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Results:

• 61. VI_2022_006_extreme

  -year return period, based on the complete ICRA dataset. Timeseries were extracted using the average value of all the grid-points within the catchment. 1M5 value is shown in red. Hálslón 2 years 5 years 10 years 25 years 50 years 100 years 3 hours 8 11 13 15 18 20 6 hours 18 23 27 31 36 39 12 hours 35 43 49 54 62 67 24 hours 60 70 78 85 94 101 48 hours 91 105 115 125 137 147 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 62. Earthquakes shake Bláfjöll ski-area

  to Earthquakes shake Bláfjöll ski-area Two earthquakes of magnitude around M4 occurred, only 5 seconds apart, 14.9.2018 On the 13th of September at 20:17, two earthquakes of magnitude /about-imo/news/earthquakes-around-blafjoll-ski-are

• 63. 2013_001_Nawri_et_al

  the Fljótsdalsheiði region . . . . . . . 47 18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48 19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49 20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50 21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51 22 Seasonal mean /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 64. Journal_of_Hydrology_Veijalainen_etal

  in flooding were evaluated at 67 sites in Finland with var- iable sizes of runoff areas using a conceptual hydrological model and 20 climate scenarios from both glo- bal and regional climate models with the delta change approach. Floods with a 100-year return period were estimated with frequency analysis using the Gumbel distribution. At four study sites depicting dif- ferent watershed types /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 65. „We need to control our footprint on mother Earth“

  /about-imo/news/we-need-to-control-our-footprint-on-mother-earth

• 66. VI_2009_013

  20 cm of observed uplift was modelled with another sill intrusion, but deeper than before, at ~6.3 km depth (Pedersen and Sigmundsson, 2005). Both intrusion episodes, in 1994 and 1999, were also detected by GPS and dry tilt measurements. Sturkell et al. (2003) modelled the data from 1999 by a point pressure source at 3.5 km depth, just south of the glacier rim. They suggested a similar model /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 67. Windspeed

  -values, average windspeed and the median for the average windspeed in m/s, km/h, and knots. Top of page Windspeed classification To ease the understanding of the m/s measurement, the following table can be used. Windspeed IN m/s Description <5 Very slow wind 5-10 Rather slow wind 10-20 Considerable wind, may lead to difficulties 20-30 Very windy, caution is advised >30 /weather/articles/nr/1283

• 68. Windspeed

  -values, average windspeed and the median for the average windspeed in m/s, km/h, and knots. Top of page Windspeed classification To ease the understanding of the m/s measurement, the following table can be used. Windspeed IN m/s Description <5 Very slow wind 5-10 Rather slow wind 10-20 Considerable wind, may lead to difficulties 20-30 Very windy, caution is advised >30 /weather/articles/nr/1283/

• 69. Markarfljót outwash plain and Öræfajökull

  currents. Because of the wide range of likely flow rheologies, three Manning's n values are assessed: 0.05, 0.1, and 0.15 s/m1/3. Results indicate that a large part of the lowland between the rivers Skaftafellsá and Breiðá (350 km2) is susceptible to flooding because of jökulhlaups descending the western and southern slopes of Öræfajökull. Characterised by average flow velocities in excess of 20 m/s /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 70. VI_2020_005

  (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf