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BACKGROUND OF THE INVENTION  
         [0001]    This invention relates to coastal breakwaters and more particularly to an improved construction for damping incoming wave energy to reduce harmful effects of incoming waves on the bottom, adjacent shore, and the like.  
           [0002]    The use of a breakwater for the protection of shore areas and the damping of incoming waves is well known in the art. All of the various designs are positioned in the natural breaker zone or closer to shore. The most common breakwater is the barrier type that is in effect a solid wall situated offshore extending from the sea bottom to above the air/water interface. This type of breakwater acts as a wall against which the energy of the incoming waves is expended so that the water area of the shoreward side of the breakwater remains relatively calm and the shore area is relatively protected against the battering and erosion by wave action. This type of breakwater by its very nature interferes with currents which, under the proper circumstances, can result in increased erosion at the margins of the breakwater and may result in undue silting on the leeward side of the breakwater. In addition, breakwaters of this type require constant care and maintenance because of the force of the incoming waves and because the currents acting against the breakwater will in time erode away the base of the breakwater which will result in damage to the breakwater.  
           [0003]    Other types of breakwaters have been devised in an attempt to avoid the massive construction generally required for barrier type breakwaters. These are normally of the floating barrier type in which a buoyant body or a plurality of buoyant bodies acting at or near the air/water interface serve to dampen the wave height, thereby to produce an area of relatively calm water behind the breakwater. Although such devices may operate satisfactorily in moderate seas, they are normally of insufficient strength to withstand very heavy seas, particularly in shallow water where wave action is most severe so that substantial repair and replacement of the buoyant bodies will be required after a period of very heavy seas. In addition, such devices require relatively complex mooring systems to retain the floating breakwater in position. More recently, restoring beaches lost to wave action is done by transporting sand from selected surplus areas to shore. Natural wave action, however, removes this material much like the original sand. Thus, this practice of replenishment is a never-ending procedure, besides it is creating new problems in the reservoir areas.  
           [0004]    The most relevant prior art is U.S. Pat. No. 4,006,598, entitled “Breakwater System,” which was granted to the present inventor, Jobst Hulsemann, on Feb. 8, 1977. The Hulsemann &#39;598 patent describes a breakwater system comprising a generally plate-like structure disposed offshore and having an upper face that defined a raised sea floor above the natural bottom. Incoming waves are crested offshore over the breakwater, and subsequently formed waves are smaller because of the reduced water depth afforded by the false sea floor of the breakwater. Open spaces are provided in the upper face of the breakwater so that water pressure on the breakwater is equalized, thereby minimizing the structural requirements of the breakwater. The Hulsemann &#39;598 patent provides for a plurality of false sea floors, each disposed at a different distance from the natural bottom so that the platform created by the plurality of false sea floors is roughly parallel to the surface of the water, and the plurality of false sea floors then forming a breakwater. Thus it can be seen that the Hulsemann &#39;598 patent discloses a method wherein the breakwater system moved the effective area for reducing the damaging forces of breaking waves below the air/water interface, thus simulating a false sea floor during certain conditions of the sea, especially those conditions of different wave heights and different levels of the sea relative to the sea floor. The present invention of a wave ramp, by inherently deviating from the breakwater system of the prior art, overcomes the limitation of the prior art, and, in addition, offers other advantages. The most decisive difference to prior art is the overall inclination of the wave ramp, namely from about the sea floor to or above the surface of the sea, thus replicating more completely the naturally rising sea floor that causes steepening, cresting and breaking of incoming waves over the sandy bottom. The advantage of the continuity of the seaward inclination is that it covers the entire spectrum of incoming waves, regardless of wave height and different levels of the sea relative to the sea floor, in but a single structure, thus rendering the construction of tiered platforms to accommodate waves of different height unnecessary as used in the breakwater system. As a constructional consequence the individual component elements are considerably less massive, rendering a substantially greater ease of handling in placement operations, and require a shorter founding depth into the compacted subsoil of the sea floor. Also, the wave ramp of the present invention has all waves run up from their first encounter with the bottom of the false sea floor as it would be the case with the natural sea floor closer to shore without the wave ramp. Furthermore, the prior art breakwater system has an inherent weakness resting in its beginning in mid-water where parts of larger waves may form smaller waves beneath the structure. Even if these may not be erosive on the bottom their pulsating oscillations exert some stress on the individual elements from below that must be compensated for by the massiveness of the structure. On the other hand, the present invention of the wave ramp offers the advantage of a simple extension above the mean storm level of the sea towards shoreward in case protection is sought from damage of rarer events of exceedingly high stands of sea level. The present invention also overcomes the foregoing deficiencies with the prior art devices and practices and provides a breakwater effective for damping incoming waves, regardless of wave height and different levels of the sea relative to the sea floor, without interfering with the normal tidal and offshore currents.  
