56 results were found for 99贵宾汇开户(3266-409-932薇Q).adw.

Results:

• 21. VI_2009_013

  striking westwards and a group of N-S-striking pressure axis dipping 45 degrees from the horizontal and more, suggesting that extensional forces play a large role. Figure 9 includes the mechanisms of 82 out of the 99 earthquakes in total located between 17 and 26 km depth and thus shows nearly the same results as described earlier for that interval, that the tension axis is chiefly horizontal /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 22. 2013_001_Nawri_et_al

  time-series. For wind energy assessments, the main emphasis is on an accurate determination of average wind power density. As discussed in previous sections, average power density is approximately propor- tional to the mean cube of wind speed. Rescaling factors for modelled wind speed time-series, interpolated to station locations, are therefore defined here as 3 q S3o=S3m. Aside from /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 23. CES_D2.4_task2_CMIP3_winds

  changes in the September-April mean geostrophic wind speed from 1971- 2000 to 2046-2065 (left) and the statistical significance of the ensemble mean change according to a standard t test (right). Light, medium and dark red shading indicate significance at the 95%, 99% and 99.9% levels, respectively. 95 % 99 % 99,9 % 4 Fig. 4. As Fig. 3, but for the autumn (September /media/ces/CES_D2.4_task2_CMIP3_winds.pdf

• 24. VI_2015_006

  Q. J. R. Meteorol. Soc., 137, 409-422. Giesen, R. H., Andreassen, L. M., Oerlemans, J., & van den Broeke, M. R. (2014). Surface energy balance in the ablation zone of Langfjordjøkelen, an arctic, maritime glacier in northern Norway. J. Glaciol., 60(219), 57-70. Seity, Y., Brousseau, P., Malardel, S., Hello, G., Bénard, P., Bouttier, F., . . . Masson, V. (2011). The AROME-France convective-scale /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 25. Crochet_Philippe_CES_2010

  and 25% coldest years All years 1971-2000 25% coldest 25% warmest Change in number of flood events (POT) between 25% warmest and 25% coldest years POT > median Q peaks (71-00) barb2right +22% +1.7°CCatchment name POT > mean annual maximum Q (71-00) SW rain-shadow barb2right +156% barb2right -56% North rain-shadow South-SW exposedCenter North Catchment name Summary • All catchments showed signs /media/ces/Crochet_Philippe_CES_2010.pdf

• 26. VI_2009_006_tt

  max Qm Qb Vm Vm Vb (m3 s 1) (m3 s 1) (Gl) (Gl) 1968 09 110 1971 07 658 532 450 230 1973 12 238 191 151 72 1975 09 307 210 172 53 1977 08 545 390 277 134 1980 01 444 351 214 121 1981 08 472 250 360 110 1983 09 222 138 177 99 1986 07 418 275 242 102 1988 08 394 301 188 106 1990 10 129 101 129 75 1994 08 968 726 330 162 1996 08 672 521 249 147 1997 07 335 169 197 60 1998 09 292 149 323 116 2000 08 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 27. VI_2022_006_extreme

  Þingvallavatn 2 years 5 years 10 years 25 years 50 years 100 years 3 hours 12 15 18 19 21 23 6 hours 26 31 35 38 41 44 12 hours 48 56 62 67 73 77 24 hours 78 90 99 107 117 124 48 hours 113 128 138 148 159 168 26 Figure 12 – 1M5 map for catchment Hálslón based on the complete ICRA dataset. Figure 13 – 1M5 map for catchment Þingvallavatn based on the complete ICRA dataset. 27 5.2 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 28. Sigurður Th. Rögnvaldsson

  1995. Absolute and relative locations of similar events with application to microearthquakes in southern Iceland. Geophys. J. Int. 123, 409 -419. Back Related topics Instructions on using earthquake /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/

• 29. Sigurður Th. Rögnvaldsson

  1995. Absolute and relative locations of similar events with application to microearthquakes in southern Iceland. Geophys. J. Int. 123, 409 -419. Back Related topics Instructions on using earthquake /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur

• 30. Cradden_Lucy_CES_2010

  Capacity (A) F r e q u e n c y control future +0.4std dev (as % of mean) -0.68max -8.32min -1.74mean % change June 2010 15 Time series 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year of control period Seasonal average rating Calculated capacity 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year under future scenario Calculated capacity Seasonal average /media/ces/Cradden_Lucy_CES_2010.pdf