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  • 1. Linnet_Ulfar_CES_2010

    °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 2. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

    /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
  • 3. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

    296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf
  • 4. IMO_AnnualReport2014

    of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
  • 5. 2005EO260001

    level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf
  • 6. Paper-Olafur-Rognvaldsson_92

    a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf
  • 7. Refsgaard_1-Welcome

    Organisers NONAM •Finnish Meteorological Institute, FMI (Adriaan Perrels) •Geological Survey of Denmark and Greenland, GEUS (Jens Christian Refsgaard and Hans Jørgen Henriksen) •Icelandic Meteorological Office, IMO (Sigrún Karlsdóttir) FIVA - International Research School of Water Resources •University of Copenhagen, KU (Frederik Uldall) Course objectives • To introduce students to the concept /media/loftslag/Refsgaard_1-Welcome.pdf
  • 8. VI_2014_005

    in an overall cold bias, compared with station measurements. To test, whether this is due to the HARMONIE model core or the external surface scheme, biases of 2-m temperature from SURFEX are com- pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is found that the negative temperature biases are due to shallow inversion layers near the ground, which are introduced /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 9. GA_2009_91A_4_Andreassen

    the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 10. Keranen_Jaana_CES_2010

    ilmiö W inter Sprin g SummerA utumn Kosteus Lauha t talve t Talvitulvat Jäätävä sade Hyyde Kova tuu li … Aikaisempi kevät ja tu lvat Ku ivuus Ku ivuvat vesiva rastot … Ku ivuus Rankkasa teet sa lamointi Rakeet … Myrskyt Rankkasateet Rou ta Jääkannen muodostaminen … yli y €yli y €Merkittävät3 x - y €x – y €Keskinkertaiset2 alle x €alle x €Vähäiset1 Mahdollisuuden tunnisteväriRiskin /media/ces/Keranen_Jaana_CES_2010.pdf

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