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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. Machguth_Horst_CES_2010

  hydrology with respect to hydropower 3 / 16 Ahlstrøm et al., 2009 • recent evaluation of the future hydropower potential (Ahlstrøm et al., 2009) • bed and surface topography (radar and LiDAR) • scenarios of ice flow, mass balance and basin delineation previous work 4 / 16 motivation Ahlstrøm et al. (2009): • only one RCM (HIRHAM4) • limitations in mass balance modelling CES project: • 2 months • conduct /media/ces/Machguth_Horst_CES_2010.pdf

• 3. 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

• 4. 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

• 5. Perrels-CBA

  Integrated • Infrastructure • Large size, indivisibilities, layers, network effects • Long lifetime, economic & spatial structuring • Public good features, implications of market organization 8/26/2011Adriaan Perrels/IL 3 26.8.2011Adriaan Perrels/IL 4 Climate change impacts – temporal profiles Duration of the state resulting from the change* Temporal profile of the unfolding of the change /media/loftslag/Perrels-CBA.pdf

• 6. GA_2009_91A_4_Andreassen

  represent annual winter precipitation sums calculatedfrom the stations and multiplied by a constant tuning factor. See Table 3 for explanation of the other runs Table 3. Correlation (r) and root mean square error (rmse) between modelled and measured winter (bw), summer (bs) and net (bn) balancesat Storbreen. bw-m1: reference modelling bw where Psolid when Tair < 1ºC, bw-m2: Psolid when Tair < 3ºC, bs-m1 /media/ces/GA_2009_91A_4_Andreassen.pdf

• 7. Group4

  ), it was decided to broaden the remit to include both mitigation and adaptation measures across the broad range of transport systems. Expected main climate effects for Finland in relation to the national road network: 1) Wetter winters with lower snowfall and more rain, 2) increase in freeze/thaw cycles in winter in the southern parts of Finland, 3) higher frequency and severity of storms, 4) hotter /media/loftslag/Group4.pdf

• 8. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  to the annual temperatures during 2003
  2007. The low AAR and the high mass balance sensitivity (e.g., Jo´hannesson 1997) to a uni- form temperature rise (Table 4) at both Torfajo¨kull and Tindfjallajo¨kull during the warm last decade are con- sistent with their low and narrow elevation range (Fig. 1). Table 3 (a) Average specific net balance (bn), at the Eyjafjallajo¨kull (E), Torfajo¨kull /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 9. vanRoosmalen_etal-2009-WRR_2007WR006760

  for the cases where abstractions and irrigation are not included (Table 3, top) and included (Table 3, bottom). The results are spatially averaged, mean annual values for the 15-year period. The net recharge is defined as the outflow from the root zone minus the sum of evapotranspiration and net flow from the groundwater zone to the overland compartment for the grids where the soil profile /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 10. IPPC-2007-ar4_syr

  economic growth and over- all emissions. {WGIII 3.2, TS.3, SPM} Aerosols have a net cooling effect and the representation of aerosol and aerosol precursor emissions, including sulphur diox- ide, black carbon and organic carbon, has improved in the post- SRES scenarios. Generally, these emissions are projected to be lower than reported in SRES. {WGIII 3.2, TS.3, SPM} Available studies indicate /media/loftslag/IPPC-2007-ar4_syr.pdf