51 results were found for 【┋添加扣46⒋1⒍85〓】杏彩登录3.

Results:

• 21. 2013_001_Nawri_et_al

  Office Halldór Björnsson, Icelandic Met Office Kristján Jónasson, University of Iceland 4 Contents 1 Introduction 9 2 Spatial and temporal variability of low-level wind 11 3 Methodology 13 3.1 Wind modelling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 3.2 Weibull statistics . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 3.3 Density /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 22. VI_2014_001

  ....................................................................................... 46 Appendix XI - Empirical and modeled instantaneous flood frequency distribu- tions for Region 1 derived with index flood model no. 6: bµ(D) = a(AP=Z)b ............ 47 Appendix XII - Empirical and modeled instantaneous flood frequency distribu- tions for Region 2 derived with index flood model no. 3: bµ(D) = a(APm)b ............. 49 6 1 Introduction /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 23. BITN_windrose_2005-2014

  (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 24 2 31 5 30 4 33 9 31 8 32 2 24 3 20 2 26 2 25 4 17 9 25 0 24 9 23 3 29 3 21 0 10 3 21 4 18 9 33 2 46 0 25 2 29 3 28 0 16 2 6 6 14 8 10 0 12 8 23 4 20 1 24 5 27 0 23 8 17 1 35 8 Wind rose BITN January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 /media/vedur/BITN_windrose_2005-2014.pdf

• 24. 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

• 25. Group2-report

  1    Adaptive management to climate change in Horsens Fjord using scenario  development    Report by Maria, Azhar, Bjarke and Kerstin  Introduction  Horsens Fjord is an eutrophic estuary situated in east coast of Jutland, Denmark with approximately 46 km2  surface area. The Fjord is a part of bigger WFD catchments area with dominated agriculture area and small  forest, wetlands, lakes, and urban /media/loftslag/Group2-report.pdf

• 26. VI_2020_004

  (Hekla) ............ 48 Figure 23 Seasonal analysis for tephra probability exceeding 1 kg/m2 (Hekla) ...................... 49 Figure 24 Seasonal analysis for tephra probability exceeding 10 kg/m2 (Hekla) .................... 50 Figure 25 Probabilistic hazard maps for a load ≥3 kg/m2 (Hekla). ........................................ 51 Figure 26 Probabilistic hazard maps for a load ≥1 kg/m2 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 27. VI_2015_007

  maximum flow. For time periods, see Table 1. 10 3 Index flood method 3.1 General principle The method has already been described in detail in Crochet (2012a,b) and Crochet & Þórarins- dóttir (2014) and so is only summarised here. The index flood method (IFM), proposed by Dalrymple (1960) can be used to estimate the T -year flood quantile at ungauged locations or at gauged sites with short records /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 28. Group-1_Scenarios-for-AWM

  Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011) 1 / 3 Scenarios for Adaptive Flood Management in Horsens Fjord, Denmark Bakhtiyor Pulatov1, Hector Guinea2 and Hongxiao Jin1 1. Lund University 2. Uppsala University Introduction (HJ) Horsens Fjord is a Danish fjord located on the east coast of Jutland. It is a shallow and eutrophic /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 29. Observations - Hallormsstaður

  Observations - Hallormsstaður | Observations | Icelandic Meteorological office Observations - Hallormsstaður Mon 1.05 14 GMT 2.4° NNE 3 Max wind : 3 / 5Precip.: 0.0 mm / 1 h 13 GMT 3.6° NW 2 Max wind : 3 / 4Precip.: 0.0 mm / 1 h 12 GMT 3.0° NW 3 Max wind : 3 / 4Precip.: 0.0 mm / 1 h 11 GMT 2.5° SW /m/observations/areas

• 30. Kok_et_al._TFSC_published_2011

  the achievement of long-term futures to series of short-term actions. In broad outlines, the methodology was similar to other projects that use participatory scenario development methods. For example, Quist and Vergragt [18] describe ve steps that effectively capture the overall methodology of the SCENES project as well: 1. Problem orientation; 2. Development of exploratory scenarios; 3 /media/loftslag/Kok_et_al._TFSC_published_2011.pdf