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• 11. Joining forces in weather forecasting and climate research

  of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 12. ces-oslo2010_proceedings

  ........................................ 34 Bergström, S. and Andréasson, J. Swedish Guidelines for Design Floods for Dams in a Changing Climate ............................................................ 36 3 HYDROLOGICAL PROJECTIONS, GLACIERS AND ICE-SHEETS Jóhannesson, T., Aðalgeirsdóttir, G., Ahlstrøm, A., Andreassen, L.M., Beldring, S., Björnsson, H., Crochet, P., Einarsson, B /media/ces/ces-oslo2010_proceedings.pdf

• 13. Adalgeirsdottir-etal-tc-5-961-2011

  near the middle of the 21st century and ∼2–3 ◦C by the end of the century, relative to the 2000– 2009 average. When compared to the reference period 1981– 2000, when the net balance of most of the Icelandic ice caps was close to zero (Guðmundsson et al., 2011; Aðalgeirsdót- tir et al., 2006; Guðmundsson et al., 2009b), the temperature increase is 2.0–2.4 ◦C near the middle of the 21st century /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 14. Horsens_case

  in MIKE SHE / MIKE 11 in order to describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3) Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure also show major highways, main roads and the topography in the area. NONAM Summerschool Copenhagen 22-26 August 2011 3 Figure 3 Zoom in on Horsens by area. Hansted å /media/loftslag/Horsens_case.pdf

• 15. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

• 16. James-Smith_Edward_CES_2010

  opportunity evaluation Case studies NOE Net SEAS-NVE Findings of case studies • Distribution companies generally well equipped for climate change – Cabling of all overhead lines well under way – Distribution boxes in areas with increased risk of flooding are elevated already – Salt spray further inland is becoming an increasing problem for substations and transformers Cabling in Denmark /media/ces/James-Smith_Edward_CES_2010.pdf

• 17. Reykholt-abstracts

  ............................................................................................................... 33 Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 3 CryoSat-2 Arctic sea-ice freeboard and thickness data product and its validation Ciaran Robb, Ian Willis and Neil Arnold ............................................................................ 34 Using airborne remote /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 18. Irafossmyndir_1-4

  
  Mynd 1
  Mynd 2 
  Mynd 3
  Mynd 4 /media/geislun/myndasafn/Irafossmyndir_1-4.doc

• 19. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  in order to reduce hunting pressure on the disturbance of waterbirds. Hydrological modelling A regional groundwater and surface model is constructed in MIKE SHE / MIKE 11 in order to describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3) Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure also show major highways /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 20. Case_A___Horsens_Fjord

  to reduce hunting pressure on the disturbance of waterbirds. Hydrological modelling A regional groundwater and surface model is constructed in MIKE SHE / MIKE 11 in order to describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3) Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure also show major highways /media/loftslag/Case_A___Horsens_Fjord.pdf