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  • 61. Publications 2017

    Monique Gosseling445,3 2017-005 The ICRA atmospheric reanalysis project for IcelandNikolai Nawri, Bolli Pálmason, Guðrún Nína Petersen, Halldór Björnsson & Sigurður Þorsteinsson 37 3,8 2017-002 Atmospheric Sounding by TAMDAR over Keflavík Airport, Iceland – Comparison with Traditional Atmospheric Sounding Methods Arnór Tumi Jóhannsson 70 2,1 /about-imo/publications/2017
  • 62. 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
  • 63. 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
  • 64. 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
  • 65. 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
  • 66. 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
  • 67. 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
  • 68. 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
  • 69. 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
  • 70. 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

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