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Propagation of surface water wave pulses over an uneven topographical bottom
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10.1063/1.2219130
/content/aip/journal/apl/89/1/10.1063/1.2219130
http://aip.metastore.ingenta.com/content/aip/journal/apl/89/1/10.1063/1.2219130
View: Figures

Figures

Image of FIG. 1.
FIG. 1.

Spatial distribution of the intensity field (left panel) and logarithm of the averaged transmission as a function of distance (right panel) for two frequencies: (a) and (b) . Here, the transmission has been averaged over 100 random configurations and normalized to eliminate the geometrical spread effect.

Image of FIG. 2.
FIG. 2.

Left column from top to bottom: time series of the origin signal (a1), averaged backscattering signal received at the origin (b1), and averaged transmitted signal received at (c1). Right column: power spectra corresponding to the signals shown in the left column. 100 random configurations are considered in the simulation.

Image of FIG. 3.
FIG. 3.

(a) Averaged backscattering signal (at the origin) and averaged transmitted signal (at ) received after the pulse is excited. (b) Power spectra. Note that the spectrum corresponding to has been amplified fivefold for clarity.

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/content/aip/journal/apl/89/1/10.1063/1.2219130
2006-07-05
2014-04-19
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752b84549af89a08dbdd7fdb8b9568b5 journal.articlezxybnytfddd
Scitation: Propagation of surface water wave pulses over an uneven topographical bottom
http://aip.metastore.ingenta.com/content/aip/journal/apl/89/1/10.1063/1.2219130
10.1063/1.2219130
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