         SUMMARY OF THE INVENTION  
         [0005]    The present invention resides in a wave ramp, a kind of sloping false sea floor, positioned seaward of the natural breakwater zone designed to induce the breaking process of the waves before they interact with the natural bottom. The wave ramp of the present invention is subjected to lower physical stresses as the result of wave encounter since the wave ramp is detached from the bottom, except for piles holding it in position, resulting in little interference with currents; and by acting at the base of incoming waves, well beneath the air/water interface, thereby reducing the height of the waves more shoreward from the wave ramp, and energy components of incoming waves against the wave ramp are significantly reduced. Accordingly, the structural strength of the system is not as critical as for prior art devices which encounter the incoming waves at the air/water interface, the point of greatest wave energy.  
           [0006]    In accordance with the present invention, the wave ramp includes a generally plate-like structure having a substantially upper planar face spaced above the natural bottom to define a false sea floor over which the depth is substantially reduced as contrasted to depth of water over the natural bottom. Incoming waves, the sustainable heights of which are a function of water depth, run up over the wave ramp until they break. The energy is released in turbulence dispensed on the solid structure of the wave ramp rather than on the natural sea floor that is composed of readily movable sand. Waves subsequently formed, landward of the wave ramp, are substantially reduced in size due to the reduced distance left to the wind to build up new waves. Because of the shallowness of the water, the waves reaching shore have less force than would be the case without the wave ramp.  
           [0007]    The upper face of the plate-like structure is provided with a plurality of spaced-apart apertures or open areas between the constituent numerous individual plate-like elements that extend through the structure to permit the passage of water therethrough, thus equalizing pressure above and below the wave ramp. Because the pressure equalization feature and because the breakwater acts substantially at the wave base rather than at the air/water interface, the stress on the structure is minimized. Consequently, damage to the wave ramp is minimal, and little or no maintenance is required. In addition, the plate-like structure of the breakwater is spaced above the natural bottom so that there is substantially no interference with the normal tidal and other near shore currents as the result of the placement of the wave ramp.  
           [0008]    In one embodiment of the invention, the wave ramp defines a generally rectangular shaped sheet or plate in which a plurality of apertures or open spaces are provided so that about 50% to about 80% of the plate upper face is solid. The wave ramp is disposed with the plate spaced above the sea bottom in a gently inclined plane from near the sea floor to near the sea surface and anchored by a plurality of piles directly in the natural bottom.  
           [0009]    The wave ramp is positioned offshore adjacent to the area to be protected and normally extends in its longitudinal dimension parallel to the area to be protected. The transverse dimension of the wave ramp, that is the distance from the landward to the seaward edges, is equal to at least 1½ wavelengths.  
