35 results were found for 킹덤홀덤〔trrt2-com〕 킹덤홀덤모바일 타임바카라‡타짜슬롯⑭타짜홀덤 RTh/.

Results:

• 31. VI_2019_009

  the automatic station shows 0 the manual station shows 15 (precipitation is more than 5 km distance) in 20 cases. In 22 cases the manual station shows 21 62 (Rain, not freezing, intermittent, moderate at time of observation) while the automatic station shows 61 (light rain). 0 250 500 750 1000 0 1 2 3 10 11 15 16 20 21 23 24 25 26 40 41 50 51 52 53 58 60 61 62 63 64 67 70 71 72 73 80 81 83 84 85 Present /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 32. 2013_001_Nawri_et_al

  the Fljótsdalsheiði region . . . . . . . 47 18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48 19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49 20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50 21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51 22 Seasonal mean /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 33. VI_2020_004

  Figure 53 Impact map for airports in case of an eruption like 1362 at Öræfajökull ................ 82 Figure 54 Impact map for power lines in case of an eruption like 1362 at Öræfajökull ......... 83 Figure 55 5% PM10 probability map for an eruption like 1362 at Öræfajökull. ...................... 84 Figure 56 25% PM10 probability map for an eruption like 1362 at Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 34. VI_2013_008

  Forecast skill evaluation over the period 01/09/2001–31/08/2005. No rescaling (Eqs. 6 and 10). All units are in m3=s Forecast range T=1 day T=2 days T=3 days Statistics ME RMSE Q95–Q5 ME RMSE Q95–Q5 ME RMSE Q95–Q5 vhm 64 – method 1 –20 103 302 –19 99 297 –20 103 298 vhm 64 – method 2 –11 44 132 –15 64 162 –18 87 201 vhm 64 – method 3 –24 64 206 –24 72 221 –25 87 241 vhm 64 – method 4 –16 47 132 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 35. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf