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How to avoid too much or too little static stabili…
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How to differentiate the value of ship design chan…
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Why the EGA shows aggregate effects of ship motion…
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Happy Holidays from DSA Ocean and the ProteusDS Te…
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ProteusDS Update November 2024
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Why you need trends when comparing ship motion dat…
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Why hull appendages are hydrodynamically superimpo…
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DSA Ocean Upcoming Events Fall 2024
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How vortex shedding can indirectly sink your moori…
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How deepwater moorings disrupt wave-powered profil…
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How to tailor an anti-roll U-tube tank design for …
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ProteusDS Update April 2024
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How to tune an anti-roll slosh tank design for a s…
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Why time domain seakeeping analysis shows the sign…
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Why frequency domain ship motion analysis instantl…
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Why seakeeping and maneuvering are integral parts …
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ProteusDS Update December 2023
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When moorings overload wave buoys (and sink data q…
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Why you should be careful about fixating on buoy d…
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How to make the most out of flotation to minimize …
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Why anchor size causes a chain reaction on operati…
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Why indirect relationships drive wave buoy mooring…
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How to give your mooring design a quick reality ch…
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Introducing the dedicated ProteusDS website
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Finding maximums part 3: How a repeating sea surfa…
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Finding maximums part 2: Why using multiple sea st…
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Finding maximums part 1: How process reveals maxim…
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When to reduce mooring recovery risk with a backup…
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Why spar floaters are so insensitive to harsh cond…
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Why you need breathing space between glass floats …
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Why tiny active stabilizers have a large effect on…
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ProteusDS Update
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How antiroll tanks work to passively reduce ship r…
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Why the sensitivity of ship roll damping makes nav…
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Why drag loads are underwhelming at damping floati…
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Why it’s hard to distinguish between the effects o…
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When you need to fine tune surface buoy damping (a…
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ProteusDS Update
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How to take the guesswork out of wave radiation fo…
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Why the added mass force can be confusing
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How to control downweight seabed clearance in wave…
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Why adapt shallow water geometric compliant moorin…
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Why shallow water mooring design takes longer than…
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How to avoid wuzzles when recovering oceanographic…
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What to keep an eye on during oceanographic moorin…
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How the anchor-last oceanographic mooring deployme…
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Why an RAO is the dynamic fingerprint of a hull
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How seakeeping analysis reveals surprising differe…
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What the playground can teach us about resonance i…
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When wave steepness pinpoints worst case sea state…
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Why you see modular oceanographic mooring design e…
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How to correct subsurface mooring knockdown
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When to check instrument depth in oceanographic mo…
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How mooring deflection disrupts oceanographic data…
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Why drag force is more than just resistance
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How to understand the nature of buoyancy
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Why free body diagrams eliminate confusion in engi…
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When profilers are optimized for control
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When profilers are specially adapted to ride ocean…
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Why profilers stop massive data processing headach…
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When it is sensible to use nonlinear Froude-Krylov…
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Why parts libraries are essential to save time in …
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When to avoid a static solver in oceanographic moo…
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How to effectively model oceanographic surface buo…
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How to systematically evaluate oceanographic moori…
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How to control uncertainty in buoy drag coefficien…
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Why uncertainty in buoy drag coefficient puts ocea…
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Why compliance is at the heart of resilient oceano…
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