{
  "bulletins": [
    {
      "regions": [
        {
          "regionID": "BYALL"
        }
      ],
      "validTime": {
        "startTime": "2021-03-07T00:00:00+01:00",
        "endTime": "2021-03-07T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "1800"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "1800"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "NE",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wind_drifted_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-03-06T19:32:25+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "In sun-exposed and wind-exposed locations small-scale snowdrift accumulations are found atop hard and icy wind and melt-freeze crust layers; on shady wind-protected slopes at higher altitudes atop loose, faceted crystals. There and in areas where the fresh snow has already been covered again by drifted snow the snowdrift accumulations are prone to triggering. Otherwise, the old snowpack has by and large solidified well and is compact. On sun-drenched slopes a breakable melt-freeze crust forms during the night which softens during the course of the day; below 1400 m on the sunny side the snow has started to vanish.  The snowdrift problem continues to diminish. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Heed small-scale snowdrifts at higher altitudes.",
      "avalancheActivityComment": "Moderate avalanche danger in the Bavarian Alps above 1600 m. The main problem are snowdrifts. Slab avalanches can be triggered in steep terrain adjacent to ridgelines in NE/S/SW aspects as well as in wind-loaded gullies in bowls in particular by large additional loading. The avalanches are predominantly small. However, above 1800 m they can occasionally grow to medium-size. Caution: both, danger of being buried in snow and danger of taking a fall. Besides that it is possible that the number of spontaneously releasing small wet and glide snow avalanches in steep sunny terrain ncreases slightly during the course of the day.",
      "bulletinID": "BYCAAMLGenID3663-BYALL"
    },
    {
      "regions": [
        {
          "regionID": "BYAMM"
        }
      ],
      "validTime": {
        "startTime": "2021-03-07T00:00:00+01:00",
        "endTime": "2021-03-07T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "1800"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "1800"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "NE",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wind_drifted_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-03-06T19:32:25+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "In sun-exposed and wind-exposed locations small-scale snowdrift accumulations are found atop hard and icy wind and melt-freeze crust layers; on shady wind-protected slopes at higher altitudes atop loose, faceted crystals. There and in areas where the fresh snow has already been covered again by drifted snow the snowdrift accumulations are prone to triggering. Otherwise, the old snowpack has by and large solidified well and is compact. On sun-drenched slopes a breakable melt-freeze crust forms during the night which softens during the course of the day; below 1400 m on the sunny side the snow has started to vanish.  The snowdrift problem continues to diminish. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Heed small-scale snowdrifts at higher altitudes.",
      "avalancheActivityComment": "Moderate avalanche danger in the Bavarian Alps above 1600 m. The main problem are snowdrifts. Slab avalanches can be triggered in steep terrain adjacent to ridgelines in NE/S/SW aspects as well as in wind-loaded gullies in bowls in particular by large additional loading. The avalanches are predominantly small. However, above 1800 m they can occasionally grow to medium-size. Caution: both, danger of being buried in snow and danger of taking a fall. Besides that it is possible that the number of spontaneously releasing small wet and glide snow avalanches in steep sunny terrain ncreases slightly during the course of the day.",
      "bulletinID": "BYCAAMLGenID3663-BYAMM"
    },
    {
      "regions": [
        {
          "regionID": "BYWFK"
        }
      ],
      "validTime": {
        "startTime": "2021-03-07T00:00:00+01:00",
        "endTime": "2021-03-07T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "1800"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "1800"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "NE",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wind_drifted_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-03-06T19:32:25+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "In sun-exposed and wind-exposed locations small-scale snowdrift accumulations are found atop hard and icy wind and melt-freeze crust layers; on shady wind-protected slopes at higher altitudes atop loose, faceted crystals. There and in areas where the fresh snow has already been covered again by drifted snow the snowdrift accumulations are prone to triggering. Otherwise, the old snowpack has by and large solidified well and is compact. On sun-drenched slopes a breakable melt-freeze crust forms during the night which softens during the course of the day; below 1400 m on the sunny side the snow has started to vanish.  The snowdrift problem continues to diminish. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Heed small-scale snowdrifts at higher altitudes.",
      "avalancheActivityComment": "Moderate avalanche danger in the Bavarian Alps above 1600 m. The main problem are snowdrifts. Slab avalanches can be triggered in steep terrain adjacent to ridgelines in NE/S/SW aspects as well as in wind-loaded gullies in bowls in particular by large additional loading. The avalanches are predominantly small. However, above 1800 m they can occasionally grow to medium-size. Caution: both, danger of being buried in snow and danger of taking a fall. Besides that it is possible that the number of spontaneously releasing small wet and glide snow avalanches in steep sunny terrain ncreases slightly during the course of the day.",
      "bulletinID": "BYCAAMLGenID3663-BYWFK"
    },
    {
      "regions": [
        {
          "regionID": "BYBVA"
        }
      ],
      "validTime": {
        "startTime": "2021-03-07T00:00:00+01:00",
