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• 21. The weather in Iceland in 2021

  station total mm 1991-2020% 2011-2020 % max 24-hr mm prec.days >=1.0 mm Reykjavík 765.3 87 82 18.6 232 150 Stykkishólmur 675.7 92 88 29.9 211 124 Hólar í Dýrafirði 1237.3 # 105 112 235 132 Litla-Ávík 836.2 # 92 45.7 225 145 Skeiðsfoss 915.6 94 /about-imo/news/the-weather-in-iceland-in-2021

• 22. BIGJ_windrose_2005-2014

  direction (%) Aerodrome Total observations: 88 Calm: 1.1% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 20 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 5 5 4 7 13 7 5 1 1 1 1 2 2 4 2 2 4 7 1 2 1 8 2 Wind rose BIGJ June /media/vedur/BIGJ_windrose_2005-2014.pdf

• 23. Paper-Olafur-Rognvaldsson_91

  and Thorsteinsson (personal communication). red dots, cf. Fig. 2), the SE-part (HSA, green dots, cf. Fig. 2) and the SW-part (HSV, blue dots, cf. Fig. 2). The solid line in Figure 2 shows the average of the observed winter precipitation, corrected to take liquid precipitation and/or win- ter ablation into account, at altitudes between 1450 and 1650 metres at locations HN, HSA and HSV. The dashed line represents /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 24. Paper-Olafur-Rognvaldsson_92

  in reasonable agreement. This is partly due to a compensation of the errors on a shorter timescale (days). Probability of false alarms (model predicts precipitation, but none is observed) is highest in N-Iceland, particularly during win- ter. The probability of missing precipitation events (precipitation ob- served but none is predicted by the model) is highest in the summer inland in N-Iceland. Secondly /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 25. 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

• 26. 2010_016

  Mean monthly temperature for Sandá í Þistilfirði (vhm 26), 1961–2005. Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Win Sum Year Mean MM5 [C°] -3.2 -3.1 -3.2 -1.6 1.8 5.8 8 7.5 4.3 1.2 -1.7 -3.1 -3.1 7.1 1.1 Mean obs. [C°] -4.3 -4.1 -3.8 -1.6 1.8 5.4 7.4 7.1 3.9 0.5 -2.5 -4.1 -4.1 6.6 0.5 Difference 1.1 1.0 0.6 0.0 0.0 0.4 0.6 0.4 0.4 0.7 0.8 1.0 1.0 0.5 0.6 Figure 3 /media/ces/2010_016.pdf

• 27. 2010_017

  ith a broke ere correc a arose wh peratures ures were a le 4 and Fi Jökulsá wat most prono lace in war vation grad ause the ad hold. Adde uch less pr 1–2005. Win Sum -3.1 7.1 -4.1 6.6 1.0 0.5 ndá í Þist n red curv ted to fit th en calibrat to the inter lso system gure 6. ershed (see unced for t m events a ient for th dition of a d unrealis onounced t Year 1.1 0.5 0.6 ilfirði e /media/ces/2010_017.pdf

• 28. NONAM_1st_workshop_summary_v3

  organization. The group went on discussing a next step: 2. Create common vision. The group here found that this would require a merging of the two loops, the regular cycle with the learning cycle. Task could be: (i) call everybody in and let them explore their visions about the area; playground, (ii) identify basic points of views and representatives, (iii) discover different win-win solutions /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 29. VI_2020_008

  /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 30. BIKF_windrose_2005-2014

  45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 33 2 55 2 79 5 88 3 64 2 42 2 49 4 59 5 52 5 38 3 42 1 40 4 41 0 55 3 63 5 55 6 47 5 39 3 34 6 31 3 33 9 33 9 36 6 48 8 53 9 52 6 47 5 33 6 22 3 19 0 16 4 13 0 9 6 11 6 12 0 15 4 Wind rose BIKF April 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIKF_windrose_2005-2014.pdf