Seiche

From Academic Kids

A seiche (pronounced say'sh) or an underwater wave is a standing wave in a body of water.

The term was first promoted by the Swiss hydrologist François-Alphonse Forel in 1890, who had observed the effect in Lake Geneva, Switzerland. The word originates in a Swiss French dialect word that means "to sway back and forth", which had apparently long been used in the region to describe oscillations in alpine lakes.

The period of a seiche in an enclosed rectangular body of water is usually represented by the formula:

<math>\mbox{Period}(T) = \frac{2L}{\sqrt{g d}}<math>

in which L is the length, d the average depth of the body of water, and g the acceleration of gravity.

Seiches are often imperceptible to the naked eye, and observers on the surface may not notice that a seiche is occurring. The effect is caused by natural resonances in a body of water. They often occur between warm and cold-water layers, notably in Loch Ness, Scotland. Some evidence cited for the Loch Ness monster and the Lake Champlain monster (see also Lake monster and Sea monster) may be traced to seiches.

Small rhythmic seiches are almost always present on larger lakes, and the frequency of the oscillation is determined by the size of the body, its depth and contours, and the water temperature. On the North American Great Lakes, seiche is often called slosh. It is always present, but is usually unnoticeable, except during periods of unusual calm. Harbours, bays, and estuaries are often prone to small seiches with amplitudes of a few inches and periods of a few minutes.

Missing image
Lake_Erie_water_level.gif
Differences in water level caused by a seiche on Lake Erie, recorded between Buffalo, New York (red) and Toledo, Ohio (blue) on November 14, 2003

Larger seiches can be caused by wind, earthquakes, or underwater landslides. Lake Erie is particularly prone to wind-caused seiches because of its shallowness and elongation. These can lead to extreme seiches of up to 15 feet (5 meters) between the ends of the lake. The effect is similar to a storm surge like that caused by hurricanes along ocean coasts, but the seiche effect can cause oscillation back and forth across the lake for some time. In 1954, Hurricane Hazel piled up water along the northwestern Lake Ontario shoreline near Toronto, causing extensive flooding, and established a seiche that subsequently caused flooding along the south shore. Lake seiches can occur very quickly: on July 13, 1995, a big seiche on Lake Superior caused the water level to fall and then rise again by three feet (one meter) within fifteen minutes, leaving some boats hanging from the docks on their mooring lines when the water retreated.

Lakes in seismically active areas, such as Lake Tahoe in California/Nevada, are significantly at risk from seiches. Geological evidence indicates that the shores of Lake Tahoe may have been hit by seiches and tsunamis as much as 30 feet (10 m) high in prehistoric times, and local researchers have called for the risk to be factored into emergency plans for the region. [1] (http://www.sciencenews.org/articles/20000610/bob9.asp)

Earthquake-generated seiches can be observed thousands of miles away from the epicentre of a quake. Swimming pools are especially prone to seiches caused by earthquakes, as the ground tremors often match the resonant frequencies of small bodies of water. The 1994 Northridge earthquake in California caused swimming pools to overflow across southern California, and the massive Good Friday Earthquake that hit Alaska in 1964 caused seiches in swimming pools as far away as Puerto Rico. Following the 2004 Indian Ocean earthquake, it was postulated that the shock waves could have induced seiches as far away as Oklahoma. [2] (http://www.muskogeephoenix.com/news/stories/20041228/localnews/1795857.html)

A related effect is the tsunami, a wave train (series of waves) generated in a body of water by a pulsating or abrupt disturbance that vertically displaces the water column. On occasion, tsunamis can produce seiches as a result of local geographic peculiarities. For instance, the tsunami that hit Hawaii in 1946 had a fifteen-minute interval between wave fronts. The natural resonant period of Hilo Bay is about thirty minutes. That meant that every second wave was in phase with the motion of Hilo Bay, creating a seiche in the bay. As a result, Hilo suffered worse damage than any other place in Hawaii, with the tsunami/seiche reaching a height of 14 m and killing 159 inhabitants. Seiche waves may continue for several days after a tsunami.

External links and references

General:

On aquatic monsters:

The French term:


de:Seiche

Seiche is also a French term for a type of cuttlefish.

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