        "endTime": "2021-03-07T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "NE",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wind_drifted_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-03-06T19:32:25+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "In sun-exposed and wind-exposed locations small-scale snowdrift accumulations are found atop hard and icy wind and melt-freeze crust layers; on shady wind-protected slopes at higher altitudes atop loose, faceted crystals. There and in areas where the fresh snow has already been covered again by drifted snow the snowdrift accumulations are prone to triggering. Otherwise, the old snowpack has by and large solidified well and is compact. On sun-drenched slopes a breakable melt-freeze crust forms during the night which softens during the course of the day; below 1400 m on the sunny side the snow has started to vanish.  The snowdrift problem continues to diminish. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Heed small-scale snowdrifts at higher altitudes.",
      "avalancheActivityComment": "Moderate avalanche danger in the Bavarian Alps above 1600 m. The main problem are snowdrifts. Slab avalanches can be triggered in steep terrain adjacent to ridgelines in NE/S/SW aspects as well as in wind-loaded gullies in bowls in particular by large additional loading. The avalanches are predominantly small. However, above 1800 m they can occasionally grow to medium-size. Caution: both, danger of being buried in snow and danger of taking a fall. Besides that it is possible that the number of spontaneously releasing small wet and glide snow avalanches in steep sunny terrain ncreases slightly during the course of the day.",
      "bulletinID": "BYCAAMLGenID3663-BYBVA"
    },
    {
      "regions": [
        {
          "regionID": "BYCHG"
        }
      ],
      "validTime": {
        "startTime": "2021-03-07T00:00:00+01:00",
        "endTime": "2021-03-07T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {},
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "NE",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wind_drifted_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-03-06T19:32:25+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "In sun-exposed and wind-exposed locations small-scale snowdrift accumulations are found atop hard and icy wind and melt-freeze crust layers; on shady wind-protected slopes at higher altitudes atop loose, faceted crystals. There and in areas where the fresh snow has already been covered again by drifted snow the snowdrift accumulations are prone to triggering. Otherwise, the old snowpack has by and large solidified well and is compact. On sun-drenched slopes a breakable melt-freeze crust forms during the night which softens during the course of the day; below 1400 m on the sunny side the snow has started to vanish.  The snowdrift problem continues to diminish. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Heed small-scale snowdrifts at higher altitudes.",
      "avalancheActivityComment": "Moderate avalanche danger in the Bavarian Alps above 1600 m. The main problem are snowdrifts. Slab avalanches can be triggered in steep terrain adjacent to ridgelines in NE/S/SW aspects as well as in wind-loaded gullies in bowls in particular by large additional loading. The avalanches are predominantly small. However, above 1800 m they can occasionally grow to medium-size. Caution: both, danger of being buried in snow and danger of taking a fall. Besides that it is possible that the number of spontaneously releasing small wet and glide snow avalanches in steep sunny terrain ncreases slightly during the course of the day.",
      "bulletinID": "BYCAAMLGenID3663-BYCHG"
    },
    {
      "regions": [
        {
          "regionID": "BYBGD"
        }
      ],
      "validTime": {
        "startTime": "2021-03-07T00:00:00+01:00",
        "endTime": "2021-03-07T23:59:59+01:00"
      },
      "source": {},
      "dangerRatings": [
        {
          "elevation": {
            "lowerBound": "1800"
          },
          "customData": [],
          "mainValue": "moderate"
        },
        {
          "elevation": {
            "upperBound": "1800"
          },
          "customData": [],
          "mainValue": "low"
        }
      ],
      "avalancheProblems": [
        {
          "dangerRating": {
            "elevation": {},
            "customData": [],
            "aspect": [
              "NE",
              "E",
              "SE",
              "S",
              "SW"
            ]
          },
          "problemType": "wind_drifted_snow"
        }
      ],
      "tendency": {
        "validTime": {}
      },
      "publicationTime": "2021-03-06T19:32:25+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "In sun-exposed and wind-exposed locations small-scale snowdrift accumulations are found atop hard and icy wind and melt-freeze crust layers; on shady wind-protected slopes at higher altitudes atop loose, faceted crystals. There and in areas where the fresh snow has already been covered again by drifted snow the snowdrift accumulations are prone to triggering. Otherwise, the old snowpack has by and large solidified well and is compact. On sun-drenched slopes a breakable melt-freeze crust forms during the night which softens during the course of the day; below 1400 m on the sunny side the snow has started to vanish.  The snowdrift problem continues to diminish. Please note: public ski areas are currently not supervised or secured from avalanche dangers.",
      "avalancheActivityHighlights": "Heed small-scale snowdrifts at higher altitudes.",
      "avalancheActivityComment": "Moderate avalanche danger in the Bavarian Alps above 1600 m. The main problem are snowdrifts. Slab avalanches can be triggered in steep terrain adjacent to ridgelines in NE/S/SW aspects as well as in wind-loaded gullies in bowls in particular by large additional loading. The avalanches are predominantly small. However, above 1800 m they can occasionally grow to medium-size. Caution: both, danger of being buried in snow and danger of taking a fall. Besides that it is possible that the number of spontaneously releasing small wet and glide snow avalanches in steep sunny terrain ncreases slightly during the course of the day.",
      "bulletinID": "BYCAAMLGenID3663-BYBGD"
    }
  ]
}