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Results:

• 71. VI_2017_009

  .................................................................................................................... 10 3 Which domain, resolution, and models of the CORDEX project should be selected for the analysis of 21st century climate change in Iceland? .............................................. 11 3.1 EURO domain versus Arctic domain ................................................................. 11 3.2 EURO-44 domain versus EURO-11 domain /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 72. BIHN_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 68 0 62 9 111 2 167 0 117 5 70 6 26 7 25 4 58 7 47 3 36 6 101 3 91 1 53 1 117 0 73 6 44 2 72 7 38 7 60 4 113 6 70 0 109 3 130 5 26 1 12 5 30 0 14 4 10 5 34 6 17 0 29 4 114 3 158 0 146 5 172 7 Wind rose BIHN January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIHN_windrose_2005-2014.pdf

• 73. BITN_windrose_2005-2014

  1 7 1 7 15 22 22 10 2 2 31 52 44 26 21 19 11 9 11 7 17 18 12 12 18 12 7 28 Wind rose BITN December 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 7 8 9 Frequency of wind direction (%) Aerodrome Total observations: 891 Calm: 4.2% Variable winds: 4.6% Average wind speed for wind direction /media/vedur/BITN_windrose_2005-2014.pdf

• 74. BIVO_windrose_2005-2014

  S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 26 8 27 9 44 9 36 0 111 1 173 2 39 3 24 9 20 7 9 0 2 9 4 7 1 0 1 4 3 3 1 6 2 6 3 5 6 8 10 1 27 3 39 0 86 7 209 6 71 4 25 7 21 5 8 2 5 4 9 4 2 9 7 7 11 8 7 1 16 0 21 5 Wind rose BIVO January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIVO_windrose_2005-2014.pdf

• 75. Hydropower, Hydrology

  Rosberg, J., Suomalainen, M., Vehviläinen, B. and Veijalainen, N. (2007). Impacts of climate change on hydrological processes in the Nordic region. In: Proceedings of the third International Conference on Climate and Water, 3-6 September, Helsinki, Finland, pp 44-50. Beldring, S., Andréasson, J., Bergström, S., Graham, L.P., Jónsdóttir, J.F., Lappegard, G., Roald, L.A., Rogozova, S., Rosberg, J /ces/publications/nr/1938

• 76. 2005EO260001

  coincide with jökulhlaups. Monitoring Systems To monitor seismic and volcanic activity in Iceland, IMO operates a nationwide digital network of 44 seismic stations (network name: SIL) [Bödvarsson et al., 1999], six volumetric borehole strain meters, and 16 continuous GPS stations (network name: ISGPS) (H. Geirs- son et al., Current plate movements across the Mid-Atlantic Ridge determined /media/jar/myndsafn/2005EO260001.pdf

• 77. Bárðarbunga 2014 - November events

  September and has given important information about the subsidence: over 20 m since then. Based on other earlier data, the total subsidence is at least 44 m since the onset of these events. 8 November 2014 12:00 - from geoscientist on duty Yesterday, an M5.4 occurred at the norteastern rim of the caldera and this is the first earthquake over 5 in magnitude since 2nd November. The number of earthquakes /earthquakes-and-volcanism/articles/nr/3023

• 78. Bardarbunga-2014_November-events

  in the centre of the Bárðarbunga caldera (see Subsidence in the header). It is likely that the antenna is covered in snow. This equipment was mounted on 11 September and has given important information about the subsidence: over 20 m since then. Based on other earlier data, the total subsidence is at least 44 m since the onset of these events. 8 November 2014 12:00 - from geoscientist on duty /media/jar/Bardarbunga-2014_November-events.pdf

• 79. Bárðarbunga 2014 - November events

  September and has given important information about the subsidence: over 20 m since then. Based on other earlier data, the total subsidence is at least 44 m since the onset of these events. 8 November 2014 12:00 - from geoscientist on duty Yesterday, an M5.4 occurred at the norteastern rim of the caldera and this is the first earthquake over 5 in magnitude since 2nd November. The number of earthquakes /earthquakes-and-volcanism/articles/nr/3023/

• 80. 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