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  • 21. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

    uncertainties. Climate change impacts and adaptation also influence a wide range of stakeholders with different interests, E. Jeppesen Aarhus University, Vejlsøvej 25, DK-8600 Silkeborg, Denmark e-mail: ej@dmu.dk H. Madsen DHI, Agern Alle 5, DK-2970 Hørsholm, Denmark e-mail: hem@dhigroup.com A. Markandya BC3 Basque Centre for Climate Change, E- 48008 Bilbao, Spain e-mail: anil.markandya@bc3research.org /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
  • 22. CES_D2.4_VMGO

    the territories of European Russia (ER) and Europe (EU) an ensemble of 9 CMIP3 [1] comprehensive global (coupled atmosphere-ocean) climate models is used in this assessment (Table 1); so called A2 scenario is considered. Both A2 and A1B scenarios are similar in terms of resulting global mean warming up to the mid-21st century IPCC [2]. The projected changes in ER and EU in many cases continue /media/ces/CES_D2.4_VMGO.pdf
  • 23. IM_flyer

    Climate and Energy Systems, 2007-2010. Information Management http://www.os.is/ces The Information management group is responsible for information dissemination, active stakeholder involvement and the public outreach. At the national level, CES-national groups will be established to secure national collaboration between the activities. All participants in the CES project have access /media/ces/IM_flyer.pdf
  • 24. ces-oslo2010_proceedings

    change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf
  • 25. Traffc-maintenance_expenditures

    229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf
  • 26. VI_2022_006_extreme

    weather. This is further illustrated by Table 5, where monthly temperature changes were calculated for each catchment based on the ICRA. January is the month with the largest increase (aroundC in all the catchments), although this is also the month with the highest amount of snow, thus the snow-fraction decrease is less significant than for November. 22 Figure 11 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
  • 27. VI_2020_008

    by the Peak-over-Threshold with MLE applied on daily and 24-hour accumulated precipitation from the ICRA. ............................... 58 8 Glossary 1M5 – Daily or 24-hour precipitation return level with a 5-year return period AMSAnnual Maxima Series CCCloseness Coefficient CDOClimate Data Operator EVA – Extreme Value Analysis GP – Generalized Pareto ICRA – Icelandic /media/vedurstofan-utgafa-2020/VI_2020_008.pdf
  • 28. NOMEK09_Report

    In addition a new lecture about forecast errors, analysis and observations was added to the schedule. In order to provide experience from the avalanche field at IMO a geophysicist and specialist in snow avalanches was included as one of the teachers giving an interesting presentation on avalanches. Participants It was agreed that participants would be accepted to the course as follows /media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf
  • 29. The segmented dyke intrusion explained

    to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038
  • 30. IMO's Organisational Chart

    The division is responsible for the day-to-day operations of the organization, e.g., record management, central service desk, real estate management, procurement management and other internal support services. CentresThe centre for Climate Services and Adaptation is a platform that services urgent projects in the field of adaptation because of climate change. The centre provides climate /about-imo/imos-organisational-chart/

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