Search

80 results were found for T 홈타이♬까똑 gttg5♬鉭영등포구타이箳영등포구타이녀출장蝮영등포구타이마사지衐영등포구타이출장💇🏼‍♂️amputator.


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

    2050s 2080s C h a n g e i n r a t i n g ( % ) 10% 50% 90% C h a n g e i n r a t i n g ( % ) C h a n g e i n r a t i n g ( % ) Each bar shows range over whole UK spatial area June 2010 13 Is the impact similar over the whole UK? • Changes in the summer minimum rating, i.e. worst-case conditions – max temperature: Rating at baseline period 1961 /media/ces/Cradden_Lucy_CES_2010.pdf
  • 24. Dyrrdal_Anita_CES_2010

    : Significant at 90% CL Norwegian Meteorological Institute met.no Fokstugu (973 m.a.s.l.) Introduction Data & Methods Results Trends in start and end: Significant at 99% CL /media/ces/Dyrrdal_Anita_CES_2010.pdf
  • 25. VI_2015_007

    reference (µi(D)) and estimated (bµi(D)) index floods. The reference index flood was defined by the arithmetic mean of the observed AMF sample at the target site and the estimated index flood was obtained by Eq. (4). RMSEµ(%) = s 1 N N i=1 µi(D) bµi(D) µi(D) 2 x100 (8) Reference and estimated flood quantiles were compared at each target site, for average recur- rence intervals T of 2, 5, 10, 20 /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

Page 3 of 8






Other related web sites


This website is built with Eplica CMS