{
  "bulletins": [
    {
      "avalancheActivity": {
        "comment": "Det kan fortsatt v\u00e6re lett \u00e5 l\u00f8se ut fokksn\u00f8flak h\u00f8yt til fjells. F\u00f8r det siste sn\u00f8fallet ble det observert kantkorn i overflaten, blandet med nysn\u00f8krystaller. Kantkornkrystallene kan ha blitt begravd av fokksn\u00f8 og danne et svakt lag som gj\u00f8r flakene mer ustabile. V\u00e6r oppmerksom p\u00e5 skytende sprekker og dr\u00f8nn i sn\u00f8en, da dette kan v\u00e6re tegn p\u00e5 at skredproblemet fortsatt er til stede.",
        "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": "800"
          }
        }
      ],
      "bulletinID": "NO-3003_2026-05-20 15:26:44",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:44",
      "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 kan ha lagt seg p\u00e5 kantkorn som tidligere var i overflaten.\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": "Generally stable conditions, but be careful in steep terrain, especially where wind deposited slabs are thin or soft, a slab avalanche is easier to trigger here."
        }
      ],
      "validTime": {
        "startTime": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Mildv\u00e6ret fortsetter og vanninnholdet i sn\u00f8dekket \u00f8ker ytterligere. Det lille sn\u00f8dekket som finnes best\u00e5r i stor grad av grovkornet, smelteomvandlet sn\u00f8 som drenerer vann godt, og forholdene er stort sett stabile. Likevel kan v\u00e5te l\u00f8ssn\u00f8skred forekomme i sv\u00e6rt bratt terreng, s\u00e6rlig der sn\u00f8en er gjennomv\u00e5t.",
        "highlights": "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. "
      },
      "bulletinID": "NO-3006_2026-05-20 15:26:44",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:44",
      "regions": [
        {
          "regionID": "NO-3006"
        }
      ],
      "snowpackStructure": {
        "comment": "I lavlandet og kystn\u00e6re str\u00f8k er det stort sett bart. Ogs\u00e5 h\u00f8yere til fjells i indre str\u00f8k har sn\u00f8dekket 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "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, spesielt i nordvendte sider. 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, 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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3007_2026-05-20 15:26:44",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:44",
      "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": "High temperatures and sunny weather 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "En overskyet natt etterfulgt av en solrik ettermiddag med h\u00f8ye temperaturer vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan smeltevann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3009_2026-05-20 15:26:44",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:44",
      "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": "High temperatures and sunny weather 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "En overskyet natt etterfulgt av en solrik ettermiddag med h\u00f8ye temperaturer vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan smeltevann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3010_2026-05-20 15:26:44",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:44",
      "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.\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": "High temperatures and sunny weather 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "En overskyet natt etterfulgt av en solrik ettermiddag med h\u00f8ye temperaturer vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan smeltevann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3011_2026-05-20 15:26:44",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:44",
      "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": "High temperatures and sunny weather 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "En overskyet natt etterfulgt av en solrik ettermiddag med h\u00f8ye temperaturer vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan smeltevann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3012_2026-05-20 15:26:44",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:44",
      "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": "High temperatures and sunny weather 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "En overskyet natt etterfulgt av en solrik ettermiddag med h\u00f8ye temperaturer vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan smeltevann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3013_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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": "High temperatures and sunny weather 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "H\u00f8ye temperaturer og sol vil gi \u00f8kt sn\u00f8smelting og mer vann i sn\u00f8dekket. Det lille sn\u00f8dekket som finnes best\u00e5r i stor grad av grovkornet, smelteomvandlet sn\u00f8 som drenerer vann godt, og forholdene er stort sett stabile. Likevel kan v\u00e5te l\u00f8ssn\u00f8skred forekomme i sv\u00e6rt bratt terreng, s\u00e6rlig der sn\u00f8en er gjennomv\u00e5t.\n\nGlideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. Slike skred er uforutsigbare, og det er lurt \u00e5 unng\u00e5 opphold i utl\u00f8psomr\u00e5der under sn\u00f8dekte svabergpartier.",
        "highlights": "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."
