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72 results were found for m 발산주점⅓(dm080.com”❇발산휴게텔♭발산건마✮발산업소♙발산주점 발산건마.


Results:

  • 11. Laboratory experiments

    of snow avalanches agains dams and retarding obstacles: A laboratory study of the interaction between supercritical, shallow flows and dams (IMO Int. Rep. 03038, 2003, authors K. M. Hákonardóttir, A. Hogg and T. Jóhannesson) (pdf 1.3 Mb) Avalanche braking mound experiments with snow. Switzerland − March 2002 (IMO Int. Rep. 03023, 2003, authors K. M. Hákonardóttir, T. Jóhannesson, F /avalanches/imo/lab/
  • 12. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

    & Ostrom, E. (2008). Will lessons from small-scale social dilemmas scale up? In A. Biel, D. Eek, T. Gärling, & M. Gustaffson (Eds.), New issues and paradigms in research on social dilemmas (pp. 189–211). Berlin: Springer. Netting, R. McC. (1981). Balancing on an alp: ecological change and continuity in a Swiss mountain com- munity. New York: Cambridge University Press. Olson, M. (1965). The logic /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf
  • 13. 2013_001_Nawri_et_al

    values. For Part 2, data files describing the local wind statistics on the regular model grid covering Iceland are made available through an online wind atlas (follow the link from http://www.vedur.is/vedur/vedurfar/vindorka/). The files contain estimates of Weibull parameters at each grid point, for twelve wind direction sectors, five heights (10, 25, 50, 100, 200 m above ground level (mAGL /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 14. VI_2020_005

    coast, wind forcing is the primary driver of sea level extremes but less so for the Kattegat/Skagerak region than for the Baltic (M. Hieronymus, J. Hieronymus, and Arneborg, 2017). Like in Norway, atmospheric pressure is the most influential contributor to mean sea level changes on timescales up to a few years in the UK but steric changes dominate on decadal timescales (Dangendorf, Calafat, et al /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 15. VI_2009_006_tt

    the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average propagation speed of the subglacial jökulhlaup flood front was found to be in the range 0.2–0.4 m s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 16. Warning due to gale winds and heavy precipitation

    Warning due to gale winds and heavy precipitation 20.7.2012 Saturday afternoon and evening, 21st July, strong southeast- and easterly winds are expected in the southern and western parts of Iceland with heavy rain. Mean wind speed will be 13 to 20 m/s and occasional /about-imo/news/nr/2501
  • 17. Machguth_Horst_CES_2010

    experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf
  • 18. IPPC-2007-ar4_syr

    of different country groupings in 2004. The percentages in the bars in both panels indicate a region’s share in global GHG emissions. {WGIII Figures SPM.3a, SPM.3b} Regional distribution of GHG emissions by population and by GDPPPP and M&Tand M& T sectoral sources of GHGs in 2004 are considered in Figure 2.1c. {WGIII 1.3, SPM} The effect on global emissions of the decrease in global energy intensity /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 19. 2015-03-12_vatnsvedurogstormar_en

    weather forecast: Two low pressure systems are forecast to reach Iceland during the period from Friday morning until Saturday evening. The forecast is for southeast 20-25 m/s, (strong gale to storm) tomorrow, Friday, but south 25-30 m/s (storm to violent storm) on Saturday. A heavy rainfall warning has also been issued for these lows.. Travel conditions will be poor in the south and west /media/frettir/myndasafn/2015/2015-03-12_vatnsvedurogstormar_en.pdf
  • 20. Wind, temperature, precipitation forecasts

    : Vindur í 10m hæð = Wind at 10 m height (m/s) Hiti í 2m hæð = Temperature at 2 m height (°C) 3ja tíma úrkoma, vindur í 10 m hæð og loftþrýstingur = 3 hrs percipitation (mm), wind at 10 m hight (m/s) and sea surface pressure (hPa) See also Instructions /weather/forecasts/elements

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