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• 41. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera

• 42. ice-chart_colour-code-standard

  less than 10/10 9+ 10/10 10 Undetermined or unknown x Concentration (C) C – Total concentration of ice in the area, reported in tenths (see symbols in table 3.1). Note: Ranges of concentration may be reported. Ca Cb Cc – Partial concentrations of thickest (Ca), second thickest (Cb) and third thickest (Cc) ice, in tenths. Note: Less than 1/10 is not reported. 10/10 of one stage of development /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 43. Ash measurements

  the quality of the data. Therefore, a mobile X-band weather radar was purchased, but while this custom made radar was being assembled and tested, another was obtained on loan from the Italian Civil Protection Agency. The mobile radar is now situated near the town of Kirkjubæjarklaustur, 80 km from the eruption site in Grímsvötn. IMO staff members monitor the progress of the eruption using /about-imo/news/nr/2183/

• 44. Eyjaf_status_2010-05-04_IES_IMO

  of the lava stream. Radar images from ICG-flight today show tunnels in Gígjökull increasing in size and continuing the build up of the cone at the crater. The size of the eruptive crater is 280 x 190 m. Lava splashes are thrown at least a few hundred meters into the air. Seismic tremor: Tremor levels decreased last night (3 May) and have decreased even further this morning at around 11:00 GMT /media/jar/Eyjaf_status_2010-05-04_IES_IMO.pdf

• 45. Gode_Jenny_CES_2010

  Projects involving sh Concise info Executive summaries Downloadable "Stakeholder friendly" info Stakeholder Relevance of the CES Project Jenny Gode, 31 May 2010 Research programme "Translators" F act sheets W eb page Stee ring co m m ittee Visits W o rkshops R efe re nce g ro up s E x . su m m a rie s M eetings Stakeholders Energy companies Energy authorities Decision makers Other stakeholders /media/ces/Gode_Jenny_CES_2010.pdf

• 46. VI_2014_001

  - Instantaneous Index flood models for Region 2.......................... 44 Appendix IX - Comparison between reference and estimated instantaneous index floods for Region 1........................................................................................ 45 Appendix X - Comparison between reference and estimated instantaneous index floods for Region 2 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 47. VI_2013_008

  Iceland. MSLP was extracted twice daily from ERA-40 (Uppala et al., 2005) for the period 1958–2001 and available ECMWF analysis from 2002 to 2006, on a 1 X 1 latitude-longitude grid. As daily precipitation, temperature and derived variables were averaged from 00 to 00UTC, only the 12UTC MSLP data were used so as to be centered on the same 24-h period. 4 Method implementation Below, details /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 48. raisanen_ruosteenoja_CES_D2.2

  as the forecast period. On the other hand, the probability distributions derived using the resampling ensemble method are in most cases wider than those produced with the normal distribution method, particularly so for precipitation change. This difference stems from the different treatment of natural variability: x In the normal distribution method, all simulations available for the same emission /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 49. VED_AnnualReport-2013_screen

  (), –; doi ./AoGA. Viggó Þór Marteinsson, Árni Rúnarsson, Andri Stefánsson, Þorsteinn Þorsteinsson, Tómas Jóhannesson, Sveinn H. Magnússon, Eyjólfur Reynisson, Bergur Einarsson, N. Wade, H. G. Morrison & E. Gaidos (). Microbial communities in the subglacial waters of the Vatnajökull ice cap, Iceland. The ISME Journal , –; doi:./ismej... Þorsteinn Þorsteinsson /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 50. 2010_003rs

  ...................................................................................................................... 63 x 5 Conclusions .................................................................................................................... 67 References ........................................................................................................................... 69 APPENDIX A –List of fault parameters /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf