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  • 51. Outline_for_the_case_Road_maintenance_in_a_changing_climate

    o t o - a g e n d a D e f i n e a n d i n v i t e s t a k e h o l d e r s T e c h n i c a l i n p u t a n d v i s i o n s - I n t e r n a l e x p e r t s - s t a k e h o l d e r e x p e r t s F r am e p r o b l e m - t r p s e r v i c e ( q u a l i t y ) l e v e l s - t y p e s o f s c e n a r i o s A n a l y z e p r o b l e m T e c h n i c a l i n p u t f r /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
  • 52. Kok_and_Veldkamp_editorial_ES-2011-4160

    Copyright © 2011 by the author(s). Published here under license by the Resilience Alliance. Kok, K., and T. (A.) Veldkamp. 2011. Scale and governance: conceptual considerations and practical implications. Ecology and Society 16(2): 23. [online] URL: http://www.ecologyandsociety.org/vol16/iss2/ art23/ Guest Editorial, part of a Special Feature on Scale and Governance Scale and Governance /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
  • 53. Eyjafjallajökull eruption 2010 - the role of IMO

    (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., Arason T., Geirsson H., Karlsdóttir S., Hjaltadóttir S., Ólafsdóttir U., Thorbjarnardóttir B., Skaftadóttir T., Sturkell E., Jónasdóttir E.B /earthquakes-and-volcanism/articles/nr/2072
  • 54. Aurora and the Earth's magnetic field

    is calculated as a weighted mean of K-indices from many magnetic observatories around the world. The K-index for each observatory is calculated from the maximum variation in the horizontal field strength over 3 hours. Observations of auroral activity The National Oceanic and Atmospheric Administration of the United States (NOAA) operates several satellites on polar orbit that measure the power /weather/articles/nr/2549/
  • 55. Eyjafjallajökull eruption 2010 - the role of IMO

    * Vogfjörð K., Jakobsdóttir S.S., Guðmundsson G.B., Roberts M.J., Ágústsson K., Arason T., Geirsson H., Karlsdóttir S., Hjaltadóttir S., Ólafsdóttir U., Thorbjarnardóttir B., Skaftadóttir T., Sturkell E., Jónasdóttir E.B., Hafsteinsson G., Sveinbjörnsson H., Stefánsson R., and Jónsson T.V., 2005, Forecasting and Monitoring a Subglacial Eruption in Iceland, Eos, Vol. 86, No. 26, p. 245-252, 28 June /earthquakes-and-volcanism/articles/nr/2072/
  • 56. 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
  • 57. 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
  • 58. 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
  • 59. 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
  • 60. 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

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