. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -1000 % a. ^ m-'^-^ ;'-^" ^ £ - -0â0 5ââ " 0 ° U-20 "1âIâIâiâI 1âI 1âIâI 1âIâI 1âI 1 r 20 la 60 80 100 120 140 160 180 AZIMUTH (degrees) Figure E-3 Artificially generated surface composed of two orthogonal trends with identical intercepts of a= , but spectral slopes of b= in the N-S direction and b= in the E-W direction. Azimuthally dependent spectral parameters are plotted below. 208. Please note that these images are extract
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -1000 % a. ^ m-'^-^ ;'-^" ^ £ - -0â0 5ââ " 0 ° U-20 "1âIâIâiâI 1âI 1âIâI 1âIâI 1âI 1 r 20 la 60 80 100 120 140 160 180 AZIMUTH (degrees) Figure E-3 Artificially generated surface composed of two orthogonal trends with identical intercepts of a= , but spectral slopes of b= in the N-S direction and b= in the E-W direction. Azimuthally dependent spectral parameters are plotted below. 208. 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
