|
Seaplane Skiplane Flying Menu >Seaplane Operations ? Preflight and Takeoffs >Takeoffs
A seaplane takeoff may be divided into four
distinct phases: (1) The displacement phase, (2) the hump or
plowing phase, (3) the planing or on the step phase, and (4)
the lift-off.
The displacement phase should be familiar from
the taxiing discussion. During idle taxi, the displacement of
water supports nearly all of the seaplane’s weight. The
weight of the seaplane forces the floats down into the water
until a volume that weighs exactly as much as the seaplane has
been displaced. The surface area of the float below the waterline
is called the wetted area, and it varies depending on the seaplane’s
weight. An empty seaplane has less wetted area than when it
is fully loaded. Wetted area is a major factor in the creation
of drag as the seaplane moves through the water.
As power is applied, the floats move faster
through the water. The water resists this motion, creating drag.
The forward portion of the float is shaped to transform the
horizontal movement through the water into an upward lifting
force by diverting the water downward. Newton’s Third
Law of Motion states that for every action, there is an equal
and opposite reaction, and in this case, pushing water downward
results in an upward force known as hydrodynamic lift.
In the plowing phase, hydrodynamic lift begins
pushing up the front of the floats, raising the seaplane’s
nose and moving the center of buoyancy aft. This, combined with
the downward pressure on the tail generated by holding the elevator
control all the way back, forces the rear part of the floats
deeper into the water. This creates more wetted area and consequently
more drag, and explains why the seaplane accelerates so slowly
during this part of the takeoff.
This resistance typically reaches its peak
just before the floats are placed into a planing attitude. Figure
4-14 shows a graph of the drag forces at work during a seaplane
takeoff run. The area of greatest resistance is referred to
as the hump because of the shape of the water drag curve. During
the plowing phase, the increasing water speed generates more
and more hydrodynamic lift. With more of the weight supported
by hydrodynamic lift, proportionately less is supported by displacement
and the floats are able to rise in the water. As they do, there
is less wetted area to cause drag, which allows more acceleration,
which in turn increases hydrodynamic lift. There is a limit
to how far this cycle can go, however, because as speed builds,
so does the amount of drag on the remaining wetted area. Drag
increases as the square of speed, and eventually drag forces
would balance the power output of the engine and the seaplane
would continue along the surface without further acceleration.
Seaplanes have been built with sufficient power
to accelerate to takeoff speed this way, but fortunately the
step was invented, and it makes further acceleration possible
without additional power. After passing over the hump, the seaplane
is traveling fast enough that its weight can be supported entirely
by hydrodynamic lift. Relaxing the back pressure on the elevator
control allows the float to rock up onto the step, and lifts
the

Figure 4-14. This graph
shows water drag and propeller thrust during a takeoff run.
rear portions of the floats clear of the water.
This eliminates all of the wetted area aft of the step, along
with the associated drag.
As further acceleration takes place, the flight
controls become more responsive, just as in a landplane. Elevator
deflection is gradually reduced to hold the required planing
attitude. As the seaplane continues to accelerate, more and
more weight is being supported by the aerodynamic lift of the
wings and water resistance continues to decrease. When all of
the weight is transferred to the wings, the seaplane becomes
airborne.
Several factors greatly increase the water
drag or resistance, such as heavy loading of the seaplane or
glassy water conditions. In extreme cases, the drag may exceed
the available thrust and prevent the seaplane from becoming
airborne. This is particularly true when operating in areas
with high density altitudes (high elevations/ high temperatures)
where the engine cannot develop full rated power. For this reason
the pilot should practice takeoffs using only partial power
to simulate the longer takeoff runs needed when operating where
the density altitude is high and/or the seaplane is heavily
loaded. This practice should be conducted under the supervision
of an experienced seaplane instructor, and in accordance with
any cautions or limitations in the AFM/POH. Plan for the additional
takeoff area required, as well as the flatter angle of climb
after takeoff, and allow plenty of room for error.
Use all of the available cues to verify the
wind direction. Besides reading the water, pick up clues to
the wind’s direction from wind indicators and streamers
on the masts of moored boats, flags on flagpoles, or rising
smoke. A boat moored to a buoy points into the wind, but be
aware that it may have a stern anchor as well, preventing it
from pointing into the wind.
Waterfowl almost always align themselves facing
into the wind.
Naturally, be sure you have enough room for
takeoff. The landing distance of a seaplane is much shorter
than that required for takeoff, and many pilots have landed
in areas that have turned out to be too short for takeoff. If
you suspect that the available distance may be inadequate, consider
reducing weight by leaving some of your load behind or wait
for more favorable weather conditions. Atakeoff that would be
dangerous on a hot, still afternoon might be accomplished safely
on the following morning, with cooler temperatures and a brisk
wind.
