{
  "bulletins": [
    {
      "avalancheActivity": {
        "comment": "Mens vinden st\u00e5r p\u00e5 og danner ferske flak vil det v\u00e6re lett \u00e5 l\u00f8se ut skred. \nF\u00f8r siste nysn\u00f8fall ble det observert  kantkornkrystaller i overflaten blandet med nysn\u00f8krystaller. Stedvis kan disse kantkorn-krystallene n\u00e5 utgj\u00f8re et svakt lag som gj\u00f8r de ferske flakene ekstra ustabile. \n",
        "highlights": "Be careful in areas with fresh wind deposited snow. There may be pockets with a persistent weak layer beneath the wind depposited snow."
      },
      "avalancheProblems": [
        {
          "problemType": "wind_slab",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE"
          ],
          "elevation": {
            "lowerBound": "400"
          }
        }
      ],
      "bulletinID": "NO-3003_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3003"
        }
      ],
      "snowpackStructure": {
        "comment": "Det har kommet ca. 10 cm sn\u00f8 i helgen. Opp til ca. 400 moh regnet det 17.mai. Nysn\u00f8en har festes seg godt til det gamle sn\u00f8dekket. \nOver ca. 400 moh finnes det flere skare- og islag i sn\u00f8dekket. Rundt disse lagene har det tidligere blitt observert aktive svake lag med kantkorn i nord- og \u00f8stvendte fjellsider, men disse er pr. n\u00e5 sv\u00e6rt vanskelig \u00e5 p\u00e5virke.\nNederst i sn\u00f8dekket ligger et godt utviklet lag med begerkrystaller, som for tiden ogs\u00e5 er sv\u00e6rt vanskelig \u00e5 p\u00e5virke."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Be careful in areas with fresh wind deposited snow. There may be pockets with a persistent weak layer beneath the wind depposited snow."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Sn\u00f8dekket best\u00e5r i stor grad av grovkornet, smelteomvandlet sn\u00f8 som normalt drenerer vann godt, men ett og annet v\u00e5tt l\u00f8ssn\u00f8skred kan likevel forekomme i sv\u00e6rt bratt terreng. Unng\u00e5 opphold i utl\u00f8psomr\u00e5der der det kommer mye regn p\u00e5 sn\u00f8en.",
        "highlights": "Mild temperatures and rain will further increase the water content in the snowpack. The snowpack consists largely of coarse\u2011grained, melt\u2011transformed snow that generally drains water well, but the occasional wet loose avalanche may still occur in very steep terrain. Avoid spending time in runout zones where heavy rain is falling on the snow."
      },
      "bulletinID": "NO-3006_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3006"
        }
      ],
      "snowpackStructure": {
        "comment": "I lavlandet og kystn\u00e6re str\u00f8k er det stort sett bart. Og ogs\u00e5 h\u00f8yere til fjells i indre str\u00f8k har sn\u00f8dekke et v\u00e5rlig preg etter kraftig smelting den siste tiden."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Mild temperatures will further increase the water content in the snowpack. The snowpack consists largely of coarse\u2011grained, melt\u2011transformed snow that generally drains water well, but the occasional wet loose avalanche may still occur in very steep terrain. "
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket stabilt, smelteomvandlet og drenerer vann godt allerede, men p\u00e5 utsatte steder kan v\u00e5te skred fortsatt l\u00f8sne naturlig i dag. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3007_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3007"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 200\u2013400 moh og oppover, avhengig av hvor i regionen du befinner deg, med mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene.\nI h\u00f8yfjellet og i skyggevendt terreng kan det fortsatt finnes eldre svake lag dypt i sn\u00f8dekket. Store skred kan ikke utelukkes ved rask oppvarming, regn eller skavlbrudd."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially if the mild temperatures become more pronounced than expected. Wet loose avalanches are the most likely problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly in northern aspects. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3009_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3009"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 200\u2013300 moh og oppover, avhengig av hvor i regionen du befinner deg. Det er mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n\nI h\u00f8yfjellet og i skyggevendt terreng kan det fortsatt finnes lagdeling og enkelte eldre svake lag dypt i sn\u00f8dekket. Ved rask oppvarming, mye regn eller skavlbrudd kan store skred ikke utelukkes."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "An overcast night followed by a sunny afternoon with high temperatures will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially on steep, sun\u2011exposed slopes. Wet loose avalanches are the most likely avalanche problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly in northern aspects. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt allerede. Men p\u00e5 utsatte steder kan v\u00e5te skred fortsatt l\u00f8sne naturlig i dag. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3010_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3010"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 200\u2013400 moh og oppover, avhengig av hvor i regionen du befinner deg, med mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene.\nI h\u00f8yfjellet og i skyggevendt terreng kan det fortsatt finnes lagdeling og enkelte eldre svake lag dypt i sn\u00f8dekket. Ved rask oppvarming, mye regn eller skavlbrudd kan store skred ikke utelukkes."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "An overcast night followed by a sunny afternoon with high temperatures will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially on steep, sun\u2011exposed slopes. Wet loose avalanches are the most likely avalanche problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly in northern aspects. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. Hvis mildv\u00e6ret n\u00e5r opp i disse h\u00f8ydene, kan smeltevann trenge ned i sn\u00f8dekket og svekke lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially if the mild temperatures become more pronounced than expected. Wet loose avalanches are the most likely problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present. If mild temperatures reach these elevations, meltwater can penetrate downward and weaken the layers, potentially producing wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3011_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3011"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 200\u2013400 moh og oppover, avhengig av hvor i regionen du befinner deg, med mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene.\nFlere skare- og islag i sn\u00f8dekket kan gi opphoping av vann ved kraftig oppvarming eller regn, og muliggj\u00f8r v\u00e5te flakskred.\n"
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "An overcast night followed by a sunny afternoon with high temperatures will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially on steep, sun\u2011exposed slopes. Wet loose avalanches are the most likely avalanche problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly in northern aspects. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. Hvis mildv\u00e6ret n\u00e5r opp i disse h\u00f8ydene, kan smeltevann trenge ned i sn\u00f8dekket og svekke lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially if the mild temperatures become more pronounced than expected. Wet loose avalanches are the most likely problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present. If mild temperatures reach these elevations, meltwater can penetrate downward and weaken the layers, potentially producing wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3012_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3012"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 300\u2013500 moh og oppover, avhengig av hvor i regionen du befinner deg, med mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "An overcast night followed by a sunny afternoon with high temperatures will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially on steep, sun\u2011exposed slopes. Wet loose avalanches are the most likely avalanche problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly in northern aspects. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3013_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3013"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 400 moh og oppover, avhengig av hvor i regionen du befinner deg, med mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene.\nI h\u00f8yfjellet og i skyggevendt terreng kan det fortsatt finnes lagdeling og enkelte eldre svake lag dypt i sn\u00f8dekket. Ved rask oppvarming, mye regn eller skavlbrudd kan store skred ikke utelukkes."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "An overcast night followed by a sunny afternoon with high temperatures will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially on steep, sun\u2011exposed slopes. Wet loose avalanches are the most likely avalanche problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly in northern aspects. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Fortsatt mildv\u00e6r og litt regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Sn\u00f8dekket best\u00e5r i stor grad av grovkornet, smelteomvandlet sn\u00f8 som ventes \u00e5 drenerer vann godt, men ett og annet v\u00e5tt l\u00f8ssn\u00f8skred kan likevel forekomme i sv\u00e6rt bratt terreng. Unng\u00e5 opphold i utl\u00f8psomr\u00e5der der det kommer mye regn p\u00e5 sn\u00f8en.\n\nGlideskred kan forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Continued mild temperatures and some rain will further increase the water content in the snowpack. The snowpack consists largely of coarse\u2011grained, melt\u2011transformed snow that generally drains water well, but wet loose avalanche may still occur in very steep terrain. Avoid spending time in runout zones where heavy rain is falling on the snow.\n\nGlide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "bulletinID": "NO-3014_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3014"
        }
      ],
      "snowpackStructure": {
