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Results:

• 21. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 22. Lorenzoni_Pidgeon_2006

  : PidgeonN@cardiff.ac.uk Climatic Change (2006) 77: 73–95 DOI: 10.1007/s10584-006-9072-z c© Springer 2006 74 I. LORENZONI AND N. F. PIDGEON national policies strongly on fossil fuels. The British Prime Minister encapsulated these tensions when he recently stated that there is “no bigger long-term question facing the global community” than climate change (BBC, 2004), whilst emphasising the need /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 23. VI_2015_009

  vhm145 Vestari-Jökulsá D+J+L 844 751 11.3 924 1971–2014 vhm167 Austari-Jökulsá D+J 553 916 28.8 1208 1985–2014 8 vhm59 vhm64 vhm66 vhm102 vhm116 vhm162 vhm233 vhm235 vhm238 vhm144 vhm145 vhm167 Figure 1. Location of river basins. 9 l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l ll l l l l l 0 100 200 300 50 15 0 25 0 35 0 Days since Sept. 1st Q (m ³/s ) vhm59 S O N D J F M A M J /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 24. Kok_JGEC658_2009

  of how events unfold over time (Gallopı´n et al., 1997; Raskin et al., 2002). The key element in the context of this paper is that scenarios can be either qualitative (told in words) or quantitative (told in numbers). In that spirit, many of the recent (global) scenario exercises have been structured as what has become known as a Story-and- Simulation (Fig. 1) approach (Alcamo, 2001). Alcamo (2001 /media/loftslag/Kok_JGEC658_2009.pdf

• 25. 2010_005_

  afterwards, strong social interactions and converging prosperity worldwide, rapid development and spread of new technologies, and a balanced use of fossil and non-fossil energy sources. The monthly fields from the various general circulation model (GCM) runs are interpolated onto a common 2 2-degree grid within the domain from 10–28 W in longitude, and 62–68 N in latitude, covering Iceland as the only land /media/ces/2010_005_.pdf

• 26. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf

• 27. VI_2015_005

  is on the northern North Atlantic and the Nordic Seas. With the southern boundary at 47 N, the study domain covers Newfoundland, but excludes various marginal and inland seas with significant independent storm activity, such as the Mediterranean and Adriatic Seas, as well as the Black and Caspian Seas. The northern boundary at 80 N takes the domain up to Fram Strait, including Svalbard, but excluding /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 28. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf

• 29. 2013_001_Nawri_et_al

  /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 30. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf