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• 21. About the implementation

  are in the forefront. Architecture It was decided to use the Eplica content management system. It is as a Java based system so specific dynamic components were written in Java. It was decided to use Servlets and the MVC pattern, with minimal usage of Eplica API. This way the components may be moved and reused with minimal efforts in other Java CMS or converted to Portlets (JSR 168) if and when /about-imo/the-web/implementation/

• 22. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 23. The weather in Iceland in 2019

  Mýri 451.4 103.2 83.7 44,0 173 105 Grímsstaðir 399.1 110.7 91.7 21.3 190 116 Dalatangi 1577.2 105.1 86.5 74.9 284 168 Höfn í Hornafirði 1295.0 # 81.3 45.9 219 150 Vatnsskarðshólar 1852.9 113.5 104.3 98.8 246 188 Hjarðarland 1161.3 # 91.8 64.0 /about-imo/news/the-weather-in-iceland-in-2019

• 24. VI_2020_011_en

  An initial volcanic hazard assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, Jacopo Selva, Simone Tarquini, Mattia de´Michieli Vitturi, Ingibjörg Jónsdóttir, Davið Egilson /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 25. The weather in Iceland 2013

  location t-mean dev 1961-1990 rank total dev 2003-2012 Reykjavík 4,9 0,6 36 143 -0,6 Stykkishólmur 4,4 0,9 26 168 -0,4 Bolungarvík 3,7 0,8 31 115 -0,4 Bergstaðir 3,5 -0,4 Akureyri 4,1 0,8 35 132 -0,4 Grímsstaðir 1,0 0,5 -0,6 Egilsstaðir 3,8 0,9 19 59 -0,1 Dalatangi 4,5 1,0 17 to 18 75 -0,1 Teigarhorn 4,6 0,9 /weather/articles/nr/2824

• 26. ved-eng-2013

  of above-normal temperatures and the 15th in Akureyri in the north. location t-mean dev 1961-1990 rank total dev 2003-2012 Reykjavík 4,9 0,6 36 143 -0,6 Stykkishólmur 4,4 0,9 26 168 -0,4 Bolungarvík 3,7 0,8 31 115 -0,4 Bergstaðir 3,5 -0,4 Akureyri 4,1 0,8 35 132 -0,4 Grímsstaðir 1,0 0,5 -0,6 Egilsstaðir 3,8 0,9 19 59 -0,1 Dalatangi 4,5 1,0 17 to 18 75 -0,1 Teigarhorn 4,6 0,9 24 /media/vedurstofan/utgafa/skylduskil/ved-eng-2013.pdf

• 27. askja_minnisblad_ens

  Minnisblað ___________________________________________________ 7 Figure 8. Right: An areal photo of the rockslide area in Suðurbotnar. There is evidence of older movement which is probably an old rockslide. Left: The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 28. IPPC-2007-ar4_syr

  significantly in eastern parts of North and South America, northern Europe and northern and central Asia whereas precipita- tion declined in the Sahel, the Mediterranean, southern Africa and parts of southern Asia. Globally, the area affected by drought has likely2 increased since the 1970s. {WGI 3.3, 3.9, SPM} Some extreme weather events have changed in frequency and/ or intensity over the last 50 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 29. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  : The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit, the edge seems to have advanced (purple area). Background: Loftmyndir ehf. Analyses: Ásta Rut Hjartardóttir and Þorsteinn Sæmundsson. Fig. 9 Figure 9. Geological map showing the outline of the rockslide, as well as eruptive fissures /avalanches/articles/nr/2929

• 30. Moellenkampetal_etal-2010

  Acteurs et Usages (UMR G-EAU), Cemagref, 4University of Architecture, Civil Engineering and Geodesy, 5Hornsby Shire Council, 6Lisode, 7UN-Water Decade Programme on Capacity Development (UNW-DPC), United Nations University, 8School of Natural and Rural Systems Management, University of Queensland, 9College of Asia and the Pacific, The Australian National University, 10Marine and Atmospheric Research /media/loftslag/Moellenkampetal_etal-2010.pdf