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• 11. Sigurður Th. Rögnvaldsson

  and beyond year 2000. Phys. Earth Planet. Inter. 113, 89 101. Roberts, R. G., A. Lindfors, A. Christoffersson, Reynir Böðvarsson og Sigurður Th. Rögnvaldsson 1993. Three-component data as an aid to seismic event detection and asociation: A case study using data from the SIL (Iceland) network. Computers and Geosciences 19, pp. 123 134. Slunga, R., Sigurður Th. Rögnvaldsson og Reynir Böðvarsson /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/

• 12. Sigurður Th. Rögnvaldsson

  and beyond year 2000. Phys. Earth Planet. Inter. 113, 89 101. Roberts, R. G., A. Lindfors, A. Christoffersson, Reynir Böðvarsson og Sigurður Th. Rögnvaldsson 1993. Three-component data as an aid to seismic event detection and asociation: A case study using data from the SIL (Iceland) network. Computers and Geosciences 19, pp. 123 134. Slunga, R., Sigurður Th. Rögnvaldsson og Reynir Böðvarsson /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur

• 13. VI_2009_013

  ). The brittle-plastic transition and depth of seismic faulting, Geol. Rundsch., 77, 319–328. Scholz, C. H. (2002). The Mechanics of Earthquakes and Faulting, 2nd ed., Cambridge Univ., Cambridge. Sibson, R. H. (1984). Roughness at the Base of the Seismogenic Zone: Contributing Factors.J. Geophys. Res., 89, B7, 5791–5799. Sigmundsson, F., P. Einarsson, R. Bilham, and E. Sturkell (1995). Rift-transform /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 14. Kok_et_al._TFSC_published_2011

  /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 15. VI_2009_006_tt

  the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s 1 while /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 16. Wind turbines

  and each spade measures 22 metres in length. When the spades are at their highest position each unit will achieve a height of 77 metres. Like all large structures, wind turbines have an inevitable visual impact. However, a permanent impact on the overall appearance of the environment is not considered high in comparison to other types of power plants. Wind turbines can be easily dismantled, leaving /about-imo/news/nr/2642

• 17. The weather in Iceland in 2020

  location temp °C dev 1961-1990 rank total Dev 2010-2019 Reykjavík 5.1 0.7 33 150 -0.4 Hvanneyri 4.3 # 16 23 -0.4 Bláfeldur 4.7 # 16 23 -0.5 Stykkishólmur 4.5 1.0 26 to 27 175 -0.4 Bolungarvík 3.8 0.9 32 123 -0.4 Litla-Ávík 3.9 /about-imo/news/the-weather-in-iceland-in-2020

• 18. 2010_012rs

  Int., 123, 409-419. 20 Stefánsson, R., Gudmundsson, G. B., Halldórsson, P. (2000). The two large earthquakes in the South Iceland seismic zone on June 17 and 21, 2000. Icelandic Meteorological Office report, VÍ-G00010-JA04. Vogfjörd, K. S., Pétursson, G. G., Kjartansson, E., Slunga, R., Ágústsson, K., Hjaltadóttir, S., Gudmundsson, G. B., Roberts, M. J., Geirsson, H. & Ármannsdóttir, S /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 19. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13
  6
  4
  1 6 39 79 84 97 A2 145 132 73 10
  10
  7
  6
  8 4 75 92 123 B2 137 119 75 16
  6
  6
  6
  5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 20. VI_2015_005

  with l l2, containing the region with frequent cyclone activity to the northeast of Iceland. Then, of the total study area, 22% fall into the western sector (itself broken up into 70% ocean and 30% land), 32% in the central sector (77% ocean, 23% land), and 46% in the eastern sector (44% ocean, 56% land). The average seasonal cyclone occurrences over the ocean and land areas in different sectors /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf