|
How do sails work?
Article by Paul Bogataj
Sails are wings that use the wind to generate a force
to move a boat. The following explanation of how this occurs can help
understand how to maximize the performance achieved from sails.
Sails are Flexible Wings
It is useful to recognize what a typical sail is. They are normally
built from a flexible material in order to allow the sail to work with
the wind on either side to allow tacking. This is a significant restriction
that prevents many shapes from being built because they would not be
able to support themselves in the wind. This leads to the traditional
triangular planform of sails, since the material below has to hang from
the material above, which eventually is reduced to a point at the top
of the mast. So, the problem becomes how to build and operate a flexible
sail in the wind to produce a substantial force component to move the
boat.
As the restriction that sails support themselves is
diminished (full battens and stiffer materials for example), sails can
evolve to be more efficient. Their appearance then becomes more wing-like
and less sail-like. Analyzing how a sail works as a wing is useful,
not just for modern sails that look more like wings, but also for very
traditional sails that, while they look like sails, operate very much
like wings.
Velocity and Pressure
Flow accelerates over the top surface of an airfoil, either because
it is at an angle to the flow, or because the top has more curvature
than the bottom, or both. When a fluid (like air or water) is accelerated,
the pressure that it imparts on an adjoining surface decreases. This
lower pressure pulling upward on the upper surface of a wing produces
lift.
Camber
If the thickness of an airfoil is ignored, it can be reduced to a thin
curved line defining the camber. The shape of this camber line determines
the amount of lift produced at a fixed angle of attack. Since a sail
has essentially no thickness, it exists only as camber. The flow over
the convex leeward side has reduced pressure (through accelerated flow)
and the flow over the concave windward side has increased pressure (through
decelerated flow). The difference in pressure across the sail holds
the flexible sail into its cambered shape and produces force to pull
the boat.
Upwash
An airfoil developing lift causes the flow approaching it to bend upward.
This is because the lower pressure on top of the airfoil pulls air up
toward it. This upward change in flow angle is called upwash.
Planform Effects
The planform of a wing is defined by the shape of the leading (front)
and trailing (back) edges.
In addition to the upwash that an airfoil causes on
itself due to the lower pressure on top influencing more air to flow
over it, additional upwash occurs due to changes in the planform of
the wing. This is because, just as the low pressure on top of the wing
influences the air some distance upstream to move upward toward it,
that low pressure also influences air a similar distance away in the
spanwise direction to alter its direction. This causes variations in
upwash along the span of the wing on adjacent sections.
Sweep
The sweep of a wing is defined as the angle between a line perpendicular
to the flow and a line (called the quarter-chord) passing through the
25% chordwise (luff to leech) positions along the span. The 25% chordwise
position is chosen because, typically, the load on a section can be
thought of as being centered there. This is because an airfoil generates
much more lift in its forward portion than it does aft, so using the
quarter-chord line as a reference is a convenient manner to characterize
the sweep of a wing.
Sweep has the effect of increasing the upwash on the
outboard wing sections. As a wing is angled aft, flow over the outboard
sections must pass by the low pressure on top of the wing sections immediately
inboard and forward. The close proximity of that low pressure to the
air just outboard causes the outboard flow to turn upward more, resulting
in higher upwash on the outboard wing.
Taper
Taper is defined as the ratio of the chordlength of the tip divided
by the chordlength of the root. For sails, where the head tapers to
nearly a point, the taper is extreme (zero), resulting in a triangular
planform.

A tapered wing has a much shorter tip section than root section. As
the wing tapers, lift produced by the shorter outboard sections is less
because they have less surface area to support lift. Since the outboard
sections are smaller than the inboard sections, they are significantly
influenced by the larger wing just inboard. Air approaching the outboard
portion of the wing is deflected by the low pressure on top of the larger
inboard wing that is still generating a large amount of lift only a
short distance away. The close proximity of that low pressure to the
outboard wing causes the flow to be pulled upward additionally over
the outboard wing. Hence, the smaller outboard sections operate with
higher upwash. This enhances the amount of lift that they produce but
does not make up for their loss of area.
