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• 41. VI_2022_006_extreme

  ............................................................................ 43 APPENDIX II. TEMPORAL CHANGES IN SNOW-FRACTION ........................................ 49 APPENDIX III. PRECIPITATION RETURN LEVELS .......................................................... 66 4 1 Introduction In Iceland, periods of intense rainfall have caused localised damage on numerous occasions. Recent examples include /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 42. The weather in Iceland in 2018

  # 14 28 -0,2 Hveravellir 0,1 1,2 14 54 -0,2 Eyrarbakki 5,0 0,9 28 126 -0,2 Keflavíkurflugvöllur 4,9 0,5 29 til 31 66 -0,5 The annual mean was highest in Surtsey, off the Southern coast, 6.3°C, but lowest -1.7°C at the glacial station Brúarjökull in the Central Highlands. The lowest annual temperature /about-imo/news/the-weather-in-iceland-in-2018

• 43. The weather in Iceland in 2020

  66 -0.2 Dalatangi 4.8 1.3 10 to 11 83 0.0 Teigarhorn 4.8 1.1 18 to 20 148 -0.1 Höfn í Hornaf. 5.3 # -0.2 Fagurhólsmýri 5.3 0.7 34 118 -0.4 Vatnsskarðshólar 5.8 0.7 26 81 -0.2 Stórhöfði 5.4 0.5 41 to 42 144 -0.3 Árnes 4.2 0.6 41 /about-imo/news/the-weather-in-iceland-in-2020

• 44. Tornado_Impacts_-_FMI_Presentation

  tornadoes rated F4 or F5 • 1,288 killer tornadoes, 4,860 fatalities • 6,574 injury tornadoes, 82,062 injuries • Most tornadoes aren’t killers: 228 tornadoes had 5+ fatalities (.045% of tornadoes), account for 66% of fatalities Casualties and F-scale Tornadoes by F-Scale 30.00% 40.00% 50.00% 0.00% 10.00% 20.00% 0 1 2 3 4 5 F-Scale Category Casualties and F-scale Fatalities by F-Scale 30.00 /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf

• 45. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  %) 14 (26%) 39 (74%) Gender Number (%) E I S N T F P J Male 100 (48%) 47 (47%) 53 (53%) 15 (15%) 85 (85%) 59 (59%) 41 (41%) 29 (29%) 71 (71%) Female 109 (52%) 66 (61%) 43 (39%) 22 (20%) 87 (80%) 43 (39%) 66 (61%) 21 (19%) 88 (81%) Climatic Change (2012) 112:233–242 237 symposia participants were not significantly different from the preferences of the U.S. general population, which was 49 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 46. VI_2020_008

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

• 47. BIHU_windrose_2005-2014

  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 11 47 3 9 6 1 7 1 10 13 10 10 66 4 14 18 2 1 1 1 6 5 24 3 Wind rose BIHU March 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 /media/vedur/BIHU_windrose_2005-2014.pdf

• 48. 2005EO260001

  ), Weather radar observa- tions of the Hekla 2000 eruption cloud, Iceland, Bull. Volcanol., 66, 457-473. Sturkell, E., P. Einarsson, F. Sigmundsson, H. Geirsson, H. Ólafsson, R. Pedersen, E. de Zeeuw-van Dalfsen, A. T. Linde, S. Sacks, and R. Stefánsson (2005), Vol- cano geodesy and magma dynamics in Iceland, J. Volcanol. Geotherm. Res., in press. Slunga, R., S. T. Rögnvaldsson, and R. Bödvarsson /media/jar/myndsafn/2005EO260001.pdf

• 49. Paper-Olafur-Rognvaldsson_92

  performance of the model. REFERENCES Førland, E. J., Allerup P., Dahlström B., Elomaa E., Jónsson T., Madsen H., Perälä J., Rissanen P., Vedin H. and Vejen F. 1996. Manual for operational cor- rection of Nordic precipitation data. DNMI Report No. 24/96 Klima, 66 pp. Benoit, R., Pellerin P., Kouwen N., Ritchie H., Donaldson N., Joe P. and Soulis E. D. 2000. Toward the use of coupled atmospheric /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 50. VI_2015_006

  radiation, the net downward shortwave radiation flux at the surface varies between a minimum of 14% over snow-covered land with overcast conditions, and a maximum of 66% over the ocean with clear-sky conditions. This incoming radiation at the Earth’s surface is then converted to other forms of energy, with a distribution in percent of the net solar radiation flux, which again de- pends /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf