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  • 11. Kok_and_Veldkamp_editorial_ES-2011-4160

    The American Political Science Review 97:233-243. Jessop, B. 2005. The political economy of scale and European governance. Tijdschrift voor Economische en Sociale Geografie 96:225-230. Katz, D., and I. Fischhendler. 2011. Spatial and temporal dynamics of linkage strategies in Arab- Israeli water negotiations. Political Geography 30 (1):13-24. doi:10.1016/j.polgeo.2010.12.002. Kok, K., R. Biggs, and M /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
  • 12. norsem_michalek

    was deployed and together with the permanent NNSN stations in that area it contained 33+ stations within span 350 x 200 km. About 1250 earthquakes of M>0.0 was recorded during the project period and new map of seismicity of that area was retrieved. The main aim of the project is to reveal the stress field in that particular region and therefore determination of stable /media/norsem/norsem_michalek.pdf
  • 13. Refsgaard_2-uncertainty

    /breakthrough curves West East Model C Model A Model B Fractured clay/ Toplayer Sand Clayey till Limestone SelandienLimestone 0 20 40 60 0 0.2 0.4 0.6 0.8 1 N or m al is ed c on ce nt ra ti on 0 20 40 60 80 100 0 0.2 0.4 0.6 0.8 1 0 40 80 120 160 200 Time in years 0 0.2 0.4 0.6 0.8 1 N or m al is ed c on ce nt ra ti on 0 100 200 300 Time in years 0 0.2 0.4 0.6 0.8 1 Model A Model B Model C Simulated /media/loftslag/Refsgaard_2-uncertainty.pdf
  • 14. Tornado_Impacts_-_FMI_Presentation

    fatalities occurred in mobile homes, although only 7.6% of U.S. housing units in 2000. • A one standard deviation in the proportion of mobile homes in housing stock (8.3 percentage points) increases fatalities by 36% and injuries by 18%. The Mobile Home Problem 50 60 70 80 90 P e r c e n t a g e o f C a t e g o r y F a t a l i t i e s Mobile Homes 0 10 20 30 40 F0 F1 F2 F3 F4 F5 F /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf
  • 15. Lettenmaier_Dennis_CES_2010pdf

    12 1 month 12 Columbia River Basin Water Resource Sensitivity to PCM Climate Change Scenarios 0% 20% 40% 60% 80% 100% 120% Portland- Vancouver Spring Flood Control Reliability Portland- Vancouver Winter Flood Control Reliability Autumn Firm Power Reliability (November) % of Control Hydropower Revenues McNary Instream Target Reliability (April- August) Middle Snake Agricultural /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
  • 16. RaisanenJouni_CES_2010

    – observed and simulated changes in global mean temperature • Pattern scaling approach – changes in mean climate and variability assumed to be proportional to the change in global mean temperature Regression coefficients of winter mean temperature: how much is climate on the average simulated to change per 1°C of global warming? X X Helsinki (60ºN, 25ºE): On average, the mean winter temperature /media/ces/RaisanenJouni_CES_2010.pdf
  • 17. TietavainenHanna_CES_2010

    and objective CES Conference, Oslo 31.5.-2.6.2010 Study area • Two study areas sized 100 x 100 km located in north-eastern (NE) and south-western (SW) part of Finland • Climatologically different zones: • NE: • between middle- and north-boreal zones • continental climate • SW: • between hemi- and south-boreal zones • maritime influence • Past and future monthly precipitation sums in May-September /media/ces/TietavainenHanna_CES_2010.pdf
  • 18. VI_2020_004

    .................... 85 8 Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86 Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87 Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88 Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 19. Ash measurements

    and the the backscatter is measured by the radar. The radar has also been successfully used in monitoring eruption plumes, recording reflections from ash particles and water droplets in the plume. The weather radar on Miðnesheiði The image shows the radar backscatter signal recorded at 14:20 hrs on 23 May 2011. Also, the maximum backscatter in the vertical plane is shown, which can be used /about-imo/news/nr/2183
  • 20. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

    more uncertain than the changes in temperature. The 5th percentile of annual mean precipitation change is positive in northern Russia, Finland and large parts of Sweden; elsewhere, it is generally negative. Conversely, the 95th percentile is in the range 10-20%. The uncertainty in seasonal mean precipitation changes is larger than that of the annual mean change. In particular, the 5-95% range /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

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