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Results:

• 1. VI_2015_006

  6 Net downward shortwave radiation flux at the surface .................................... 18 7 Net downward longwave radiation flux at the surface ..................................... 19 8 Net downward total radiation flux at the surface............................................ 20 9 Upward sensible heat flux from the ground .................................................. 22 10 Air /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. 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

• 4. Eyjafjallajokull_status_2010-05-07_IES_IMO

  ; IMO hydrological data; IMO weather radar measurements, MERIS satellite image; reports from sent through the IMO web site, information from commercial flights. Eruption plume: Height (a.s.l.): 7 km according to IMO weather radar measurements at 1155h. Commercial flight heading towards Keflavík at 15:18h: 20,000- 25,000ft (7-7.6 km). Heading: Southeast Colour: Colour: Dark /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

• 5. 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

• 6. Traffc-maintenance_expenditures

  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 grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 7. Perrels-CBA

  26.8.2011Adriaan Perrels/IL 6 Review of climate change effects in built-up areas (1) Source: IPCC 4AR_2 Source: IPCC 4AR_2 26.8.2011Adriaan Perrels/IL 7 Source: IPCC 4AR_2 Review of climate change effects in built-up areas (2) 26.8.2011Adriaan Perrels/IL 8 Cost-benefit analysis – the basics 1 • CBA: • assess for the estimated lifetime of a project the annual expenditures (investment funding cost /media/loftslag/Perrels-CBA.pdf

• 8. GA_2009_91A_4_Andreassen

  ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf

• 9. vanRoosmalen_etal-2009-WRR_2007WR006760

  number of parameters compli- cates using such models. [7] At present, very few studies have quantified the combined effects of future climate and land use changes on hydrology [Quilbe et al., 2008]. Pfister et al. [2004] studied changes in peak flows in the Rhine and Meuse basins due to climate and land use change from a historic perspective to gain a better understanding of the dominating processes /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 10. IPPC-2007-ar4_syr

  Arctic sea ice extent has shrunk by 2.7 [2.1 to 3.3]% per decade, with larger decreases in summer of 7.4 [5.0 to 9.8]% per decade. Mountain glaciers and snow cover on average have declined in both hemispheres. The maximum areal extent of sea- sonally frozen ground has decreased by about 7% in the Northern Hemisphere since 1900, with decreases in spring of up to 15%. Temperatures at the top /media/loftslag/IPPC-2007-ar4_syr.pdf