Flow Conditions in Earth's
Boundary Layer
Identifying the flow conditions that sails operate in is very useful
for understanding how they work. The wind blows over the surface of
the earth and, as with any fluid flowing over a surface, has friction
with it. This friction slows the air closest to the surface and through
shear causes the air immediately above it to slow some, too. This effect
continues upward until at some distance above the surface the air is
all moving at a similar speed. This behavior is called the boundary
layer. While it occurs at a very small scale in the water flowing along
the surface of hulls and keels, it occurs at quite a large scale in
the air flowing over the earth. This means that the true wind speed
is increasing up the entire height of a mast.
Apparent Wind
Apparent wind is the wind velocity experienced by the sails on a moving
boat. This is the wind speed and direction that can be directly measured
(felt) from the boat while it is moving. It is a combination of the
true wind and the wind generated by the motion of the boat. The figure
shows how these two wind components are added to create the apparent
wind.
Notice that the apparent wind vector at the bottom
of the rig, where the true wind speed is slower, is shorter (slower)
and angled from a more forward direction, than the apparent wind vector
at the top of the rig, where the true wind speed is faster. The true
wind is coming from a single direction in this example, but varies in
speed with height due to the earth's boundary layer. This variation
in true wind speed not only causes the variation of apparent wind speed
with height, but also its variation in angle. This is because all of
the mast and sail are moving at the same speed and in the same direction
as the boat across the moving air. Since the wind solely due to the
movement of the boat is identical at all heights, the apparent wind
speed and direction resulting from its addition to different true wind
speeds at various heights is different.
While in this example the true wind velocity only
varied in strength with height, it is possible that a variation in true
wind direction can occur with height. In that situation, each tack will
experience different apparent wind twist than the other.
Twist
Since the flowfield that a sail experiences is twisted due to the movement
of the boat through the earth's boundary layer, the sail needs to incorporate
some twist in order to fly in that flowfield. The increase of apparent
wind angle with height is a factor that influences a sail to fly in
a twisted manner, where the top is angled more off-center from the boat
than the bottom. Other factors affecting how much twist is appropriate
are sweep and taper as they alter the amount of upwash along the span
of the sail.
Isolated Sails
A mainsail by itself (cat rig) is tapered, but if the mast is close
to vertical is actually swept forward. Recall that sweep is measured
relative to the 25% chord line, which in the case of a tapered sail
on an upright mast is angled forward. In this case, the forward sweep
would have somewhat of a canceling effect on the increased upwash due
to taper. The actual degree of upwash depends on the magnitudes of taper,
sweep, and aspect ratio (height/width) of the sail. The sail still operates
in the twisted flowfield caused by the boat moving through the earth's
boundary layer, so an amount of twist would be appropriate. Raking the
mast back increases sweep and will cause additional upwash on the top
of the sail, necessitating more twist to the sail.
Genoas and jibs are very tapered and swept. Those
two features, combined with the already twisted apparent wind, cause
significant upwash toward the head of the sail.
Sails in Combination
Each sail by itself is much simpler than the combination of a foresail
and mainsail as in the sloop rig. The sails are operating so close to
each other that they both have significant interaction with the other.
The most interesting feature of this is that the two sails together
produce more force to pull the boat than the sum of their forces if
they were each alone.
Earlier, upwash was identified as the increase in
flow angle immediately upstream of a wing. There is also a corresponding
change in angle, called downwash, just behind a wing, where the flow
leaving the wing has been turned to an angle lower than the original
flow. This is the cause of the well known "bad-air" that a
boat just to windward and behind another boat experiences.

The mainsail of a sloop rig operates in the downwash of the forward
sail, causing the flow angle approaching the mainsail to be significantly
reduced from what it would be otherwise. This decreases the amount of
force that the mainsail produces. The observed affect commonly referred
to as "backwinding" is partially a result of downwash from
the foresail, but is also due to the higher pressure on the windward
side of the genoa being very close to the forward, leeward side of the
mainsail, causing the flexible material of the mainsail to move away
from that higher pressure.
