Difference between revisions of "Longshore current"

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{{Definition|title=Longshore current / Nearshore current
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{{Definition|title=Longshore current
|definition= The longshore current is the dominating current in the [[nearshore]] zone (upper shoreface), it is running parallel to the shore. The longshore current is generated by the shore-parallel component of the stresses associated with the breaking process for obliquely incoming waves, the so-called radiation stresses, and by the surplus water which is carried across the [[breaker zone]] towards the [[shoreline]]<ref name="Karsten">Mangor, Karsten. 2004. “Shoreline Management Guidelines”. DHI Water and Environment, 294pp.</ref>.
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|definition=Current running parallel to the shore generated by obliquely incident waves.  
 
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==Notes==
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The longshore current is generated by the shore-parallel component of the stresses associated with the breaking process of obliquely incoming waves, the so-called [[radiation stress]]es. It is often the dominating current in the [[surf zone]]. <ref name="Karsten">Mangor, Karsten. 2004. “Shoreline Management Guidelines”. DHI Water and Environment, 294pp.</ref>.
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==See also==
 
==See also==

Revision as of 14:26, 6 October 2021

Definition of Longshore current:
Current running parallel to the shore generated by obliquely incident waves.
This is the common definition for Longshore current, other definitions can be discussed in the article


Notes

The longshore current is generated by the shore-parallel component of the stresses associated with the breaking process of obliquely incoming waves, the so-called radiation stresses. It is often the dominating current in the surf zone. [1].


See also

Shallow-water wave theory

For more coastal definitions and a sketch, see also Definitions of coastal terms.

References

  1. Mangor, Karsten. 2004. “Shoreline Management Guidelines”. DHI Water and Environment, 294pp.