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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. VI_2022_006_extreme

    77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
  • 13. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

    can be found in Huntjens et al. (2007), Chapter 4 of NeWater Deliverable 1.7.9a (http://www.newater.info). Climate change adaptation in European river basins 265 123 interactions, by private and public actors, to achieve adaptation and to enhance the capacity of processes, institutional arrangements and actors to adapt to future environmental changes (Huitema et al. 2009). Adaptive governance /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
  • 14. 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
  • 15. Mo_Birger_CES_2010

    Simulation results Hydropower Thermal production Energy balance CO2-emissions 4 Summary and concluding remarks Sintef Energy Research Quantitative system analysis 8 of 21 Introduction Electricity system model Simulation results Summary and concluding remarks Hydropower Thermal production Energy balance CO2-emissions Annual average in ow over the year, GWh 0 14 28 42 52 0 500 1;000 1;500 2;000 2;500 /media/ces/Mo_Birger_CES_2010.pdf
  • 16. The weather in Iceland in 2020

    to the 10-year average. It was relatively warmer in coastal areas but colder in the inland.JuneJune was warm and favorable. It was relatively warmest in the Northeast but cooler in the southwestern part. Wind and precipitation were close to average.July July was rather cold compared to recent years, although the mean was above the 1961 to 1990 average. Yet the weather was not unfavorable /about-imo/news/the-weather-in-iceland-in-2020
  • 17. 2010_012rs

    ) closest stations, respectively. The 40 highest correlating events are then inverted for the best location. For comparison the manual locations, obtained by an analyst are shown in yellow. The final locations of the events are all within an approximately 1 km2 area, even though their original, automatic locations are up to 5 km away. They are also within a few hundred meters from the manual /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
  • 18. News

    are aligned above the eastern rim of the Katla caldera, which lurks underneath the ice-cap. In the center of the caldera, the ice is over 500 m thick. Melt water from the surface of the glacier has collected in the bowl, giving the blue colour, but that is irrelevant to the activity discussed in this article /about-imo/news/bigimg/3369
  • 19. Cradden_Lucy_CES_2010

    superimpose both heating and cooling effects, i.e., – wind = cooling – temperature, solar radiation = heating June 2010 5 • Limit to how much heat the wire can be exposed to • Amount of allowable current based on ambient conditions is known as ‘rating’ Network capacity (ampacity) Too much heat causes ‘sag’ where minimum ground clearance is not achieved June 2010 6 How are ratings determined /media/ces/Cradden_Lucy_CES_2010.pdf
  • 20. The weather in Iceland 2014

    prec.days >=1.0 mm Reykjavík 963.1 121 112 37.6 223 160 Stafholtsey 829.4 97 28.0 182 144 Bláfeldur 1460.7 97 32.0 272 195 Stykkishólmur 678.8 96 87 20.0 218 136 Litla-Ávík 835.0 96 34.1 267 164 Bergstaðir 458.2 98 22.6 177 92 Sauðanesviti 1017.5 115 28.2 239 158 Akureyri 743.7 152 133 23.0 225 133 Grímsstaðir 514.8 /about-imo/news/nr/3082

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