Difference between revisions of "Bar"
From Coastal Wiki
Tasomerville (talk | contribs) m |
|||
(2 intermediate revisions by one other user not shown) | |||
Line 1: | Line 1: | ||
{{Definition|title=Bar | {{Definition|title=Bar | ||
|definition= | |definition= | ||
− | A submerged shore parallel embankment of sand or gravel built in the breaker zone due to the action of breaking waves and cross-currents. | + | A submerged shore parallel embankment of sand or gravel built in the breaker zone due to the action of breaking waves and cross-currents<ref name=”Karsten”>Mangor, Karsten. 2004. “Shoreline Management Guidelines”. DHI Water and Environment, 294pp.</ref>. |
}} | }} | ||
− | == | + | ==Definition of Bar - Further notes== |
*There can be several rows of bars. | *There can be several rows of bars. | ||
*Bars are very mobile formations, which tend to be in mobile equilibrium with the presently occurring wave and tide conditions, which means that they are constantly changing. | *Bars are very mobile formations, which tend to be in mobile equilibrium with the presently occurring wave and tide conditions, which means that they are constantly changing. | ||
*The overall tendency is that the bars are moving seawards during storm wave conditions and landwards during conditions dominated by smaller waves and swell. | *The overall tendency is that the bars are moving seawards during storm wave conditions and landwards during conditions dominated by smaller waves and swell. | ||
− | *At intervals there are gaps in the bars formed by the [[rip | + | *At intervals there are gaps in the bars formed by the [[rip current]]s. |
+ | |||
+ | |||
+ | ==References== | ||
+ | <references/> |
Revision as of 12:22, 21 September 2008
Definition of Bar:
A submerged shore parallel embankment of sand or gravel built in the breaker zone due to the action of breaking waves and cross-currents[1].
This is the common definition for Bar, other definitions can be discussed in the article
|
Definition of Bar - Further notes
- There can be several rows of bars.
- Bars are very mobile formations, which tend to be in mobile equilibrium with the presently occurring wave and tide conditions, which means that they are constantly changing.
- The overall tendency is that the bars are moving seawards during storm wave conditions and landwards during conditions dominated by smaller waves and swell.
- At intervals there are gaps in the bars formed by the rip currents.
References
- ↑ Mangor, Karsten. 2004. “Shoreline Management Guidelines”. DHI Water and Environment, 294pp.