Windshear
- The best defense against the hazards of low altitude windshear is:
1. Taking precautions before windshear is encountered.
2. Knowledge of standard operating techniques related to windshear.
3. The ability to perform specific recovery techniques in the event of an
inadvertent windshear encounter.
Avoidance is emphasized as the best defense against the hazards of low
altitude windshear.
Pilots should learn as much as they can about the effects of windshear and
the practices that may be employed to recognize, avoid, and cope with
inadvertent windshear encounters.
Hazardous wind variations at low altitudes can result from:
1. Temperature inversions.
2. Frontal systems.
3. Thunderstorms.
Wind variations at low altitude have long been recognized as a serious
hazard to airplanes during takeoff and approach. These wind variations can
result from a large variety of meteorological conditions such as:
1. Topographical conditions.
2. Temperature inversions.
3. Frontal systems.
4. Strong surface winds.
5. Thunderstorms and rain showers.
The most violent forms of wind change occur in the vicinity of thunderstorms
and rain showers.
Pilots must learn to recognize conditions producing windshear in order to
avoid windshear encounters.
Airmass thunderstorms appear to be randomly distributed in unstable air and
develop from localized heating at the earth's surface.
Compared to airmass thunderstorms, frontal thunderstorms are more severe.
The downdraft of a typical thunderstorm is fairly large, about 1 to 5 miles
in diameter. Resultant outflows may produce large changes in wind speed.
Though wind changes near the surface occur across an area sufficiently large
to lessen the effect, thunderstorms always present a potential hazard to
airplanes. Regardless of whether a thunderstorm contains windshear, however,
the possibility of heavy rain, hail, extreme turbulence, and tornadoes make
it critical that pilots avoid thunderstorms.
The majority of documented windshear-associated accidents and incidents have
occurred in the United States.
Observations suggest that approximately five percent of all thunderstorms
produce a microburst.
Downdrafts associated with microbursts are typically only a few hundred to
3000 feet across. When the downdraft reaches the ground, it spreads out
horizontally and may form one or more horizontal vortex rings around the
downdraft. The outflow region is typically 6000 to 12,000 feet across. The
horizontal vortices may extend to over 2000 feet AGL.
Microburst outflows are sometimes symmetric, sometimes not.
More than one microburst can occur in the same weather system.
After they contact the ground, microbursts typically dissipate within 5
minutes after a initially contacting the ground.
An encounter during the initial stage of microburst development may not be
considered significant, but an airplane following may experience an airspeed
change two to three times greater.
Microbursts typically dissipate within 10 to 20 minutes after ground
contact.
The wind speed change a pilot might expect when flying through the average
microburst at its point of peak intensity is about 45 knots.
Some microbursts cannot be successfully escaped with known techniques.
Even windshears which were within the performance capability of the airplane
have caused accidents.
If cumulus clouds are present in the sky, the greatest potential for
microburst windshear exists. Even if there are only subtle signs of
convective weather, such as weak cumulus cloud forms, suspect the
possibility of microbursts, particularly if the air is hot and dry.
Microbursts can be associated with both heavy rain, as in thunderstorm
conditions, and much lighter precipitation associated with convective
clouds. Microbursts have occurred in relatively dry conditions of light rain
or virga (moisture that evaporates before reaching the earth"s surface).
Example: air below a cloud base (up to approximately 15,000 feet AGL) is
very dry. Virga from convective clouds falls into low humidity air &
evaporates. This cooling causes the air to plunge downward. As the
evaporative cooling process continues, the downdraft accelerates. Pilots are
cautioned not to fly beneath convective clouds producing virga conditions.
They may encounter a dry microburst.
The primary lesson learned is that the best defense against windshear is to
avoid it altogether. This is especially important because shears will exist
which are beyond the capability of any pilot or airplane. In most windshear
accidents, several clues -- LLWAS alerts, weather reports, visual signs --
were present that would have alerted the flight crew to the presence of a
windshear threat. In all instances, however, these clues were either not
recognized or not acted upon. Flight crews must seek and heed signs alerting
them to the need for avoidance.
In a typical windshear encounter during takeoff - after liftoff, for the
first 5 seconds after liftoff, the takeoff appeared normal.
Successful recovery from an inadvertent windshear encounter after liftoff
requires
maintaining or increasing pitch attitude and accepting lower than usual
airspeed.
