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Results:

• 61. ces-glacier-scaling-memo2009-01

  and ice caps may be derived from data about the area distribution of ice bodies in the drainage basin. Since the exponents g in the volume–area scalings v = csg for both ice caps and glaciers TóJ 3 5.12.2009 Memo Area (km2) Volume (km 3 ) 50 100 50 100 150 200 250 50 100 150 200 250 a71 a71a71 a71 a71 10 50 500 500020 1000 1 5 10 0 100 0 2 2 0 20 0 200 0 100 10000 Icelandic ice /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 62. VI_2013_006

  lightning strikes can be over 10 km in length and are sometimes tilted and to the side of the volcanic column must be taken into account. This adds to the lightning location uncertainty, which is often a few km. Furthermore, the volcanic column may be swayed downwind, e.g. see Figure 1. Therefore, location of a single lightning can be misleading but by calculating average location of many /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 63. ces_flyer_glacierssnowandice

   shown for the year 1990. Note that the figure  shows only the southern part of the Vatnajökull ice cap,  south of the main east–west ice divide. Future  climate  change  is  likely  to  have  pronounced  effects on glaciers, glacial  rivers and  hydro‐resources  of Iceland. Icelandic glaciers store a total of 3600 km3 of  ice  and  are  retreating  and  thinning  rapidly  at  present.  Figure 1 /media/ces/ces_flyer_glacierssnowandice.pdf

• 64. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  1 Citation: Polar Research 2011, 30, 7282, DOI: 10.3402/polar.v30i0.7282 et al. 2004; Pa´lsson et al. 2007; Bjo¨rnsson & Pa´lsson 2008; Gudmundsson et al. 2009). This is consistent with the warming in Iceland that has taken place since 1994 (e.g., Bjo¨rnsson et al. 2005; Jo´hannesson et al. 2007). Model- ling studies have shown that these large ice caps could lose most of their mass within 200 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 65. Minor jökulhlaup in Grímsvötn

  Gígjukvísl on road no. 1. The pictures show an increase in discharge from 10th to 13th of October. The map shows approximately the floods pathway underneath the glacier. It is assumed that the maximum discharge in Gígjukvísl river will be lower than the maximum discharge from Grímsvötn because it will be affected by the lagoons in front Skeiðarárjökull glacier. The flood pathway outside the glacier /about-imo/news/minor-jokulhlaup-in-grimsvotn

• 66. Supercomputer in Iceland

  place 28th April 2016, see photo galleries (1-5). Expand the webpage (five plus signs) to see relevant photos. After the reception (1), the chambers were explored (2). Then lectures (3) were given in English (recording available) and finally a celebration took place (4). Then a reception was given at the Danish Embassy (5). At the Danish Embassy, from left to right: Acting Dir. General of IMO /about-imo/news/nr/3309

• 67. VI_2009_002rs

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_002rs.pdf

• 68. GA_2009_91A_4_Andreassen

  to highly negative summer balances, but also lower bw than the average for 1949–2006. Calculated change in specific mass balance for a ±1°C change in air tem- perature was ±0.55 m w.e., whereas a ±10 % in- crease in precipitation represented a change of ± 0.20 m w.e. Model results further indicated that for a 2°C warming, the ablation season will be extend- ed by c. 30 days and that the period /media/ces/GA_2009_91A_4_Andreassen.pdf

• 69. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  and provide a narrative approach for tool enhancement. r 2007 Elsevier Ltd. All rights reserved. Keywords: Groundwater management; Bayesian belief networks; Qualitative interview; Adaptive management; IWRM; Tool enhancement; Participatory integrated assessment; Social learning; Newater; Organizational complexity 1. Introduction and indexes are available e.g. poverty index, water stress index etc /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 70. The weather in Iceland 2009

  stations and ranking (1 = warmest, 3 = third warmest etc.). station temperature anomaly rank of Reykjavík (SW) 5.55 1.24 10 139 Stykkishólmur (W) 4.70 1.22 14 165 Bolungarvík (NW) 3.87 0.93 20 113 Grímsey (N) 3.69 1.25 10 136 Akureyri (N) 4.06 0.77 31 129 Grímsstaðir (NE) 1.62 1.12 20 103 Egilsstaðir (E) 3.92 0.98 17 60 Dalatangi (E /weather/articles/nr/1802