41 results were found for 首商网外推排名495455411(Q)冯...ecr7ni..fnz.

Results:

• 21. Paper-Olafur-Rognvaldsson_91

  The role of orography was found to be crucial in determining the precipitation dis- tribution and amount. Atmospheric flow over Iceland was simulated for the period January 1961 through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale model (Grell et al., 1995). The domain used is 123× 95 points, centered at 64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 22. Paper-Olafur-Rognvaldsson_92

  performance of the model. REFERENCES Førland, E. J., Allerup P., Dahlström B., Elomaa E., Jónsson T., Madsen H., Perälä J., Rissanen P., Vedin H. and Vejen F. 1996. Manual for operational cor- rection of Nordic precipitation data. DNMI Report No. 24/96 Klima, 66 pp. Benoit, R., Pellerin P., Kouwen N., Ritchie H., Donaldson N., Joe P. and Soulis E. D. 2000. Toward the use of coupled atmospheric /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 23. VI_2014_006

  properly even if the sample size is increased and systematic biases may be expected. 2.2.3 Predictors Mean sea level pressure (MSLP), geopotential height (Z), specific humidity (q) and tempera- ture (T) at different pressure levels are considered in this study to describe the meteorological situations at the synoptic scale and to identify weather analogues. The MSLP and geopotential height (Z) describe /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 24. VI_2015_005

  water. Since, in this study, the focus is on large-scale storm systems, persisting for at least one day, variability on shorter time-scales (mainly the diurnal cycle and atmospheric tides) is eliminated by calculating averages from the four 6-hourly reanalysis fields of each day (6-hourly precip- 8 Figure 1. Top: Average fields of 500 hPa geopotential height in winter (DJF 1989-90) and summer (JJA /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 25. VI_2009_006_tt

  farvegarins undir jöklinum út frá rúmmáli vatns sem þar hefur safnast fyrir benda til þess að viðnám gegn vatnsrennsli við jökul- botn minnki eftir því sem líður á hlaupið. Undir lok hlaupsins runnu á bilinu 80– 90 m3 s 1 um farveg sem var einungis einn þriðji hluti af rúmmáli farvegar sem flutti svipað vatnsmagn á fyrsta eða öðrum degi eftir að hlaupið hófst við jökuljaðar. Þessi niðurstaða er /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 26. VI_2014_005

  absolute errors (MAEs) are listed in Table 1. For temperature, the overall bias in January is reduced by 86%, with a reduction in overall MAE of 17%. For wind speed, the overall January bias is reduced by 74%, with a reduction in overall MAE of 9%. Both, for temperature and wind speed, the main benefit of the correction procedure is a reduction of differences between monthly mean values. Mean absolute /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 27. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  o t o - a g e n d a D e f i n e a n d i n v i t e s t a k e h o l d e r s T e c h n i c a l i n p u t a n d v i s i o n s - I n t e r n a l e x p e r t s - s t a k e h o l d e r e x p e r t s F r am e p r o b l e m - t r p s e r v i c e ( q u a l i t y ) l e v e l s - t y p e s o f s c e n a r i o s A n a l y z e p r o b l e m T e c h n i c a l i n p u t f r /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 28. VI_2016_006_rs

  horizontal displacement of the most active part of Þófi since the start of the measurements is mostly in the range 10–35 cm (maximum 69 cm), whereas the movement in Neðri-Botnar is slower, with the more active points having total displacement mostly in the range 5–10 cm (maximum 46 cm). The maximum measured velocity of the horizontal movement in the Þófi area was 92 cm/a over a two-month period in late /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 29. VI_2015_006

  contours). Bottom panel: manned and automated surface observations over Iceland. 13 Figure 4. Hourly rainfall during 3 September 2012, based on HARMONIE model simula- tions. Times are in UTC (local time). 14 Figure 5. Distribution of low- (red crosses), medium- (green vertical lines), and high- level (blue horizontal lines) cloud cover of at least 90%, based on HARMONIE model simulations. Terrain /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 30. 2013_001_Nawri_et_al

  approximately centred around Iceland: the outer domain with 43 42 grid points spaced at 27 km (1134 1107 km), the intermediate domain with 95 90 grid points spaced at 9 km, and the inner domain with 196 148 grid points spaced at 3 km. The northwest corner of the outer domain covers a part of the southeast coastal region of Greenland. Otherwise, the only landmass included in the model domain /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf