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Results:

• 11. 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

• 12. 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

• 13. 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

• 14. 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

• 15. 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

• 16. 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

• 17. 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

• 18. 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

• 19. 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

• 20. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011 …………………………………………………………………………………………………………………………………………………………………… 1 Outline for the case Road maintenance in a changing climate Introduction Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010 /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf