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Results:

• 61. Water_resources_man_Veijalainen_etal

  8 76. 2 76. 6 2070–99 Water level (m ) Water level (m ) Water level (m ) Month Month Month (c) (d) (e) (f) (g) (h) (i) Fig. 4 Average daily water level (m) in Lake Pielinen (a–c), Lake Syväri (d–f) and Lake Saimaa (g–i) in the reference period (blue) and in 2010–2039 (left), 2040–2069 (middle) and 2070–2099 (right). The results are with unmodified regulations and 12 GCM climate scenarios (red /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 62. i-frame services

  i-frame services i-frame services Other web-sites can be configured to display information automatically from vedur.is /about-imo/the-web/iframes/

• 63. Cradden_Lucy_CES_2010

  2050s 2080s C h a n g e i n r a t i n g ( % ) 10% 50% 90% C h a n g e i n r a t i n g ( % ) C h a n g e i n r a t i n g ( % ) Each bar shows range over whole UK spatial area June 2010 13 Is the impact similar over the whole UK? • Changes in the summer minimum rating, i.e. worst-case conditions – max temperature: Rating at baseline period 1961 /media/ces/Cradden_Lucy_CES_2010.pdf

• 64. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf

• 65. Bardarbunga_kafli20140825

  frequency during the last 1100 years is 1 eruption per 50 years on average. Eruptions on the ice covered part of the system have the potential to cause major floods in several rivers flowing southwards and northwards from the Vatnajökull ice cap. _________________________________________________________________________ Central volcano: Bárðarbunga Lat, lon: 68°38´N, 17°31´W Elevation: 2009 /media/jar/Bardarbunga_kafli20140825.pdf

• 66. VI_2009_012

    Acknowledgements ................................................................................................................ 32  References .............................................................................................................................. 32  I Appendix – the local moment magnitude ............................................................................ 34  II /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 67. isskyrsla_14122010

  Hafísskýrsla TF-SIF 14. desember 2010 Flug nr. 17610.025 Óformleg ískönnun 14. desember 2010 Óformleg ískönnun var gerð og kom eftirfarandi í ljós. Ísröndin samkvæmt ratsjá TF-SIF 1) 68 03.0N 17 19.0W 2) 67 41.0N 18 19.0W 3) 67 36.0N 19 09.0W 4) 67 21.0N 19 43.0W 5) 66 53.0N 20 21.0W 6) 66 45.0N 19 58.0W 7) 66 38.0N 20 42.0W 8) 67 02.0N 21 /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf

• 68. norsem_mantyniemi

  Macroseismology in Finland from the 1730s to the 2000s: From an obligation of the learned elite to citizen science Päivi Mäntyniemi Institute of Seismology, Department of Geosciences and Geography, P.O. Box 68, FI-00014 University of Helsinki, Finland, e-mail: paivi.mantyniemi@helsinki.fi The presentation is based on a snapshot of macroseismology in Finland from the 1730s to the 2000s that has /media/norsem/norsem_mantyniemi.pdf

• 69. Dyrrdal_Anita_CES_2010

  Permanent snow cover Snow depth Aug Jun Maximum snow depth Accumulative winter precipitation Number of snow days (snow depth > 0) Snow season duration Introduction Data & Methods Results Norwegian Meteorological Institute met.no Simulated temperature & precipitation Observed snow depth Time series • Period I: 1931-60 – 55 stations • Period II: 1961-90 – 298 stations • Period III: 1979 /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 70. Kok_JGEC658_2009

  Change 19 (2009) 122–133 A R T I C L E I N F O Article history: Received 14 November 2007 Received in revised form 21 August 2008 Accepted 25 August 2008 Keywords: Fuzzy Cognitive Maps Scenario Participation Resilience Brazil A B S T R A C T The main drawback of the Story-and-Simulation approach is the weak link between qualitative and quantitative scenarios. A semi-quantitative tool, Fuzzy /media/loftslag/Kok_JGEC658_2009.pdf