        "comment": "I lavlandet og kystn\u00e6re str\u00f8k er det stort sett bart. Og ogs\u00e5 h\u00f8yere til fjells har sn\u00f8dekke et v\u00e5rlig preg etter kraftig smelting den siste tiden.\n\nP\u00e5 Hinn\u00f8ya finnes det sammenhengende sn\u00f8 fra cirka 300 moh. og oppover, men i resten av regionen m\u00e5 man enda h\u00f8yere til fjells for \u00e5 finne skif\u00f8re."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "High temperatures and strong sunshine will increase snowmelt and add more water to the snowpack. The limited snow cover that remains is mostly coarse\u2011grained, melt\u2011transformed snow that drains water well, and overall stability is good. However, wet loose avalanches may still occur in very steep terrain, especially where the snow is thoroughly saturated.\n\nGlide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. These avalanches are unpredictable, and it is wise to avoid spending time in runout zones below snow\u2011covered slabby terrain."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3015_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3015"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 400-600 moh. og oppover, avhengig av hvor i regionen du befinner deg. Det er mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "An overcast night followed by a sunny afternoon with high temperatures will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well. However, wet avalanches may still release naturally in exposed terrain, especially on steep, sun\u2011exposed slopes. Wet loose avalanches are the most likely avalanche problem. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly in northern aspects. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3016_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3016"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 600 moh. og oppover, med lokale variasjoner avhengig av hvor i regionen du befinner deg. Det er mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "High temperatures and strong sunshine will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well, but wet avalanches may still release naturally in exposed terrain. Wet loose avalanches are the most likely avalanche problem, especially on steep, sun\u2011exposed slopes. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly on north\u2011facing slopes. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3017_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3017"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 600 moh. og oppover, med lokale variasjoner avhengig av hvor i regionen du befinner deg. Det er mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene.\nObservasjoner viser at det finnes lag av fuktige begerkrystaller ved bakken / dypt i sn\u00f8dekket. Ved rask oppvarming, mye regn eller skavlbrudd kan store skred ikke utelukkes."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "High temperatures and strong sunshine will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well, but wet avalanches may still release naturally in exposed terrain. Wet loose avalanches are the most likely avalanche problem, especially on steep, sun\u2011exposed slopes. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly on north\u2011facing slopes. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6r og regn vil \u00f8ke vanninnholdet i sn\u00f8dekket ytterligere. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig dersom mildv\u00e6ret blir mer omfattende enn ventet. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "Rain will further increase the water content in the snowpack, and wet avalanches may still release naturally in exposed areas.\n\nWet loose avalanches are the most likely avalanche problem. Most of these avalanches are expected to be small, but medium\u2011sized avalanches may also occur. Remember that even small avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, dense snow.\n\nAt higher elevations, there is still layering in the snowpack. When meltwater penetrates downward, these layers can weaken and produce wet slab avalanches. Such avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. In addition, glide avalanches may occur where water accumulates above smooth bed surfaces such as rock slabs."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3018_2026-05-19 15:31:41",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:41",
      "regions": [
        {
          "regionID": "NO-3018"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8overflaten har et tydelig v\u00e5rlig preg, og det har v\u00e6rt kraftig smelting den siste tiden. Sammenhengende sn\u00f8 finnes fra omtrent 600 moh. og oppover, med lokale variasjoner avhengig av hvor i regionen du befinner deg. Det er mest sn\u00f8 i nordvendt terreng og i indre str\u00f8k.\n \nSn\u00f8dekket er i hovedsak smelteomvandlet. Likevel kan det fortsatt finnes noe lagdeling igjen i skyggesider og p\u00e5 de h\u00f8yeste toppene."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "High temperatures and strong sunshine will increase the water content in the snowpack. In many areas, the snowpack is melt\u2011transformed, coarse\u2011grained, and drains water well, but wet avalanches may still release naturally in exposed terrain. Wet loose avalanches are the most likely avalanche problem, especially on steep, sun\u2011exposed slopes. Most are expected to be small, but medium\u2011sized avalanches may occur.\n\nAt higher elevations, layering in the snowpack is still present, particularly on north\u2011facing slopes. With strong meltwater production, water can percolate downward and weaken these layers, potentially triggering wet slab avalanches. These avalanches are difficult to forecast and can be larger than typical loose\u2011snow avalanches. Glide avalanches may also occur where water accumulates above smooth bed surfaces such as rock slabs. In addition, cornices may weaken and break as temperatures rise."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det blir enda varmere. Sn\u00f8en blir fort myk og etterhvert r\u00e5tten. Ogs\u00e5 i nord. De fleste steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "The absence of overnight frost combined with warm temperatures increases the avalanche danger. Wet avalanches, both loose snow avalanches and slab avalanches, may release naturally in exposed areas. Also in northfacing terrain. "
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1100"
          }
        }
      ],
      "bulletinID": "NO-3022_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3022"
        }
      ],
      "snowpackStructure": {
        "comment": "Stort sett er det smelteomvandla sn\u00f8dekke, men det er fortsatt lagdeling i igjen i h\u00f8yden i nord og \u00f8stvendte sider. \nDet er observert flakskred str 2 p\u00e5 \u00f8stsiden av Trolltind og \u00c5bittind 19. mai. Disse har antagelig l\u00f8snet av seg selv p\u00e5 grunn av varmen. Dette bekrefter noen svake lag i sn\u00f8dekket som kan gi flakskred."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break, and glide avalanches are possible, but unpredictable by nature."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det blir enda varmere. Sn\u00f8en blir fort myk og etterhvert r\u00e5tten. Ogs\u00e5 i nord. De fleste steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Antagelig er det mest utbredt i indre deler av regionen.  I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "The absence of overnight frost combined with warm temperatures increases the avalanche danger. Wet avalanches, both loose snow avalanches and slab avalanches, may release naturally in exposed areas. Also in northfacing terrain. "
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1100"
          }
        }
      ],
      "bulletinID": "NO-3023_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "regions": [
        {
          "regionID": "NO-3023"
        }
      ],
      "snowpackStructure": {
        "comment": "Stort sett smelteomvandla sn\u00f8dekke der det er sn\u00f8, kanskje litt lagdeling igjen mot nord p\u00e5 de aller h\u00f8yeste toppene. \n\nNysn\u00f8en som har kommet den siste uken ligger fremdeles igjen som kald sn\u00f8 i helninger som vender vekk fra solen. S\u00f8rvendte helninger har mer smelteomdannet sn\u00f8.\n\nTynt sn\u00f8dekke med bare rygger og mye oppstikkende stein. \nFlakskred i \u00f8stvendt side rett p\u00e5 grensen til Trollheimen ble registrert 19.mai. Dette tyder p\u00e5 svake lag h\u00f8yt til fjells enkelte steder."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break, and glide avalanches are possible, but unpredictable by nature."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det blir enda varmere. Sn\u00f8en blir fort myk og etterhvert r\u00e5tten. Ogs\u00e5 i nord. De fleste steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt. Likevel kan v\u00e5te skred fortsatt l\u00f8sne naturlig p\u00e5 utsatte steder. De fleste ventes \u00e5 v\u00e6re sm\u00e5, men middels store skred kan forekomme.\n\nH\u00f8yt til fjells finnes det fortsatt lagdeling i sn\u00f8dekket. N\u00e5r smeltevann trenger ned i sn\u00f8dekket, kan disse lagene svekkes og gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Antagelig er det tilstede f\u00e5 steder i indre deler av regionen.  I tillegg kan glideskred forekomme der vann samler seg over glatte underlag som svaberg.",
        "highlights": "The absence of overnight frost combined with warm temperatures increases the avalanche danger. Wet avalanches, both loose snow avalanches and slab avalanches, may release naturally in exposed areas. Also in northfacing terrain. "
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1100"
          }
        }
      ],
      "bulletinID": "NO-3024_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "regions": [
        {
          "regionID": "NO-3024"
        }
      ],
      "snowpackStructure": {
        "comment": "Stort sett smelteomvandla sn\u00f8dekke der det er sn\u00f8, kanskje litt lagdeling igjen mot nord p\u00e5 de aller h\u00f8yeste toppene. \nFlakskred i \u00f8stvendt side p\u00e5 grensen mellom Trollheimen og Romsdal ble registrert 19.mai. Dette tyder p\u00e5 at svake lag h\u00f8yt til fjells fortsatt kan finnes enkelte steder."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break, and glide avalanches are possible, but unpredictable by nature."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det blir enda varmere. Sn\u00f8en blir fort myk og etterhvert r\u00e5tten. Ogs\u00e5 i nord. V\u00e5te l\u00f8ssn\u00f8skred kan l\u00f8sne av seg selv i alle himmelretninger. Likevel mest utsatt der sola tar. Mest sannsynlig med sm\u00e5 skred men st\u00f8rrelse 2 kan ikke utelukkes. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. \n\n",
        "highlights": "The avalanche danger varies during the day. The danger is at its highest in steep sun exposed slopes and in the afternoon when the air temperature is high. But, with this high temperatures, avalanches may occur in all aspects."
