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      "avalancheActivityHighlights": "Avalanche danger increases significantly due to new snow",
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        "endTime": "2021-03-15T23:59:59+01:00"
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      "avalancheActivityHighlights": "Avalanche danger increases significantly due to new snow",
      "avalancheActivityComment": "Above 1600 m, the avalanche danger in the Bavarian Alps is considerable. Main problem: fresh snow. On steep slopes in all aspects where new fallen snow is impacted and transported by wind and has bonded, slab avalanches can even be triggered by one sole skier and can reach medium-size; in the Allg\u00e4u they can also grow to large size. Avalanche prone locations are especially numerous above 1600 m in steep terrain adjacent to ridgelines, in wind-loaded gullies and bowls as well as in sparsely wooded places in forest transition zones. In areas where snowfall has been heavy, medium-sized loose snow avalanches can be expected to trigger naturally in steep rocky terrain.  On steep grass covered slopes which had previously become bare of snow, the snow masses can start gliding over the ground in the form of glide snow avalanches.",
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      "validTime": {
        "startTime": "2021-03-15T00:00:00+01:00",
        "endTime": "2021-03-15T23:59:59+01:00"
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      "dangerRatings": [
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      "wxSynopsisComment": null,
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      "avalancheActivityHighlights": "Avalanche danger increases significantly due to new snow",
      "avalancheActivityComment": "Above 1600 m, the avalanche danger in the Bavarian Alps is considerable. Main problem: fresh snow. On steep slopes in all aspects where new fallen snow is impacted and transported by wind and has bonded, slab avalanches can even be triggered by one sole skier and can reach medium-size; in the Allg\u00e4u they can also grow to large size. Avalanche prone locations are especially numerous above 1600 m in steep terrain adjacent to ridgelines, in wind-loaded gullies and bowls as well as in sparsely wooded places in forest transition zones. In areas where snowfall has been heavy, medium-sized loose snow avalanches can be expected to trigger naturally in steep rocky terrain.  On steep grass covered slopes which had previously become bare of snow, the snow masses can start gliding over the ground in the form of glide snow avalanches.",
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