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        of the spectral family in Table 2, and takes the maximum.  The extreme values provided by the latter
        are up to 16% larger than those by the former method. This is understandable because the sample size
        (or exposure time) for the latter is relatively larger.  In this example, extreme values for H, with risk
        parameter a = 1  are directly applied. Obviously, the final extreme values of responses are dependent
        on the designer's discretion and choice of Ifs

        4.2 Long-term Extreme Approach
        To predict a long-term extreme value, a long-term initial cumulative probability distribution function
        P(x)  of  responses is  required.  Although  function P(x) cannot  be  predicted  explicitly due  to  the
        complications of  the  responses  in  various  sea  states,  it  can  be  built  up  approximately through
        accumulations of short-term statistical analyses. Generally,  P(x) can be assumed to be in the form of
                                    P(x) = 1 - exp[-q(x)]           (q(420)     (3)
        In practice, a Weibull distribution or log-normal distribution is commonly used for P(x). In this paper a
        generalized fonn suggested by Ochi (1981) is used to achieve higher accuracy in the curve fitting. i.e.,
        q(x) = cxm exp(-pxk),  in  which  c, m, p,  and  k are four  constant parameters to  be  determined  by
        nonlinear least-squared  fitting. Once the mathematical  expression of P(x) in Eq.  3 is obtained, the
        long-term PEV can be determined by


        Here a is the possibility level as in Eq. 2.  Here N is the number of observations or cycles related to the
        return period.  In  the design  of offshore structures, a return  period of  IO0 years is widely  used  for
        estimating the long-term extreme values. When the WSD is applied, the P(x) above can be obtained by
        using the definition of probability density function of maxima
                                 1 "ijkl  p<wij  ) Pr(Qk  Pr(A1 )pgk/ (x)
                           p(x) = UkJ                                           (5)
                                   c  "ijkl  pr(w&  Pr(a k ) pr(Al)
                                  WJ
        where
        Pr(w,):  normalized joint wave probability of (HdzJ,mJ) or cell w# in WSD,  CPr(wii) = 1.
                                                                 iJ
        Pr(a,):  probability of wave in direction a,  CPr(ak) = 1.
                                          k
        Pr(A,):  probability (or percentage) of loading pattern A, during service, XPr(Al) = 1.
                                                              I
        n,,,:   average number of responses in T, corresponding to cell wil of WSD, wave direction ak and
                loading pattern A,.
        p,&):   the probability density function of short-term response maxima associated with n,,,.
        Figure 7 displays the long-term p(x) of stress responses to waves W156 and W391. It is obvious that
        the  wave  environment is the  dominant factor affecting the  long-term  probability distribution; the
        effects of spectral shape are not significant.
        Afier the mathematical  formula of q(x) in Eq. 3 has been determined by curve fitting, the extreme
        value can be calculated by  Eq. 4.  Figure 8 compares the long-term extreme values for wave zones
        W156  and  W391  using the  JONSWAP and  Bretschneider spectra.  The  extreme values of  stress
        dynamic components are listed in Table 4. By comparing the long-term extreme values to those short-
        term extreme values listed in Table 3, it is found that the extreme values provided by the long-term
        approach are larger up to 9%.  Because the long-term  approach uses the probability distribution of
        responses directly, it can avoid  the uncertainty  caused by the choice of extreme If, and associated
        wave spectral family (a series of Tp). Based on this point  of view,  the long-term  approach is more
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