. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -1000 â & ^. SloP^ .bâb tL. B^bâb- TâIâIâr- 20 40 ~1 1 1 1 1 1 T" 60 80 100 120 AZIMUTH (degrees) â '§ Figure E-4 Artificially generated surface composed of orthogonal trends with spectral parameters b= , a= in the N-S direction, and b= , a= in the E-W direction. Azi- muthally dependent spectral parameters are plotted below. 211. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -1000 â & ^. SloP^ .bâb tL. B^bâb- TâIâIâr- 20 40 ~1 1 1 1 1 1 T" 60 80 100 120 AZIMUTH (degrees) â '§ Figure E-4 Artificially generated surface composed of orthogonal trends with spectral parameters b= , a= in the N-S direction, and b= , a= in the E-W direction. Azi- muthally dependent spectral parameters are plotted below. 211. 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
