0.1,7 / January 30, 2017
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Description

In fluid dynamics, a breaking wave is a wavewhose amplitude reaches a critical level at which some process cansuddenly start to occur that causes large amounts of wave energy tobe transformed into turbulent kinetic energy. At this point, simplephysical models that describe wave dynamics often become invalid,particularly those that assume linear behaviour.

The most generally familiar sort of breaking wave is thebreaking of water surface waves on a coastline. Because of thehorizontal component of the fluid velocity associated with the wavemotion, wave crests steepen as the amplitude increases; wavebreaking generally occurs where the amplitude reaches the pointthat the crest of the wave actually overturns—though the types ofbreaking water surface waves are discussed in more detail below.Certain other effects in fluid dynamics have also been termed"breaking waves," partly by analogy with water surface waves. Inmeteorology, atmospheric gravity waves are said to break when thewave produces regions where the potential temperature decreaseswith height, leading to energy dissipation through convectiveinstability; likewise Rossby waves are said to break[1] when thepotential vorticity gradient is overturned. Wave breaking alsooccurs in plasmas,[2] when the particle velocities exceed thewave's phase speed.

In fluid dynamics, thebreaking wave is a wave Whose amplitude Reaches the level criticalat Which some process can suddenly start to Occur que causes largeAmounts of wave energy to be Transformed into turbulent kineticenergy. At this point, simple physical models que describe wavedynamics Often Become invalid, Particularly Those que assumeslinear behavior.

The most familiar Generally sort of breaking wave is thebreaking of water surface waves on the coastline. Because of thehorizontal component of the fluid velocity associated with the wavemotion, wave crests steepen the the amplitude Increases; wavebreaking Generally Occurs where the amplitude Reaches the point quethe crest of the wave overturns Actually, though the types ofbreaking water surface waves are Discussed in more detail below.Certain other effects in fluid dynamics have Been Also termed"breaking waves," partly by analogy with water surface waves. Inmeteorology, atmospheric gravity waves are said to break When thewave produces regions where the potential temperature decreaseswith height, leading to energy dissipation through convectiveinstability; likewise Rossby waves are said to break [1] When thepotential vorticity gradient is overturned. Wave breaking AlsoOccurs in plasmas, [2] When the particle velocities Exceed thewave's phase speed.

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SURF 0.1,7 APK
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In fluid dynamics, a breaking wave is a wavewhose amplitude reaches a critical level at which some process cansuddenly start to occur that causes large amounts of wave energy tobe transformed into turbulent kinetic energy. At this point, simplephysical models that describe wave dynamics often become invalid,particularly those that assume linear behaviour.The most generally familiar sort of breaking wave is thebreaking of water surface waves on a coastline. Because of thehorizontal component of the fluid velocity associated with the wavemotion, wave crests steepen as the amplitude increases; wavebreaking generally occurs where the amplitude reaches the pointthat the crest of the wave actually overturns—though the types ofbreaking water surface waves are discussed in more detail below.Certain other effects in fluid dynamics have also been termed"breaking waves," partly by analogy with water surface waves. Inmeteorology, atmospheric gravity waves are said to break when thewave produces regions where the potential temperature decreaseswith height, leading to energy dissipation through convectiveinstability; likewise Rossby waves are said to break[1] when thepotential vorticity gradient is overturned. Wave breaking alsooccurs in plasmas,[2] when the particle velocities exceed thewave's phase speed.In fluid dynamics, thebreaking wave is a wave Whose amplitude Reaches the level criticalat Which some process can suddenly start to Occur que causes largeAmounts of wave energy to be Transformed into turbulent kineticenergy. At this point, simple physical models que describe wavedynamics Often Become invalid, Particularly Those que assumeslinear behavior.The most familiar Generally sort of breaking wave is thebreaking of water surface waves on the coastline. Because of thehorizontal component of the fluid velocity associated with the wavemotion, wave crests steepen the the amplitude Increases; wavebreaking Generally Occurs where the amplitude Reaches the point quethe crest of the wave overturns Actually, though the types ofbreaking water surface waves are Discussed in more detail below.Certain other effects in fluid dynamics have Been Also termed"breaking waves," partly by analogy with water surface waves. Inmeteorology, atmospheric gravity waves are said to break When thewave produces regions where the potential temperature decreaseswith height, leading to energy dissipation through convectiveinstability; likewise Rossby waves are said to break [1] When thepotential vorticity gradient is overturned. Wave breaking AlsoOccurs in plasmas, [2] When the particle velocities Exceed thewave's phase speed.
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