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41 results were found for 外推发帖( q)1716160940翟...99jde9..qav.


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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

    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

  • 25. VI_2009_006_tt

    236 1992 09 167 124 167 98 1995 07 1994 1759 599 368 1995 10 96 62 73 37 1997 07 921 728 330 184 2000 08 1240 1083 365 221 2002 09 689 582 267 160 2003 11 241 207 139 98 2006 04 1370 1340 300 270 2008 10 1350 1290 300 265 The origin of the 1957, 1960, 1964 and 1966 jökulhlaups is not certain but is most likely the eastern cauldron. The discharge and volume for the 1995 jökulhlaup are a sum from /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

  • 29. 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
  • 30. 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

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