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  • 31. VI_2019_009

    - 26,83,84 - 27,87 - 70,71 - 72,73 - 74. ............................ 28 21 From left to right, the horizontal axis has the following SYNOP codes (manual station): The first is 10, the second is 11 & 41, the third is 40 and to the right is 46. 29 22 Number of records as a function of height of the 1st cloud layer from the manual and automatic stations /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 32. BIIS_windrose_2005-2014

    of observations for wind direction) Icelandic Met Office 02. júl. 2015 2 6 3 2 14 2 23 3 46 0 72 5 34 3 10 8 2 5 5 4 3 5 1 2 5 1 6 2 6 2 5 5 3 11 8 10 6 6 2 3 5 2 7 1 2 1 3 3 1 1 6 6 Wind rose BIIS July 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 5 10 /media/vedur/BIIS_windrose_2005-2014.pdf
  • 33. Sigurður Th. Rögnvaldsson

    Conference on Preparedness and Mitigation for Natural Disasters '92, 28 29 Maí, Reykjavík. Reynir Böðvarsson, Sigurður Th. Rögnvaldsson, Steinunn S. Jakobsdóttir, R. Slunga og Ragnar Stefánsson 1996. The SIL data acquisition and monitoring system. Seism. Res. Lett. 67, 35 46. Reynir Böðvarsson, Sigurður Th. Rögnvaldsson, R. Slunga og Einar Kjartansson 1999. The SIL data acquisition system - at present /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/
  • 34. Sigurður Th. Rögnvaldsson

    Conference on Preparedness and Mitigation for Natural Disasters '92, 28 29 Maí, Reykjavík. Reynir Böðvarsson, Sigurður Th. Rögnvaldsson, Steinunn S. Jakobsdóttir, R. Slunga og Ragnar Stefánsson 1996. The SIL data acquisition and monitoring system. Seism. Res. Lett. 67, 35 46. Reynir Böðvarsson, Sigurður Th. Rögnvaldsson, R. Slunga og Einar Kjartansson 1999. The SIL data acquisition system - at present /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur
  • 35. Group2-report

    1    Adaptive management to climate change in Horsens Fjord using scenario  development    Report by Maria, Azhar, Bjarke and Kerstin  Introduction  Horsens Fjord is an eutrophic estuary situated in east coast of Jutland, Denmark with approximately 46 km2  surface area. The Fjord is a part of bigger WFD catchments area with dominated agriculture area and small  forest, wetlands, lakes, and urban /media/loftslag/Group2-report.pdf
  • 36. Bárðarbunga 2015 - January events

  • 37. Bárðarbunga 2015 - January events

  • 38. Bardarbunga-2015_January-events

  • 39. VI_2009_012

    Appendix – near-field constraint ........................................................................................ 35  III Appendix – PGV and PGA versus distance for all events ................................................. 36  List of figures Figure 1. Map of SW Iceland showing the epicenters of 46 earthquakes used in the study.. 10  Figure 2. CMT-moment magnitude estimates vs /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 40. VI_2022_006_extreme

    towards the northern part of Vatnajökull. Table 8 – Median 1M5 values (mm 24-h-1) for eleven hydropower catchments with and without climate projections for the period 2080 – 2100. Catchment 1M5 median value mm 24-h-1 Original RCP 2.6 RCP 8.5 10% 50% 90% 10% 50% 90% Blönduvirkjun 48 41 49 58 42 50 61 Búðarháls 46 40 47 56 40 48 59 Hágöngulón 63 55 65 76 55 66 81 Hálslón 85 75 88 104 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

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