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Results:

• 61. Gode_Jenny_CES_2010

  Projects involving sh Concise info Executive summaries Downloadable "Stakeholder friendly" info Stakeholder Relevance of the CES Project Jenny Gode, 31 May 2010 Research programme "Translators" F act sheets W eb page Stee ring co m m ittee Visits W o rkshops R efe re nce g ro up s E x . su m m a rie s M eetings Stakeholders Energy companies Energy authorities Decision makers Other stakeholders /media/ces/Gode_Jenny_CES_2010.pdf

• 62. norsem_korja

  of earthquakes. Reference: [1] Korja, A. and Kosonen, E. M. (eds.) 2015. Seismotectonic framework and seismic source area models in Fennoscandia, Northern Europe. Univ. Helsinki, Instit. Seismology, Report S-63, 284 p. http://www.seismo.helsinki.fi/pdf/Seismotectonic_S63_Korja_Kosonen.pdf [2] Nørbech, T., Engsager, K., Jivall, L., Knudsen, O., Koivula, H., Lidberg, M., Ollikainen, M. & Weber, M., 2008 /media/norsem/norsem_korja.pdf

• 63. Water_resources_man_Veijalainen_etal

  Based on a report by Verta et al. (2007) 92. 5 93. 0 93. 5 94. 0 94. 5 95. 0 M A MJ F J J A S O N D Mean 19702000 Min and max 1970–2000, natural rating curve Target water level zone 1 Target water level zone 2 Q=+20% Q=+10% Q= 0% Q=15% Q=30% 92.90 m snow target 1 92.70 m snow target 2 Water level (m ) Month the regulation limits Lake Syväri has target water level zones, which are not legally /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 64. Hock_Regine_CES_2010rs

  elevation complete for Scandinavia Icelandic Inventory (data from O. Sigurdsson) Data Climate data, calibration period Monthly air temperature: ERA-40 reanalysis (0.5°×0.5°), 1958-2001 Monthly precipitation: Precipitation climatology VASClimO, 1951-2000, 0.5°×0.5° (Beck et al., 2005) Elevation-dependent mass balance data for individual glaciers Mass-balance data Future projections Glacier /media/ces/Hock_Regine_CES_2010rs.pdf

• 65. Bardarbunga-2014_August-events

  in reversed order. In combination, the monthly articles give an overview of events: August, September, October, November, December, January, February and the current update. Calendar Below is a calendar with a short-cut to each day of this month's events: August: 16-17-18-19-20-21-22-23-24-25-26-27-28-29-30-31 - on the Bárðarbunga central volcano Panoramic view towards the eruptive site /media/jar/Bardarbunga-2014_August-events.pdf

• 66. ces-oslo2010_proceedings

  ............................................................................... 20 Räisänen, J. Probability distributions of monthly-to-annual mean temperature and precipitation in a changing climate ......... 22 Nikulin, G., Kjellström, E., Hansson, U., Strandberg G. and Ullerstig A. Nordic weather extremes as simulated by the Rossby Centre Regional Climate Model: Model evaluation and future projections /media/ces/ces-oslo2010_proceedings.pdf

• 67. Paper-Olafur-Rognvaldsson_91

  -2B. Mon. Wea. Rev., 132, 2184– 2203. Dickinson, R. E., Errico R. M., Giorgi F. and Bates G. T. 1989. A regional cli- mate model for the western United States. Clim. Change, 15, 383–422. Giorgi, F. 1990. On the simulation of regional climate using a limited area model nested in a general circulation model. J. Climate, 3, 941–963. Giorgi, F., and Mearns L. O. 1999. Introduction to special section /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 68. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 69. Case_A___Horsens_Fjord

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/Case_A___Horsens_Fjord.pdf

• 70. Horsens_case

  level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Summerschool Copenhagen 22-26 August 2011 2 Physical features and ecosystem The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations /media/loftslag/Horsens_case.pdf