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Results:

• 21. 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

• 22. 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

• 23. ces_geus_paakitsoq_full_report

  ) is shown. At the margin the grid boxes of the RCAO RCM are visible. The area between Illulisat and Swiss camp is commonly called Paakitsôq. respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and Box, 2001). The locations of the stations are indicated in Fig. 1, further details /media/ces/ces_geus_paakitsoq_full_report.pdf

• 24. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  such as Spain, will be most negatively affected within the EU [4]. The much higher temperatures that would have during summer would make Spain an unpleasant destination for many tourists [5]. Moreover, the snow-based tourism will be affected because of the unavailability of natural snow [2]. The tourism industry represents more than 10% of the Spanish GDP and more than 13% of the employment /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

• 25. 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

• 26. Reykholt-abstracts

  and Gareth Rees Scott Polar Research Institute (SPRI), University of Cambridge, UK Calculation of glacier velocity from repeat lidar survey Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 5 Tómas Jóhannesson Icelandic Meteorological Office, Iceland Flow paths of subglacial water detected by lidar measurements of changes in the ice surface elevation of glaciers /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 27. VI_2020_005

  5 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 60 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 61 Appendix: Description of the usage of the ACER method to find return periods and an adopted Hunter method to calculate allowances in Norway . . . . . . . . . . . . . . 73 1 Introduction The dynamic /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 28. Perrels-CBA

  / design, availability, materials, ICT, modal split) 26.8.2011Adriaan Perrels/IL 5 Categorising stages of adaptation Passive Adaptation - automatic in nature and economy - only ex post measures (no anticipation) Active Adaptation - automatic in nature and economy - ex ante and ex post policies Emission scenario dependent baseline (A1-T, B1, A2, etc.) Reference costs and benefits /media/loftslag/Perrels-CBA.pdf

• 29. Journal_of_Hydrology_Veijalainen_etal

  when the spring floods decreased and autumn and winter floods increased. The differences between the scenarios were estimated by com- paring the average changes of the scenarios (marked with dia- monds in Fig. 5). The differences between different emission scenarios with the same GCM were rather small; the average changes in floods differed on average by 1.7% units in 2070– 2099. The B1 scenario /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

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

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf