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Results:

• 21. 2010_016

  and the groundwater module. The coupling between both modules was done by a net boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each /media/ces/2010_016.pdf

• 22. 2010_017

  of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf

• 23. Bardarbunga-2014_August-events

  in 1991. The blue dashed line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm /media/jar/Bardarbunga-2014_August-events.pdf

• 24. Bárðarbunga 2014 - August events

  line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm at Bárðarbunga on Saturday /earthquakes-and-volcanism/articles/nr/3000/

• 25. NONAM_1st_workshop_summary_v3

  /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 26. norsem_gunnar

  Seismic activity in Iceland 2015 – 2016 and testing of near-real time automatic relative locations Gunnar B. Guðmundsson¹ and the Natural Hazards monitoring team ¹Icelandic Meteorological Office, Bústaðavegi 7-9, 108 Reykjavík, Iceland, gg@vedur.is At present, in September 2016 the SIL seismic monitoring network consists of around 70 seismic stations. The number of earthquakes located /media/norsem/norsem_gunnar.pdf

• 27. The weather in Iceland 2014

  rank of dev. 2004-2013 Reykjavík 6.0 1.7 2 144 0.6 Stykkishólmur 5.3 1.8 3 169 0.6 Bolungarvík 4.7 1.7 5 117 0.7 Bergstaðir 4.7 2 37 0.9 Grímsey 4.9 1 141 1.3 Akureyri 5.3 2.1 2 133 1.0 Grímsstaðir 2.8 2.3 1 108 1.3 Egilsstaðir 5.1 2.2 1 60 1.3 Dalatangi 5.3 1.9 1 76 0.7 Teigarhorn 5.8 2.1 1 142 1.1 Höfn í /about-imo/news/nr/3082

• 28. ved-eng-2014

  month of the year. Table 1. Temperature in 2014 station temp °C dev. 1961-1990 rank of dev. 2004-2013 Reykjavík 6.0 1.7 2 144 0.6 Stykkishólmur 5.3 1.8 3 169 0.6 Bolungarvík 4.7 1.7 5 117 0.7 Bergstaðir 4.7 2 37 0.9 Grímsey 4.9 1 141 1.3 Akureyri 5.3 2.1 2 133 1.0 Grímsstaðir 2.8 2.3 1 108 1.3 Egilsstaðir 5.1 2.2 1 60 1.3 Dalatangi 5.3 1.9 1 76 0.7 Teigarhorn /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf

• 29. Reports and publications

  ) Ragnar Stefánsson et al. 108 9.2 2005 Management and resource usage summary Months 19 - 24: August 1, 2004 - January 31, 2005 (PDF) Ragnar Stefánsson, Barði Þorkelsson 16 1,3 2005 Seismic activity in Iceland during 2004 (PDF) Sigurlaug Hjaltadóttir, Halldór Geirsson, Þórunn Skaftadóttir 13 2,8 2005 Forecasting and Monitoring a Subglacial Eruption in Iceland (PDF) Kristín Vogfjörð /earthquakes-and-volcanism/reports-and-publications/

• 30. The weather in Iceland in 2022

  156 Stykkishólmur 794.1 108 107 29.8 211 136 Hólar í Dýrafirði 940.9 # 79 62.5 236 132 Litla-Ávík 874.1 # 100 30.2 245 149 Sauðanesviti 1252.5 142 133 57.9 234 153 Akureyri 600.9 105 92 33.2 203 115 Grímsstaðir 551.4 141 123 23.9 234 124 /about-imo/news/the-weather-in-iceland-in-2022