wave amplitude

In this case, the increase is in wave amplitude.

The coherent superposition of wave amplitudes is called first order interference.

Their wave amplitudes are usually in the tens of meters and very large wavelengths.

This leads to an exponential growth in the vortex wave amplitude.

Wave amplitude and energy could be defined as:

The wave speeds are diminished and the wave amplitudes are increased.

Hence, the wave amplitude and the bubble density vary slowly compared with the period of the oscillations.

For the case of infinitesimal wave amplitude, the terminology is linear frequency dispersion.

The relationship between the spectrum and the wave amplitude for a wave component is:

This showed peak wave amplitudes, above the mean, of approximately .011 inches over a two inch span.

As a result, it describes the variations in wave amplitude, or equivalently wave height.

Because the wave amplitude increases with decreasing density this easterly acceleration process is not effective at fairly high levels.

The effect of capillary waves is more pronounced for small asperities with heights comparable to the wave amplitude.

The waves will seek equilibrium by attempting to displace the waves amplitude because of gravity.

In other mice, both a - and b - wave amplitude reductions were seen, due in part to poor pupillary dilation.

To second order - in wave amplitude a - the components of the radiation stress tensor for progressive periodic waves are:

Vessel weight is also a critical consideration: it affects wave amplitude, and therefore the energy transferred to the wave for a given hull length.

From the wave amplitude, the amplitude of the flow velocity oscillations underneath the water surface can also be computed.

The graviton (the proposed messenger particle of the gravitational force), for example, is predicted by the theory to be a string with wave amplitude zero.

Aslavital has similar effects on the wave amplitude, whereas the changes produced in the wave frequency are generally more superficial and transitory.

A megatsunami is meant to refer to a tsunami with an initial wave amplitude (height) measured in several tens, hundreds, or possibly thousands of meters.

Distinguishable on high resolution wideband spectrographs, the wave amplitude grows linearly then switches to non-linear.

The frequency used sweeps from some few kHz to MHz, keeping the sine wave amplitude constant.

In a standing wave the nodes are a series of locations at equally spaced intervals where the wave amplitude (motion) is zero (see animation above).

In shallow water, the low-order Stokes expansion breaks down (gives unrealistic results) for appreciable wave amplitude (as compared to the depth).