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  • 21. Bárðarbunga 2014 - August events

    line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm at Bárðarbunga on Saturday /earthquakes-and-volcanism/articles/nr/3000
  • 22. 2010_016

    –5 months per year depending on watershed. Mean yearly maximum snow thickness decreases by 0–80%. Winter flow is predicted to increase on average due to a higher number of melt events at relatively high and flat heath areas of the watersheds. For Sandá í Þistilfirði, vhm 26, the snowmelt generated spring/summer discharge peak largely disappears and the seasonal discharge becomes more evenly /media/ces/2010_016.pdf
  • 23. 2010_017

    of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf
  • 24. Bardarbunga-2014_August-events

    in 1991. The blue dashed line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm /media/jar/Bardarbunga-2014_August-events.pdf
  • 25. VI_2020_005

    ) and are Global Navigation Satellite System (GNSS) data providers (SONEL, n.d.). The North Sea is home to one of the most dense tide gauge networks in the world, with over 15 tide gauge series that span at least 100 years along its coastline (Quante and Colijn, 2016). In Denmark, 17 the national tide gauge network consists of 90 automatic stations run in cooperation of the Danish Meteorological /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 26. VI_2014_005

    and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 27. Bárðarbunga 2014 - August events

    line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm at Bárðarbunga on Saturday /earthquakes-and-volcanism/articles/nr/3000/
  • 28. NONAM_1st_workshop_summary_v3

    Summary of the break-out sessions on road infrastructure By Adriaan Perrels (FMI) 1. Introduction The break-out sessions, three in total, were interspersed between the various oral presentations on Thursday afternoon, Friday morning and Friday afternoon. Each session was 60 to 80 minutes. The participants had two assignments: 1. deliberate 7 questions on issues pertaining subsequent /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
  • 29. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    in the data used in making the decision and the factors are interlinked, all of which makes the problem highly complex. The part of the net defined by variables and links is relatively easily communicated to stakeholders (Henriksen et al., 2007b). However the tal Management 88 (2008) 1025–1036 quantitative part, with the conditional probability tables (CPTs), the numbers, is the step where /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 30. 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

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