      },
      "bulletinID": "NO-3014_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "regions": [
        {
          "regionID": "NO-3014"
        }
      ],
      "snowpackStructure": {
        "comment": "I lavlandet og kystn\u00e6re str\u00f8k er det stort sett bart. Ogs\u00e5 h\u00f8yere til fjells har sn\u00f8dekket et v\u00e5rlig preg etter kraftig smelting den siste tiden.\n\nP\u00e5 Hinn\u00f8ya finnes det sammenhengende sn\u00f8 fra cirka 350 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "En overskyet natt etterfulgt av en solrik ettermiddag med h\u00f8ye temperaturer vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan smeltevann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3015_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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": "High temperatures and sunny weather 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "H\u00f8ye temperaturer og kraftig sol vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan vann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3016_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "H\u00f8ye temperaturer og kraftig sol vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan vann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3017_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "H\u00f8ye temperaturer og kraftig sol vil \u00f8ke vanninnholdet i sn\u00f8dekket. Mange steder er sn\u00f8dekket smelteomvandlet, grovkornet og drenerer vann godt, men v\u00e5te skred kan likevel l\u00f8sne naturlig p\u00e5 utsatte steder. V\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet, s\u00e6rlig i bratte solvendte sider. 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, spesielt i nordvendte sider. Ved kraftig sn\u00f8smelting kan vann trenge ned i sn\u00f8dekket og svekke disse lagene, noe som kan gi v\u00e5te flakskred. Slike skred er vanskelige \u00e5 varsle og kan bli st\u00f8rre enn typiske l\u00f8ssn\u00f8skred. Glideskred kan ogs\u00e5 forekomme der vann samler seg over glatte underlag som svaberg. I tillegg kan skavler svekkes og knekke n\u00e5r temperaturen stiger.",
        "highlights": "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."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "1000"
          }
        }
      ],
      "bulletinID": "NO-3018_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "I bratt terreng kan du l\u00f8se ut sm\u00e5 v\u00e5te skred, eller de kan l\u00f8sne av seg selv. \n\nV\u00e6r oppmerksom p\u00e5 at faren for at skavler kan brekke og falle ned \u00f8ker med langvarig varme. Det er ogs\u00e5 fare for glideskred ved bakken. Disse er vanskelige \u00e5 forutse, men hvis du legger merke til at glidesprekker utvider seg er dette et tegn p\u00e5 \u00f8kt fare.",
        "highlights": "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."
      },
      "bulletinID": "NO-3022_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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. "
      },
      "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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "I bratt terreng kan du l\u00f8se ut sm\u00e5 v\u00e5te skred, eller de kan l\u00f8sne av seg selv. \n\nV\u00e6r oppmerksom p\u00e5 at faren for at skavler kan brekke og falle ned \u00f8ker med langvarig varme. Det er ogs\u00e5 fare for glideskred ved bakken. Disse er vanskelige \u00e5 forutse, men hvis du legger merke til at glidesprekker utvider seg er dette et tegn p\u00e5 \u00f8kt fare.",
        "highlights": "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."
      },
      "bulletinID": "NO-3023_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "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. "
      },
      "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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "I bratt terreng kan du l\u00f8se ut sm\u00e5 v\u00e5te skred, eller de kan l\u00f8sne av seg selv. \n\nV\u00e6r oppmerksom p\u00e5 at faren for at skavler kan brekke og falle ned \u00f8ker med langvarig varme. Det er ogs\u00e5 fare for glideskred ved bakken. Disse er vanskelige \u00e5 forutse, men hvis du legger merke til at glidesprekker utvider seg er dette et tegn p\u00e5 \u00f8kt fare.",
        "highlights": "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."
      },
      "bulletinID": "NO-3024_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "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. "
      },
      "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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "I bratt terreng kan du l\u00f8se ut sm\u00e5 v\u00e5te skred, eller de kan l\u00f8sne av seg selv. \n\nV\u00e6r oppmerksom p\u00e5 at faren for at skavler kan brekke og falle ned \u00f8ker med langvarig varme. Det er ogs\u00e5 fare for glideskred ved bakken. Disse er vanskelige \u00e5 forutse, men hvis du legger merke til at glidesprekker utvider seg er dette et tegn p\u00e5 \u00f8kt fare.",
        "highlights": "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."
