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Results:

• 41. esa_flyer_new

  EA Analyse A/S and Optensys Energianalys will forecast energy system variables, while SINTEF Energy Research will make assumptions for the energy system in different cases, include new inputs in the EMPS model and carry out simulations. Cl i ma t e Sc e nar i os G ro u p R i s ø St o c h as t i c v a r i a b l e s Clima t e s c e n a r i o NV E S M H I FE I N o r w a y S w e d e n F inla n /media/ces/esa_flyer_new.pdf

• 42. Heavy rainfall and increased river discharge

  Warning against increased risk 25.9.2015 A low is approaching Iceland Saturday morning and high precipitation levels are forecast until early Sunday morning for much of S- and W-Iceland. Heavy rainfall is expected in the southeastern part of the country, leading /about-imo/news/nr/3197

• 43. Sea ice in March 2007

  was well within the median and closest to shore, about 50n.m. NW off Straumsnes and 60n.m. W off Barði. The ice-edge density was extensively 4/10 or less than 7-9/10 north off 67°20'N. A considerable diagenis was discovered in the southernmost part of the exploratory territory. No other dispatches were made during the month. Easterly and later northeasterly winds were common in the Greenland /sea-ice/monthly/2007/nr/2300

• 44. Sea ice in April 2011

  was seen just within the jurisdiction of Greenland. No large floes were seen on radar beyond the ice edge. No observations were received from ships but 3rd April one observation was received from land, reporting an ice berg in location 65°42' N 32°07'W. On the Greenland Straight easterlies were predominant but occasionally strong southwesterly wind prevailed for a few days /sea-ice/monthly/2011/nr/2375

• 45. ces_SA_group_flyer_new

  series analysis Regional series are compiled based on regions having similar climatological characteristics and streamflow regimes. These series are also useful for evaluating patterns and trends, both in time and by region. Regional series for precipitation, temperature and runoff are being compiled, updated and analysed within the CES project. - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 /media/ces/ces_SA_group_flyer_new.pdf

• 46. BIGJ_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 35 62 48 77 8 4 83 63 64 22 19 14 7 4 11 11 14 41 1 5 24 25 18 45 64 41 3 2 93 35 11 17 7 11 47 16 24 67 36 Wind rose BIGJ January 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 2 4 6 8 10 12 Frequency of wind /media/vedur/BIGJ_windrose_2005-2014.pdf

• 47. 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

• 48. 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

• 49. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 50. BIBD_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 36 2 69 4 138 2 187 3 151 2 106 7 83 1 58 1 36 0 20 3 17 6 14 5 14 9 11 0 10 6 13 0 16 7 29 8 55 2 73 0 95 6 140 7 98 9 41 9 20 2 17 7 8 1 6 4 4 8 3 7 5 7 4 4 4 5 7 3 9 2 18 5 Wind rose BIBD January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIBD_windrose_2005-2014.pdf