. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. 10« 10- S 10-=' St % 10-3 o lU N 10- 10-5 10- 100 200 300 DISTANCE (KILOMETERS) 400 SLOPE = INTERCEPT :.410-083. 10- 10-2 ,0' 10° FREQUENCY (CYQES/KILOMETER) 10' Figure 5-10 Amplitude spectrum of a long bathymetrlc profile, which encompasses several statistically homogeneous provinces. The inclusion of non-stationary segments into the analyses results in a spectral slope parameter which approaches b= 73. Please note that these images are extracted from scanned page
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. 10« 10- S 10-=' St % 10-3 o lU N 10- 10-5 10- 100 200 300 DISTANCE (KILOMETERS) 400 SLOPE = INTERCEPT :.410-083. 10- 10-2 ,0' 10° FREQUENCY (CYQES/KILOMETER) 10' Figure 5-10 Amplitude spectrum of a long bathymetrlc profile, which encompasses several statistically homogeneous provinces. The inclusion of non-stationary segments into the analyses results in a spectral slope parameter which approaches b= 73. 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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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
