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Results:

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

  SPOT 5 HRS images), which is less than the AAR of about 35% obtained for the Langjo¨kull ice cap in 2004; the AAR of Langjo¨kull has varied between 20 and 45% over the last decade (Pa´lsson et al. 2007). This is in agreement with the more negative specific net mass balance on Eyjafjallajo¨kull than Lang- jo¨kull (1.5 and 1.3 m yr1 w. eq., respectively) for the period from 1998 to 2004. The mean /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 12. 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

• 13. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Relative Changes When Comparing the A2 and B2 Scenarios to the Current Climatea Scenario Net Recharge Horizontal Boundary Outflow Drain Flow Base Flow Water Supply Irrigation Simulations Not Including Abstractions and Irrigation Current climate 550 23 279 252 A2 scenario + 67 (12%) + 1 (4%) + 56 (20%) + 13 (5%) B2 scenario + 113 (21%) + 1 (4%) + 92 (33%) + 22 (9%) Simulations Including Abstractions /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 14. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf

• 15. Reykholt-abstracts

  Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Abstract volume Lidar map of the ice-covered stratovolcano Öræfajökull in S-Vatnajökull, S-Iceland, surveyed by TopScan GmbH in August 2011 Lidar measurements of the cryosphere /media/vatnafar/joklar/Reykholt-abstracts.pdf

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

  961–975, 2011 966 G. Aðalgeirsdóttir et al.: 20th and 21st century evolution of Hoffellsjökull glacier Table 1. Specific winter (bw), summer (bs) and net balance (bn) for Hoffellsjökull in mw.e. a−1. A conservative error estimate is on the order of 15–20 % for both bw and bs. Glacier year bw bs bn 1935–1936 2.0 −3.4 −1.4 1936–1937 2.4 −2.1 0.3 1937–1938 1.7 −2.4 −0.6 2000–2001 2.0 −2.1 −0.1 2001 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 17. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 18. Case_A___Horsens_Fjord

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/Case_A___Horsens_Fjord.pdf

• 19. Horsens_case

  level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Summerschool Copenhagen 22-26 August 2011 2 Physical features and ecosystem The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations /media/loftslag/Horsens_case.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