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  • 41. VI_2009_012

    Appendix – near-field constraint ........................................................................................ 35  III Appendix – PGV and PGA versus distance for all events ................................................. 36  List of figures Figure 1. Map of SW Iceland showing the epicenters of 46 earthquakes used in the study.. 10  Figure 2. CMT-moment magnitude estimates vs /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 42. VI_2022_006_extreme

    towards the northern part of Vatnajökull. Table 8 – Median 1M5 values (mm 24-h-1) for eleven hydropower catchments with and without climate projections for the period 2080 – 2100. Catchment 1M5 median value mm 24-h-1 Original RCP 2.6 RCP 8.5 10% 50% 90% 10% 50% 90% Blönduvirkjun 48 41 49 58 42 50 61 Búðarháls 46 40 47 56 40 48 59 Hágöngulón 63 55 65 76 55 66 81 Hálslón 85 75 88 104 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
  • 43. aerodrome_summaries_20140603

    M (171FT ) FRE Q UENCIE S (PE R CENT ) O F OCCU R RENC E O F CONCURREN T WIN D DIRECTIO N (I N 30 0 SEC T ORS ) AN D SPEE D (I N KN O TS ) WITHI N SPECIFIE D RANGE S ANN U A L WIN D WIN D SPEE D (KT) ) DIRECTIO N CAL M 1– 5 6–1 0 11–1 5 16–2 0 21–2 5 26–3 0 31–3 5 36–4 0 41–4 5 46–5 0 >5 0 T O T A L V ARIABL E 0 0 0 0 0 0 0 0 0 0 0 0 0 35-36-0 1 3 2 3 3 2 1 1 0 0 0 0 0 14 02-03-0 4 0 2 4 4 3 1 0 0 /media/vedur/aerodrome_summaries_20140603.pdf
  • 44. FMI_-_Disaster_Mitigation

    Construction • Using the same method we can estimate what the reduction in damages would have been if the best construction practices were in place in all homes. • Potential damage reduction, based on this method, would have been as much as $46 million or 25% less than the permit value of $182 million Potential Economic Impact of Better Construction • Another useful comparison is to look /media/loftslag/FMI_-_Disaster_Mitigation.pdf
  • 45. CES_D2.4_solar_CMIP3

    regional temperature and precipitation change estimates for Europe under four SRES scenarios applying a super-ensemble pattern-scaling method. Clim. Change, 81, 193-208. 7 Räisänen, J. and K. Ruosteenoja, 2008: Probabilistic forecasts of temperature and pre- cipitation change based on global climate model simulations. CES deliverable 2.2, 46 pp. Available from http://www.atm.helsinki.fi /media/ces/CES_D2.4_solar_CMIP3.pdf
  • 46. BIAR_windrose_2005-2014

    speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 33 0 14 7 7 9 4 5 2 2 2 2 2 7 3 5 2 3 4 0 2 9 4 0 7 1 12 1 20 8 32 3 35 3 46 0 64 2 58 2 27 8 15 7 9 3 5 1 3 4 2 9 1 7 3 2 3 1 8 3 14 4 25 0 24 6 34 3 52 1 44 1 Wind rose BIAR October 2005−2014 90 80 70 60 50 40 30 2010360350340 /media/vedur/BIAR_windrose_2005-2014.pdf
  • 47. BIEG_windrose_2005-2014

    of wind direction (%) Aerodrome Total observations: 6845 Calm: 17% Variable winds: 3.6% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 40 9 60 0 29 8 14 6 6 1 5 6 4 3 6 2 8 6 3 6 2 0 3 0 1 8 2 9 11 2 12 9 15 3 36 7 33 7 44 8 46 /media/vedur/BIEG_windrose_2005-2014.pdf
  • 48. BIRK_windrose_2005-2014

    16 3 9 0 5 3 4 7 6 7 13 5 17 7 22 9 21 8 24 8 33 6 26 1 29 0 21 1 16 3 17 6 15 8 17 6 20 8 18 3 16 2 12 5 16 5 14 0 21 0 20 6 25 1 46 9 37 5 17 0 19 4 23 1 19 5 22 2 Wind rose BIRK August 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 Frequency of wind direction (%) Aerodrome Total /media/vedur/BIRK_windrose_2005-2014.pdf
  • 49. 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
  • 50. Paper-Olafur-Rognvaldsson_92

    been used to downscale over Iceland the 6-hourly analysis of the ECMWF over a pe- riod of 46 years. A systematic comparison with observed precipitation for the sub-period 1987–2003 has been presented as well as comparison of simulated discharge with observed discharge. The main results are: Table 1: Comparison of observed and simulated discharge [m3s−1] at six discharge stations using unscaled /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

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