      },
      "bulletinID": "NO-3027_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "regions": [
        {
          "regionID": "NO-3027"
        }
      ],
      "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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "H\u00f8yt til fjells kan flakskred fortsatt v\u00e6re 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. Det er fortsatt usikkert hvor ustabil sn\u00f8en er, men det ble registrert flere personutl\u00f8ste skred p\u00e5 de h\u00f8yeste toppene i regionen p\u00e5 s\u00f8ndag.\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": "1700"
          }
        }
      ],
      "bulletinID": "NO-3028_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "regions": [
        {
          "regionID": "NO-3028"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8dekket er fortsatt tykt og fint p\u00e5 1400 moh. Fra 1400 moh og oppover er det lagdelt sn\u00f8. Under denne h\u00f8yden er sn\u00f8en mer homogent og usammenhengende. Det er mest sn\u00f8 i nord- og \u00f8stvendte heng.\nKantkorn og rim i forrige uke ble f\u00f8yket ned h\u00f8yt til fjells. S\u00f8ndag var det skredaktivitet og ustabile testresultat. 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": "There are still persistent weak layers in the snowpack that in a few places at higher elevations, can be triggered. Rising temperatures and the lack of overnight freezing increase the water content in the snow, which in turn raises the likelihood of both wet slab avalanches and loose wet avalanches."
        }
      ],
      "validTime": {
        "startTime": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Der sn\u00f8en blir veldig v\u00e5t og myk er det fare for v\u00e5te l\u00f8ssn\u00f8skred i bratt terreng. \u00d8kende temperatur og regn \u00f8ker sannsynligheten. Etter hvert vil ogs\u00e5 solen varme opp sn\u00f8en.\u00a0",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3029_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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": "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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "I bratt terreng kan du l\u00f8se ut sm\u00e5 v\u00e5te skred, eller de kan l\u00f8sne av seg selv. \n\nV\u00e6r oppmerksom p\u00e5 at faren for at skavler kan brekke og falle ned \u00f8ker med langvarig varme. Det er ogs\u00e5 fare for glideskred ved bakken. Disse er vanskelige \u00e5 forutse, men hvis du legger merke til at glidesprekker utvider seg er dette et tegn p\u00e5 \u00f8kt fare.",
        "highlights": "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."
      },
      "bulletinID": "NO-3031_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Der sn\u00f8en blir veldig v\u00e5t og myk er det fare for v\u00e5te l\u00f8ssn\u00f8skred i bratt terreng. \u00d8kende temperatur og regn \u00f8ker sannsynligheten. Etter hvert vil ogs\u00e5 solen varme opp sn\u00f8en.\u00a0",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3032_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break."
        }
      ],
      "validTime": {
        "startTime": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "I bratt terreng kan du l\u00f8se ut sm\u00e5 v\u00e5te skred, eller de kan l\u00f8sne av seg selv. \n\nV\u00e6r oppmerksom p\u00e5 at faren for at skavler kan brekke og falle ned \u00f8ker med langvarig varme. Det er ogs\u00e5 fare for glideskred ved bakken. Disse er vanskelige \u00e5 forutse, men hvis du legger merke til at glidesprekker utvider seg er dette et tegn p\u00e5 \u00f8kt fare.",
        "highlights": "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."
      },
      "bulletinID": "NO-3034_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "regions": [
        {
          "regionID": "NO-3034"
        }
      ],
      "snowpackStructure": {
        "comment": "Stort sett smelteomvandla sn\u00f8dekke der det er sn\u00f8 igjen. I nordvendte sider p\u00e5 de h\u00f8yeste toppene kan det stedvis v\u00e6re noe lagdeling."
      },
      "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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Der sn\u00f8en blir veldig v\u00e5t og myk er det fare for v\u00e5te l\u00f8ssn\u00f8skred i bratt terreng. \u00d8kende temperatur og regn \u00f8ker sannsynligheten. Etter hvert vil ogs\u00e5 solen varme opp sn\u00f8en.\u00a0",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3035_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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": "Generally stable conditions. Warm temperatures may increase the danger of wet loose avalanches in steep, high alpine terrain. Cornices may weaken and break."
        }
      ],
      "validTime": {
        "startTime": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    },
    {
      "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_2026-05-20 15:26:45",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-21"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-20T15:26:45",
      "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. 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": "2026-05-21T00:00:00",
        "endTime": "2026-05-21T23:59:59"
      }
    }
  ]
}