The Physics Behind Your Edge

SailEdge™ starts from your ORC certificate and keeps the certified polar as the baseline anchor. From there, the runtime resolves apparent wind, force balance, heel, resistance, and depower to explain where each sail comparison gains or gives up speed. This page explains how those deltas are derived and why they matter.

Explore Your Edge Read the walkthrough →
Foundation

It Starts with the Certificate

Every SailEdge computation begins with an ORC certificate — your hull lines, rig dimensions, sail inventory, displacement, and the complete polar table produced by the official ORC VPP. That polar is the immutable floor. SailEdge never overrides it, never adjusts it, never second-guesses it.

The certificate defines what the boat can do in ideal conditions with the rated sail plan. Everything SailEdge adds is built on top of that baseline. Built on ORC, not around it.


Wind Model

From True Wind to Apparent Wind

ORC reports true wind speed at a 10-meter reference height. SailEdge takes that true wind vector and converts it to apparent wind at the sail plan — accounting for boat speed, heel angle, and leeway. The apparent wind speed and angle that arrive at each sail drive everything downstream: the forces, the loads, the balance.

Get the apparent wind wrong and every downstream delta is wrong with it. This conversion is the first thing the runtime resolves because both the baseline and the candidate have to be compared on the same physical footing.


Aero Forces

Lift, Drag, and Everything in Between

Each sail in the plan — main, jib, genoa, spinnaker, code zero — gets its own force decomposition. Lift and drag coefficients are computed from the sail’s geometry and the apparent wind angle. Those coefficients produce the drive force (forward) and side force (heeling) that let the baseline sailplan and the candidate be compared at the same wind condition.

Sails don’t operate in isolation. When a headsail sits in the main’s wind shadow at tight angles, the model accounts for blanketing — the reduction in effective wind that the downstream sail actually sees. The shape of each foil matters too: aspect ratio, overlap, roach. Different sail shapes produce different force profiles at the same wind angle.

At the professional tier, loft-specific sail shapes feed directly into these coefficients. The generic geometry is replaced with measured cut-sheet data.

Force decomposition diagram showing sail planform with lift, drag, drive, and side force vectors from center of effort — aero and boat reference frames

Hydro Forces

The Boat Pushes Back

Aero forces drive the boat forward. Hydrodynamic forces resist that motion. In the current runtime, SailEdge uses a boat-integrated Delft Series Hydro backbone grounded in ORC certificate geometry and approved boat-carried hydro fields. Upright hull resistance, heel influence, appendage resistance, sideforce/leeway, rudder interaction, and approved wave resistance are resolved as named hydro lanes where the boat data supports them.

Your boat’s resistance profile is unique. When a lane is authoritative, the model uses your boat’s carried data and the live DSH runtime for both sides of the comparison. When a lane is bounded or waiting on better input, SailEdge discloses that instead of pretending to know more than it does.


Equilibrium

Where the Forces Balance

Drive force wants to push the boat forward. Side force wants to heel it over. Hull resistance wants to slow it down. The righting moment wants to stand it back up. Change the crew weight and righting moment shifts — the entire equilibrium recomputes. SailEdge solves for the equilibrium state that lets baseline and candidate sailplans be compared under the same wind condition — iteratively, not by lookup.

The runtime converges on a single deterministic answer for each wind condition and sail comparison. Same certificate, same sails, same conditions, same answer. No random variation, no Monte Carlo, no stochastic noise.

Tune the righting moment for form vs ballast stability. Form-stabilized hulls need increasing RM correction at high heel angles where waterplane advantage fades.

Heel equilibrium chart showing heeling moment and righting moment curves intersecting at equilibrium angle of 20.3 degrees

Depower

When the Wind Overpowers the Rig

Real sails don’t hold their designed shape in all conditions. As wind builds past the sail’s effective range, the crew depowers — and the model does too. SailEdge applies multiple independent depower effects, each one specific to the sail type and the condition that triggers it.

Reefing the main is not the same as easing the traveler. Furling a headsail is not the same as flattening it. Each depower mechanism changes the force profile differently — reducing drive, reducing heel, or both — and SailEdge tracks each effect separately.

The result is a depower model that behaves the way sails actually behave: progressively, sail-by-sail, with each mechanism doing its own work.


Speed

From Force Balance to Boat Speed

Once the runtime resolves equilibrium, the ORC polar remains the certified anchor for the comparison. SailEdge evaluates how a candidate sailplan behaves relative to that baseline at the same wind condition, with hull-speed fences, stability thresholds, and minimum-drive requirements keeping the comparison inside a qualified envelope.

Baseline stays untouched as the reference. Candidate upside is published only inside the allowed compare fence, and any blocked or unstable condition is reported as such instead of being passed off as a replacement certified speed. Every limit is attributed so you can see what bounded the answer and why.

The certificate is the contract. SailEdge publishes directional deltas from that contract, not official ORC speed changes.


Output

Every Cell Tells the Full Story

The Edge Map is the output surface. Each cell is one wind condition (TWA and TWS), one baseline-versus-candidate sail comparison, and one published speed delta. The color encodes that delta. Tap a cell and the detail card opens.

What you see in that card depends on your tier — the decision layer shows the answer, the diagnosis layer shows the force balance, and deeper layers preserve the baseline, candidate, and delta correspondence. Three levels of depth. The compare semantics stay the same throughout.

See what’s inside a cell →

Edge Map grid with selected cell highlighting Code Zero advantage of +1.04 kt, connected to three-tier detail card showing Edge, Expert Mode, and Engineering data layers

See It on Your Boat

Upload your ORC certificate. See where a sail change moves the boat relative to baseline.

Explore Your Edge Anatomy of a cell →