           [0010]    In another embodiment of the invention, the wave ramp is defined by a plurality of generally plate-shaped elements, each one slightly offset from it&#39;s neighbors in transverse direction, i.e. seaward and shoreward, which are disposed above the natural sea bottom and in combination define a generally rectangular rising plate-like configuration. The upper surfaces of the plates comprise a substantially planar upper face and the size of the plates and the spacing therebetween is such that not more than about 80% of the upper face area is solid surface. The combination of plates is so arranged as to transversely extend at least a distance of about 1½ wavelengths thereby rising from the sea floor to the surface. Whereas the wave ramp in transverse direction always begins near the bottom on it&#39;s seaward side it extends on it&#39;s shoreward side to above the mean level of the sea surface at regular or extreme stands of sea level. The size of the plates or constituent elements and the spacing therebetween can be varied across the transverse dimension of the wave ramp.  
           [0011]    Other features and advantages of the present invention will become apparent from the following detailed description taken in conjunction with the drawings and from the appended claims. 
       
    
    
     BRIEF DESCRIPTION OF THE DRAWINGS  
       [0012]    [0012]FIG. 1 is a sectional side elevation illustrating schematically a section of sea floor and the action of incoming waves.  
         [0013]    [0013]FIG. 2 is a side sectional view of the sea floor of FIG. 1 and showing a wave ramp, constructed in accordance with the invention disposed on the sea bottom for damping incoming waves.  
         [0014]    [0014]FIG. 3 is a plan view of the wave ramp of FIG. 2.  
         [0015]    [0015]FIG. 4 is a side elevation of an individual plate element of the wave ramp of FIG. 3 showing the plate element secured in its operating position in the sea bottom.  
         [0016]    [0016]FIG. 5 is a plan view of the plate element of FIG. 4.  
         [0017]    [0017]FIG. 6 is a perspective view, partially in section, of a wave ramp constructed in accordance with another embodiment of the invention.  
     
    
     DESCRIPTION OF THE INVENTION  
       [0018]    As shown in FIG. 1 a section of typical sea bottom  10  adjacent to a shore area is covered by water which normally cycles, because of tides, between a median low water level  12  and a medium high water level  14 . During storms, however, the water may reach an even higher level and this level is designated as the storm level  16 .  
         [0019]    As used herein the term “natural high water level” designates the mean high water level, such as that reached during high tides. It should be clear, however, that a specific storm water level cannot be precisely defined because of the variations in frequency and intensity of storms, the geography of the shore area, the nature of the body of water and other factors. Accordingly, determination of the natural storm water level can only be made after a period of observations and collection of data at the location.  
         [0020]    Incoming waves  17 , generally generated by wind, can occur at any of the aforementioned water levels. These incoming waves, upon reaching the shallow waters adjacent to the shore, crest and break and, depending upon the wave height, may result in erosion of the bottom. In addition, the battering force of the waves, that is the force of the waves applied in a generally horizontal plane, is also largely dependent upon the height of the incoming waves.  
         [0021]    Wave height is a factor of both wind velocity and water depth and as an incoming wave  17  approaches the shore, the water depth decreases to a point where the wave height is greater than the water depth can support. As water depth decreases, the front of the wave  17  becomes increasingly steeper until the wave collapses which results in the breaking of the wave, as indicated in  17   a.  The area where the breaking of the incoming waves occurs is commonly called the breaker zone. Typically, the bottom of the breaker zone is characterized by a greatly variable topography, often with holes and rises. It is presently believed that cresting and breaking will occur when the height of the wave, that is, the vertical distance from the trough to the top of the wave, exceeds about 1.5 times the mean depth of the water. Cresting of the wave creates a vertical component of energy  18  due to falling water and the magnitude of the vertical component is related to wave height. If the water is shallow enough and the vertical component  18  sufficiently large, particles from the bottom  10  will be lifted and suspended in the water, where they are eventually carried away by tidal current or near shore currents, if present, and subsequently deposited as silt or sand elsewhere.  
         [0022]    In addition to the vertical energy component  18 , a horizontal energy component  20 , which is also related to wave height, is generated by the incoming wave  17 , which accounts for the battering force of the wave. The horizontal component  20  is greatest at the air/water interface or surface of the wave  17 .  
         [0023]    After cresting and breaking, as at  17   a,  new wave forms  17   b  are generated and cresting is repeated, as at  17   c.  The new wave forms  17   b  are reduced in height as contrasted to the parent wave  17 , because they are formed in shallower water. However, the new wave forms even though of reduced height may still have sufficient vertical and horizontal energy components to be destructive to shore areas and installations located there along.  
         [0024]    In accordance with the present invention, it has been found that by raising the sea bottom and reducing the water depth in a selected offshore area, incoming waves are caused to crest offshore in an area where the vertical component  18  can do little or no erosion damage to the sea bottom  10 . The wave ramp of the present invention, in effect, represents an artificially raised sea floor or false bottom. As the waves run up they do crest and break and collapse much like they do in the natural breaker zone without a wave ramp; the decisive difference, however, is that this breaking process occurs over the likewise non-erodable wave ramp  22  (FIG. 2) and not over the loose and movable grained sea floor  10 . In addition, hydrostatic pressure above and below the wave ramp is always balanced due to the spaced apart arrangement of the individual elements  24  (FIG. 2), and there is no interference with normal tidal and near shore currents because of the open spaces between the pilings  24 .  
         [0025]    As is more particularly shown in FIGS. 2 and 3, a wave ramp, shown generally as  22 , comprises a plurality of individual plate units  24  which are arranged in spaced relation off the shore area to be protected. The plate units, even though they may have planar upper faces  25 , are slightly set off to define a generally elongated plate-like structure having a substantially inclined upper face extending between the sea surface and the bottom  10  to define a false sea floor which acts on the incoming waves in the same manner as the natural sea bottom in shallower waters adjacent to the shore. Thus, as the incoming waves  17  pass over the upper faces  25  of the wave ramp  22  the mean depth of the water is substantially decreased, and, should the wave height be less than about 1.5 times the mean depth of the water as now determined by the upper face of the wave ramp  22 , the waves will crest as at  17   a  and break thereby discharging their energy (FIG. 1:  18 ) on top of the faces  25  of the wave ramp  22 . Because the true bottom  10  is well below the false bottom simulated by the wave ramp  22  the particles will not be lifted by the turbulence at the bottom of the breaking waves  17  and not be suspended and transported as when the breaking occurs in naturally shallower water without a wave ramp. Subsequently formed waves will be of substantially reduced heights so that waves eventually reaching the shore area are of greatly reduced force.  
         [0026]    The wave ramp  22  is preferably located in the offshore waters with its longitudinal axis extending substantially parallel to the shore line, or to the installation being protected. The precise offshore distance of the wave ramp  22  is not critical although it is highly preferred to locate it far enough offshore so that the cresting waves  17   a  which are induced by the wave ramp  22  will have substantially little or no effect on the sea bottom  10 . This is always seaward of the natural breaker zone. Wave ramp  22  is spaced above the sea bottom  10  so that the upper faces  25  will lie substantially in an inclined plane vertically spaced from the bottom  10  rising to above the mean storm level (FIG. 1:  16 ) over a distance of at least 1.5 times the wavelength. Although the upper faces  25  of the wave ramp  22  are described as substantially planar, the upper faces may be contoured in conformity with the contour of the bottom  10  at the point of installation.  
         [0027]    The longitudinal dimension of the wave ramp  22  is not critical and it may be as long as required to protect a particular shore area or installation. The transverse dimension of the wave ramp  22  is selected as to be equal to at least 1½ times the wavelength and preferably the transverse dimension is equivalent to three or more wavelengths. As used herein, a wavelength will vary depending upon the location, the depth of the body of water, the slope of the sea bottom and the like. Thus, for example, in North Sea locations the wavelength is relatively short, while on the West Coast of the United States wavelengths are generally longer.  
