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Results:

• 31. 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

• 32. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 33. Hare-2011-ParticipatoryModelling

  25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Fr am ew o rk Cr ite ria u se d M ain pu rp o se o fframewor k Participator y m od ell in g purpos e Particip ator y structur e Contro lo f
  ow of in for m a tio n betwee n stakeholder s Timin g of event s Participatio n mod e Mo de l typ e Participator y m et ho ds use d Actor sinvolve d (at eac h /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 34. vanRoosmalen_etal-2009-WRR_2007WR006760

  to the description of the geological settings in the model, such that groundwater flow can be described at high spatial resolution (horizontal discretization is 500 m and vertically 16 model layers are used). The DK model was developed for water resources assessment and planning and as 99% of the water supply in Denmark is based on groundwater, it is important that this model accurately describes /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 35. VI_2009_013

  striking westwards and a group of N-S-striking pressure axis dipping 45 degrees from the horizontal and more, suggesting that extensional forces play a large role. Figure 9 includes the mechanisms of 82 out of the 99 earthquakes in total located between 17 and 26 km depth and thus shows nearly the same results as described earlier for that interval, that the tension axis is chiefly horizontal /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 36. VI_2015_006

  - cast (with a cloud cover of at least 99%). As shown in Section 3, high-level clouds have a very limited impact on the surface radiation budget, and are therefore excluded. At each grid point, the total cloud cover is then determined as either the low- or mid-level cloud cover, depending on which is greater. In addition to cloud conditions, over land (excluding inland waterbodies), a distinction /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 37. BIVM_windrose_2005-2014

  N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 114 8 128 7 84 9 36 1 26 0 13 9 24 3 65 4 136 4 250 3 366 4 298 8 189 6 146 9 99 9 160 6 111 5 83 5 86 1 86 4 80 0 82 6 92 4 96 3 97 5 124 9 109 5 127 7 122 4 115 3 88 0 61 9 52 3 55 3 96 0 109 9 Wind rose BIVM January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 /media/vedur/BIVM_windrose_2005-2014.pdf

• 38. VI_2019_009

  /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 39. Journal_of_Hydrology_Veijalainen_etal

  /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 40. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf