Page 414 - Laboratory Manual in Physical Geology
P. 414

Panel on Climate Change (IPCC) of the United Nations   surges. A  storm surge  is an abnormal rise of
        Environment Programme (UNEP) has suggested that sea   water pushed landward by high winds and/or low
        level will continue to rise and is now expected to achieve a   atmospheric pressure associated with storms. The storm
        mean global rise of at least 0.17–0.32 m (6.7–13.6 inches)   surge is over and above the normal tide, and NOAA
        by 2046–2065. Note that these figures are for mean   expresses it as the height above the  expected tide level.
        (average) changes of global sea level. Specific locations may   NOAA also measures  storm tide —which it defines as
        experience more or less of a rise in sea level. For example,   the water level height caused by a combination of the
        although TOPEX/Poseidon satellite altimetry indicates   normal tide level and the storm surge. Storm surges can
        that sea level is rising at a global rate of 2.9 mm/yr, NOAA   cause the ocean to rise by about 1–10 feet above the
        tide gauge records indicate that sea level at Ocean City,   normal astronomical tide, depending on the magnitude
        Maryland (FIGURE 15.7), has been rising nearly twice as fast   of the storm and other factors. However, except for
        (5.48 mm/yr since 1975).                             hurricanes, most storm surges are in the range of
              Sea level also fluctuates both above and below   2–3 feet.
        mean sea level during daily tidal cycles and storm





                                 Breakwater
                              (Offshore sea wall)             Jetties           Groins
                                                  Harbor
               Sea wall










                                                                              Wind
                                  Longshore current









          FIGURE 15.6    Coastal structures.           Sea walls  are constructed along the shore to stop erosion of the shore or extend the shoreline (as
        sediment is used to fill in behind them).   Breakwaters  are a type of offshore sea wall constructed parallel to shoreline. The breakwaters stop
        waves from reaching the beach, so the longshore drift is broken and sand accumulates behind them (instead of being carried down shore with
        the longshore current).  Groins  are short walls constructed perpendicular to shore. They trap sand on the side from which the longshore current
        is carrying sand against them.  Jetties  are long walls constructed at entrances to harbors to keep waves from entering the harbors. However,
        they also trap sand just like groins.


























        382  ■  L ABOR ATORY  15
   409   410   411   412   413   414   415   416   417   418   419