Coastal region and small island papers 19 |
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10 |
Currents
Background While waves are the most important process
moving sediment particles on a
beach,
currents also have a role to play. |
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Measuring longshore currents |
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When the waves approach the beach at an angle, they generate a longshore current which moves parallel to the beach (see Figure 20). While this current is not in itself strong enough to pick up sediment particles from the sea bottom, it can move material that has already been stirred up by the waves. The longshore current is responsible for moving material from one part of the beach to another. When a structure such as a jetty or groyne is built out into the sea, this longshore current results in sand building up on one side of the structure (see Figure 21).
Measurements of longshore currents are best combined with wave measurements. So if longshore currents are being monitored, then waves should also be measured (see Chapter 9). Together, these provide a picture of the processes moving sand around on the beach. The
longshore current flows in a direction
roughly parallel to the beach, near where the waves break. The
current
speed and direction can be measured. Current speeds are recorded in feet
per second or cm per second. Current direction is recorded in degrees
and is the direction towards which the current is going. So if
a current is going from north to south, the current direction is
recorded as south or south-going; similarly, a current going from east
to west is recorded as west or west-going. (This is opposite to wind and
wave direction, which are recorded as the direction from which the wind
is blowing or the waves are coming.) |
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The distance moved after five minutes is used to determine the current speed in ft/second or cm/second. The direction in which the dye moved must also be recorded. These measurements can be repeated at several different places along the beach to see if the current speed and direction is the same or whether it varies.
If the dye does not move much, but just remains in
a pool near the stick, then this means there is no
longshore current on
that day. |
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When to measure |
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As with the wave measurements, this will depend on
the nature of the monitoring and the time available. While the time is
not likely to be available for daily measurements, weekly or twice
monthly measurements will yield some interesting information. |
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Figure 22 shows current speed and direction based on once/month measurements in 2000. The speed was highest in the winter months when the current direction was south-going. While in the middle months of the year, the current speed was lower and the direction of current movement was north-going.
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Further activities |
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Relate the direction of the longshore current to the source of beach material (see also Chapter 5); possibly some of the material at the monitored beach originates from an adjacent beach or coral reef. Discuss the impact of groynes and jetties in your area and the role of longshore currents. Often beachfront home owners build such structures to try and protect their homes, but sometimes homeowners on the other side of the groyne or jetty may experience erosion as a result of the structure. Discuss such measures in the context of the entire beach, not just the affected homeowners. Suggest the students carry out research into who owns the beach in your country. What does the law say? Are there any particular building restrictions near beaches so as to protect the public’s right to use the beach? |