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Results:

• 11. ces-oslo2010_proceedings

  ....................................... 16 CLIMATE PROJECTIONS Kjellström, E., Drews, M., Christensen, J.H., Haugen, J.E., Haakenstad, H. and Shkolnik, I. An ensemble of regional climate change scenarios for the Nordic countries........................................................ 18 Benestad, R.E. An analysis of simulated and observed storm characteristics /media/ces/ces-oslo2010_proceedings.pdf

• 12. 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  is completely saturated and the unsaturated zone no longer active.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

• 13. 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

• 14. Group4

  ); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf

• 15. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 16. 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

• 17. Horsens_case

  fiord area. Adaptive challenges due to changes in regional groundwater level An increase in sea level will cause more frequent flooding in the town due to its low lying position by the fjord. In 2006, the local town hall was flooded when sea level rose to 1.76 m above normal. Simultaneously, increased net precipitation and increased rainfall intensity put pressure on the sewage system /media/loftslag/Horsens_case.pdf

• 18. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 19. Case_A___Horsens_Fjord

  increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/Case_A___Horsens_Fjord.pdf

• 20. Bárðarbunga 2014 - August events

  line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm at Bárðarbunga on Saturday /earthquakes-and-volcanism/articles/nr/3000