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Results:

• 31. 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

• 32. BIVM_windrose_2005-2014

  N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 114 8 128 7 84 9 36 1 26 0 13 9 24 3 65 4 136 4 250 3 366 4 298 8 189 6 146 9 99 9 160 6 111 5 83 5 86 1 86 4 80 0 82 6 92 4 96 3 97 5 124 9 109 5 127 7 122 4 115 3 88 0 61 9 52 3 55 3 96 0 109 9 Wind rose BIVM January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 /media/vedur/BIVM_windrose_2005-2014.pdf

• 33. 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

• 34. VI_2009_012

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 35. ces-oslo2010_proceedings

  ................................................................................................................................... 88 Melvold, K. and Laumann, T. A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate scenarios (CES) ..................................................................................................................................................... 90 Thorsteinsson, Th., Sigurðsson, O. and Einarsson, B. Monitoring changes /media/ces/ces-oslo2010_proceedings.pdf

• 36. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 37. raisanen_ruosteenoja_CES_D2.2

  /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 38. VI_2009_006_tt

  the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s 1 while /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 39. Journal_of_Hydrology_Veijalainen_etal

  /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 40. VI_2009_013

  kinematics in south Iceland: Deformation from Global Positioning System measurements, 1986–1992. J. Geophys. Res., 100, 6235–6248. Slunga, R., S. T. Rögnvaldsson and R. Bödvarsson (1995). Absolute and relative locations of similar events with application to microearthquakes in southern Iceland. Geophys. J. Int., 123, 409–419. Stefánsson R., R. Böðvarsson, R. Slunga, P. Einarsson, S /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf