. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -1000 t. i - U '0 UJ z 96 ^l3 I- o . 0 a â s. -1-0-|âIâIâIâIâIâIâIâIâIâIâIâIâIâIâIâI r 0 20 40 . 60 80 100 120 140 160 180 AZIMUTH (degrees) Figure E-1 Artificially generated surface composed of two identical orthogonal trends, both with spectral slope b= , and spectral intercept a= Viewpoint is^from^ the southwest. Below, the variation of parameters a and b are shown versus azimuth. 204. Please note that these images are extracted from scanned page image
. Description, analysis and predictions of sea floor roughness using spectral models. Ocean bottom; Submarine geology. -1000 t. i - U '0 UJ z 96 ^l3 I- o . 0 a â s. -1-0-|âIâIâIâIâIâIâIâIâIâIâIâIâIâIâIâI r 0 20 40 . 60 80 100 120 140 160 180 AZIMUTH (degrees) Figure E-1 Artificially generated surface composed of two identical orthogonal trends, both with spectral slope b= , and spectral intercept a= Viewpoint is^from^ the southwest. Below, the variation of parameters a and b are shown versus azimuth. 204. 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
