41 results were found for ( q)4100506Mtime时光网自助留痕蜘蛛池龚...j5jnsl..7de.

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

  hydrological model. J. Hydrol., 267, 40–52. Jasper, K., and Kaufmann P. 2003. Coupled runoff simulations as validation tools for atmospheric models at the regional scale. Q. J. R. Meteorol. Soc., 129, 673–692. Jóhannesson, T., Aðalgeirsdóttir G., Björnsson H., Crochette P., Elíasson E. B., Guðmundsson S., Jónsdóttir J. F., Ólafsson H., Pálsson F., Rögnvaldsson Ó., Sigurðsson O., Snorrason Á /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

  relationship with the forcing variable. Grid-point correlations are calculated separately for winter and summer months. This effectively removes the impact of the seasonal cycle. The coefficient of determination between mean sea level pressure (MSLP) and total precipi- tation, is shown in Figure 4. Grid points at which correlation is not statistically significant at the 95% confidence level /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 25. VI_2009_006_tt

  the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average propagation speed of the subglacial jökulhlaup flood front was found to be in the range 0.2–0.4 m s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 26. VI_2014_005

  : 3601/B2007.EEA53004 and 3601/RO/CLC/ B2007.EEA52971, Landmælingar Íslands, Reykjavik, Iceland. Bechtold, P., Köhler, M., Jung, T., Doblas-Reyes, F., Leutbecher, M., Rodwell, M. J., Vitart, F., and Balsamo, G. (2008). Advances in simulating atmospheric variability with the ECMWF model: from synoptic to decadal time-scales. Q. J. R. Meterol. Soc., 134:1337–1351. Brousseau, P., Berre, L., Bouttier /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

  /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 29. VI_2015_006

  #, and relative to SW# for the other fluxes. SW# LW" SH" LH" Net# Snow-free land & Clear 228 (24%) 103 (45%) 48 (21%) 71 (31%) 6 (3%) Snow-free land & Overcast 137 (14%) 29 (21%) 67 (49%) 45 (33%) -4 (-3%) Snow-covered & Clear 116 (12%) 87 (75%) -38 (-33%) 19 (16%) 48 (42%) Snow-covered & Overcast 54 (6%) 18 (34%) 3 (6%) 6 (11%) 27 (49%) Ice-free ocean & Clear 282 (30%) 99 (35%) 10 (4%) 48 (17%) 125 (44 /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