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352                                                  Part Ill Fatigue and Fracture

                  where C is a calibrated constant and g is a calibrated exponent. The long-term wave height
                  distribution is represented by the sum of two Weibull distribution: one for normal condition Ho,
                  the other for hurricane condition HI: :

                       ACT = CHOg for normal condition                               (1 8.15)
                       ACT = CH,g for hurricane condition                            (1 8.16)
                  Based on the methodology described in Chapter 19, the cumulative fatigue damage may be
                  easily derived for normal condition and hurricane condition respectively. The formulae for the
                  cumulative  fatigue  damage  based  on  the  deterministic  method  may  be  found  form  the
                  commentary on fatigue in API RP 2A - WSD.


                                   -
                                          ...........
                               fi     -------'---
                               &  .....................................   .^ .......
                               HI   ......................................................................................................













                                   I                                       Log N

                              Figure 18.1  Stress Distribution Illustration



                  18.3.4  Long Term Stress Distribution - Spectral Approach
                  A spectral approach requires a more comprehensive description of the environmental data and
                  loads, and a more detailed knowledge of these phenomena. Using the spectral approach, the
                  dynamic effects and irregularity of the waves may be more properly accounted for.
                  This approach involves the following steps:
                     Selection  of  major  wave  directions.  The  same  considerations  as discussed  for  the
                     deterministic approach apply,
                     For each wave direction, select a number of sea states and the associated duration, which
                     adequately describe the long-term distribution of the wave,
                     For each sea state, calculate the short-term distribution of stress ranges using a spectral
                     method,
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