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  • 1. VI_2015_006

    ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 2. Machguth_Horst_CES_2010

    experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf
  • 3. James-Smith_Edward_CES_2010

    for distribution companies Influence climate change will have on: • Infrastructure/security of supply • Distributed generation • Demand • Income Character scale • -10 for very negative influence • 0 for no influence • 10 for very positive influence Winter Spring SummerAutumn - - - - - - … - - - - - - - - - - … - - - - - - - … - - - - - - - - - - … Inclusion of climate element - seasonal clock Risk /media/ces/James-Smith_Edward_CES_2010.pdf
  • 4. 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
  • 5. ces_geus_paakitsoq_full_report

    22N) from till Illulisat DMI 50 10 105 497382 7681278 Ta 1.1.81 6.4.06 Station 437 ASIAQ 275 340 311 531316 7709513 Ta 5.9.83 1.6.06 Swiss Camp GC-net 1150 1115 780 566396 7719204 Ta, Sin 1.1.95 8.5.06 Crawford GC-net 2022 1795 1982 654464 7757807 Ta, Sin 24.5.95 2.5.06 2 2.3 RCM Data Output from two RCMs is used: (1) the regional coupled ocean-atmosphere model RCAO (Döscher et al., 2002) and (2 /media/ces/ces_geus_paakitsoq_full_report.pdf
  • 6. Perrels-CBA

    operational cost, etc.) and the annual revenues • consider an appropriate discount rate and assess NPV (net present value), IRR (internal rate of return), and net cash flows • rank alternatives by score level • SCBA: social CBA – total benefits -/- total costs for society, in this case benefits and costs often don’t accrue (entirely) to the same organisation due to the public nature of a project /media/loftslag/Perrels-CBA.pdf
  • 7. Traffc-maintenance_expenditures

    047 13 903 11 197 - - - 522 610 1 406 449 1980 42 409 153 761 14 024 212 220 - 5 257 17 816 10 410 9 234 - - - 465 133 1 420 546 Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land /media/loftslag/Traffc-maintenance_expenditures.pdf
  • 8. GA_2009_91A_4_Andreassen

    to highly negative summer balances, but also lower bw than the average for 1949–2006. Calculated change in specific mass balance for a ±1°C change in air tem- perature was ±0.55 m w.e., whereas a ±10 % in- crease in precipitation represented a change of ± 0.20 m w.e. Model results further indicated that for a 2°C warming, the ablation season will be extend- ed by c. 30 days and that the period /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 9. Gudmundsson-etal-2011-PR-7282-26519-1-PB

    of Eyjafjallajo¨kul), Hveravellir (Hv; 641 m a.s.l., ca. 100 km north of Tindfjallajo¨kull and Torfajo¨kull) and Ho´lar (Ho) in Hornafjo¨rdur (18 m a.s.l.). The plot shows the elevation distribution of the Eyjafjallajo¨kull, Tindfjallajo¨kull and Torfajo¨kull ice caps as area (km2) per 10 m elevation interval. Mass balance of three ice caps in southern Iceland S. Gudmundsson et al. 2 (page number /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
  • 10. 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

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