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Results:

• 21. VI_2014_005

  mode ................................................... 14 5 Errors associated with SURFEX .................................................................... 15 6 Statistical correction of model results .............................................................. 19 7 Original and corrected 2-m air temperature .................................................... 22 8 Original and corrected 10-m /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 22. 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

• 23. 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

• 24. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  in the data used in making the decision and the factors are interlinked, all of which makes the problem highly complex. The part of the net defined by variables and links is relatively easily communicated to stakeholders (Henriksen et al., 2007b). However the tal Management 88 (2008) 1025–1036 quantitative part, with the conditional probability tables (CPTs), the numbers, is the step where /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 25. VI_2020_005

  glacier, and a general land rise along the southern coast and in the countries interior (figure 1). This rise results from recent melt of the Icelandic glaciers, which have been melting since the late 19th century. An acceleration in land uplift is even evident in the Southeast. STL analysis of vertical GPS measurements in 1997- 2015 from Höfn in Hornafjörður show over 8 mm/yr uplift in the first /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 26. Group4

  construction and maintenance. 7. Path dependency, meaning that roads will likely continue to exist even if the underlying need for them decreases. 8. Social shifts, personal ownership of cars no longer seen as necessary. Car-sharing becomes part of a suite of mobility options within the collective transportation system. 9. Behavioral shifts, mobility no longer dominant variable in daily life /media/loftslag/Group4.pdf

• 27. ces-oslo2010_proceedings

  ............................................................................................................... 8 PAST AND PRESENT CHANGES IN CLIMATE AND HYDROLOGY Dyrrdal, A.V., Vikhamar-Schuler, D., Stranden, H.B. and Skaugen, T. Analysis of past snow conditions in Norway – Time periods 1931-60, 1961-90 and 1979-08 ............................. 10 Crochet, P. Impacts of historic climate variations on streamflow characteristics in Icelandic rivers /media/ces/ces-oslo2010_proceedings.pdf

• 28. Linnet_Ulfar_CES_2010

  °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf

• 29. 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

• 30. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  increase that will affect existing facilities. It will affect the most important touristic destinations of the country [7]. South-eastern Spain hosts some of the most popular destinations for tourists from the UK and other European countries. According to the IPCC [8], Spain could lose 40% of its German tourists and up to 100% of its British tourists. Hein [5] estimates that climate change /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf