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Centered disturbances

These are disturbances for which the ray paths of k project backwards in time to a common point in the x, t-plane, which represents a virtual source point at which a finite total energy has been injected with ordered phases and a given wave number spectrum tex2html_wrap_inline5529 . Let the virtual source be taken as x = 0, t = -a, then the required tex2html_wrap_inline5425 for a centered disturbance is

displaymath5539

such that (1.25) becomes

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Now (1.27) and (1.32) require that

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Integration by parts gives

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recognizing that tex2html_wrap_inline5547 . Thus (1.26) takes the form

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where b is an arbitrary constant of integration. Finally, from (1.32)

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and hence (1.31) takes the form

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Thus

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which implies that, except for a scaling factor tex2html_wrap_inline5559 , the spectral distribution of energy versus wave number (or frequency) is conserved for a centered disturbance.

In the following examples we will shift the time origin to the virtual source, which means we replace tex2html_wrap_inline5561 by t. Equation (1.35) the becomes tex2html_wrap_inline5565 where tex2html_wrap_inline5479 now represents the value of M vs. k at t = a.


next up previous contents
Next: Short gravity waves Up: Special cases Previous: Non-dispersive wave group

Steve Baum
Sun May 19 00:59:05 CDT 1996