. Deep-sea moorings; design and use with unmanned instrument stations. Deep-sea moorings; Oceanographic buoys. ASSUMED HORIZONTAL VELOCITY PROFILE Vand V'^vs. d Knofs^ 1000 bJ O 2 a: Z) CO 5 Q X 1500 2000 WIRE PROFILE. 2500 ANCHOR Force Vectors linch= 100 lbs. —1 300 T 0 100 200 Fig. 13. Graphic solution of deep-mooring configuration. in fact, occurs, it is sufficient to vise as a basis for calculating the magnitude of the effects of a buoyant pennant. The force parallel to the sea surface is expressed by Fh = FpCos[90°-(e„.i-Ae)] (22) = FpSin {e^.^-^6). Please note that these images are e
. Deep-sea moorings; design and use with unmanned instrument stations. Deep-sea moorings; Oceanographic buoys. ASSUMED HORIZONTAL VELOCITY PROFILE Vand V'^vs. d Knofs^ 1000 bJ O 2 a: Z) CO 5 Q X 1500 2000 WIRE PROFILE. 2500 ANCHOR Force Vectors linch= 100 lbs. —1 300 T 0 100 200 Fig. 13. Graphic solution of deep-mooring configuration. in fact, occurs, it is sufficient to vise as a basis for calculating the magnitude of the effects of a buoyant pennant. The force parallel to the sea surface is expressed by Fh = FpCos[90°-(e„.i-Ae)] (22) = FpSin {e^.^-^6). 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 Isaacs, John D. (John Dove). Berkeley, University of California Press
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