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Results:

• 31. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

• 32. James-Smith_Edward_CES_2010

  opportunity evaluation Case studies NOE Net SEAS-NVE Findings of case studies • Distribution companies generally well equipped for climate change – Cabling of all overhead lines well under way – Distribution boxes in areas with increased risk of flooding are elevated already – Salt spray further inland is becoming an increasing problem for substations and transformers Cabling in Denmark /media/ces/James-Smith_Edward_CES_2010.pdf

• 33. ces-oslo2010_proceedings

  of communication. However, it could be 9 improved e.g. by making it more simple and easy to grasp. The list of publications is important, but at present the publications cannot be downloaded. A future improvement would be to have a list of downloadable publications. A substantial improvement would be executive summaries of publications adapted for stakeholders. Fact sheets could be an important /media/ces/ces-oslo2010_proceedings.pdf

• 34. Reykholt-abstracts

  ................................................................................................................... 8 Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9 Lidar measurements of Norwegian glaciers – an overview Neil Arnold* and Gareth Rees .............................................................................................. 10 Calculation of glacier velocity from repeat /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 35. Horsens_case

  lying areas in the City is illustrated for present climate in Figure 5. It is expected that the future water level of the Horsens fiord will increase by 1 meter by the end of this century. Station 270045: Upstream Lake Nørrestrand 0 0.5 1 1.5 2 2.5 3 3.5 4 1 2 3 4 5 6 7 8 9 10 11 12 Month M ea n d is ch ar g e (m 3 / s) Present: Mean A2: Mean Station 280001: Upstream Bygholm Lake 0 1 2 3 4 5 6 /media/loftslag/Horsens_case.pdf

• 36. 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

• 37. 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

• 38. 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

• 39. 2010_016

  The effect of climate change on runoff from two watersheds in Iceland Bergur Einarsson Sveinbjörn Jónsson VÍ 2010-016 Report The effect of climate change on runoff from two watersheds in Iceland VÍ 2010-016 ISSN 1670-8261 Report +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Bergur Einarsson, Icelandic Meteorological Office /media/ces/2010_016.pdf

• 40. 2010_017

  Iceland VÍ 2010-017 ISSN 1670-8261 Report +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Bergur Einarsson, Icelandic Meteorological Office Sveinbjörn Jónsson, Icelandic Meteorological Office   5 Contents FIGURES /media/ces/2010_017.pdf