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      "avalancheActivityHighlights": "Caution: Naturally releasing loose snow avalanches in extremely steep terrain and ridgeline snowdrifts!",
      "avalancheActivityComment": "Above 1800 m avalanche danger in the Berchtesgaden Alps is considerable; in the rest of the Bavarian Alps above 2000 m. At altitudes lower than that the avalanche danger is moderate. The main problem stems from the new snow of the last few days. Small to medium-sized loose snow avalanches are to be expected on very steep slopes in all aspects which can trigger naturally in extremely steep terrain. Small to medium-sized slab avalanches can trigger below rock faces, in particular by large additional loading. Fresh snowdrift accumulations in ridgeline terrain can be triggered as small slabs even by low additional loading. Above 1800 m in the Berchtesgaden Alps they can reach medium size. Above 2000 m slab avalanches can grow to large size where more deeply embedded weak layers are triggered by large additional loading such as a group of skiers not maintaining sufficient distances or a surface avalanche. Small or medium-sized glide snow avalanches are possible below 1800 m on very steep slopes with smooth ground. Glide cracks are indicators of imminent danger.",
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      "publicationTime": "2021-03-19T18:54:56+01:00",
      "wxSynopsisComment": null,
      "snowpackStructureComment": "50 cm of fresh snow has fallen widespread in the Bavarian Alps; from place to place even more than one meter. During Friday night, moderate northerly winds are generating fresh small-scale snowdrift accumulations. Weak intermediate layers are embedded in the new snow and snowdrift accumulations of the last few days that are partly still prone to triggering, in particular at high altitude. Below rock faces there are spots, where spatially-limited graupel layers are embedded which are trigger-sensitive. At intermediate altitudes the bonding between new snow and old snow is good, but deteriorates with ascending altitude. At lower altitudes the snow is deposited on previously bare ground and is wet at ground level.  Avalanche danger levels are not expected to change significantly. Please note: ski runs are currently not supervised and not secured from avalanches.",
      "avalancheActivityHighlights": "Caution: Naturally releasing loose snow avalanches in extremely steep terrain and ridgeline snowdrifts!",
      "avalancheActivityComment": "Above 1800 m avalanche danger in the Berchtesgaden Alps is considerable; in the rest of the Bavarian Alps above 2000 m. At altitudes lower than that the avalanche danger is moderate. The main problem stems from the new snow of the last few days. Small to medium-sized loose snow avalanches are to be expected on very steep slopes in all aspects which can trigger naturally in extremely steep terrain. Small to medium-sized slab avalanches can trigger below rock faces, in particular by large additional loading. Fresh snowdrift accumulations in ridgeline terrain can be triggered as small slabs even by low additional loading. Above 1800 m in the Berchtesgaden Alps they can reach medium size. Above 2000 m slab avalanches can grow to large size where more deeply embedded weak layers are triggered by large additional loading such as a group of skiers not maintaining sufficient distances or a surface avalanche. Small or medium-sized glide snow avalanches are possible below 1800 m on very steep slopes with smooth ground. Glide cracks are indicators of imminent danger.",
      "bulletinID": "BYCAAMLGenID3689-BYWFK"
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    {
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        "startTime": "2021-03-20T00:00:00+01:00",
        "endTime": "2021-03-20T23:59:59+01:00"
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      "dangerRatings": [
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      "snowpackStructureComment": "50 cm of fresh snow has fallen widespread in the Bavarian Alps; from place to place even more than one meter. During Friday night, moderate northerly winds are generating fresh small-scale snowdrift accumulations. Weak intermediate layers are embedded in the new snow and snowdrift accumulations of the last few days that are partly still prone to triggering, in particular at high altitude. Below rock faces there are spots, where spatially-limited graupel layers are embedded which are trigger-sensitive. At intermediate altitudes the bonding between new snow and old snow is good, but deteriorates with ascending altitude. At lower altitudes the snow is deposited on previously bare ground and is wet at ground level.  Avalanche danger levels are not expected to change significantly. Please note: ski runs are currently not supervised and not secured from avalanches.",
      "avalancheActivityHighlights": "Caution: Naturally releasing loose snow avalanches in extremely steep terrain and ridgeline snowdrifts!",
      "avalancheActivityComment": "Above 1800 m avalanche danger in the Berchtesgaden Alps is considerable; in the rest of the Bavarian Alps above 2000 m. At altitudes lower than that the avalanche danger is moderate. The main problem stems from the new snow of the last few days. Small to medium-sized loose snow avalanches are to be expected on very steep slopes in all aspects which can trigger naturally in extremely steep terrain. Small to medium-sized slab avalanches can trigger below rock faces, in particular by large additional loading. Fresh snowdrift accumulations in ridgeline terrain can be triggered as small slabs even by low additional loading. Above 1800 m in the Berchtesgaden Alps they can reach medium size. Above 2000 m slab avalanches can grow to large size where more deeply embedded weak layers are triggered by large additional loading such as a group of skiers not maintaining sufficient distances or a surface avalanche. Small or medium-sized glide snow avalanches are possible below 1800 m on very steep slopes with smooth ground. Glide cracks are indicators of imminent danger.",
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