         [0028]    Referring again to FIG. 1, one can note that the geography of the sea floor is normally a continuation of the geography of the land mass above the high water line. When there is a gradual slope to the beach, the slope continues at the same relative slope under water. Due to the effects of erosion, the inclination of the sea floor closer to the beach area may be greater than the inclination of the sea floor at a greater off-shore location. The geographies of the wave zones can thus be separated by the inclination of the sea floor. Table 1 shows examples of the relationships between the wave zones.  
                                                                         TABLE 1                                   Sea Floor   Breaker Zone   Common Beach   Very Steep Beach                                    Rise:   1-500   1:200   1:100   1:50   1:30   1:30   1:20   1:10       Angle:   0.1°   0.3°   0.6°   1.1°   1.9°   1.9°   2.9°   5.7°       Percent:   0.2%   0.5%   1%   2%   3.3%   3.3%   5%   10%                  
 
         [0029]    The inclination of the wave ramp can then be selected based on the inclination of the sea floor. The angle of inclination of the wave ramp structure may be greater or less than the angle of inclination of the sea floor. As an example, a wave ramp structure may be selected wherein the first set of plate units  24  will be placed parallel to the shore such that the upper surface  25  is about 12 meters below the mean level of the sea surface where wave heights may only be 5 meters. As another example, Table 2 shows the approximate transverse width (from shore-side to ocean-side) of the wave ramp based on the length of the wavelength. The first three columns represent wavelengths from about 30 meters to about 80 meters, and the last two columns represent wavelengths from about 30 meters and less.  
                                   TABLE 2                           Wavelength   80 m   80 m   80 m   30 m   30 m       Inclination:   1:20   1:25   1:30   1:10   1:50       Wave ramp   240 m   300 m   360 m   100 m   100 m                  
 
         [0030]    Where the wavelength is about 30 meters, two different sloping segments may be simultaneously employed, based on the inclination of the sea floor. For example, where the inclination is 1:10, the first segment may be placed where the first set of plate units  24  placed parallel to the shore such that the upper surface  25  is about 10 meters below the mean level of the sea surface, and the first set of plate units  24  for the second segment may be placed parallel to the shore such that the upper surface  25  is about 2 meters below the mean level of the sea surface.  
         [0031]    As is more particularly shown in FIGS. 4 and 5, the plate units  24  each comprise a shaft or pile  26 , including preferably a lower threaded end portion  28 , adapted for anchoring in the sea bottom  10 , and an upper end portion  29  extending above the sea bottom and carrying a plate  30  in spaced relation to the sea bottom. The upper surface of the plate  30  in combination with adjacent plates defines the upper face  25  of the wave ramp  22 , which acts on the wave in the manner described to induce early cresting and breaking, thereby discharging the vertical energy component  18  and the horizontal component  20  of the incoming wave  17  on top of the plate units  24 . The plates  24  are preferably constructed of a fairly high strength material and in this connection reinforced concrete has been found to be an excellent construction material in view of its high strength and ready availability. With reinforced concrete it has been found that the preferred proportions of the plate  30  diameter to the diameter of the pile  26  be maintained on the order of about 5:1 to about 7:1. In typical sandy bottom the portion of the pile  26  in the sea bottom  10  rarely needs to extend more than a fixed length into the consolidated bottom, e.g. 5 m, to insure proper anchoring of the plate unit  24 . However, under certain conditions of the sea floor, other ratios between the diameter of plate  30  and pile  26  may be selected. Further, other material for plate  30  and pile  26  may be selected, such as stainless steel, wood, or composites such as carbon or fiber. Any material that can resist the corrosive effects of the environment may be used for plate  30  and pile  26  may be selected.  
         [0032]    The spacing between the individual plate units  24  is an important element of the present invention, since, if the units are spaced too far apart, the efficiency of the wave ramp  22  is reduced. On the other hand, if the units are spaced too closely together, the wave ramp  22  will be exposed to undue structural stress due to the force exerted by the water passing over the breakwater system. Accordingly, it has been found that good results are achieved when the units are spaced so that the upper surfaces of the plates  30  comprise between about 50% to about 80% of the total area of the upper face  25  of the wave ramp  22 . In this manner sufficient surface is provided to efficiently induce the cresting and breaking of the waves yet sufficient open space is provided to permit equalization of the pressures above and below the wave ramp  22 .  
         [0033]    In some cases it may be desirable to provide a series of wave ramps  22 , in which the upper faces  25  are disposed at different distances from the shore line, so that, for example, an outer wave ramp is followed by a more shoreward wave ramp, as is the case above where the wavelength is about or less than 30 meters.  
         [0034]    Although the wave ramp of the present invention has been described in connection with a plurality of plate units  24  which are individually anchored in the sea bottom  10  to define a false sea floor, it should be clear that other structural arrangements can be utilized to induce the early cresting of waves in accordance with the present invention. For example, a platform unit can be utilized in place of the plurality of plate units  24 .  
         [0035]    As is more specifically shown in FIG. 6, a wave ramp  22 ′ comprises a unitary rectangular platform  38  having a substantially planar upper face  40  including a plurality of openings  42 , which extend through the platform for the equalization of pressure. The platform  38  is anchored in the sea bottom  10  by a plurality of piles  44  which extend above the sea bottom for carrying the platform  38  substantially between the bottom  10  and the sea surface for the purpose already described. The openings  42  are distributed over the platform  38  and are of sufficient size and number so that the solid portion of the surface of the platform comprises between about 50% to about 80% of the total platform area. The transverse dimension of the platform  38  is equal to between 1½ to about three or more wavelengths. In this embodiment, the wave ramp  22 ′ can comprise sections of the platforms  38  arranged in end to end relation so as to extend parallel to the shoreline or installation being protected.  
         [0036]    The operation of the wave ramp  22 ′ is as described above. That is to say, the upper surface  40  of the platform  38  defines a false sea floor, which causes early cresting and breaking of the larger incoming waves, while waves subsequently formed over the system are substantially smaller because of the reduced water depth provided by the false sea floor, the short distance to the shore, and the length of time the wind operates on the surface of the water.  
         [0037]    From the foregoing it will be seen that the wave ramp of the present invention provides a false sea floor, which is in spaced relation to the natural sea bottom, to act upon the base portions of incoming waves to induce early cresting and breaking of incoming waves at a point offshore, where the vertical component of wave energy can do substantially little or no damage to the sea bottom. The transverse dimension of the system is sufficiently large to inhibit the subsequent formation of large waves. The waves that do form shoreward of the wave ramp are of substantially less height than would normally occur in the absence of the wave ramp, and the horizontal components and the vertical components of wave energy are greatly reduced on the shoreward side of the wave ramp. In view of the structural design of the wave ramp and the manner in which it acts on the incoming waves, the forces exerted on the construction are minimized. Moreover, since the wave ramp is raised on pilings above the sea bottom, there is substantially no interference with normal currents.  
         [0038]    While the invention has been described above in connection with certain embodiments thereof, it will be clear that changes and modifications may be made to the wave ramp system of the present invention without departing from the spirit or the scope of the appended claims. For example, the individual plate units  24  of the preferred embodiments have been shown to be disk-shaped, however, plates of any geometric design may be used. In addition, a wave ramp structure may constructed such that plate units  24  may be inclined relative to the general surface of the water.

Summary:
The present invention describes an off-shore wave ramp for inducing early cresting of waves to prevent damage and erosion along a shoreline, consisting of at least one platform supported above the natural sea floor by support means firmly affixed to the sea floor, the platform being arranged according to a predetermined regular pattern such that the area of the platform covers between about 50 and 80 percent of the area of the sea floor under the platform and forming a false sea floor seawardly inclined between the high water level to a selected distance above the sea floor. The wave ramp platform is comprised of an array of a selected number spaced-apart, unconnected, rigid, non-buoyant, stationary plate-shaped elements with a seaward inclination of the wave ramp is at a selected angle relative to the sea floor.