. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. to" 10' 10' I0« 10^ 0 10' "e 10' uTio* io» io» - 10' - 10= « 'Ts '^^. BALMINO ET AL. (1973) WARREN (1973) BRETHERTON (1969) COX a SANOSTROM (1962 ) ABYSSAL HILLS 10" 10" 10* 10"* 10*' I0-' K, cyc/km 10" 10' 10* Figure 4-4 Spectral estimates collected by T. H. Bell (1975b) from various sources. The linear distribution of the data illustrates the power law form of submarine topography spectra for a wide range of scales. Notice that this spec- trum i
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. to" 10' 10' I0« 10^ 0 10' "e 10' uTio* io» io» - 10' - 10= « 'Ts '^^. BALMINO ET AL. (1973) WARREN (1973) BRETHERTON (1969) COX a SANOSTROM (1962 ) ABYSSAL HILLS 10" 10" 10* 10"* 10*' I0-' K, cyc/km 10" 10' 10* Figure 4-4 Spectral estimates collected by T. H. Bell (1975b) from various sources. The linear distribution of the data illustrates the power law form of submarine topography spectra for a wide range of scales. Notice that this spec- trum is plotted versus power (amplitude squared) which results in a doubling of the ordinate and the slope of an amplitude spectrum. Refer to Bell (1975b) for data sources. 27. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Fox, Christopher Gene; United States. Naval Oceanographic Office. Bay St. Louis, Miss. : Naval Oceanographic Office
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