In addition to wind, consider the effects of
the current when choosing the direction for takeoff. Keep in
mind that when taxiing in the same direction as the current,
directional control may be reduced because the seaplane is not
moving as quickly through the water. In rivers or tidal flows,
make crosswind or calm wind takeoffs in the same direction as
the current. This reduces the water forces on the floats. Suppose
the seaplane lifts off at 50 knots and the current is 3 knots.
If winds are calm, the seaplane needs a water speed of 47 knots
to take off downstream, but must accelerate to a water speed
of 53 knots to become airborne against the current. This difference
of 6 knots requires a longer time on the water
and generates more stress on the floats. The situation becomes
more complex when wind is a factor. If the wind is blowing against
the current, its speed can help the wings develop lift sooner,
but will raise higher waves on the surface. If the wind is in
the same direction as the current, at what point does the speed
of the wind make it more worthwhile to take off against the
current? In the previous example, a wind velocity of 3 knots
would exactly cancel the benefit of the current, since the air
and water would be moving at the same speed. In most situations,
take off into the wind if the speed of the
wind is greater than the current.
Unlike landplane operations at airports, many
other activities are permitted in waters where seaplane operations
are conducted. Seaplane pilots encounter a variety of objects
on the water, some of which are nearly submerged and difficult
to see. These include items that are stationary, such as pilings
and buoys, and those that are mobile, like logs, swimmers, water
skiers, and a variety of watercraft. Before beginning the takeoff,
it is a good practice to taxi along the intended takeoff path
to check for any hazardous objects or obstructions.
Make absolutely sure the takeoff path ahead
is free of boats, swimmers, and other water traffic, and be
sure it will remain so for the duration of the takeoff run.
Powerboats, wind-surfers, and jet-skis can move quickly and
change direction abruptly. As the seaplane’s nose comes
up with the application of full power, the view ahead may be
completely blocked by the cowling. Check to the sides and behind
the seaplane as well as straight ahead, since many watercraft
move much faster than the normal taxi speed and may be passing
the seaplane from behind. In addition to the vessels themselves,
also scan for their wakes and try to anticipate where the wakes
will be during takeoff. Operators of motorboats and other watercraft
often do not realize the hazard caused by moving their vessels
across the takeoff path of a seaplane. It is usually better
to delay takeoff and wait for the swells to pass rather than
encountering them at high speed. Even small swells can cause
dangerous pitching or rolling for a seaplane, so taxi across
them at an angle rather than head-on. Remember to check for
other air traffic and make any appropriate radio calls.
Be sure to use the pre-takeoff checklist on
every takeoff. All checks are performed as the seaplane taxies,
including the engine runup. Hold the elevator control all the
way back throughout the runup to minimize spray around the propeller.
If there is significant wind, let the seaplane turn into the
wind for the runup. As r.p.m. increases, the nose rises into
the plowing position and the seaplane begins to accelerate.
Since this is a relatively unstable position, performing the
runup
into the wind minimizes the possibility of crosswinds, rough
water, or gusts upsetting the seaplane. Waste no time during
the runup checks, but be thorough and precise. Taxi speed will
drop as soon as the power is reduced.
Water rudders are normally retracted before
applying takeoff power. The buffeting and dynamic water pressure
during a takeoff can cause serious damage if the water rudders
are left down.
As full power is applied during takeoff in
most seaplanes, torque and P-factor tend to force the left float
down into the water. Right rudder pressure helps to maintain
a straight takeoff path. In some cases, left aileron may also
help to counter the tendency to turn left at low speeds, by
increasing drag on the right side of the seaplane.
Density altitude is particularly important
in seaplane flying. High, hot, and humid conditions reduce engine
power and propeller efficiency, and the seaplane must also attain
a higher water speed in order to generate the lift required
for takeoff. This increase in water speed means overcoming additional
water drag. All of these factors combine to increase takeoff
distances and decrease climb performance. In high density altitude
conditions, consider not only the length of the water run, but
the room required for a safe climbout as well.
The land area around a body of water is invariably
somewhat higher than the water surface. Tall trees are common
along shorelines, and in many areas, steep or mountainous terrain
rises from the water’s edge. Be certain the departure
path allows sufficient room for safe terrain clearance or for
a wide climbing turn back over the water.
There are specific takeoff techniques for different
wind and water situations. Large water areas almost always allow
a takeoff into the wind, but there are occasionally circumstances
where a crosswind or downwind takeoff may be more appropriate.
Over the years, techniques have evolved for handling rough water
or a glassy smooth surface. Knowing and practicing these techniques
not only keep skills polished so they are available when needed,
they also increase overall proficiency and add to the enjoyment
of seaplane flying.
|