How Foiling Works

The physics of flying on water — from Bernoulli's principle to the apparent wind revolution

Quick Facts

PrincipleInverted wing generating upward lift as boat speed increases
Foil TypesL-foil T-foil
Takeoff SpeedTypically 8–15 knots depending on boat and foil design
Speed Gain15 knots wind → 20–30 knots boat speed in foiling mode
Key InventionWand-controlled T-foil ride height (Moth dinghy, late 1990s)
Drag ReductionHull drag eliminated; only small foil wetted surface remains

A foiling sailboat does something that looks impossible: it lifts its entire hull clear of the water and sails through the air on thin carbon struts, touching the water only where the foil blades penetrate below the surface. At speed, the hull — the heaviest, most drag-producing part of the boat — becomes irrelevant. What remains is the rig generating thrust and the foil blades generating lift, connected by struts, sailing through two fluids simultaneously: water below, air above.

The physics behind this are not exotic. They are the same principles that keep aircraft aloft, applied upside down and underwater. Understanding them changes how you read foiling performance figures and why foiling boats can achieve speeds that would have seemed implausible to a sailor from even twenty years ago.

Bernoulli's Principle: The Inverted Wing

A foil works on the same principle as an aircraft wing. An aerofoil shape — curved on one surface, flatter on the other — creates a pressure difference when fluid flows over it. The fluid moving over the curved surface must travel a longer path in the same time, so it accelerates. Faster-moving fluid has lower pressure. The pressure differential between the two surfaces generates a net force perpendicular to the flow direction: lift.

On an aircraft, the wing is oriented so lift points upward, opposing gravity. On a sailing foil, the wing is inverted and submerged: the curved surface faces downward, the flat surface faces up. As water flows over the foil, the same pressure differential develops — but now the net force points upward, directly opposing the weight of the boat. When that upward force equals the weight of the boat and crew, the hull lifts clear of the water.

The critical relationship is between speed and lift. Lift increases with the square of flow velocity — double the speed and you get four times the lift. At low speeds, a foil generates little lift and the boat sails in conventional displacement or planing mode. As speed increases past a threshold, lift builds rapidly until it exceeds the boat's weight. The hull rises. Drag drops dramatically. The boat accelerates further. This is the "takeoff" that foiling sailors describe.

L-Foil vs T-Foil: Two Approaches to the Same Problem

Two basic foil shapes dominate modern foiling sailboats, and they solve the ride-height problem in fundamentally different ways.

The L-foil is the simpler design: a vertical strut descending from the hull with a horizontal wing at the bottom, forming an L-shape. The horizontal wing generates lift. The vertical strut provides lateral resistance, replacing the daggerboard or centerboard function. L-foils are passive — the lift they generate depends entirely on boat speed and foil angle. As speed changes, lift changes. Controlling ride height requires the sailor to actively trim the boat through body weight, rudder, and sail trim. L-foils are used on entry-level foilers and catamarans where the two-hull platform provides inherent stability.

The T-foil is more sophisticated: a vertical strut with a horizontal wing at the bottom, plus a second smaller horizontal wing (the elevator) at the base of the rudder. The T designation refers to the cross-section of the foil assembly: strut on top, wing below, forming a T. Critically, the angle of the main foil wing can be changed in real time — either mechanically or via an automated control system. This allows the lift generated to be varied independently of boat speed, giving the sailor active control of ride height. T-foil boats can maintain a set height above the water across a range of speeds, dramatically improving stability and control.

The Wand System: Automated Ride Height Control

The breakthrough that made modern foiling accessible was the development of the wand-controlled T-foil system, pioneered in the Moth dinghy class through the late 1990s and early 2000s. Before this, foiling was largely an academic curiosity — boats could foil, but controlling ride height required superhuman reflexes.

The wand system works through elegant mechanical feedback. A thin carbon wand extends from the bow of the boat and floats on the water surface. As the hull rises, the wand angle relative to the hull changes. That change in angle is transmitted mechanically — through pushrods and linkages — to the flap on the main foil, adjusting its angle of attack. As the hull rises too high, the wand signals the foil to reduce lift. As the hull drops, the wand signals for more lift. The entire system operates without electronics, without sensors, without software: purely mechanical feedback at sailing speeds.

More recent foiling designs, particularly in the America's Cup and SailGP, have replaced the wand with sophisticated electronic flight control systems — sensors measuring boat attitude, speed, and foil loading feed into computers that make hundreds of adjustments per second. But the Moth's wand system remains the elegant proof of concept, and understanding it clarifies how active foil control works in principle.

The Performance Envelope: Takeoff and the Crash-Stall Cycle

Every foiling boat has a minimum speed at which it can sustain flight. Below that speed, the foil generates insufficient lift and the hull drops back into the water. For small foiling dinghies like the Moth and Waszp, takeoff typically requires 8–12 knots of boat speed. Larger foiling catamarans may need somewhat less. The AC75 America's Cup boats, with their enormous sail area and optimized foils, can fly in remarkably light air.

The takeoff itself is threshold behavior: the boat sails in displacement mode, speed builds slowly, and then at a critical speed the lift exceeds weight and the hull rises rapidly. The sudden reduction in drag causes an immediate speed surge — which generates more lift — which raises the hull further. This positive feedback loop is what gives foiling its dramatic "pop" character.

For learning sailors, this threshold behavior produces the characteristic crash-stall cycle. The boat takes off, the sailor loses control of ride height, the hull rises too high, the foil breaches the surface and loses lift, and the boat crashes off the foil — typically nose-diving if speed is lost suddenly, or rolling if control of heel is lost. Recovery involves getting the boat flat, regaining displacement-mode speed, and attempting takeoff again. Experienced foilers make this look effortless. In early sessions, it is anything but.

