Search

More than 100 results were found for K 와이즈프로토 CDDC7.COM ㅿ보너스번호 b77ㅿ오산 프로토⍮더클래스카지노ॅ네임드사다리배팅사이트ἑ벳인포토토ྈ와이즈프로토사용 lapstrake/.


Results:

  • 11. norsem_slunga

    an Hoek (1978) published a very often referenced picture showing observed crustal stresses by plotting the depth against the ratio between the mean horizontal stress and the vertikal stress. This ratio is often denoted k and thus k = (SH+Sh)/2/Sv. The main feature of the data set was the clear excess of horizontal stresses at very shallow depths, especially above some 300m. A large number /media/norsem/norsem_slunga.pdf
  • 12. 2013_001_Nawri_et_al

    rather than from the data directly. This reduces the amount of data that needs to be disseminated to a few parameters, that describe each wind speed distribution. Of the various probability density functions for boundary-layer wind speeds, s, the 2-parameter Weibull distribution, f (s;A;k) = k A s A k 1 exp s A k ; (1) is the one most commonly employed for wind energy studies (Morgan /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 13. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

    at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
  • 14. Kok_JGEC658_2009

    to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf
  • 15. Protective measures

    On protective measures Protective measures On avalanches Reports and papers on protective measures with regard to avalances: An overview of the need for avalanche protection measures in Iceland (IMO Rep. 96004, 1996, authors T. Jóhannesson, K. Lied, S /avalanches/imo/protective/
  • 16. Climate and Modeling Scenarios

    of temperature and precipitation, Geophys. Res. Lett., 35, L20709, doi:10.1029/2008GL035694. Elíasson, J., Rögnvaldsson, Ó. & Jónsson, T. (2009). Extracting statistical parameters of extreme precipitation from a NWP model. Hydrol. Earth Syst. Sci., 13, 2233-2240, November 2009. Jylhä, K., Tuomenvirta, H., Ruosteenoja, K., Niemi-Hugaerts, H., Keisu, K. & Karhu, J.A. (2010). Observed and projected future /ces/publications/nr/1680
  • 17. Climate and Modeling Scenarios

    of temperature and precipitation, Geophys. Res. Lett., 35, L20709, doi:10.1029/2008GL035694. Elíasson, J., Rögnvaldsson, Ó. & Jónsson, T. (2009). Extracting statistical parameters of extreme precipitation from a NWP model. Hydrol. Earth Syst. Sci., 13, 2233-2240, November 2009. Jylhä, K., Tuomenvirta, H., Ruosteenoja, K., Niemi-Hugaerts, H., Keisu, K. & Karhu, J.A. (2010). Observed and projected future /ces/publications/nr/1680/
  • 18. VI_2015_005

    the two reanalyses exist primarily over Green- land, where the amplitude of the seasonal cycle in ERA-Interim is reduced, with up to 5 K higher temperatures than ERA-40 in winter, and up to 5 K lower temperatures in summer (not shown). Elsewhere, differences are small and unsystematic. As described by Simmons et al. (2006) and Berrisford et al. (2009), compared with ERA-40, sev- eral improvements /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 19. VI_2020_005

    variability pattern on a decadal scale, mainly through wind and pressure forcing but also through steric effects (Dangendorf, Calafat, et al., 2014; Dangendorf, Wahl, et al., 2012; Madsen, 2009; K. Richter, Nilsen, and Drange, 2012; Yan, Tsimplis, and Woolf, 2004). Decadal sea level variability over open North Atlantic ocean, especially the Subpolar North Atlantic, in the satellite altimetry era /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 20. Paper-Olafur-Rognvaldsson_92

    a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

Page 2 of 10






Other related web sites


This website is built with Eplica CMS