. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -500 4 £-50 X O- 175 O 400 0 ,01 - to 10° 10- QIO-H ^ 10 i; io-« I 10-5 10-6 10- 16 32 48 64 80 DISTANCE (KILOMETERS) 96 1)2 128. 10' 10° 10' FREQUENCY (CYQES/KILOMETER) 102 Figure 5-12 Typical amplitude spectrum of profiles collected on the Continental Rise, east coast All fourteen profiles examined in this province (shown in Figure 5-13) show nearly identical patterns. The two linear segments^ in this example intersect at ~ cycles/km., with b = , t = 0jpi
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -500 4 £-50 X O- 175 O 400 0 ,01 - to 10° 10- QIO-H ^ 10 i; io-« I 10-5 10-6 10- 16 32 48 64 80 DISTANCE (KILOMETERS) 96 1)2 128. 10' 10° 10' FREQUENCY (CYQES/KILOMETER) 102 Figure 5-12 Typical amplitude spectrum of profiles collected on the Continental Rise, east coast All fourteen profiles examined in this province (shown in Figure 5-13) show nearly identical patterns. The two linear segments^ in this example intersect at ~ cycles/km., with b = , t = 0jpi42 m. for the longer wavelength model, and b * , a = m. for the shorter wavelength model. 76. 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
