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


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  • 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

  • 25. VI_2009_006_tt

    leads to c = h1u1 h2u2 h1 h2 : (3.2) Using the Manning equation for discharge per unit width, q, q = 1 n0 hR2=3H S 1=2 0 ; (3.3) where n0 is the Manning coefficient, h is the flow depth, RH is the hydraulic radius and S0 is mean channel slope; the relationships: u h2=3, q h5=3 and u q2=5 can 18 be derived for a wide rectangular channel for which RH h and u = q=h. Now using u1h1 = q1, u2h2 /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_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
  • 29. 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
  • 30. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    s fro m climat e ch ang e an d cr o ss bou ndar y adaptatio n measu res . In th e Netherl and s fo r hyd rodyna m ic mod el syst em s lik e SOB EK- W AQ UA (loca lleve l) an d e.g . fo rR hi ne flo w (ba sin wi de )c o n sid er ab le u n ce rta in tie s ex ist (W ee rts et al .200 3) D ev el op m en to fi nt eg ra te d ba sin m o de l( flo od ing an d poll ution) . 2: St at ist ic al /q ua lit /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

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