{
  "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 godt utviklet 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. ",
        "highlights": "Avalanches may be very easy to trigger where wind slabs rest on near-surface faceted crystals. Whumpf sounds and shooting cracks are clear signs of instability."
      },
      "avalancheProblems": [
        {
          "problemType": "persistent_weak_layers",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE"
          ],
          "elevation": {
            "lowerBound": "400"
          }
        }
      ],
      "bulletinID": "NO-3003_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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. \nNysn\u00f8en la seg over et l\u00f8st lag med kantkorn.\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": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Det er generelt stabile forhold. V\u00e5te l\u00f8ssn\u00f8skred kan likevel forekommer i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bare steiner/klipper.",
        "highlights": "Generally stable conditions, but danger of small wet avalanches in sun-exposed mountainsides."
      },
      "bulletinID": "NO-3006_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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 indrestr\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 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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Dersom det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest utbredte skredproblemet, s\u00e6rlig i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bar stein/klipper. De fleste skredene vil v\u00e6re sm\u00e5, men middels store skred kan ogs\u00e5 forekomme. Husk ogs\u00e5 at selv sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge sn\u00f8mass\u00ader.\n\nV\u00e6r ogs\u00e5 oppmerksom p\u00e5 at enkelte v\u00e5te flakskred og/eller glideskred kan forekomme der smeltevann samler seg p\u00e5 gamle skarelag dypere i sn\u00f8dekket eller p\u00e5 omr\u00e5der med svaberg.",
        "highlights": "The avalanche danger varies significantly across the region and depends largely on local overnight temperatures. Where there has been no overnight freeze due to cloud cover, and mild temperatures extend high into the mountains, the avalanche danger will already be elevated in the morning. The combination of wet snow and strong sunshine further weakens the snowpack.\n\nWet loose avalanches are the most widespread avalanche problem, particularly in very steep, sun\u2011exposed terrain and below areas with exposed rock or cliffs. Most avalanches will be small, but medium\u2011sized avalanches may also occur. Remember that even small wet loose avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, wet snow.\n\nBe aware that wet slab avalanches and/or glide avalanches may also occur where meltwater accumulates on old crust layers deeper in the snowpack or in areas with smooth bedrock."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3007_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Dersom det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest utbredte skredproblemet, s\u00e6rlig i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bar stein/klipper. De fleste skredene vil v\u00e6re sm\u00e5, men middels store skred kan ogs\u00e5 forekomme. Husk ogs\u00e5 at selv sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge sn\u00f8mass\u00ader.\n\nV\u00e6r ogs\u00e5 oppmerksom p\u00e5 at enkelte v\u00e5te flakskred og/eller glideskred kan forekomme der smeltevann samler seg p\u00e5 gamle skarelag dypere i sn\u00f8dekket eller p\u00e5 omr\u00e5der med svaberg.",
        "highlights": "The avalanche danger varies significantly across the region and depends largely on local overnight temperatures. Where there has been no overnight freeze due to cloud cover, and mild temperatures extend high into the mountains, the avalanche danger will already be elevated in the morning. The combination of wet snow and strong sunshine further weakens the snowpack.\n\nWet loose avalanches are the most widespread avalanche problem, particularly in very steep, sun\u2011exposed terrain and below areas with exposed rock or cliffs. Most avalanches will be small, but medium\u2011sized avalanches may also occur. Remember that even small wet loose avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, wet snow.\n\nBe aware that wet slab avalanches and/or glide avalanches may also occur where meltwater accumulates on old crust layers deeper in the snowpack or in areas with smooth bedrock."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3009_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "regions": [
