. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. 100 10' -I ^10° g 10-' â Sio-^' ^ 10-'-I a UJ N 5^10 10-5. 10-* 10- 16 24 32 40 DISTANCE (KILOMETERS) 48 56. 10' 10° 10' FREQUENCY (CYQES/KIIOMETER) 10' Typical amplitude spectrum of profiles collected on the Tufts Abyssal Plain. Spectrum shows two distinct straight-line segments * which Intersect at a spatial frequency of ~ cycles/km. The longer wavelength portion Is described by b » , a = m. The shorter wavelength segment Is described by b = , S = 0.
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. 100 10' -I ^10° g 10-' â Sio-^' ^ 10-'-I a UJ N 5^10 10-5. 10-* 10- 16 24 32 40 DISTANCE (KILOMETERS) 48 56. 10' 10° 10' FREQUENCY (CYQES/KIIOMETER) 10' Typical amplitude spectrum of profiles collected on the Tufts Abyssal Plain. Spectrum shows two distinct straight-line segments * which Intersect at a spatial frequency of ~ cycles/km. The longer wavelength portion Is described by b » , a = m. The shorter wavelength segment Is described by b = , S = m. Profiles from the Cascadia Basin province have similar spectra, however the model parameters are slightly different. 74. 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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License: Licensed
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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
