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Results:

• 41. VI_Arsskyrsla_2018_vef

  ÁRSSKÝRSL A 2018 2 Á R S S K Ý R S L A 2 0 1 8 3 Frá forstjóra 4 Veðurstofan 2009–2019 12 Náttúrufar 18 Rannsóknir 20 Fjármál og rekstur 22 Ritaskrá starfsmanna ?Veðurstofa Íslands 2019 Bústaðavegi 7–9, 108 Reykjavík ISSN 2251-5607 Efni ársskýrslunnar var unnið af starfsmönnum Veðurstofu Íslands Ritstjórn: Sigurlaug Gunnlaugsdóttir Hönnun og umbrot: Hvíta húsið Prentun: Prentmet /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 42. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  Public Choice (2010) 143: 293–301 DOI 10.1007/s11127-010-9626-5 Foundations of the Ostrom workshop: institutional analysis, polycentricity, and self-governance of the commons Michael D. McGinnis · James M. Walker Received: 25 January 2010 / Accepted: 22 February 2010 / Published online: 8 April 2010 ³ Springer Science+Business Media, LLC 2010 Abstract This paper highlights important lessons /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 43. Observations - Holtavörðuheiði

  Observations - Holtavörðuheiði | Observations | Icelandic Meteorological office Observations - Holtavörðuheiði Mon 1.05 13 GMT -0.3° NNE 7 Max wind : 7 / 10Road temp. : 1.4° 12 GMT -1.8° NNE 7 Max wind : 7 / 10Road temp. : 0.3° 11 GMT -2.3° NNE 7 Max wind : 8 / 10Road temp. : 0.1° 10 GMT -2.8° NNE /m/observations/areas

• 44. 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

• 45. 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

• 46. 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

• 47. Risk Assessments

  riskianalyysit - ilmaston muutoksen synnyttämät riskit ja mahdollisuudet. 12.03.2009, Research Report VTT-R-01942-09, Tampere. 13 p. + app. 24 p. Linnerud, Kristin (2009) Test and evaluation of a climate risk assessment procedure. Case study: The Norwegian hydro power company SFE. CICERO, University of Oslo. Report 2009:3. Feb.2009. 44 p. ISSN:0804-4562. Linnerud, Kristin (2009) Climate change /ces/publications/nr/1941

• 48. 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

• 49. 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

• 50. 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