74 results were found for m 공항동출장Τ〈dm080.com”✰공항동아로마▼공항동마사지 공항동휴게텔 공항동업소 공항동키스방.

Results:

• 11. 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

• 12. 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/

• 13. 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

• 14. 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

• 15. 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

• 16. 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

• 17. 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

• 18. 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

• 19. Reykholt-abstracts

  ................................................................................................................... 8 Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9 Lidar measurements of Norwegian glaciers – an overview Neil Arnold* and Gareth Rees .............................................................................................. 10 Calculation of glacier velocity from repeat /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 20. 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