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  • 41. Eyjafjallajökull eruption 2010 - the role of IMO

    of the volcanic behaviour, plume activity and interaction between plume and weather. For further information, a slide show from a lecture on the subject (pdf 1.4 Mb) is available. Also, other articles on the Eyjafjallajökull eruption 2010 can be read on our web-site as well as the then current news on the subject. Reference * Vogfjörð K., Jakobsdóttir S.S., Guðmundsson G.B., Roberts M.J., Ágústsson K /earthquakes-and-volcanism/articles/nr/2072
  • 42. Gudmundsson-etal-2011-PR-7282-26519-1-PB

    Reykjavı´k IS-101, Iceland 2 Centre National de la Recherche Scientifique, Universite´ de Toulouse, Laboratoire d’Etudes en Ge´ophysique et Oce´anographie Spatiale, Universite´ de Toulouse, 14 Avenue Edouard Belin, Toulouse FR-31400, France 3 National Space Institute, Technical University of Denmark, Lyngby DK-2800, Denmark Keywords Remote sensing; glacier mass balance; regional warming /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
  • 43. VI_2020_004

  • 44. Tony_Rosqvist_(VTT,_Fin)

    Literature: [1] Perrels, A., Veijalainen, N., Jylhä, K., Aaltonen, J., Molarius, R., Porthin, M., Silander, J., Rosqvist, T., Tuovinen, T. (2010), The Implications of Climate Change for Extreme Weather Events and their Socio-economic Consequences in Finland, VATT Research report 158 [2] Riitta Molarius, Adriaan Perrels, Markus Porthin, Tony Rosqvist (2008), Testing a Flood Protection /media/loftslag/Tony_Rosqvist_(VTT,_Fin).pdf
  • 45. Burnett_Dougal_CES_2010

    of Solar Irradiation • Weather stations use pyranometers and pyrheliometers • Campbell-Stokes Recorder - measures sunshine duration UK Solar Resource present and future index clearnesssky clear averagemonthly index clearnessdaily averagemonthly sun block the cloudst significan nothat fraction time where = = = clear clear K K f2     = clear clear K Kf Conversion /media/ces/Burnett_Dougal_CES_2010.pdf
  • 46. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

    ORIGINAL ARTICLE The role of uncertainty in climate change adaptation strategies—A Danish water management example J. C. Refsgaard & K. Arnbjerg-Nielsen & M. Drews & K. Halsnæs & E. Jeppesen & H. Madsen & A. Markandya & J. E. Olesen & J. R. Porter & J. H. Christensen Received: 10 November 2011 /Accepted: 4 February 2012 # The Author(s) 2012. This article is published with open access /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
  • 47. vanRoosmalen_etal-2009-WRR_2007WR006760

    such as irrigation, CO2 effects on transpiration, and land use changes affect the water balance to a lesser extent. Citation: van Roosmalen, L., T. O. Sonnenborg, and K. H. Jensen (2009), Impact of climate and land use change on the hydrology of a large-scale agricultural catchment, Water Resour. Res., 45, W00A15, doi:10.1029/2007WR006760. 1. Introduction [2] The most recent Intergovernmental Panel /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 48. CES_D2.4_solar_CMIP3

    and sunnier climate in the south, a wetter and darker climate in the north. Accordingly, changes in the conditions of solar and hydropower energy pro- duction are compensatory. At present, of course, the rôle of solar energy is negligible compared to hydropower production, but the status may alter in the future. REFERENCES Jylhä K., Ruosteenoja K., Räisänen J., Venäläinen A., Tuomenvirta H /media/ces/CES_D2.4_solar_CMIP3.pdf
  • 49. Refsgaard_etal-2007-Uncertainty-EMS

    and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 50. 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

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