41 results were found for ( q)1716160940在线标准北京时间校对排名代做贺...6hjlgw..83r.

Results:

• 21. Paper-Olafur-Rognvaldsson_91

  of Icelandic glaciers 1992–1997). Rep. OS-98082 (in Icelandic), National Energy Authority, Reykjavík. Sigurðsson, O., Thorsteinsson Th., Ágústsson S. M. and Einarsson B. 2004. Afkoma Hofsjökuls 1997–2004. (Mass balance of Hofsjökull 1997–2004.) Rep. OS-2004/029, National Energy Authority, Reykjavík. Uppala, S.M., and 45 co-authors 2005. The ERA-40 re-analysis. Q. J. R. Mete- orol. Soc., 131, 2961 /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

  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

  varð mest 123 m3 s 1 en rennsli hlaupsins við jökuljaðar varð mest 97 m3 s 1. Þetta hlaup er ekki hægt að skýra með viðteknum kenningum um jökulhlaup fremur en önnur Skaftárhlaup. Heildarrúmmál hlaupsins var 53 Gl. Geymsla vatns í hlaupfar- veginum undir jöklinum var reiknuð út frá rennslisgögnunum en hún varð mest 35 Gl, sem samsvarar tveimur þriðju af heildarrúmmáli hlaupsins. Geymslan í /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