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  • 41. ces_SA_group_flyer_new

    by season (%) between 1991-2007 and 1961-1990 in the Baltic countries 1 9 0 0 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 - 1 5 - 1 0 - 5 0 5 1 0 1 5 P r e c i p i t a t i o n a n o m a l y ( % ) R e g i o n 1 R e g i o n 2 R e g i o n 3 R e g i o n 4 F un c t ion P lo t 5 1 9 0 0 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 - 1 . 5 - 1 - 0 . 5 0 0 . 5 1 1 . 5 T e m p e r a t u r e a n o m /media/ces/ces_SA_group_flyer_new.pdf
  • 42. VI_2009_006_tt

    to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 43. VI_2013_008

    In Iceland, floods are primarily of three different origins (Snorra- son et al., 2012): (i) meteorological floods induced by rain and which are often combined with melting of snow and ice, (ii) floods due to ice formation and release within river channels, and (iii) glacier outburst floods which originate in marginal lakes, formed in glacier dammed side valleys, or subglacial lakes, formed as a result /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
  • 44. 2013_001_Nawri_et_al

  • 45. „We need to control our footprint on mother Earth“

    and water, „we are the only country with the word „ice“ in its name. I welcome you all, in particular those who have come from abroad. I hope you have a nice time here in Iceland. I hope you will feel the warmth here – even though there is little or no volcanic activity going on as we speak, and even though we worry about a warming world. There is good warmth and there is bad warmth“ Mr /about-imo/news/we-need-to-control-our-footprint-on-mother-earth
  • 46. Keranen_Jaana_CES_2010

    nostaa, m utta oh ijuoksutu ksia tulee Sähkönvas tus kasvaa -> energ iahäv iö ita Muuntajien elinikä lyhenee Jääkannen m uodostaminen h idastuu Very likely, the probab ility that the next decade is warmer is 90% . Ilm iö 1 .1 – korkeammat läm pötilat etenkin talvella Skenario 1. Lä mpimäpi i lmasto O ma luokitteluOma luokit te lu Nykyiset t ai tuleva t varautumiskahdo llisuudet /media/ces/Keranen_Jaana_CES_2010.pdf
  • 47. norsem_sahar

    Email: SR: sahar@hi.is, BH: skykkur@hi.is In earthquake engineering the estimation of the impact of subsoil characteristics on site effects, and modeling the distribution of ground motion amplitudes are known as key elements in accurate seismic hazard assessment programs. Recently, the deployment of Icelandic strong-motion arrays, ICEARRAY I in the SISZ and ICEARRAY II in the TFZ, has /media/norsem/norsem_sahar.pdf
  • 48. AnneFleig_May2010_CES

    E l b e i n D r e s d e n , A p r i l 2 0 0 7 CES conference, Oslo, Norway, 31 May - 2 June 2010 Typical features • develop slowly, • become severe when they cover a large region and persist for an extended period. E l b e i n D r e s d e n , A p r i l 2 0 0 7 ( s p i e g e l . d e ) Anne K. Fleig et al. “Regional hydrological droughts and weather types in north /media/ces/AnneFleig_May2010_CES.pdf
  • 49. VI_2014_001

    ...................................................................................... 31 7 References .................................................................................................. 32 Appendix I - Daily Index flood models for Region 1. .......................................... 35 Appendix II - Daily Index flood models for Region 2. ........................................ 36 Appendix III - Comparison between /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
  • 50. Kjellstrom_Erik_CES_2010

    ANN−10 −5 0 5 10 15 20 delta w (% ) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17C h a n g e i n g e o s t r o p h i c w i n d s p e e d ( % ) Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling Chen and Aschberger, 2006 17 CM IP G CM s A need for regional ensemble simulations head2right Changes are uncertain head2right Size and sometimes even sign /media/ces/Kjellstrom_Erik_CES_2010.pdf

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