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Results:

• 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. 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

• 3. 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

• 4. Joining forces in weather forecasting and climate research

  Snorrason, Director General of the IMO. The new supercomputer can perform 4,000 trillion calculations per second, which is more than half a million calculations per second for every person on the planet. It will handle state of the art weather models with more than 6 million lines of code –the Mars Curiosity Rover was built on 5 million- which will produce high resolution weather predictions /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 5. 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

• 6. ces_geus_paakitsoq_full_report

  ) is shown. At the margin the grid boxes of the RCAO RCM are visible. The area between Illulisat and Swiss camp is commonly called Paakitsôq. respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and Box, 2001). The locations of the stations are indicated in Fig. 1, further details /media/ces/ces_geus_paakitsoq_full_report.pdf

• 7. Perrels-CBA

  / design, availability, materials, ICT, modal split) 26.8.2011Adriaan Perrels/IL 5 Categorising stages of adaptation Passive Adaptation - automatic in nature and economy - only ex post measures (no anticipation) Active Adaptation - automatic in nature and economy - ex ante and ex post policies Emission scenario dependent baseline (A1-T, B1, A2, etc.) Reference costs and benefits /media/loftslag/Perrels-CBA.pdf

• 8. GA_2009_91A_4_Andreassen

  and asimplified mass balance model suggests that airtemperature and albedo is satisfactorily parameter-ised, at least for the AWS altitude. However, thecompared period covers only 5 of the 58 modelledyears in this study. Furthermore, the specific win-ter, summer and net balances measured at Stor-breen in 2001–2006 deviate markedly from the mean for the whole observation period. A combi-nation /media/ces/GA_2009_91A_4_Andreassen.pdf

• 9. vanRoosmalen_etal-2009-WRR_2007WR006760

  is completely saturated and the unsaturated zone no longer active. The net horizontal boundary outflow is the Figure 5. Observed and simulated groundwater heads at locations A and B in Figure 2. W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE 9 of 18 W00A15 net outflow across the catchment boundary and accounts primarily for groundwater flow to the sea. Drain flow includes drainage from groundwater /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 10. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf