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Encyclopedia > Swell (ocean)
Look up swell in Wiktionary, the free dictionary.

A swell, in the context of an ocean, is a formation of long wavelength ocean surface waves on the sea. Swells are far more stable in their directions and frequency than normal oceanic waves since they are formed by tropical storms and by stable wind systems. A swell, in the context of an ocean, is a formation of long wavelength waves in the surface of the sea. ... Wikipedia does not have an article with this exact name. ... Wiktionary (a portmanteau of wiki and dictionary) is a multilingual, Web-based project to create a free content dictionary, available in over 150 languages. ... Animated map exhibiting the worlds oceanic waters. ... Ocean waves Ocean surface waves are surface waves that occur at the surface of an ocean. ...


From a surfing perspective, swells are often created by storms thousands of miles/kilometers away from the beach where they are surfed. This distance allows the waves comprising the swells to become more stable, clean, and free of chop as they travel toward the coast. Waves generated by storm winds having the same speed will group together and travel with each other, while others traveling at even a fraction of a second slower will lag behind, ultimately arriving many minutes later due to the distance traveled. This is a well known fact for surfers, swell waves come in sets. So Catching the first wave may allow you time to also catch a wave at the end of the set.


Information on swell size and period is useful for surfers, as swells are generally more desirable to surf on than normal, locally-generated waves and chop. Swell size is typically the average height of the largest 33% of waves in a set, measured from the highest point of a wave (peak) to the lowest point (trough). Swell size is also known as the significant wave height and it is the cube of the significant wave height that typically is used as the important component of the equation to calculate how much energy that wave has to erode a coastline. Period is the average length of time between each wave in a set. The significant period is the average period between the third largest waves in a wave record.[1] An equation is a mathematical statement, in symbols, that two things are the same (or equivalent). ... This article does not cite any references or sources. ...


Since swell-generated waves are mixed with normal sea waves, they can be difficult to detect with the naked eye (particularly away from the shore) if they are not significantly larger than the normal waves. From a signal analysis point of view, swells can be thought of as a fairly regular (though not continual) wave signal existing in the midst of strong noise (i.e., normal waves and chop).


Swells were used by Polynesians to maintain course when no other clues where available, such as on foggy nights. Carving from the ridgepole of a Māori house, ca 1840 Polynesia (from Greek: πολύς many, νῆσος island) is a large grouping of over 1,000 islands scattered over the central and southern Pacific Ocean. ...


References

  1. ^ http://www.stormsurf.com/page2/tutorials/wavebasics.shtml

External links


  Results from FactBites:
 
SwellInfo.com Product Information (2200 words)
At any given time, there may be multiple swells at any location, so the swell plots split the significant wave height you see on the wave maps into the multiple concurrent open ocean swells.
In order to use the swell plots to interpret how the surf will be at your local beach, it is useful to have some local knowledge to understand what makes your local breaks turn on.
Where the swell plots give you the open ocean concurrent swells, the surf plots give you an idea of what that means for wave face size at the beach.
The Rhythmic Movements Of The Ocean, Tides, Swell, And Waves (5983 words)
THE manifestations of the life of the terrestrial globe, its general movements, the perturbations it is subjected to, the spasms of its crust, and the manifestation of electricity and magnetism which traverse it, as well as all that communicates this incessant restlessness to the Earth, have their origin in the Sun.
When the wind begins to freshen and rise, the ridges of water which constitute the undulations of the swell lose their beautiful regularity; they cease to be symmetrical, becoming steep while their surfaces are covered with ripples and subsidiary wavelets.
The most simple manifestation of undulatory movement at the surface of the sea is the swell characterised by the absence of that white foam which sailors call "white horses." It forms at the surface of the sea regular ridges, with regularly curved sides and which move majestically over the water when the atmosphere is calm.
  More results at FactBites »


 

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