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32 results were found for 구로룰렛(trrt2¸com)ଐ금천카지노實금천포커㗧금천슬롯噁금천블랙잭🧍🏼‍♀️braindrain/.


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  • 21. VI_2015_005

    mean surface air temperature anomalies ....................................... 28 14 Surface air temperature anomalies over Scandinavia ...................................... 29 15 Composite mean precipitation anomalies..................................................... 30 6 1 Introduction Extratropical low-pressure systems, persisting for at least a few days, have long been recognised as one /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 22. VI_2015_009

    and review of some methods for regional flood frequency anal- ysis. J. Hydrol., 186, 63–84. GREHYS. (1996b). Inter-comparison of regional flood frequency procedures for Canadian rivers. J. Hydrol., 186, 85–103. Grover, P.L., Burn, D.H. & Cunderlik, J.M. (2002). A comparison of index flood estimation procedures for ungauged catchments. Can. J. Civ. Eng., 29, 734–741. Hosking, J.R.M. & Wallis, J.R. (1993 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 23. Hare-2011-ParticipatoryModelling

    ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 24. Kok_JGEC658_2009

    it will be one of the main aspects of this paper. 2.3. Properties The elements of a Fuzzy Cognitive Map are as follows:  Concepts: C1, C2, . . ., Cn. These represent the drivers and constraints that are considered of importance to the issue under consideration.  State vector: A = (a1, a2, . . ., an), where ai denotes the state of the node Ci. The state vector represents the value of the concepts /media/loftslag/Kok_JGEC658_2009.pdf
  • 25. Lorenzoni_Pidgeon_2006

    level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 26. Reykholt-abstracts

    for ice, ocean and land applications Snævarr Guðmundsson, Hrafnhildur Hannesdóttir and Helgi Björnsson ....................... 15 Post-Little Ice Age (1891–2011 AD) volume loss of Kotárjökull glacier, southeastern Iceland, as established from historical photograph and lidar Sverrir Guðmundsson, Eyjólfur Magnússon, Helgi Björnsson, Finnur Pálsson, Tómas Jóhannesson and Etienne Berthier /media/vatnafar/joklar/Reykholt-abstracts.pdf
  • 27. VI_2016_006_rs

    ................................................................. 25 6 Analog hazard situations in the Alps and implemented or planned mitigation measures..................................................................................................... 29 6.1 Kerschbaumsettlement/Navis.................................................................... 29 6.2 Gschliefgraben /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
  • 28. VI_2019_009

    22,70,71 72 72,73 25 24,56,66 73 74,75 30 12,28 81 80 51 50,51 85 85 52 52,52 87 86 53 54,55 Figure 13 shows the frequency of present weather records from both manual and automatic sta- tions. Both stations show no weather, 0, most frequently, the automatic station in 1019 cases and the manual station in 1031 cases. In figure 14 the most frequent records (no weather) have been removed. The automatic /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 29. 2013_001_Nawri_et_al

    . . . . . . . . . . . 56 27 Directional mean wind power density within the Langanes region . . . . . . . . . . 57 28 Seasonal mean wind power density within the Langanes region . . . . . . . . . . . 58 29 Directional mean wind power density within the Meðallandssveit region . . . . . . 59 30 Seasonal mean wind power density within the Meðallandssveit region . . . . . . . 60 31 Directional mean /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 30. VI_2020_004

    49 Probabilistic hazard map for a load ≥1000 kg/m2 (Öræfajökull) ............................ 78 Figure 50 Seasonal analysis for 1 kg/m2 (~1mm) tephra ground load (Öræfajökull). ............ 79 Figure 51 Seasonal analysis for 10 kg/m2 (~1 cm) tephra ground load (Öræfajökull). ........... 80 Figure 52 Impact map for roads in case of an eruption like 1362 at Öræfajökull ................... 81 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

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