The foresail of a sloop rig operates in the upwash
of the mainsail. The wind as far upstream as the luff of a genoa is
influenced by the upwash created by the mainsail. Hence, a jib or genoa
in front of a mainsail has a higher flow angle than it otherwise would
have by itself, causing an increase in the amount of force that the
forward sail produces. So, while the mainsail is experiencing detrimental
interference from the foresail, the foresail benefits from the interference
of the mainsail. Notice that more air is directed around the curved
leeward side of the foresail. This causes higher velocity (lower pressure)
and more force. The net result is that the total force of the two-sail
system is increased, with the foresail gaining more than the mainsail
loses.
There is a converse affect to a windward boat receiving
"bad air" (downwash) from a boat ahead and to leeward. A leeward
boat gains additional upwash ("good-air"?) from a boat just
to windward and slightly behind that acts like a lifting windshift until
it moves ahead of the windward boat. This is the same phenomenon from
which a foresail of a sloop rig benefits.
Another consequence of the difference in flow angles
that the two sails experience in each others' presence is that the mainsail
must be trimmed to a much closer angle with the boat's centerline than
the foresail, which is able to be trimmed to a lead position well outboard.
This angle represents the difference in upwash on the foresail and downwash
on the mainsail due to each other.
Masthead Rig
On a masthead rig, where the forestay is attached to the top of the
mast and both sails taper to basically zero chordlength at their heads
in a similar fashion, the interference effects of the sails on each
other are similar along the entire height of the mast. The mainsail
ends up being rather tightly trimmed all the way up because of the genoa's
downwash, and the genoa gains from favorable upwash all the way up.
Fractional Rig
A fractional rig has the more complicated characteristic that the top
of foresail is not as high as the top of the mainsail. This means that
the top of the foresail is very close to the front of the mainsail at
a height where there is still an ample amount of chordlength in the
mainsail. As the foresail luff approaches the mainsail luff, the upwash
on the foresail due to the mainsail increases, because the low pressure
behind the mainsail has more affect the closer the flow gets to it.
This causes the top of the foresail to experience even more upwash and
contributes to a fractional rig's foresail being trimmed more twisted
than a masthead rig's foresail.
The top of the main on a fractional rig extends well
above the foresail, leaving the upper portion of the mainsail free to
experience the apparent wind without the downwash interference of the
foresail. Apparent wind toward the top of the mast comes from a much
higher angle, so the mainsail above the foresail experiences much higher
wind angles than the lower portion of the mainsail where the genoa is
causing substantial downwash. This change in flow angle with height
on a mainsail is quite dramatic with a fractional rig and leads to trimming
a fractional rig's mainsail with more twist than a masthead rig's mainsail.
Flow Angles
Reviewing all of the affects so far reveals that both sails experience
increasing flow angle with height. The foresail operates in the twisted
flow of the apparent wind, with upwash induced by itself due to taper
and sweep, and in the upwash field of the mainsail. The mainsail is
operating in the same twisted apparent wind, with additional upwash
caused by its taper, but somewhat lessened by its forward sweep. It
is also flying in the downwash field of the foresail, which is probably
twisted because the foresail flies in a twisted fashion. This is particularly
exaggerated with a fractional rig.
Sail Shape
With the flow directions established, it is now useful to consider the
ramifications of sail shape. Previously, it was stated that a sail section
exists solely as camber. Now it is interesting to explore the differences
in camber that are possible and what would be most beneficial.
Since a sail is constructed of flexible material,
its cambered shape is supported by the pressure difference that it generates.
It follows that the leading edge entry angle of the sail must be reasonably
aligned with the incoming flow angle. If the entry angle is too high
the sail will luff, and if it is too low the sail will stall, since
the flow would be required to turn an impossibly sharp corner around
the luff. It is also apparent that the entry angle should increase with
height to match the twisted flowfield. There are two remaining issues.
Where should the trailing edge be, which defines the angle of attack
at each height, thus twist? What path to take to get there, or what
should the specific cambered shape of the sail be?
The trailing edge location in relation to the leading
edge locations establishes the angle of attack of a particular section.
Lift increases proportionally with angle of attack, so, since a sailboat
is trying to extract as much force as possible from the wind (until
overpowered into heeling too much), it would seem best to position the
trailing edge (leech) as close to the boat's centerline as possible.
This would achieve the highest angle of attack and hopefully the most
lift, but unfortunately the ability to trim a sail to unlimited angles
of attack is not possible.
Click here to continue...
|