80 results were found for T 홈타이▼ㄲr톡 GTTG5▼昪서농동아가씨출장ڒ서농동아로마垾서농동아로마출장서농동아로마테라피🔏optimistically/.

Results:

• 21. Statistical Analysis

  Of Precipitation In Latvia. XXV Nordic Hydrological conference, Northern Hydrology and its Global Role, 11-13 August, 2008, Reykjavik, Iceland. ISBN 978-9979-68-238-7. NHP Report No. 50, P. 134-142. Hisdal, H., Barthelmie, R., Lindström, G., Kolcova, T., Kriauciuniené, J. & Reihan, A. (2007). Statistical Analysis. In: J. Fenger (Ed.) Impacts of Climate Change on Renewable Energy Sources: Their role /ces/publications/nr/1943

• 22. VI2010-006_web

  tímabilið 1949–2009. T P1d P2d P3d P5d 1 22 29 35 43 2 26 35 41 51 5 32 43 50 61 10 36 49 56 68 20 40 55 62 75 50 46 62 71 85 og 5 daga tímabil fyrir veðurstöðina á Akureyri. Taflan sýnir úrkomu sem svarar til 1, 2, 5, 10, 20 og 50 ára endurkomutíma, þ.e. tölfræðileg greining bendir til að úrkoma verði ekki meiri en sem nemur gildunum í töflunni oftar en endurkomutíminn segir til um þegar til langs /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 23. Cradden_Lucy_CES_2010

  ? • Based on thermodynamic and heat transfer models accounting for: Wire resistance Solar heating Radiative cooling Convective cooling June 2010 7 How are ratings determined? • UK network standards assume seasonal average temperatures and worst-case wind conditions, i.e. low wind speeds Summer → 20˚C; Spring/Autumn → 9˚C; Winter → 2˚C • Real-time monitoring (‘dynamic rating’) is not commonly /media/ces/Cradden_Lucy_CES_2010.pdf

• 24. Dyrrdal_Anita_CES_2010

  Results W i n t e r t e m p e r a t u r e Max snow depth Trend slope Number of snow days Period II P e r i o d I I I Max snow depth Number of snow days Norwegian Meteorological Institute met.no Correlation analysis (1961-08) 138 mutual stations Introduction Data & Methods Results Correlation with winter temperature Correlation with winter precipitation In warmer regions both snow parameters /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 25. VI_2015_007

  0.95 vhm149 1.46 vhm205 1.01 vhm206 1.28 vhm221 0.9 vhm265 1.16 vhm277 0.87 vhm278 -0.12 18 l l l l l llll l llll lll ll lll lllll lllll ll l l l l l l l l l l l −2 0 2 4 6 0 1 2 3 4 −ln(−ln(1−1/T)) Q/ E[ Q] 1 2 5 10 20 50 100 T (years) l l l l l l l l vhm148 vhm149 vhm205 vhm206 vhm221 vhm265 vhm277 vhm278 Regional +/− 95% CI H1 0.995 H2 −0.877 l l l l l l l l l l l l l l l l l l l l l l l /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 26. VI_2015_009

  lllll lll l l ll l l l l l −2 0 2 4 6 0 40 0 80 0 120 0 −ln(−ln(1−1/T)) Q (m ³/s ) 1 2 5 10 50 T (years) l l l Ref: vhm238 IFM−ROI 5 IFM−ROI−ref CDF Annual Max. Inst. Q with best IFM µ(D)=(θ0)(AP)(θ1) l l lll lllll llll llll lllllll llllll llll l l l l l l l −2 0 2 4 6 0 20 0 60 0 −ln(−ln(1−1/T)) Q (m ³/s ) 1 2 5 10 50 T (years) l l l Ref: vhm144 IFM−ROI 5 IFM−ROI−ref l lll llll /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 27. ces_SA_group_flyer_new

  a l y ( ° C ) 1900 1920 1940 1960 1980 2000 -20 -10 0 1 0 2 0 R u n o f f a n o m a l y ( % ) 1900 1920 1940 1960 1980 2000 -40 -30 -20 -10 0 1 0 2 0 3 0 E v a p o r a t i o n a n o m a l y ( % ) Large-scale atmospheric patterns and hydroclimatological variables Large-scale atmospheric circulation patterns, are more accurately assessed by Global Climate Models than are local variations /media/ces/ces_SA_group_flyer_new.pdf

• 28. ces_risk_flyer

  including, for example, ensuring dam safety. The goal of the new Climate and Energy Systems project is to look at climate impacts closer in time and assess the a n o ect ves o  t e    ro ect An evaluation of risk under increased uncertainty in order to improve decision making in a changing climate was carried out through the following steps: development of the Nordic electricity system for the next /media/ces/ces_risk_flyer.pdf

• 29. The design of avalanche protection dams

  years, IMO has participated in extensive research supported by the European Commission, EC, and various other funds, which is meant to improve this situation. The results of the collective research were published in 2009 in a book called The design of avalanche protection dams - Recent practical and theoretical developments. The design of protective measures in the run-out zones of avalanches /about-imo/news/nr/1631

• 30. VI_2013_008

  Forecast skill evaluation over the period 01/09/2001–31/08/2005. No rescaling (Eqs. 6 and 10). All units are in m3=s Forecast range T=1 day T=2 days T=3 days Statistics ME RMSE Q95–Q5 ME RMSE Q95–Q5 ME RMSE Q95–Q5 vhm 64 – method 1 –20 103 302 –19 99 297 –20 103 298 vhm 64 – method 2 –11 44 132 –15 64 162 –18 87 201 vhm 64 – method 3 –24 64 206 –24 72 221 –25 87 241 vhm 64 – method 4 –16 47 132 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf