too turbid or deep to image the bed from aerial platforms ... too swift or deep to wade to obtain physical samples ... spatial variability is so great its impractical to sample using conventional methods
too turbid or deep to image the bed from aerial platforms ... too swift or deep to wade to obtain physical samples ... spatial variability is so great its impractical to sample using conventional methods
too turbid or deep to image the bed from aerial platforms ... too swift or deep to wade to obtain physical samples ... spatial variability is so great its impractical to sample using conventional methods
any river or stream navigable by small boat. Sufficient quality for bed imaging in shallow streams Automate sonar processing, positioning, and substrate classification
shallow riverine benthic sediments. A new automated, spatially explicit and physically based method for texture lengthscales in sidescan echograms Not a direct measure of grain size could provide a basis for objective, automated riverbed sediment classification
shallow riverine benthic sediments. A new automated, spatially explicit and physically based method for texture lengthscales in sidescan echograms Not a direct measure of grain size could provide a basis for objective, automated riverbed sediment classification
shallow riverine benthic sediments. A new automated, spatially explicit and physically based method for texture lengthscales in sidescan echograms Not a direct measure of grain size could provide a basis for objective, automated riverbed sediment classification
shallow riverine benthic sediments. A new automated, spatially explicit and physically based method for texture lengthscales in sidescan echograms Not a direct measure of grain size could provide a basis for objective, automated riverbed sediment classification
(n - ( nW 2 n (s) δy))2 W 2 n (s)δy Location along scan (pixel) Wavelet power spectrum (function of location and scale) Metres between pixels Buscombe et al., Journal of Hydraulic Engineering, in review