To recognize and respond to a windshear encounter, you may have only 5 to 15
seconds.
Regarding windshear encounters on the runway, they may be difficult to
recognize since the only indication may be a slower than normal airspeed
increase.
One way to improve a flight crew's ability to recognize and respond quickly
to a windshear encounter is to: Develop effective crew coordination,
particularly standard callouts, for routine operational use.
Lack of timely and appropriate response, affected by weather conditions,
inadequate crew coordination, and limited recognition time, was a
significant factor in delaying recovery initiation in the typical accident
involving a windshear encounter on approach.
Gradual application of thrust during approach may have masked the initial
decreasing airspeed trend. Poor weather conditions caused increased workload
and complicated the approach. Transition from instruments to exterior visual
references may have detracted from instrument scan. Inadequate crew
coordination may have resulted in failure to be aware of flight path
degradation.
An increasing headwind (or decreasing tailwind) shear increases indicated
airspeed and thus increases performance.
A rapid or large airspeed increase on approach should be viewed as a
possible indication of a forthcoming airspeed decrease and thus may be
reason for discontinuing the approach. Thus, a large airspeed increase may
be reason for discontinuing the approach. However, since microbursts are
often asymmetric and the headwind may not always be present, headwind shears
must not be relied upon to provide early indications of subsequent tailwind
shears. Be prepared!
An airplane encountering a decreasing headwind shear may tend to pitch down
to regain trim speed
Vertical winds exist in every microburst and increase in intensity with
altitude. Such winds usually reach peak intensity at heights greater than
500 feet above the ground.
Downdrafts with speeds greater than 3000 feet per minute can exist in the
center of a strong microburst.
The severity of the downdraft the airplane encounters depends on both the
altitude and lateral proximity to the center of the microburst.
An airplane flying through a series of horizontal vortices generated by
microbursts experiences alternating updrafts and downdrafts causing pitch
changes without pilot input.
The most significant impact of rapidly changing vertical winds in a
microburst is to increase pilot workload during the recovery
Large crosswind shears tend to cause the airplane to roll and/or yaw. Large
crosswind shears may require large or rapid control wheel inputs. These
shears may result in significantly increased workload and distraction. In
addition, if an aircraft encounters a horizontal vortex, severe roll forces
may require up to full control wheel input to counteract the roll and
maintain aircraft control.
-
- The use of the stick shaker as a guide to airplane performance limits
presumes that: Dual stick shaker systems are installed; The angle-of-attack
vane is heated, the input from the stabilizer to the stick shaker computer
is functioning correctly, and wing leading edges are clean and smooth and
alpha vanes are undamaged.
During callouts and instrument scan in a windshear, use of radio and/or
barometric altimeters must be tempered by the characteristics of each. Since
radio altitude is subject to terrain contours, the indicator may show a
climb or descent due to falling or rising terrain, respectively. The
barometric altimeter may also provide distorted indications due to pressure
variations within the microburst.
During a windshear encounter, the vertical speed indicator may significantly
lag actual airplane rate of climb/descent.
When evaluating available weather data, clues to possible windshear might be
found by checking terminal forecasts for potential thunderstorms,
rainshowers, gusty winds, and low level windshear.
The following weather information should be examined for any potential
windshear conditions affecting the flight:
Terminal forecasts.
Hourly sequence reports.
Severe weather watch reports.
LLWAS reports.
SIGMET’s & convective SIGMET’s.
Visual clues from the cockpit.
PIREPS.
Airborne weather radar.
With regard to a low level windshear alert system installed at an airport,
detected windshear magnitudes may be underestimated
The value of recognizing microbursts by visual clues from the cockpit cannot
be overemphasized. Pilots must remember that microbursts occur only in the
presence of convective weather indicated cumulus type clouds, thunderstorms,
rain showers, and virga. (Other types of windshear can occur in the absence
of convective weather.)
Pilots must become aware that visual clues are often the only means to
identify the presence of severe windshear.
The use of airborne weather radar to detect convective cells should be
considered a matter of routine. Weather radar provides extremely useful
information for the avoidance of thunderstorms in the airport terminal area,
but cannot directly detect windshear.