      },
      "bulletinID": "NO-3027_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3027"
        }
      ],
      "snowpackStructure": {
        "comment": "Sammenhengende sn\u00f8dekke fra ca 800moh litt avhengig av hvor i regionen en befinner seg. Stort sett smelteomvandla sn\u00f8dekke der det er sn\u00f8, kanskje litt lagdeling igjen mot nord p\u00e5 de aller h\u00f8yeste toppene. "
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break, and glide avalanches are possible, but unpredictable by nature."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "H\u00f8yt til fjells kan flakskred fortsatt v\u00e6re sv\u00e6rt lette \u00e5 l\u00f8se ut, s\u00e6rlig dersom regn og stigende temperaturer gj\u00f8r sn\u00f8overflaten myk. Kantkorn og rim som l\u00e5 i overflaten forrige uke har blitt f\u00f8yket ned og gitt flere skred de siste dagene. Det er ogs\u00e5 registrert ustabile testresultater enkelte steder. \n\nDet er ogs\u00e5 mulig \u00e5 l\u00f8se ut v\u00e5te l\u00f8ssn\u00f8skred dersom sn\u00f8overflaten er v\u00e5t og l\u00f8s.",
        "highlights": "Localized wind slabs may rest on buried facets, while small wet loose avalanches will be easy to trigger in steep terrain."
      },
      "avalancheProblems": [
        {
          "problemType": "persistent_weak_layers",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1500"
          }
        }
      ],
      "bulletinID": "NO-3028_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3028"
        }
      ],
      "snowpackStructure": {
        "comment": "Det er sammenhengende sn\u00f8dekke fra rundt 1000 moh. Det er fortsatt lagdelt sn\u00f8 fra ca. 1400 moh. og oppover. Under denne h\u00f8yden er sn\u00f8en smelteomvandlet og v\u00e5t. Det er mest sn\u00f8 i \u00f8stvendte heng, s\u00f8r- og vestvendte heng har det smeltet mye sn\u00f8. \nKantkorn og rim i forrige uke har n\u00e5 blitt f\u00f8yket ned h\u00f8yt til fjells. Siste dagers skredaktivitet og ustabile testresultat viser at skredproblemet er tilstede. I nord- og \u00f8stvendte heng, kan det ogs\u00e5 finnes vedvarende svake lag dypere i sn\u00f8dekket, men disse vurderes som vanskelige \u00e5 p\u00e5virke under de r\u00e5dende forholdene."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Localized wind slabs may rest on buried facets, while small wet loose avalanches will be easy to trigger in steep terrain."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det er ingen aktive skredproblem n\u00e5, men senere p\u00e5 dagen kan stigende temperatur og sol gj\u00f8re det lett \u00e5 l\u00f8se ut sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred i enkelte bratte heng. V\u00e6r spesielt oppmerksom dersom sn\u00f8overflaten blir v\u00e5t og myk.",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3029_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3029"
        }
      ],
      "snowpackStructure": {
        "comment": "Det er fortsatt sammenhengende sn\u00f8 over 900\u20131000 moh. Sn\u00f8dekket er grovkornet og v\u00e5tt opp til ca 1200-1300 moh og drenerer godt. Over dette niv\u00e5et er det fortsatt lagdelt sn\u00f8, spesielt i skyggesider mot nord og \u00f8st. I bratte s\u00f8rvendte sider har sn\u00f8en smeltet bort.\nTidligere kantkornlag lengre nede i sn\u00f8en antas i stor grad \u00e5 v\u00e6re smelteomvandlet og utgj\u00f8r ikke et skredproblem. "
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det blir enda varmere. Sn\u00f8en blir fort myk og etterhvert r\u00e5tten. Ogs\u00e5 i nord. V\u00e5te l\u00f8ssn\u00f8skred kan l\u00f8sne av seg selv i alle himmelretninger. Likevel mest utsatt der sola tar. Mest sannsynlig med sm\u00e5 skred men st\u00f8rrelse 2 kan ikke utelukkes. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. \n\n",
        "highlights": "The avalanche danger varies during the day. The danger is at its highest in steep sun exposed slopes and in the afternoon when the air temperature is high. But, with this high temperatures, avalanches may occur in all aspects."
