. Designing a U-style mooring for use with current Oceanography. 1. Velocity profile with depth is calculated. 2. Depth of each station is calculated for the mooring in the no-current, no-stretch condition (Figure B-12) 1 tZ(1) 2--Z(2) stations depths of 3 __ z(3) stations 4-Lz(4) FIGURE B-12 - Z(l) REPRESENTS THE DEPTH CF STATION I. 3. Equivalent current speed acting on each section is calculated, as previously discussed. 4. Current acts on sections. Sections are considered separately, and there is continuity in tension from the bottom of one section to the top of the next. Correctio
. Designing a U-style mooring for use with current Oceanography. 1. Velocity profile with depth is calculated. 2. Depth of each station is calculated for the mooring in the no-current, no-stretch condition (Figure B-12) 1 tZ(1) 2--Z(2) stations depths of 3 __ z(3) stations 4-Lz(4) FIGURE B-12 - Z(l) REPRESENTS THE DEPTH CF STATION I. 3. Equivalent current speed acting on each section is calculated, as previously discussed. 4. Current acts on sections. Sections are considered separately, and there is continuity in tension from the bottom of one section to the top of the next. Corrections are made for any concentrated weights or buoys on the mooring. Sections incline (Figure B-13). section 1 section 2 section 3 FIGURE B-13 ~ THE CURRENT ACTS ON SECTIONS AND THERE IS TENSION CONTINUITY FROM ONE SECTION TO THE 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 Picciulo, Jonathan Monterey, California: U. S. Naval Postgraduate School
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Keywords: ., bookcentury1900, bookcollectionamerican, booksubjectoceanography