Pilots have become adept at avoiding thunderstorms while enroute and at
altitude. However, relatively little emphasis has been placed on their use
near the terminal area. Most thunderstorms with heavy rain near the airport
can be detected with conventional weather radar by a careful use of tilt
control to scan above the intended flight altitude (15,000 to 20,000 feet).
One significant aspect of weather radar use is attenuation. Attenuation is
caused by heavy rainfall reducing the ability of the radar signal to
penetrate, causing the radar to present an incomplete picture of the weather
area. In the terminal area, comparison of ground returns to weather echoes
is a useful technique to identify when attenuation is occurring.
Tilt the antenna down and observe ground returns around the radar echo. With
very heavy intervening rain, ground returns behind the echo will not be
present. This area lacking ground returns is referred to as a shadow and may
indicate a larger area of precipitation than is shown on the indicator.
Areas of shadowing should be avoided.
Even though significant emphasis on simulator training is recommended in
pilot training curriculums, avoidance must be the first line of defense.
Simulators are valuable for teaching windshear recognition and recovery.
However, pilots are cautioned not to develop the impression that real-world
windshear encounters can be successfully negotiated simply because they have
received simulator training. In an airplane, complicating factors (i.e.
turbulence, precipitation noise, instrument errors, etc.) may make shears
much more difficult than in a simulator. In addition, simulator motion
systems are limited in their capability to reproduce all the dynamics of an
actual windshear encounter.
When implementing takeoff precautions due to possible windshear activity in
the area, maximum rated takeoff thrust should be used for takeoff. This
shortens the takeoff roll and reduces overrun exposure. Full thrust also
provides the best rate of climb, thus increasing altitude available for
recovery if required. Lastly, full thrust takeoffs may eliminate resetting
thrust in a recovery, thereby maximizing acceleration capability and
reducing crew workload.
To properly calculate increased rotation speed (VR) as a precautionary
technique for takeoff in possible windshear conditions Increase the actual
weight VR speed by 10% (not to exceed 20 knots over actual weight VR). Add
20 knots to the actual weight VR speed. Add the value of any reported
windshear airspeed loss to your actual weight VR.
Use the field length limit maximum weight VR (up to 20 knots over actual
weight VR).
If increased VR is to be used, the technique for scheduling & using it is:
Determine V1, VR, & V2 speeds for actual airplane gross weight & flap
setting. Set airspeed bugs to these values in the normal manner. Determine
field length limit maximum weight and corresponding VR for selected runway.
If field length limit VR is greater than actual GW VR, use the higher VR (up
to 20 kts. in excess of actual GW VR) for takeoff. Airspeed bugs shouldn’t
be reset to higher speeds. Rotate to normal initial climb attitude at the
increased VR & maintain this attitude. This technique produces a higher
initial climb speed which slowly bleeds off to the normal initial climb
speed.
When commencing an approach into suspected windshear conditions and
precautions are being taken, auto throttles: Should be monitored closely for
inappropriate thrust reductions.
When calculating your approach speed for suspected windshear conditions
which indicate precautions should be taken, you should remember that: You
should not add any extra speed. An additional 20 knots at touchdown can
increase your stopping distance by as much as 25 percent. Any increased
approach speed must be bled off in the flare prior to touchdown. Approach
speed may be increased up to the amount of any reported windshear. Increased
airspeed on approach improves climb performance capability and reduces the
potential for flight at stick shaker during recovery from an inadvertent
windshear encounter. If available landing field length permits, airspeed may
be increased up to a maximum of 20 knots. This increased speed should be
maintained to flare. Touchdown must occur within the normal touchdown zone
-- do not allow the airplane to float down the runway. Warning - Increased
touchdown speeds increase stopping distance. An additional 20 knots at
touchdown can increase stopping distance by as much as 25% and in some cases
may exceed brake energy limits.
It is important for crews to remain alert for any change in conditions,
remembering that windshear can be quick to form and to dissipate. The shears
that proved to be most deadly are those which caught crews by surprise.
Crews should be aware of normal vertical flight path indications so that
windshear induced deviations are more readily recognized. On takeoff, this
would include attitude, climb rate, and airspeed buildup. On approach,
airspeed, attitude, descent rate, and throttle position provide valuable
information. Awareness of these indications assures that flight path
degradation is recognized as soon as possible.
