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PORT WORKS DESIGN MANUAL PART 5 Guide to Design of ...

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35<br />

following paragraphs.<br />

5.5.1 Coordinate System<br />

Shoreline computations involve the determination <strong>of</strong> longshore transport rates and directions<br />

due <strong>to</strong> different incoming wave conditions in different periods. As longshore transport can<br />

take place in either directions <strong>of</strong> the shore, it is necessary <strong>to</strong> set up a coordinate system <strong>to</strong><br />

avoid confusion <strong>of</strong> directions in longshore transport computations. The coordinate system<br />

defines the sign conventions <strong>of</strong> incident wave angles and longshore transport directions.<br />

The original shoreline is usually chosen for convenience as the x-axis. The y-axis takes<br />

account <strong>of</strong> the variability <strong>of</strong> longshore transport perpendicular <strong>to</strong> the shore. As longshore<br />

transport is related <strong>to</strong> long-term change <strong>of</strong> the shoreline, the mean sea level may be taken as<br />

the zero reference datum for the vertical z-axis. An example <strong>of</strong> the coordinate system is<br />

shown in Figure 10.<br />

5.5.2 Longshore Transport Rates and Directions<br />

A number <strong>of</strong> longshore transport formulae have been developed <strong>to</strong> calculate the longshore<br />

transport rates and directions at a point <strong>of</strong> the shore. An example is the CERC formula,<br />

which can be written as follows (CUR, 1987) :<br />

s = BH 2 c K 2 sinφ cosφ<br />

l o o rb b b<br />

or<br />

s l<br />

= BH 2 b<br />

c b<br />

sin 2φ b<br />

where s l = longshore transport due <strong>to</strong> breaking waves.<br />

B = a constant equal <strong>to</strong> about 0.025.<br />

H o = deepwater significant wave height.<br />

H b = significant wave height at breaker line.<br />

c o = deepwater wave velocity.<br />

c b = wave velocity at the breaker line.<br />

K rb = refraction coefficient at the breaker line.<br />

φ b<br />

= wave angle at breaker line.<br />

Other longshore transport formulae include those developed by Bijker, Van Rijn, Bailard and<br />

so forth. Longshore transport models are normally equipped with these formulae for<br />

designers <strong>to</strong> apply in the computations. More details <strong>of</strong> these formulae can be found in

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