The Apparent Wind Revolution

The most counterintuitive aspect of foiling performance is the apparent wind effect. A conventional sailing boat moving at, say, 6 knots in 12 knots of true wind experiences apparent wind from a direction somewhere between the true wind direction and dead ahead, at a speed somewhat higher than 12 knots. The faster the boat goes, the further forward the apparent wind comes and the more it increases in speed.

A foiling boat exploits this effect to a degree that seems to break the rules. Consider a Moth sailing in 12 knots of true wind, achieving 25 knots of boat speed on a reach. At that speed, the apparent wind is coming from nearly dead ahead and blowing at 30+ knots. The boat is not sailing with the wind — it is sailing almost into a wind of its own creation. The sail must be trimmed accordingly: almost flat, driving the boat forward against this self-generated headwind.

The performance implication is profound. A foiling boat does not stop accelerating when it reaches the wind speed. It can continue accelerating past wind speed, generating ever-more apparent wind from ahead, which it converts into forward thrust. The theoretical limit is drag, not wind speed. In practice, this is why foiling boats can achieve velocities that are multiples of the true wind speed — ratios of 2:1 or higher are achievable in optimal conditions.

Drag Reduction: Why Foiling Is So Fast

The reason foiling produces such dramatic speed gains comes down to drag. A displacement hull moving through water creates two kinds of drag: skin friction from the wetted surface and wave-making drag from pushing water aside. Wave-making drag increases with the square of speed and becomes the dominant limit for non-planing hulls — this is why displacement boats have a theoretical hull speed beyond which additional power produces almost no additional speed.

When a foiling boat lifts its hull clear of the water, hull drag — both skin friction and wave-making — drops to essentially zero. What remains is the drag of the foil struts, the small foil blade wetted area, and the aerodynamic drag of the rig. Compared to the drag of a planing hull at the same speed, this is a fraction. The power available from the rig — unchanged — now overcomes a vastly smaller resistance. Speed increases dramatically.

This is the core engineering insight behind foiling. It is not that the foil provides extra thrust — it provides a path to dramatically lower drag. The sail rig was always capable of driving a boat at 25 knots. The hull drag was the barrier. Remove the hull from the water and the barrier largely disappears.

Foiling Classes and Boats

From the Waszp and Moth to the SailGP F50 and AC75 — see the full guide to foiling sailboat classes: Foiling Classes →  |  Learning to Foil →

← Foiling & High-Performance Sailing  |  Foiling Classes →

Frequently Asked Questions

What is the basic physics principle that allows a hydrofoil to lift a boat out of the water? A hydrofoil operates on the same Bernoulli principle as an aircraft wing — but inverted to generate upward lift rather than downward force. The curved upper surface of the foil accelerates water flow, reducing pressure; the flat lower surface has higher pressure, and the pressure differential pushes the foil — and the hull above it — upward. Once the hull clears the water surface, all hull drag disappears and the boat accelerates dramatically.

What is the difference between an L-foil and a T-foil and which is used on cruising foilers? An L-foil is a passive design: an L-shaped strut with a fixed horizontal wing at the bottom. It provides lift at speed but has no active height control, so the ride height varies with boat speed and cannot be adjusted. A T-foil is an active design with a variable-angle elevator at the rudder base that adjusts foil angle in real time to maintain consistent flying height regardless of speed changes. Cruising foilers like the Gunboat G4 use T-foil systems for stable, controllable flight.

How does the wand-controlled T-foil system work without electronics? The wand is a simple mechanical arm that floats on the water surface ahead of the windward foil. As the boat rises too high, the wand drops and mechanically reduces the foil's angle of attack, reducing lift. As the boat sinks too low, the wand rises and increases foil angle, generating more lift. The entire feedback loop is purely mechanical — a wand connected by rods and levers to the foil flap — with no sensors, no electronics, and no software. This system was pioneered on the Moth dinghy and proved the concept for larger foiling sailboats.

What is the apparent wind revolution and why does it transform how foiling boats sail? As a foiling boat accelerates, it generates its own apparent wind component from forward motion. At 25 knots boat speed in 12 knots of true wind, the apparent wind angle shifts to nearly dead ahead and the apparent wind speed reaches 30 or more knots — creating a self-reinforcing acceleration cycle where going faster generates more apparent wind, which drives more speed. This is why foiling boats can sail significantly faster than the true wind and why foiling upwind at angles previously impossible for any displacement sailboat is achievable in foiling mode.

At what wind speed does a typical foiling sailboat lift onto its foils and what speeds can it reach? Most production foiling sailboats require 8 to 15 knots of wind to achieve takeoff, depending on displacement, foil area, and sea state. Once foiling, a boat in 15 knots of true wind can sustain 20 to 30 knots of boat speed in foiling mode — two to three times the wind speed — compared with 6 to 8 knots for the same hull sailing in displacement mode. The transition from displacement sailing to foiling is called takeoff, and learning to manage the crash-stall cycle is the primary skill for new foiling sailors.

How do AC75 and SailGP foiling systems differ from the mechanical wand systems used on smaller boats? America's Cup AC75s and SailGP F50s use fully electronic flight control systems: onboard sensors measure ride height, heel angle, pitch, and foil loads at high frequency and feed data to hydraulic actuators that adjust foil rake and flap angle in milliseconds — far faster than any mechanical wand system could respond. These systems keep a 6,500-kilogram AC75 flying at 50-plus knots with millimeter precision over wave faces. The wand system used on Moths and early cruising foilers is a brilliantly simple analogue solution to the same control problem the AC75 solves with computing power.