Archive image from page 236 of Description, analysis and predictions of. Description, analysis and predictions of sea floor roughness using spectral models descriptionanaly00foxc Year: 1985 -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 isfrom the southwest. Below, the variation of parameters a and b are shown versus azimuth. 2


Archive image from page 236 of Description, analysis and predictions of. Description, analysis and predictions of sea floor roughness using spectral models descriptionanaly00foxc Year: 1985 -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 isfrom the southwest. Below, the variation of parameters a and b are shown versus azimuth. 204


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