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• 21. Terms and conditions

  no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.) The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove /about-imo/the-web/conditions

• 22. Avalanche danger scale

  of snow avalanches Veðurstofa Íslands 17.1.2013 On IMO's avalanche forecast maps, an international colour code is used, see below. The table and the icons are from EAWS. A specific map is presented for each of three selected high risk areas. Additionally, IMO issues /avalanches/articles/nr/2619

• 23. Avalanches in Iceland

  observations of avalanches as well as avalanche conditions and avalance forecast for selected areas. An avalanche map viewer is also available, aimed at easing user access to avalanche and landslide data gathered and processed at IMO. North West A passage has been made through snow on the road. Súðavík, Súðavíkurhlíð, in the West fjords, 7 April 2010. Photo: Þórður Sigurðsson. South /avalanches/avalanches

• 24. Avalanche bulletin

  Avalanche bulletin Avalanche conditions Snow is in spring conditions, generally homogeneous and stable. A thin layer of new snow can be found in places. Small, loose avalanches may occur with solar radiation and cornices can collapse.Written /avalanches/forecast

• 25. Avalanche bulletin - Eastfjords

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/east_fjords

• 26. Avalanche bulletin - Eyjafjörður (experimental)

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/inner_eyjafjordur

• 27. Avalanche bulletin - Northern Westfjords

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/northern_westfjords

• 28. Avalanche bulletin - Southwest corner

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/southwest_corner

• 29. Avalanche bulletin - Tröllaskagi

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/trollaskagi

• 30. Climate of Iceland

  (IPCC) UN Framework Convention on Climate Change NOAA Climate Program Office NASA Climate and Radiation Branch Climate Institute Real Climate /climatology/iceland