      },
      "bulletinID": "NO-3031_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3031"
        }
      ],
      "snowpackStructure": {
        "comment": "Stort sett smelteomvandla sn\u00f8dekke der det er sn\u00f8, kanskje litt lagdeling igjen mot nord p\u00e5 de aller h\u00f8yeste toppene. "
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break, and glide avalanches are possible, but unpredictable by nature."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det er ingen aktive skredproblem n\u00e5, men senere p\u00e5 dagen kan stigende temperatur og regn gj\u00f8re det lett \u00e5 l\u00f8se ut sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred i enkelte bratte heng. V\u00e6r spesielt oppmerksom dersom sn\u00f8overflaten blir v\u00e5t og myk.",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3032_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3032"
        }
      ],
      "snowpackStructure": {
        "comment": "Det er fortsatt sn\u00f8 i \u00f8st- og nordvendte heng over ca 1200 moh. Under denne h\u00f8yden er sn\u00f8en v\u00e5t og r\u00e5tten. I bratte s\u00f8rvendte sider har sn\u00f8en smeltet bort.\nI prim\u00e6rt nordvendte sider fra ca 1300 moh og oppover finnes det kantkorn ved bakken. Det utgj\u00f8r ikke et skredproblem for \u00f8yeblikket men kan bli et problem ved kraftig mildv\u00e6r. "
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det blir enda varmere. Sn\u00f8en blir fort myk og etterhvert r\u00e5tten. Ogs\u00e5 i nord. V\u00e5te l\u00f8ssn\u00f8skred kan l\u00f8sne av seg selv i alle himmelretninger. Mest utsatt der det regner eller der sola tar. Typisk vestlandsv\u00e6r. Mest sannsynlig med sm\u00e5 skred men st\u00f8rrelse 2 kan ikke utelukkes. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. \n\n",
        "highlights": "Favorable conditions. Rain and high temperatures high up give increased danger of wet avalanches. Glide avalanches are possible."
      },
      "bulletinID": "NO-3034_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3034"
        }
      ],
      "snowpackStructure": {
        "comment": "Stort sett smelteomvandla sn\u00f8dekke der det er sn\u00f8, kanskje litt lagdeling igjen mot nord p\u00e5 de aller h\u00f8yeste toppene. "
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break, and glide avalanches are possible, but unpredictable by nature."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det er ingen aktive skredproblem n\u00e5, men senere p\u00e5 dagen kan stigende temperatur og regn gj\u00f8re det lett \u00e5 l\u00f8se ut sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred i enkelte bratte heng. V\u00e6r spesielt oppmerksom dersom sn\u00f8overflaten blir v\u00e5t og myk.",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3035_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3035"
        }
      ],
      "snowpackStructure": {
        "comment": "Det er fortsatt sammenhengende sn\u00f8 over ca 1200 moh. Det er mest sn\u00f8 i \u00f8st- og nordvendte heng. I bratte s\u00f8rvendte sider har sn\u00f8en smeltet bort."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Der det finnes sn\u00f8 er det stort sett stabilt. I bratte sider kan det v\u00e6re mulig at v\u00e5te l\u00f8ssn\u00f8skred l\u00f8sner.\n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. ",
        "highlights": "Generally stable conditions. Some rain may lead to wet loose avalanches in steep terrain in the high alpine."
      },
      "bulletinID": "NO-3037_2026-05-19 15:31:42",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-20"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-19T15:31:42",
      "regions": [
        {
          "regionID": "NO-3037"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8grensen kryper oppover. Sn\u00f8dekket er i stort sett smelteomvandla der det er sn\u00f8."
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "Generally stable conditions. Some rain may lead to wet loose avalanches in steep terrain in the high alpine."
        }
      ],
      "validTime": {
        "startTime": "2026-05-20T00:00:00",
        "endTime": "2026-05-20T23:59:59"
      }
    }
  ]
}