Crews should be prepared to execute the recommended recovery procedure
immediately if deviations from target conditions in excess of the following
occur during takeoff:
+/- 15 knots indicated airspeed.
+/- 500 feet per minute vertical speed.
+/- 5 degrees pitch attitude.
Crews should be prepared to execute the recommended recovery procedure
immediately if deviations from target conditions in excess of the following
occur during approach:
+/- 15 knots indicated airspeed.
+/- 500 feet per minute vertical speed.
+/- 5 degrees pitch attitude.
+/- 1 dot glideslope displacement.
Unusual throttle position for a significant period of time.
The most effective technique for recovering from a windshear encounter for
turbojet aircraft when airborne is: Increasing thrust to maximum rated and
increasing pitch attitude until the stick shaker is encountered. Maintaining
the maximum lift/drag airspeed. Applying necessary thrust and rotating
initially toward 15 degrees pitch up attitude. Reducing airplane drag by
raising flaps, if possible.
Extensive analysis and pilot evaluations were conducted to establish a
windshear recovery technique. Although a range of recovery attitudes
(including 15 degrees and the range of all-engine initial climb attitudes)
provides good recovery capability for a wide variety of windshears, 15
degrees was chosen as the initial target pitch attitude for both takeoff and
approach. Additional advantages of 15 degrees initial target pitch attitude
are that it is easily recalled in emergency situations and it is prominently
displayed on attitude director indicators.
During recovery from an airborne windshear encounter, the correct use of
power is to:
Use only maximum rated thrust.
Aggressively apply thrust as necessary to ensure adequate airplane
performance.
Engage the auto throttles.
Automatically select full "overboost" engine thrust.
Use of thrust in recovery: Aggressively apply necessary thrust to ensure
adequate airplane performance. Disengage the auto throttle if necessary.
Avoid engine overboost unless required to avoid ground contact. When
airplane safety has been ensured, adjust thrust to maintain engine
parameters within specified limits.
To recover from a windshear encounter during takeoff after liftoff, what
should be done with flaps and landing gear?
Configuration: maintain flap and gear position until terrain clearance is
assured. Although a small performance increase is available after landing
gear retraction, initial performance degradation may occur when landing gear
doors open for retraction. While extending flaps during a recovery after
liftoff may result in a performance benefit, it is not a recommended
technique because:
Accidentally retracting flaps (the usual direction of movement) has a large
adverse impact on performance;
If landing gear retraction had been initiated prior to recognition of the
encounter, extending flaps beyond a takeoff flap setting might result in a
continuous warning horn which distracts the crew.
A flight director and/or autoflight system which is not specifically
designed for operation in windshear may command a pitch attitude change to
follow target airspeeds or a fixed pitch attitude regardless of flight path
degradation.
This guidance may be in conflict with the proper procedures for windshear
recovery. Such systems must be disregarded if recovery is required and, time
permitting, switched off by the pilot-not-flying.
During a windshear encounter recovery, always respect the stick shaker. Use
intermittent stick shaker as the upper pitch limit. In a severe shear, stick
shaker may occur below 15 degrees pitch attitude.
Immediately following a successful windshear recovery, a pilot should: As
soon as possible, report the encounter to the tower. The airplane following
may not have the performance required to recover from the same windshear
encounter. The windshear also may be increasing in intensity making flight
through it even more dangerous. Pilots & controllers must be aware that
their timely actions may prevent a pending disaster -- seconds may save
lives! Pilot reports for windshear encounters should contain the following:
Maximum loss or gain of airspeed; altitude at which shear was encountered;
location of shear with respect to runway in use; airplane type; use the term
"PIREP" to encourage a rebroadcast of the report to other aircraft.
When a windshear is encountered on the runway after V1 but before VR,:
Overboost thrust will ensure that the airplane accelerates to liftoff speed.
Rotate toward 15 degrees pitch attitude by 2000 feet of runway remaining.
Delay rotation as long as possible in an attempt to attain VR.
Avoid aft body contact during rotation.
Controlling pitch when encountering windshear during takeoff on the runway
after V1:
When VR is reached, rotate at normal rate toward 15 degrees pitch attitude.
In severe windshear encounters, however, VR might not be reached and the
option to reject the takeoff may not exist. If this is the case, rotation
must be initiated no later than 2000 feet from the end of the usable
surface.
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