In
oceanography
Oceanography (), also known as oceanology and ocean science, is the scientific study of the oceans. It is an Earth science, which covers a wide range of topics, including ecosystem dynamics; ocean currents, waves, and geophysical fluid dynamic ...
wind fetch, also known as fetch length or simply fetch, is the length of water over which a given
wind has blown without obstruction.
Fetch is used in
geography and
meteorology and its effects are usually associated with
sea state and when it reaches shore it is the main factor that creates
storm surge
A storm surge, storm flood, tidal surge, or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low-pressure weather systems, such as cyclones. It is measured as the rise in water level above the n ...
which leads to coastal
erosion and
flooding. It also plays a large part in
longshore drift
Longshore drift from longshore current is a geological process that consists of the transportation of sediments (clay, silt, pebbles, sand, shingle) along a coast parallel to the shoreline, which is dependent on the angle incoming wave direction ...
.
Fetch length, along with the wind speed (wind strength), and duration, determines the size (
sea state) of
waves produced. If the
wind direction is constant, the longer the fetch and the greater the wind speed, the more wind energy is transferred to the water surface and the larger the resulting sea state will be.
[''November's fury'' by Michael Schumaker University of Minnesota Press] Sea state will increase over time until local energy dissipation balances energy transfer to the water from the wind and a fully developed sea results.
See also
*
Gale
*
Sea state
*
Ocean surface wave
*
Storm surge
A storm surge, storm flood, tidal surge, or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low-pressure weather systems, such as cyclones. It is measured as the rise in water level above the n ...
References
Coastal geography
Oceanography
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