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  • 31. VI_2013_008

    of the analogue method is introduced. In Section 3 hydrological and me- teorological data used in the analysis are presented. Section 4 describes the different strategies considered for implementing the method and Section 5 presents some results. Some concluding remarks are made in Section 6. 2 The analogue method Let X(t) be a state of a dynamical system at time t, known through the observation of k variables /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
  • 32. Tornado_Impacts_-_FMI_Presentation

    -scale Category 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 Permanent Homes Casualties and Timing Casualties and Time of Day 150 200 250 I n d e x V a l u e Fatalities 0 50 100 Overnight Morning Early Afternoon Late Afternoon Late Evening I n d e x V a l u e Injuries Nocturnal Tornadoes 7 8 9 10 R a t i o N i g h t t o O t h e r T i m e s 0 1 2 3 4 5 6 F0 F1 F2 F3 F4 F /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf
  • 33. Lettenmaier_Dennis_CES_2010pdf

    model regional projections. • Development of multiple 50-km regional climate scenarios for use in impacts assessments. • Evaluation of regional model performance over North America. www.narccap.ucar.edu 50-km Grid GFDL CGCM3 HADCM3 CCSM MM5 X X1 RegCM X1** X CRCM X1** X HADRM X X1 RSM X1 X WRF X X1 Red = run completed Drawbacks of dynamical downscaling • Requires postprocessing for bias /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
  • 34. 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
  • 35. 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
  • 36. VI_2015_005

    This is also the case with cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are cyclones in the neighbouring sector, in which case pressure tendencies are reversed. 21 Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com- posite mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 37. Lorenzoni_Pidgeon_2006

    level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 38. Linnet_Ulfar_CES_2010

    °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 39. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

    /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
  • 40. Ash measurements

    in estimating the height of the plume. At this time, the plume reached heights of 8 - 12 km. During the 2010 Eyjafjallajökull eruption, the weather radar proved to be a very useful tool, but the great distance to the eruption site (160 km) reduced the quality of the data. Therefore, a mobile X-band weather radar was purchased, but while this custom made radar was being assembled and tested, another /about-imo/news/nr/2183

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