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Results:

• 41. Milly_etal-2008-Stationarity-dead-Science

  ), S. Solomon et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–18; www.ipcc.ch/press/index.htm. 5. IPCC, in Climate Change 2007: Climate Change Impacts, Adaptation and Vulnerability, Contribution of WG2 to AR4, M. L. Parry et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–16. 6. I. M. Held, B. J. Soden, J. Clim. 19, 5686 (2006). 7. T. P. Barnett, J. C. Adam, D. P. Lettenmaier /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 42. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 43. Recent publications

  The Icelandic Meteorological Office annually publishes a variety of reports, journals and articles. Below are examples of recent publications, most of which contribute to Arctic issues in general. Large-scale atmospheric conditions associated with major avalanche cycles and cold season weather hazards in Iceland (2013) The wind energy potential of Iceland (2013) Surface wind and air temperature over /about-imo/arctic/completed-projects/publications/

• 44. Aurora and the Earth's magnetic field

  currents in its outer core. At the surface, about 90% of the field can be described by a simple dipole field tilting about 10° from the rotation axis. The currents in the Earth's core are slowly varying causing slow changes of the magnetic field, typically on timescales of years and ages. A flow of charged particles from the sun, called the solar wind, hits steadily the magnetic field and bends /weather/articles/nr/2549

• 45. raisanen_ruosteenoja_CES_D2.2

  Model Institution BCCR-BCM2.0 Bjerknes Centre for Climate Research, Norway CGCM3.1 (T47) Canadian Centre for Climate Modelling and Analysis CGCM3.1 (T63) same as previous CNRM-CM3 Météo-France CSIRO-MK3.0 CSIRO Atmospheric Research, Australia ECHAM5/MPI-OM Max Planck Institute (MPI) for Meteorology, Germany ECHO-G University of Bonn and Model & Data Group, Germany; Korean Meteorological Agency GFDL /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 46. Lorenzoni_Pidgeon_2006

  for people to conceptualise and to relate to their daily activities, arguably because it cannot be easily translated into the language of popular culture (Ungar, 2000; see also mental models of cli- mate change by Bostrom et al., 1994; Kempton, 1997; discussed later). Secondly, the various datasets available detailing public opinions and attitudes on climate PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 47. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 48. VI_2015_009

  flood models 1–24 (Eqs. 8 and 9 applied with variables 1–12). Ratio between esti- mated and reference index flood (solid black line). The solid blue line corresponds to the reference index flood (Ratio=1), estimated as the arithmetic mean of the observed AMF sample and the dashed blue lines the 95% CI derived from the GEV distribution. Large red symbol indicates overall best model. 18 4.2.2 Flood /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 49. QA on the eruption in Eyjafjallajökull 2010

  health, for example the respiratory system. The fluorine content is approximately 850 mg/kg according to chemical analysis carried out by the Institute of Earth Sciences, University of Iceland, on a sample taken 19 April. An earlier sample since 14 April only measured 25-35 mg/kg of fluorine because the water vapour from melting ice rinsed the ash. When the eruption progressed, water became less /earthquakes-and-volcanism/articles/nr/1880

• 50. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  & Hautala, R. 2009. Benefits and value of meteorological information services – the case of the Finnish Meteorological Institute, Meteorological Applications, 16, pp. 369–379. Meyer, M.D., Amekudzi, A., O’Har, J.P. (2009), Transportation Asset Management Systems and Climate Change: An Adaptive Systems Management Approach, paper for Transportation Research Board 2010 Annual Meeting, CD-ROM /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf