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  • 11. VI_2014_005

    ..................................................... 29 21 Monthly mean 10-m wind speed for different wind directions over Þórisvatn ...... 30 6 1 Introduction In the spring of 2013, the Icelandic Meteorological Office (IMO) started a reanalysis project, using the HARMONIE numerical weather prediction model. Operationally, this model has been in use at IMO since the autumn of 2011, and has proven /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 12. vanRoosmalen_etal-2009-WRR_2007WR006760

    with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 13. Journal_of_Hydrology_Veijalainen_etal

    ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 14. 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
  • 15. 2010_005_

    GCM simulations of mean annual surface air temperature: mean fields in degrees centigrade during the 1961–90 control period, differences in degrees between the control period and the 2021– 50 reference period, and linear trends in degrees per decade within the 2004–50 period, for the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . 30 9 Mean annual total precipitation in millimetres per /media/ces/2010_005_.pdf
  • 16. VI_2020_005

    measurements are still performed with newer instruments today, making it the worlds longest sea level data series (SMHI, 2018b). Today, The Swedish Meteorological and Hydrological Institude (SMHI) runs a network of 24 tide gauges that measure sea level averaged over 10 minute periods in a relative elevation system. The data is gathered every hour and presented online2 within 30 minutes, relative /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 17. 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
  • 18. Adalgeirsdottir-etal-tc-5-961-2011

    of the glacier is projected to be reduced by 30 % with respect to the present at the end of this century. If the climate warms, as suggested by most of the climate change scenarios, the model projects this glacier to almost disappear by the end of the 21st century. Runoff from the glacier is predicted to increase for the next 30–40 yr and decrease after that as a consequence of the diminishing ice-covered area /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
  • 19. Reykholt-abstracts

    H. Haraldsson and Tómas Jóhannesson .............................................................................. 29 The mass balance of Brúarjökull, outlet of N-Vatnajökull Ice cap Iceland, in the 20th and 21st century Chris Polashenski ................................................................................................................... 30 Applications of terrestrial lidar /media/vatnafar/joklar/Reykholt-abstracts.pdf
  • 20. Hare-2011-ParticipatoryModelling

    Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

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