41 results were found for 4100506(q)智通人才网外推代做路...petipt..ryb.

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

  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

  is on the northern North Atlantic and the Nordic Seas. With the southern boundary at 47 N, the study domain covers Newfoundland, but excludes various marginal and inland seas with significant independent storm activity, such as the Mediterranean and Adriatic Seas, as well as the Black and Caspian Seas. The northern boundary at 80 N takes the domain up to Fram Strait, including Svalbard, but excluding /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

  : 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

  wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 29. VI_2015_006

  cover. At night, the differences between land and ocean are small. However, during the day, especially with clear skies, as the land heats up faster than the surrounding water, the terrestrial longwave radiation losses can exceed those over the nearby cloud-free ocean by up to 80 W m 2. The total radiation received by the Earth’s surface is determined by factors that oppositely af- fect the short /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 30. 2013_001_Nawri_et_al

  by the manufacturers. Enercon E44 Vestas V80 Rotor diameter [m] 44 80 Hub height [m] 55 67 Rated power [kW] 900 2000 Cut-in speed [m s 1] 3 4 Rated speed [m s 1] 15 16 Cut-out speed [m s 1] 28 25 For any given turbine, there are three important characteristic wind speeds. The cut-in speed is the lowest wind speed at which a turbine can generate usable power. The rated speed is the lowest wind speed at which /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf