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• 11. 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/

• 12. 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

• 13. 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

• 14. 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

• 15. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 16. IMO_AnnualReport2014

  of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 17. VI_2022_006_extreme

  Þingvallavatn 2 years 5 years 10 years 25 years 50 years 100 years 3 hours 12 15 18 19 21 23 6 hours 26 31 35 38 41 44 12 hours 48 56 62 67 73 77 24 hours 78 90 99 107 117 124 48 hours 113 128 138 148 159 168 26 Figure 12 – 1M5 map for catchment Hálslón based on the complete ICRA dataset. Figure 13 – 1M5 map for catchment Þingvallavatn based on the complete ICRA dataset. 27 5.2 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 18. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 19. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf

• 20. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf