Page 65 - Marine Structural Design
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42                                                 Part I Structural Design Principles


              3.2.4  Wave Scatter Diagram
              Long-term descriptions are required to describe the variation of sea-states. The wave scatter
              diagram  provides  a joint  probability  table  of  significant  wave  heights  and  characteristic
              periods for a site. Beck et a1 (1989) outlined methods of collecting ocean wave data:
              (a) Visual estimates of wave conditions (of heights and periods) by trained observers aboard
                 weather ships: Hogben and Lumb (1967) collected log entries of some 500 British ships
                 from 1953 to 1961 in oceans of worldwide.
              (b) Point Spectra from wave measurements using a ship borne meter: Pierson and Moskowitz
                 (1964) evaluated the wave generation process and hlly developed spectra in particular.
              (c) Directional spectra
              (d) US Naval hindcast wave climatology: An alternative to wave data is to calculate a set of
                 spectra from the  comprehensive wind data that have been  collected for years over the
                 important trade routes worldwide, see e.g. Bales et a1 (1 982).
              Figure 3.2 compares contours of two wave scatter diagrams retrieved from a wave database for
              a site in the North Sea (W156) and a site in the Gulf of Mexico (W391). As observed, the
              wave environment at site W156 is much more severe than that at site W391. In order to obtain
              a wave scatter diagram, various short-term wave data that have been accumulated over a long
              period  of time  (for example,  10 to  20 years) and cover all  sea-states defined by  different
              combinations of pairs  (Hs, 7J,  are statistically averaged. The statistical value based  on the
              long-term description of sea-states is referred to as long-term. The wave directional probability
              corresponding to each wave scatter diagram table should also be provided.  Figure 3.3 shows
              the wave  directional probability distributions at  two  grid zones, W156 and W391, with  24
              equally  divided  directional  divisions.  The  radius  for  each  direction  shown  in  Figure  3.3
              describes the probability for that direction.





                                            12.5
                                                                          12.5
                                           9.5                            9.5  8
                                                                              h
                                                                              z.
                                           6.5                            6.5
                        -3.5                                              3.5
                       0.5   3.5   6.5   9.5   12.5    0.5  3.5   6.5  9.5  1 2 .5
                                                               Hs (4
                                Hs (m)

                     (a) A site in the North Sea      (b)A site in Gulf of Mexico
                         Figure 3.2   Graphic Comparison of Wave Scatter Diagrams for Two
                                     Locations (Zhao, Bai & Shin, 2001)
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