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  • 61. norsem_mantyniemi

    of Finland, the Seismological station of the University of Helsinki, the Sodankylä Geophysical Observatory of the Finnish Academy of Science and Letters, and the Department of Physics of the University of Oulu. The later generations belonged to the Institute of Seismology, University of Helsinki. At the turn of the 2000s the questionnaire was placed on the Internet /media/norsem/norsem_mantyniemi.pdf
  • 62. Group1-Adaptive_Management_in_a_relation_to_climate_change2

    -Community training Low taxation Scenario building Risk Perception Socio Economic Development H ig h Lo w Scenario 1 Scenario 2 Present time 2030 2020 Scenario 1 Scenario 1opt. Flood Warning System • The operator, based on analysis of the received weather data and other information from the Internet makes the decision whether to warn inhabitants • A computer /media/loftslag/Group1-Adaptive_Management_in_a_relation_to_climate_change2.pdf
  • 63. Refsgaard_1-Welcome

    – Print yourselves • Case descriptions and tasks/questions • Lecturers’ presentations – Handouts during the week – Pdfs will be uploaded at website afterwards Practicalities • PC login – Internet access • Printing • Lunch • Coffee – tea • Posters Monday afternoon + refreshments • Dinner Tuesday at 19:00 Students • Brief presentation round – now • 2-minutes presentation of research topics /media/loftslag/Refsgaard_1-Welcome.pdf
  • 64. IMO receives Special Achievement Award for Exceptional Application of Geospatial

    to improve our world," says Esri president Jack Dangermond. "Each year I look forward to being part of this ceremony. It is a tradition that means a great deal to Esri and to GIS professionals." More information is available about the 2011 Special Achievement in GIS Award winners, including project information and photos. There, examples of IMO's work can be seen /about-imo/news/nr/2241
  • 65. norsem_atakan_ip

    and sustainable society. The main vision of the European Plate Observing System (EPOS) is to address the three basic challenges in Earth Sciences: (i) unravelling the Earth's deformational processes which are part of the Earth system evolution in time, (ii) understanding the geo-hazards and their implications to society, and (iii) contributing to the safe and sustainable use of geo-resources /media/norsem/norsem_atakan_ip.pdf
  • 66. PhD_course-Programme_26Aug2011-final

    /j.jenvman.2007.05.009 Huntjens P, Pahl-Wostl C, Grin J (2010) Climate change adaptation in European river basins. Reg. Environ. Change, 10, 263-284. DOI 10.1007/s10113-009-0108- 6 IPCC (2007) Climate Change 2007: Synthesis Report. Contribution of Working Groups I, II and III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. IPCC, Geneva, Switzerland, 104 pp /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
  • 67. CES_D2.4_task1

    1 Probability distributions of monthly-to-annual mean temperature and precipitation in a changing climate (CES Climate Modelling and Scenarios Deliverable D2.4, task I) Jouni Räisänen Department of Physics, P.O. Box 48, FI-00014 University of Helsinki, Finland Email: jouni.raisanen@helsinki.fi 17 November 2009 AVAILABLE FROM: http://www.atm.helsinki.fi/~jaraisan/CES_D2.4 /media/ces/CES_D2.4_task1.pdf
  • 68. Crochet_Philippe_CES_2010

    ≤   ≤ >− 0 00 0 )( TTif TTifTTDDFsnow   ≤ >− 0 00 0 )( TTif TTifTTDDFice Mean annual temperature difference Difference relative to 1971-2000 Difference between 25% warmest and 25% coldest years barb2right +1°C (25% warmest) barb2right -0.7°C (25% coldest) barb2right +1.7°C Catchment elevation (m.a.s.l) Catchment elevation (m.a.s.l) s n o w m e l t ( m m / d ) g l a c i a l m e l t /media/ces/Crochet_Philippe_CES_2010.pdf
  • 69. VI_2020_011_en

    of lava erupted and the duration of the eruption. Instantaneous measurements of lava flow rates are much higher than these averages, for example during the 1973 Eldfell eruption, lava flow rates of 5.3–99.4 m3/s were measured at different times during the eruption (Williams & Moore, 1976) 4 Surtur II lava shield 5 Surtur I lava shield 19 Figure 4: Isopach lines of the cumulative /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 70. Climate and Modeling Scenarios

    -Skaugen, T., Haugen, J.E., & Hanssen-Bauer, I. (2008). Dynamically downscaled climate scenarios available at the Norwegian Meteorological Institute - per December 2008, met.no report 24/2008. Gregow, H. & Ruosteenoja, K. (2010). Estimating the effect of climate change on surface geostrophic winds in Northern Europe (CES Climate Modelling and Scenarios Deliverable D2.4). Finnish Meteorological /ces/publications/nr/1680

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