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Results:

• 51. Karlsdottir-Risk_analysis_IMO_SK

  in animals  followed by death intoxicated grass Ash dispersion in the free atmosphere threat to aviation Natural Hazards – IMO’s Domestic Collaboration IMO Civil Protection Department – National Commissioner of the Icelandic Police Civil Aviation Authority ISAVIA – Air Navigation Service Provider Icelandic Maritime Administration Universities in Iceland Icelandic Road Authority Icelandic /media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf

• 52. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  is the differential exposure to stress experienced by different exposure units, and is also a dynamic process, changing over a variety of inter-linked time scales. Social vulnerability is rooted in the actions and multiple attributes of human actors. Social networks drive and bound vulnerability in the social, economic, political and environmental context. Therefore, social and economic vulnerability /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 53. Eriksson_Garvill_Nordlund_2006

  0.31 0.25 0.27 0.30 Table 4 Correlation matrix of variables in the models of improved public transport column (S1) are correlation coefficients in sub-sample 1 (N ¼ 462), and th PRO-ENV PROBLEM PN W S1 S2 S1 S2 S1 S2 S1 PROBLEM 0.422 0.430 PN 0.278 0.356 0.450 0.510 W 0.298 0.319 0.402 0.492 0.641 0.618 PUB FREE 0.128 0.174 0.180 0.145 0.051ns 0.117 0.105 OWN 0.116 0.170 0.162 0.227 0.109 0.249 /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 54. 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

• 55. 2013_001_Nawri_et_al

  of the underlying surface, and the adjustment of the wind to the free atmospheric conditions above the boundary layer. Temporal variability of the atmosphere is linked to processes with a wide range of dominant time- scales. Seasonal and diurnal cycles are directly related to the planet’s motion within the solar system. The seasonal cycle in wind speed at mid- and high-latitudes is due to the intensification /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 56. Water_resources_man_Veijalainen_etal

  Lake Syväri and Lake Pielinen these floods occur during late spring or early summer. Due to long lake routes causing long time delays, the highest water levels in Lake Saimaa typically occur in late summer, although high water levels have also taken place in autumn and winter after prolonged heavy precipitation. The outflows of Lakes Pielinen and Saimaa mostly follow the natural rating curve, where /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 57. GA_2009_91A_4_Andreassen

  of ice melt at the AWS location will increase from c. 40 to c. 80 days. Key words: glacier, mass balance, albedo, temperature, precipita-tion, precipitation, climate IntroductionTo predict how a glacier will react to climate change or to reconstruct a glacier’s mass balanceback in time, a mass balance model is needed to relate the surface mass balance to prevailing cli- mate conditions. A whole /media/ces/GA_2009_91A_4_Andreassen.pdf

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

  as a ref- erence map for co-registering the SPOT5 HRS-DEM (pixel resolution of 40× 40 m), using the ice free areas surround- ing Hoffellsjökull and the correlation method described by Guðmundsson et al. (2011). This comparison revealed a hor- izontal shift of the HRS-DEM by 15 m and 5 m towards east and north, respectively, and a vertical offset of 2.3 m. Gaps in the HRS DEM, due to low contrast /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 59. Lorenzoni_Pidgeon_2006

  AND USA PERSPECTIVES 75 change differ on a range of factors, including: the precise question (phrasing and stimulus terms) posed to study participants; the timeframes of data collection and publication; and the geographical extent of the studies. Furthermore, as with many other environmental issues, the changing social context at any particular point in time (e.g. the activities of interest groups /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 60. Moellenkampetal_etal-2010

  some form of collective planning and organization activities because of the stakes, time, and budgets involved in their implementation. Despite the potential importance of these collective processes for managing complex water-related social–ecological systems, little research focusing on the project teams that design and organize participatory water management processes has ever been undertaken. We /media/loftslag/Moellenkampetal_etal-2010.pdf