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  • 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. News

    News Public domain © Wikipedia Almyrkvi á sólu. / Total eclipse of the sun /about-imo/news/bigimg/1363
  • 3. 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
  • 4. VI_2017_009

    .................................................................................................................... 7 2 Data and methods ........................................................................................................... 8 2.1 Data and time frame .............................................................................................. 8 2.2 Domain and spatial resolution /media/vedurstofan-utgafa-2017/VI_2017_009.pdf
  • 5. Hazard zoning

    a year, or its variations with the season. The maps are available in small and large domain. The numbers reported in brackets on the large domain map correspond to the number of times that some UST stations (marked with grey dots) measured a concentration higher than the threshold the map is referring to. The numbers refer to hourly averaged concentration of SO2. At a specific location /pollution-and-radiation/volcanic-gas/hazard-zoning/
  • 6. Hazard zoning

    a year, or its variations with the season. The maps are available in small and large domain. The numbers reported in brackets on the large domain map correspond to the number of times that some UST stations (marked with grey dots) measured a concentration higher than the threshold the map is referring to. The numbers refer to hourly averaged concentration of SO2. At a specific location /pollution-and-radiation/volcanic-gas/hazard-zoning
  • 7. 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
  • 8. Global Cryosphere Watch

    system and provides one of the most useful indicators of climate change, it is arguably the most under-sampled domain in the climate system. The contribution of the cryosphere to sea-level rise in a changing climate is a critical issue for society. The cryosphere, being frozen water, is an intrinsic part of the global water cycle, for example, impacting water, weather, energy and agriculture /about-imo/news/nr/2390
  • 9. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

    that were available in the ENSEMBLES Research Theme 3 data base 6 in mid-June 2009 and (i) had been run at 25 km resolution for the A1B scenario (ii) in a domain considered sufficiently large for our analysis, and (iii) for which no technical problems were detected in an initial inspection of the model output. The data for most of the RCMs were available as interpolated to a regular 0.25° × 0.25 /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
  • 10. 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

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