T07:30:00+01:00",
      "avalancheActivityHighlights": "Caution: fresh/older small drifts at high altitude; wet-snow problem due to warmth, solar radiation",
      "wxSynopsisComment": "Dry mountain weather, temperatures rising at all altitudes. Lots of sun despite high-altitude cloudbanks, in early afternoon hampered by intermittent cloud cover, creating diffuse light. In classic foehn-exposed regions, quite windy. Temperature at 2000 m: -2 to +4 degrees. Moderate W/SW winds at high altitudes.",
      "snowpackStructureComment": "Intermittently strong W/NW (later SW) winds transported the snow somewhat, generated snowdrift accumulations, depositing them on loose, soft layers at high altitudes: they are prone to triggering. All in all, the snowpack is well consolidated. Particularly on high-altitude shady slopes, faceted crystals at mid-level in the snowpack constitute weak layers. At low and intermediate altitudes the snowpack is thoroughly wet due to warmth and rainfall. After a night of predominantly clear skies and mild temperatures, a breakable melt-freeze crust formed at low altitudes; this will rapidly soften during the daytime.",
      "avalancheActivityComment": "Avalanche danger is predominantly moderate. Main danger: fresh/older small snowdrift accumulations which can easily be triggered, require cautious assessment. Avalanche prone locations are found in ridgeline terrain, on wind-loaded steep slopes above 2000 m, with ascending altitude the danger zones increasing in size and frequency. In high alpine terrain, high-altitude steep slopes and seldom skied shady slopes, slabs can fracture down to deeper layers in the old snowpack and grow to larger size (usually by large additional loading, e.g. groups not maintaining distances). Such danger zones are not visible. They lie particularly in transitions from shallow to deep snow and in shallow-snow spots. As a result of higher temperatures, naturally triggered small wet-snow avalanches are increasingly possible below 2000 m. Caution urged in all areas below glide cracks.",
      "bulletinID": "DibosBulletinDeID5935-AT8R1"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-02"
        }
      ],
      "validTime": {
        "startTime": "2021-02-18T07:30:00+01:00",
        "endTime": "2021-02-19T07:30:00+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "W",
              "NW"
            ]
          },
          "problemType": "wind_drifted_snow"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "2000"
            },
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "On Friday, heavily overcast to start with, gradually becoming quite sunny during the daytime amid mild temperatures. Saturday will be sunny, the zero-degree level ascending to 3000 m. Avalanche danger will be subject to the classic daytime danger cycle.\r\nBernhard Anwander\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-02-18T07:30:00+01:00",
      "avalancheActivityHighlights": "Caution: fresh/older small drifts at high altitude; wet-snow problem due to warmth, solar radiation",
      "wxSynopsisComment": "Dry mountain weather, temperatures rising at all altitudes. Lots of sun despite high-altitude cloudbanks, in early afternoon hampered by intermittent cloud cover, creating diffuse light. In classic foehn-exposed regions, quite windy. Temperature at 2000 m: -2 to +4 degrees. Moderate W/SW winds at high altitudes.",
      "snowpackStructureComment": "Intermittently strong W/NW (later SW) winds transported the snow somewhat, generated snowdrift accumulations, depositing them on loose, soft layers at high altitudes: they are prone to triggering. All in all, the snowpack is well consolidated. Particularly on high-altitude shady slopes, faceted crystals at mid-level in the snowpack constitute weak layers. At low and intermediate altitudes the snowpack is thoroughly wet due to warmth and rainfall. After a night of predominantly clear skies and mild temperatures, a breakable melt-freeze crust formed at low altitudes; this will rapidly soften during the daytime.",
      "avalancheActivityComment": "Avalanche danger is predominantly moderate. Main danger: fresh/older small snowdrift accumulations which can easily be triggered, require cautious assessment. Avalanche prone locations are found in ridgeline terrain, on wind-loaded steep slopes above 2000 m, with ascending altitude the danger zones increasing in size and frequency. In high alpine terrain, high-altitude steep slopes and seldom skied shady slopes, slabs can fracture down to deeper layers in the old snowpack and grow to larger size (usually by large additional loading, e.g. groups not maintaining distances). Such danger zones are not visible. They lie particularly in transitions from shallow to deep snow and in shallow-snow spots. As a result of higher temperatures, naturally triggered small wet-snow avalanches are increasingly possible below 2000 m. Caution urged in all areas below glide cracks.",
      "bulletinID": "DibosBulletinDeID5935-AT8R2"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-03"
        }
      ],
      "validTime": {
        "startTime": "2021-02-18T07:30:00+01:00",
        "endTime": "2021-02-19T07:30:00+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "W",
              "NW"
            ]
          },
          "problemType": "wind_drifted_snow"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "2000"
            },
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "On Friday, heavily overcast to start with, gradually becoming quite sunny during the daytime amid mild temperatures. Saturday will be sunny, the zero-degree level ascending to 3000 m. Avalanche danger will be subject to the classic daytime danger cycle.\r\nBernhard Anwander\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-02-18T07:30:00+01:00",
      "avalancheActivityHighlights": "Caution: fresh/older small drifts at high altitude; wet-snow problem due to warmth, solar radiation",
      "wxSynopsisComment": "Dry mountain weather, temperatures rising at all altitudes. Lots of sun despite high-altitude cloudbanks, in early afternoon hampered by intermittent cloud cover, creating diffuse light. In classic foehn-exposed regions, quite windy. Temperature at 2000 m: -2 to +4 degrees. Moderate W/SW winds at high altitudes.",
      "snowpackStructureComment": "Intermittently strong W/NW (later SW) winds transported the snow somewhat, generated snowdrift accumulations, depositing them on loose, soft layers at high altitudes: they are prone to triggering. All in all, the snowpack is well consolidated. Particularly on high-altitude shady slopes, faceted crystals at mid-level in the snowpack constitute weak layers. At low and intermediate altitudes the snowpack is thoroughly wet due to warmth and rainfall. After a night of predominantly clear skies and mild temperatures, a breakable melt-freeze crust formed at low altitudes; this will rapidly soften during the daytime.",
      "avalancheActivityComment": "Avalanche danger is predominantly moderate. Main danger: fresh/older small snowdrift accumulations which can easily be triggered, require cautious assessment. Avalanche prone locations are found in ridgeline terrain, on wind-loaded steep slopes above 2000 m, with ascending altitude the danger zones increasing in size and frequency. In high alpine terrain, high-altitude steep slopes and seldom skied shady slopes, slabs can fracture down to deeper layers in the old snowpack and grow to larger size (usually by large additional loading, e.g. groups not maintaining distances). Such danger zones are not visible. They lie particularly in transitions from shallow to deep snow and in shallow-snow spots. As a result of higher temperatures, naturally triggered small wet-snow avalanches are increasingly possible below 2000 m. Caution urged in all areas below glide cracks.",
      "bulletinID": "DibosBulletinDeID5935-AT8R3"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-04"
        }
      ],
      "validTime": {
        "startTime": "2021-02-18T07:30:00+01:00",
        "endTime": "2021-02-19T07:30:00+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "W",
              "NW"
            ]
          },
          "problemType": "wind_drifted_snow"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "2000"
            },
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "On Friday, heavily overcast to start with, gradually becoming quite sunny during the daytime amid mild temperatures. Saturday will be sunny, the zero-degree level ascending to 3000 m. Avalanche danger will be subject to the classic daytime danger cycle.\r\nBernhard Anwander\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-02-18T07:30:00+01:00",
      "avalancheActivityHighlights": "Caution: fresh/older small drifts at high altitude; wet-snow problem due to warmth, solar radiation",
      "wxSynopsisComment": "Dry mountain weather, temperatures rising at all altitudes. Lots of sun despite high-altitude cloudbanks, in early afternoon hampered by intermittent cloud cover, creating diffuse light. In classic foehn-exposed regions, quite windy. Temperature at 2000 m: -2 to +4 degrees. Moderate W/SW winds at high altitudes.",
      "snowpackStructureComment": "Intermittently strong W/NW (later SW) winds transported the snow somewhat, generated snowdrift accumulations, depositing them on loose, soft layers at high altitudes: they are prone to triggering. All in all, the snowpack is well consolidated. Particularly on high-altitude shady slopes, faceted crystals at mid-level in the snowpack constitute weak layers. At low and intermediate altitudes the snowpack is thoroughly wet due to warmth and rainfall. After a night of predominantly clear skies and mild temperatures, a breakable melt-freeze crust formed at low altitudes; this will rapidly soften during the daytime.",
      "avalancheActivityComment": "Avalanche danger is predominantly moderate. Main danger: fresh/older small snowdrift accumulations which can easily be triggered, require cautious assessment. Avalanche prone locations are found in ridgeline terrain, on wind-loaded steep slopes above 2000 m, with ascending altitude the danger zones increasing in size and frequency. In high alpine terrain, high-altitude steep slopes and seldom skied shady slopes, slabs can fracture down to deeper layers in the old snowpack and grow to larger size (usually by large additional loading, e.g. groups not maintaining distances). Such danger zones are not visible. They lie particularly in transitions from shallow to deep snow and in shallow-snow spots. As a result of higher temperatures, naturally triggered small wet-snow avalanches are increasingly possible below 2000 m. Caution urged in all areas below glide cracks.",
      "bulletinID": "DibosBulletinDeID5935-AT8R4"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-05"
        }
      ],
      "validTime": {
        "startTime": "2021-02-18T07:30:00+01:00",
        "endTime": "2021-02-19T07:30:00+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "W",
              "NW"
            ]
          },
          "problemType": "wind_drifted_snow"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "2000"
            },
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "On Friday, heavily overcast to start with, gradually becoming quite sunny during the daytime amid mild temperatures. Saturday will be sunny, the zero-degree level ascending to 3000 m. Avalanche danger will be subject to the classic daytime danger cycle.\r\nBernhard Anwander\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-02-18T07:30:00+01:00",
      "avalancheActivityHighlights": "Caution: fresh/older small drifts at high altitude; wet-snow problem due to warmth, solar radiation",
      "wxSynopsisComment": "Dry mountain weather, temperatures rising at all altitudes. Lots of sun despite high-altitude cloudbanks, in early afternoon hampered by intermittent cloud cover, creating diffuse light. In classic foehn-exposed regions, quite windy. Temperature at 2000 m: -2 to +4 degrees. Moderate W/SW winds at high altitudes.",
      "snowpackStructureComment": "Intermittently strong W/NW (later SW) winds transported the snow somewhat, generated snowdrift accumulations, depositing them on loose, soft layers at high altitudes: they are prone to triggering. All in all, the snowpack is well consolidated. Particularly on high-altitude shady slopes, faceted crystals at mid-level in the snowpack constitute weak layers. At low and intermediate altitudes the snowpack is thoroughly wet due to warmth and rainfall. After a night of predominantly clear skies and mild temperatures, a breakable melt-freeze crust formed at low altitudes; this will rapidly soften during the daytime.",
      "avalancheActivityComment": "Avalanche danger is predominantly moderate. Main danger: fresh/older small snowdrift accumulations which can easily be triggered, require cautious assessment. Avalanche prone locations are found in ridgeline terrain, on wind-loaded steep slopes above 2000 m, with ascending altitude the danger zones increasing in size and frequency. In high alpine terrain, high-altitude steep slopes and seldom skied shady slopes, slabs can fracture down to deeper layers in the old snowpack and grow to larger size (usually by large additional loading, e.g. groups not maintaining distances). Such danger zones are not visible. They lie particularly in transitions from shallow to deep snow and in shallow-snow spots. As a result of higher temperatures, naturally triggered small wet-snow avalanches are increasingly possible below 2000 m. Caution urged in all areas below glide cracks.",
      "bulletinID": "DibosBulletinDeID5935-AT8R5"
    },
    {
      "regions": [
        {
          "regionID": "AT-08-06"
        }
      ],
      "validTime": {
        "startTime": "2021-02-18T07:30:00+01:00",
        "endTime": "2021-02-19T07:30:00+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "moderate"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "W",
              "NW"
            ]
          },
          "problemType": "wind_drifted_snow"
        },
        {
          "dangerRating": {
            "elevation": {
              "upperBound": "2000"
            },
            "customData": [],
            "aspect": [
              "N",
              "NE",
              "E",
              "SE",
              "S",
              "SW",
              "W",
              "NW"
            ]
          },
          "problemType": "wet_snow"
        }
      ],
      "tendency": {
        "validTime": {},
        "tendencyComment": "On Friday, heavily overcast to start with, gradually becoming quite sunny during the daytime amid mild temperatures. Saturday will be sunny, the zero-degree level ascending to 3000 m. Avalanche danger will be subject to the classic daytime danger cycle.\r\nBernhard Anwander\r\nTranslated by Jeffrey McCabe"
      },
      "publicationTime": "2021-02-18T07:30:00+01:00",
      "avalancheActivityHighlights": "Caution: fresh/older small drifts at high altitude; wet-snow problem due to warmth, solar radiation",
      "wxSynopsisComment": "Dry mountain weather, temperatures rising at all altitudes. Lots of sun despite high-altitude cloudbanks, in early afternoon hampered by intermittent cloud cover, creating diffuse light. In classic foehn-exposed regions, quite windy. Temperature at 2000 m: -2 to +4 degrees. Moderate W/SW winds at high altitudes.",
      "snowpackStructureComment": "Intermittently strong W/NW (later SW) winds transported the snow somewhat, generated snowdrift accumulations, depositing them on loose, soft layers at high altitudes: they are prone to triggering. All in all, the snowpack is well consolidated. Particularly on high-altitude shady slopes, faceted crystals at mid-level in the snowpack constitute weak layers. At low and intermediate altitudes the snowpack is thoroughly wet due to warmth and rainfall. After a night of predominantly clear skies and mild temperatures, a breakable melt-freeze crust formed at low altitudes; this will rapidly soften during the daytime.",
      "avalancheActivityComment": "Avalanche danger is predominantly moderate. Main danger: fresh/older small snowdrift accumulations which can easily be triggered, require cautious assessment. Avalanche prone locations are found in ridgeline terrain, on wind-loaded steep slopes above 2000 m, with ascending altitude the danger zones increasing in size and frequency. In high alpine terrain, high-altitude steep slopes and seldom skied shady slopes, slabs can fracture down to deeper layers in the old snowpack and grow to larger size (usually by large additional loading, e.g. groups not maintaining distances). Such danger zones are not visible. They lie particularly in transitions from shallow to deep snow and in shallow-snow spots. As a result of higher temperatures, naturally triggered small wet-snow avalanches are increasingly possible below 2000 m. Caution urged in all areas below glide cracks.",
      "bulletinID": "DibosBulletinDeID5935-AT8R6"
    }
  ]
}