        {
          "regionID": "NO-3009"
        }
      ],
      "snowpackStructure": {
        "comment": "Sn\u00f8dekket er smelteomvandlet, med hard skare om morgenen der nattefrost gir gjenfrysing, men myk og v\u00e5t overflate fra starten av dagen der dette uteblir.  Det kan finnes lagdelt sn\u00f8 i nordvendt terreng h\u00f8yt til fjells.\n\nDet er generelt lite sn\u00f8 under 150 moh, men stort sett sammenhengende skif\u00f8re fra ca 200-300 moh de fleste steder i regionen.\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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Dersom det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest utbredte skredproblemet, s\u00e6rlig i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bar stein/klipper. De fleste skredene vil v\u00e6re sm\u00e5, men middels store skred kan ogs\u00e5 forekomme. Husk ogs\u00e5 at selv sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge sn\u00f8mass\u00ader.\n\nV\u00e6r ogs\u00e5 oppmerksom p\u00e5 at enkelte v\u00e5te flakskred og/eller glideskred kan forekomme der smeltevann samler seg p\u00e5 gamle skarelag dypere i sn\u00f8dekket eller p\u00e5 omr\u00e5der med svaberg.",
        "highlights": "The avalanche danger varies significantly across the region and depends largely on local overnight temperatures. Where there has been no overnight freeze due to cloud cover, and mild temperatures extend high into the mountains, the avalanche danger will already be elevated in the morning. The combination of wet snow and strong sunshine further weakens the snowpack.\n\nWet loose avalanches are the most widespread avalanche problem, particularly in very steep, sun\u2011exposed terrain and below areas with exposed rock or cliffs. Most avalanches will be small, but medium\u2011sized avalanches may also occur. Remember that even small wet loose avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, wet snow.\n\nBe aware that wet slab avalanches and/or glide avalanches may also occur where meltwater accumulates on old crust layers deeper in the snowpack or in areas with smooth bedrock."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3010_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren varierer betydelig i regionen og avhenger i stor grad av lokale temperaturforhold gjennom natten. Der det ikke har v\u00e6rt nattefrost p\u00e5 grunn av skydekke, og mildv\u00e6ret strekker seg h\u00f8yt til fjells, vil skredfaren v\u00e6re forh\u00f8yet allerede fra morgenen. Kombinasjonen av v\u00e5t sn\u00f8 og sterk sol gir ytterligere svekkelse av sn\u00f8dekket.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest utbredte skredproblemet, s\u00e6rlig i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bar stein/klipper. De fleste skredene vil v\u00e6re sm\u00e5, men middels store skred kan ogs\u00e5 forekomme. Husk ogs\u00e5 at selv sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge sn\u00f8mass\u00ader.\n\nV\u00e6r ogs\u00e5 oppmerksom p\u00e5 at enkelte v\u00e5te flakskred og/eller glideskred kan forekomme der smeltevann samler seg p\u00e5 gamle skarelag dypere i sn\u00f8dekket eller p\u00e5 omr\u00e5der med svaberg.",
        "highlights": "The avalanche danger varies significantly across the region and depends largely on local overnight temperatures. Where there has been no overnight freeze due to cloud cover, and mild temperatures extend high into the mountains, the avalanche danger will already be elevated in the morning. The combination of wet snow and strong sunshine further weakens the snowpack.\n\nWet loose avalanches are the most widespread avalanche problem, particularly in very steep, sun\u2011exposed terrain and below areas with exposed rock or cliffs. Most avalanches will be small, but medium\u2011sized avalanches may also occur. Remember that even small wet loose avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, wet snow.\n\nBe aware that wet slab avalanches and/or glide avalanches may also occur where meltwater accumulates on old crust layers deeper in the snowpack or in areas with smooth bedrock."
      },
      "bulletinID": "NO-3011_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Dersom det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest utbredte skredproblemet, s\u00e6rlig i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bar stein/klipper. De fleste skredene vil v\u00e6re sm\u00e5, men middels store skred kan ogs\u00e5 forekomme. Husk ogs\u00e5 at selv sm\u00e5 v\u00e5te skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge sn\u00f8mass\u00ader.\n\nV\u00e6r ogs\u00e5 oppmerksom p\u00e5 at enkelte v\u00e5te flakskred og/eller glideskred kan forekomme der smeltevann samler seg p\u00e5 gamle skarelag dypere i sn\u00f8dekket eller p\u00e5 omr\u00e5der med svaberg.",
        "highlights": "The avalanche danger varies significantly across the region and depends largely on local overnight temperatures. Where there has been no overnight freeze due to cloud cover, and mild temperatures extend high into the mountains, the avalanche danger will already be elevated in the morning. The combination of wet snow and strong sunshine further weakens the snowpack.\n\nWet loose avalanches are the most widespread avalanche problem, particularly in very steep, sun\u2011exposed terrain and below areas with exposed rock or cliffs. Most avalanches will be small, but medium\u2011sized avalanches may also occur. Remember that even small wet loose avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, wet snow.\n\nBe aware that wet slab avalanches and/or glide avalanches may also occur where meltwater accumulates on old crust layers deeper in the snowpack or in areas with smooth bedrock."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3012_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Dersom det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest utbredte skredproblemet, s\u00e6rlig i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bare steiner/klipper. De fleste skredene vil v\u00e6re sm\u00e5, men middels store skred kan ogs\u00e5 forekomme. Husk ogs\u00e5 at selv sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge sn\u00f8mass\u00ader.\n\nV\u00e6r ogs\u00e5 oppmerksom p\u00e5 at enkelte v\u00e5te flakskred og/eller glideskred kan forekomme der smeltevann samler seg p\u00e5 gamle skarelag dypere i sn\u00f8dekket eller p\u00e5 omr\u00e5der med svaberg.",
        "highlights": "The avalanche danger varies significantly across the region and depends largely on local overnight temperatures. Where there has been no overnight freeze due to cloud cover, and mild temperatures extend high into the mountains, the avalanche danger will already be elevated in the morning. The combination of wet snow and strong sunshine further weakens the snowpack.\n\nWet loose avalanches are the most widespread avalanche problem, particularly in very steep, sun\u2011exposed terrain and below areas with exposed rock or cliffs. Most avalanches will be small, but medium\u2011sized avalanches may also occur. Remember that even small wet loose avalanches can be dangerous in steep and exposed terrain, as they consist of heavy, wet snow.\n\nBe aware that wet slab avalanches and/or glide avalanches may also occur where meltwater accumulates on old crust layers deeper in the snowpack or in areas with smooth bedrock."
      },
      "avalancheProblems": [
        {
          "problemType": "wet_snow",
          "aspects": [
            "N",
            "NE",
            "E",
            "SE",
            "S",
            "SW",
            "W",
            "NW"
          ],
          "elevation": {
            "lowerBound": "700"
          }
        }
      ],
      "bulletinID": "NO-3013_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "V\u00e5te l\u00f8ssn\u00f8skred er det mest utbredte skredproblemet, s\u00e6rlig i sv\u00e6rt bratt, solvendt terreng og under omr\u00e5der med bare steiner/klipper. De fleste skredene vil v\u00e6re sm\u00e5, men middels store skred kan ogs\u00e5 forekomme. Husk ogs\u00e5 at selv sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge sn\u00f8mass\u00ader.\n\nGlideskred kan forekomme der vann samler seg over glatte underlag som svaberg.\n",
        "highlights": "Sunny weather and high day temperatures mean that wet loose avalanches may release naturally on steep, solar aspects."
      },
      "bulletinID": "NO-3014_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Der det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. Selv om de fleste ventes \u00e5 v\u00e6re sm\u00e5, er det viktig \u00e5 huske at ogs\u00e5 sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge og kompakte sn\u00f8mass\u00ader.\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 avalanche danger is largely controlled by local temperature conditions. A solid overnight freeze can provide a short-term stabilising effect, but once the temperatures rise and sunshine weakens the snowpack the avalanche danger increases.\n\nWet loose avalanches are the most likely problem. Although most of these avalanches are expected to be small, it is important to remember that even small wet loose 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, and 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": "1100"
          }
        }
      ],
      "bulletinID": "NO-3015_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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, 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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Der det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. Selv om de fleste ventes \u00e5 v\u00e6re sm\u00e5, er det viktig \u00e5 huske at ogs\u00e5 sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge og kompakte sn\u00f8mass\u00ader.\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 avalanche danger is largely controlled by local temperature conditions. A solid overnight freeze can provide a short-term stabilising effect, but once the temperatures rise and sunshine weakens the snowpack the avalanche danger increases.\n\nWet loose avalanches are the most likely problem. Although most of these avalanches are expected to be small, it is important to remember that even small wet loose 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, and 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": "1100"
          }
        }
      ],
      "bulletinID": "NO-3016_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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, 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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Der det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. Selv om de fleste ventes \u00e5 v\u00e6re sm\u00e5, er det viktig \u00e5 huske at ogs\u00e5 sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge og kompakte sn\u00f8mass\u00ader.\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 avalanche danger is largely controlled by local temperature conditions. A solid overnight freeze can provide a short-term stabilising effect, but once the temperatures rise and sunshine weakens the snowpack the avalanche danger increases.\n\nWet loose avalanches are the most likely problem. Although most of these avalanches are expected to be small, it is important to remember that even small wet loose 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, and 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": "1100"
          }
        }
      ],
      "bulletinID": "NO-3017_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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, 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.\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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren styres i stor grad av de lokale temperaturforholdene. Der det kommer nattefrost, kan sn\u00f8dekket f\u00e5 en kortvarig stabilisering, og skredfaren vil mange steder kunne oppleves som lav, spesielt tidlig p\u00e5 dagen. N\u00e5r mildv\u00e6ret og sola f\u00e5r tak svekkes sn\u00f8dekket likevel raskt, og skredfaren \u00f8ker tilsvarende.\n\nV\u00e5te l\u00f8ssn\u00f8skred er det mest sannsynlige skredproblemet. Selv om de fleste ventes \u00e5 v\u00e6re sm\u00e5, er det viktig \u00e5 huske at ogs\u00e5 sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred kan v\u00e6re farlige i bratt og eksponert terreng, ettersom de best\u00e5r av tunge og kompakte sn\u00f8mass\u00ader.\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 avalanche danger is largely controlled by local temperature conditions. A solid overnight freeze can provide a short-term stabilising effect, but once the temperatures rise and sunshine weakens the snowpack the avalanche danger increases.\n\nWet loose avalanches are the most likely problem. Although most of these avalanches are expected to be small, it is important to remember that even small wet loose 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, and 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": "1100"
          }
        }
      ],
      "bulletinID": "NO-3018_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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, 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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Stort sett stabilt sn\u00f8dekke, men der sn\u00f8en blir v\u00e5t og myk utover dagen kan det g\u00e5 enkelte v\u00e5te l\u00f8ssn\u00f8skred. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. ",
        "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."
      },
      "bulletinID": "NO-3022_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "regions": [
        {
          "regionID": "NO-3022"
        }
      ],
      "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": "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. "
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Stort sett stabilt sn\u00f8dekke, men der sn\u00f8en blir v\u00e5t og myk utover dagen kan det g\u00e5 enkelte v\u00e5te l\u00f8ssn\u00f8skred. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. ",
        "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."
      },
      "bulletinID": "NO-3023_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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. "
      },
      "source": {
        "provider": {
          "name": "NVE",
          "website": "https://www.varsom.no/en/avalanches/avalanche-warnings/"
        }
      },
      "tendency": [
        {
          "comment": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Stort sett stabilt sn\u00f8dekke, men der sn\u00f8en blir v\u00e5t og myk utover dagen kan det g\u00e5 enkelte v\u00e5te l\u00f8ssn\u00f8skred. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. ",
        "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."
      },
      "bulletinID": "NO-3024_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Stort sett stabilt sn\u00f8dekke, men der sn\u00f8en blir v\u00e5t og myk utover dagen kan det g\u00e5 enkelte v\u00e5te l\u00f8ssn\u00f8skred. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. ",
        "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."
      },
      "bulletinID": "NO-3027_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "H\u00f8yt til fjells kan flakskred fortsatt v\u00e6re sv\u00e6rt lette \u00e5 l\u00f8se ut, s\u00e6rlig dersom sol og stigende temperaturer gj\u00f8r sn\u00f8overflaten myk. Det har g\u00e5tt flere skred de siste dagene, og det er observert dr\u00f8nn i sn\u00f8dekket. Det er ogs\u00e5 registrert ustabile testresultater enkelte steder. Kantkorn og rim som l\u00e5 i overflaten forrige uke har blitt f\u00f8yket ned. \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_2026-05-18 15:48:36",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "moderate",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:36",
      "regions": [
        {
          "regionID": "NO-3028"
        }
      ],
      "snowpackStructure": {
        "comment": "I helga kom det 5-10 cm nysn\u00f8. Sn\u00f8grensa ligger rundt 1000 moh, med gode skiforhold over denne h\u00f8yden. Det er fortsatt lagdelt sn\u00f8 fra ca. 1400 moh. og oppover. Under denne h\u00f8yden er sn\u00f8en smelteomvandlet. \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": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren \u00f8ker n\u00e5r solen kommer frem og temperaturen stiger. V\u00e6r spesielt oppmerksom om sn\u00f8overflaten blir v\u00e5t og myk. I enkelte bratte heng kan det v\u00e6re lett \u00e5 l\u00f8se ut sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred.",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3029_2026-05-18 15:48:37",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:37",
      "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": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Stort sett stabilt sn\u00f8dekke, men der sn\u00f8en blir v\u00e5t og myk utover dagen kan det g\u00e5 enkelte v\u00e5te l\u00f8ssn\u00f8skred. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. ",
        "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."
      },
      "bulletinID": "NO-3031_2026-05-18 15:48:37",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:37",
      "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": "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."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren \u00f8ker n\u00e5r temperaturen stiger. V\u00e6r spesielt oppmerksom om sn\u00f8overflaten blir v\u00e5t og myk. I enkelte bratte heng kan det v\u00e6re lett \u00e5 l\u00f8se ut sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred.",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3032_2026-05-18 15:48:37",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:37",
      "regions": [
        {
          "regionID": "NO-3032"
        }
      ],
      "snowpackStructure": {
        "comment": "Det er fortsatt mye 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 nord- og \u00f8stvendte h\u00f8yfjellsomr\u00e5der finnes det stedvis fortsatt et lagdelt sn\u00f8dekke. Her kan det ogs\u00e5 finnes et vedvarende svake lag av kantkorn og begerkrystaller n\u00e6r bakken, men disse utgj\u00f8r ikke et skredproblem for \u00f8yeblikket."
      },
      "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": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Stort sett stabilt sn\u00f8dekke, men der sn\u00f8en er v\u00e5t kan det fortsatt g\u00e5 enkelte v\u00e5te l\u00f8ssn\u00f8skred. \n\nUnng\u00e5 \u00e5 oppholde deg under glidesprekker og hold avstand til skavler som kan knekke i varmen. ",
        "highlights": "It\u2019s mainly stable snow, but it is possible to trigger small avlanches in steep terrain where the snow is very wet. Keep a safe distance to cornices and glide cracks."
      },
      "bulletinID": "NO-3034_2026-05-18 15:48:37",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:37",
      "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": "Favorable conditions. Rain and high temperatures high up give increased danger of wet avalanches. Glide avalanches are possible."
        }
      ],
      "validTime": {
        "startTime": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Skredfaren \u00f8ker n\u00e5r temperaturen stiger. V\u00e6r spesielt oppmerksom om sn\u00f8overflaten blir v\u00e5t og myk. I enkelte bratte heng kan det v\u00e6re lett \u00e5 l\u00f8se ut sm\u00e5 v\u00e5te l\u00f8ssn\u00f8skred.",
        "highlights": "The snowpack is generally stable, but be cautious in steep terrain if the snow surface is wet and soft."
      },
      "bulletinID": "NO-3035_2026-05-18 15:48:37",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:37",
      "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": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    },
    {
      "avalancheActivity": {
        "comment": "Stort sett stabilt sn\u00f8dekke, men der sn\u00f8en blir v\u00e5t av regn kan det fortsatt g\u00e5 enkelte v\u00e5te l\u00f8ssn\u00f8skred. \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, especially at higher elevations where the water drains more slowly through the snowpack."
      },
      "bulletinID": "NO-3037_2026-05-18 15:48:37",
      "customData": {
        "ALBINA": {
          "mainDate": "2026-05-19"
        }
      },
      "dangerRatings": [
        {
          "mainValue": "low",
          "validTimePeriod": "all_day"
        }
      ],
      "publicationTime": "2026-05-18T15:48:37",
      "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": "2026-05-19T00:00:00",
        "endTime": "2026-05-19T23:59:59"
      }
    }
  ]
}