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Results:

• 1. Benestad_Rasmus_CES_2010

  wind Obs=ERAINT (reanalysis) righttoleftmark Storm statistics Domain: 12°W-38°E/48-66°N (Same as RCM) Historical reanalysis ERAINT Little trend! Historical analysis: N CCI on small domain: restricted RCM domain Domain: 80°W-40°E/20- 75°N Different story! Geographical distribution? Storm statistics: Whole North Atlantic Homogeneous? Historical analysis: |v| Southern Norway SLP 'triangulation /media/ces/Benestad_Rasmus_CES_2010.pdf

• 2. VI_2017_009

  in the reference period was +4.9°C. When this value is inserted into the best fitting linear trends in Figure 7 it yields a temperature rise of +1.8°C for RCP4.5 and +3.1°C for RCP8.5 in the 21st century. Spatial and seasonal trends We expect the warming of the land to be greater than the warming of the ocean. Since the ocean covers more than 70% of the Iceland domain it is interesting to look /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 3. 2013_001_Nawri_et_al

  approximately centred around Iceland: the outer domain with 43 42 grid points spaced at 27 km (1134 1107 km), the intermediate domain with 95 90 grid points spaced at 9 km, and the inner domain with 196 148 grid points spaced at 3 km. The northwest corner of the outer domain covers a part of the southeast coastal region of Greenland. Otherwise, the only landmass included in the model domain /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 4. News

  News Public domain © Wikipedia Almyrkvi á sólu. / Total eclipse of the sun /about-imo/news/bigimg/1363

• 5. HARMONIE - numerical weather prediction model 

  convection-permitting NWP and is operated at 2.5 km horizontal resolution over a domain that covers Iceland and the surrounding seas. The development and maintainance of the model is a research cooperation of European meteorological institutes that was founded in 2005 when two research consortia joined forces. One of these consortium was the HIRLAM programme (High Resolution Limited Area /weather/articles/nr/3232

• 6. 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

• 7. 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

• 8. Paper-Olafur-Rognvaldsson_91

  The role of orography was found to be crucial in determining the precipitation dis- tribution and amount. Atmospheric flow over Iceland was simulated for the period January 1961 through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale model (Grell et al., 1995). The domain used is 123× 95 points, centered at 64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 9. ces_geus_paakitsoq_full_report

  domain and data followed by the description of the mass balance model. Subsequently modeled mass balance will be presented along with the evaluation of the RCM output. Finally we will discuss the relationship of modeled mass balance and biases in the RCM data and will conclude on the suitability of the latter for future scenarios. 2 Model Domain and Data 2.1 Model Domain Paakitsôq is the name /media/ces/ces_geus_paakitsoq_full_report.pdf

• 10. Karlsdottir-Risk_analysis_IMO_SK

  /terminology-2009-eng.html Mitchell J.K. (ed. 1996): The long road to recovery: Community responses to industrial disasters. UN University Press, 307 p. Mitchell J.K. (ed. 1999): Crucibles of hazards: Mega-cities and disasters in transition. UN University Press, 535 p. WMO/trj Observations Inventory Accounting Thematic event maps Hazard potential Sector domain Intensity or magnitude Occurrence /media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf