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Results:

• 51. The weather in Iceland 2015

  in the Southwest. The weather in December was stormy. The year 2015 was the coldest in Iceland since 2000, but this period has generally been abnormally warm so the average temperature was close to the 1961-1990 mean. In most parts of the country the precipitation was well above normal. Temperature The average temperature in Reykjavík was 4.5°C, 0.2°C above the 1961-1990 mean. This is the 20th /about-imo/news/nr/3273

• 52. What is Bárðarbunga?

  is Bárðarbunga? Information on the central volcano 10.12.2014 There are about 30 known central volcanoes, or volcanic systems, in Iceland. Bárðarbunga, the second highest mountain of Iceland; ca 2000 meters above sea-level, is one of them. The volcano is placed /about-imo/news/nr/2968

• 53. The ice cap Snæfellsjökull is thinning rapidly

  Lowering of Snæfellsjökull. The year 2000 margin is shown with a red curve /weather/articles/nr/1618

• 54. The ice cap Snæfellsjökull is thinning rapidly

  Lowering of Snæfellsjökull. The year 2000 margin is shown with a red curve /weather/articles/nr/1618/

• 55. Tomas_Johannesson_(IMO,_Ice)

  period. A new hazard zoning method was developed in Iceland after the snow avalanche accidents in 1995 and in 2000 a new regulation on avalanche hazard zoning was issued. The method and regulation are based on individual risk, or annual probability of death due to avalanches. The major components of the method are the estimation of avalanche frequency, run-out distribution /media/loftslag/Tomas_Johannesson_(IMO,_Ice).pdf

• 56. norsem_begga

  Office (IMO). The better constrained earthquakes in the SIL earthquake catalog of the IMO (~1/3 of total) tend to have location uncertainties of ~1.0 km, which is too high for the significance level required.. To improve location accuracy of the IMO catalog, the relative earthquake location algorithm of Waldhauser and Ellsworth (2000) (W&E) is being applied. The algorithm minimizes measured /media/norsem/norsem_begga.pdf

• 57. CES_D2_2_poster_3x3

  the uncertainty mainly comes from natural variability and differences between climate models. DATA AND METHODS The results shown here are based on simulations by 19 global climate models. This so-called CMIP3 data set is described by Meehl et al. (2007). The probabilistic forecasts are constructed using simulations for SRES A1B scenario (Naki enovi and Swart 2000). A resampling technique /media/ces/CES_D2_2_poster_3x3.pdf

• 58. ces_SA_group_flyer_new

  a l y ( ° C ) 1900 1920 1940 1960 1980 2000 -20 -10 0 1 0 2 0 R u n o f f a n o m a l y ( % ) 1900 1920 1940 1960 1980 2000 -40 -30 -20 -10 0 1 0 2 0 3 0 E v a p o r a t i o n a n o m a l y ( % ) Large-scale atmospheric patterns and hydroclimatological variables Large-scale atmospheric circulation patterns, are more accurately assessed by Global Climate Models than are local variations /media/ces/ces_SA_group_flyer_new.pdf

• 59. Alam_Ashraful_CES_2010

  growth Carbon dioxide concentration at th t h Regeneration distribution, growth rate of different species Different tree e a mosp ere Mortality 10 Input data  Finnish NFI data • total 2816 permanent sample plots for the whole of Finland (south: 1855; north: 961)  FMI - Climatic data • Current climate (1971-2000) • Changing climate during 2010-2099 (2010-2039; 2040-2069; 2070-2099) A2 /media/ces/Alam_Ashraful_CES_2010.pdf

• 60. Eriksson_Garvill_Nordlund_2006

  www.elsevier.com/locate/yjevp evaluations of coercive and noncoercive TDM measures Steg & Vlek, 1997), car users’ evaluations of the three Widegren, 1998). In the value-belief-norm (VBN) theory of environmentalism (Stern et al., 1999; see also Stern, 2000), pro-environmental behavior is explained by a hierarchical sequence of variables. According to the theory, values, general environmental beliefs /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf