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Results:

• 41. IMO_AnnualReport2014

  in Askja 8 Projects 9 The weather in Iceland 2014 10 Finance 11 Sta?publications I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 3 One of the main goals of the merger of the Hydrological Service, HS, and the Icelandic Meteorological Office, IMO, was to improve the capabilities regarding monitoring, warnings and emergency response due to natural hazards. Prior /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 42. 2005EO260001

  bursts of seismic tremor (1–3 Hz), and later becoming periodic with energy between 2 and 8 Hz. After 18 October, seismicity increased to three events per day (Figure 2b). Synchronous with this increase, the ISGPS station SKRO (Figure 1b) moved 9 mm westward over the following eight days, and returned to its original position on 1 November (Figure 2c), suggesting subsurface magma movement /media/jar/myndsafn/2005EO260001.pdf

• 43. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 44. Program

  An overview of past and future surveys of Iceland conducted by the NERC ARSF Eric Lutz, Bob Hawley, Michelle Hofton, John Sonntag, Kelly Brunt and Roseanne Dominguez, Department of Earth Sciences, Dartmouth College, USA. Validation of NASA laser altimeters at Summit, Greenland Finnur Pálsson, Eyjólfur Magnússon, Sverrir Guðmundsson, Helgi Björnsson, Hannes H. Haraldsson, and Tómas Jóhannesson /lidar/lidar-2013/program/

• 45. Refsgaard_etal-2007-Uncertainty-EMS

  be broader than stated? (7) Further elicit and specify the distribution (shape and percentiles or characterising parameters). (8) Verify with the expert that the distribution that you constructed from the expert’s re- sponses correctly represents the expert’s beliefs. (9) Decide whether or not to aggregate the distributions elicited from dif- ferent experts (this only makes sense if the experts /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 46. Bárðarbunga 2014 - August events

  activity is in the dyke and at similar depth as before (8-12km). One earthquake of M5 occurred at 08:13 AM by the northern rim of the Bardarbunga caldera. Two minutes earlier (08:11) another event of M3.9 occurred at a similar location. A few earthquakes were detected near Askja, the biggest one of M2.7. Dyngjujökull - flight today The edge Dyngjujökull by Holuhraun, view to the north. Note /earthquakes-and-volcanism/articles/nr/3000

• 47. Bardarbunga-2014_August-events

  18:14 - from geoscientist on duty Since midnight over 1100 earthquakes have been detected by the automatic system. The dyke does not appear to have migrated further north since noon. The main activity is in the dyke and at similar depth as before (8-12km). One earthquake of M5 occurred at 08:13 AM by the northern rim of the Bardarbunga caldera. Two minutes earlier (08:11) another event /media/jar/Bardarbunga-2014_August-events.pdf

• 48. Bárðarbunga 2014 - August events

  activity is in the dyke and at similar depth as before (8-12km). One earthquake of M5 occurred at 08:13 AM by the northern rim of the Bardarbunga caldera. Two minutes earlier (08:11) another event of M3.9 occurred at a similar location. A few earthquakes were detected near Askja, the biggest one of M2.7. Dyngjujökull - flight today The edge Dyngjujökull by Holuhraun, view to the north. Note /earthquakes-and-volcanism/articles/nr/3000/

• 49. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  regimes of Number of flood and drought disasters in the past decades per case study 0 2 4 6 8 10 12 1977-1986 1987-1996 1997-2006 Time period Total number of flood and drought disaster s Rivierenland Alentejo Upper Tisza - Hungary Upper Tisza - Ukraine Fig. 1 Number of reported flood and drought disasters in the past decades in Rivierenland, Alentejo, Hungarian part of Upper Tisza, and Ukrainian /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 50. Forecasts - Gufuskálar

  GMT 4° ENE 10 Cloud cover: 100% 20 GMT 3° ENE 10 Cloud cover: 100% 21 GMT 2° ENE 9 Cloud cover: 0% 22 GMT 2° ENE 8 Cloud cover: 0% 23 GMT 1° ENE 8 Cloud cover: 0% Tue 2.05 00 GMT 1° ENE 7 Cloud cover: 0% 01 GMT 1° ENE 8 Cloud cover: 0% 02 GMT 1° ENE 8 Cloud cover: 0% 03 GMT 1° ENE 8 Cloud cover: 0% 04 GMT 0° ENE 8 /m/forecasts/areas