Atmospheric Hazards to Flight - Princeton Universitystengel/MAE331Lecture24.pdf · Geometry and...
Transcript of Atmospheric Hazards to Flight - Princeton Universitystengel/MAE331Lecture24.pdf · Geometry and...
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Atmospheric Hazards to Flight!Robert Stengel, !
Aircraft Flight Dynamics, MAE 331, 2016
!! Microbursts!! Wind Rotors!! Wake Vortices!! Clear Air
Turbulence
Copyright 2016 by Robert Stengel. All rights reserved. For educational use only.http://www.princeton.edu/~stengel/MAE331.html
http://www.princeton.edu/~stengel/FlightDynamics.html
Frames of Reference
!! Inertial Frames!! Earth-Relative!! Wind-Relative (Constant Wind)
!! Non-Inertial Frames!! Body-Relative!! Wind-Relative (Varying Wind)
Earth-Relative Velocity Wind Velocity
Air-Relative Velocity
Angle of Attack, !!
Flight Path Angle, ""
Pitch Angle, ##
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Pitch Angle and Normal Velocity Frequency Response to Axial Wind
! !
"# j$( )"Vwind j$( )
! VN!" j#( )!Vwind j#( )
MacRuer, Ashkenas, and Graham, 1973
!! Pitch angle resonance at phugoid natural frequency!! Normal velocity (~ angle of attack) resonance at phugoid and
short period natural frequencies
Pitch Angle and Normal Velocity Frequency Response to Vertical Wind
MacRuer, Ashkenas, and Graham, 1973
!! Pitch angle resonance at phugoid and short period natural frequencies!! Normal velocity (~ angle of attack) resonance at short period natural frequency
!
!" j#( )VN!$wind j#( )
=!" j#( )
!"wind j#( )
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Sideslip and Roll Angle Frequency Response to Vortical Wind
=!" j#( )!pwind j#( )
=!" j#( )!pwind j#( )
MacRuer, Ashkenas, and Graham, 1973
!! Sideslip angle resonance at Dutch roll natural frequency!! Roll angle is integral of vortical wind input
Sideslip and Roll Angle !Frequency Response to Side Wind
MacRuer, Ashkenas, and Graham, 1973
!! Sideslip and roll angle resonance at Dutch roll natural frequency
!" j#( )!"wind j#( )
=!" j#( )
!$wind j#( )
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Microbursts
1/2-3-km-wide Jet impinges on surface
High-speed outflow from jet core
Ring vortex forms in outlow
Outflow strong enough to knock down trees
The Insidious Nature of Microburst Encounter
!! The wavelength of the phugoid mode and the disturbance input are comparable
DELTA 191 (Lockheed L-1011)http://www.youtube.com/watch?v=BxxxevZ0IbQ&NR=1
HeadwindDowndraft
TailwindLanding Approach
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Importance of Proper Response !to Microburst Encounter
!! Stormy evening July 2, 1994!! USAir Flight 1016, Douglas DC-9, Charlotte!! Windshear alert issued as 1016 began descent along glideslope!! DC-9 encountered 61-kt windshear, executed missed approach!! Plane continued to descend, striking trees and telephone poles
before impact!! Go-around procedure was begun correctly -- aircraft's nose rotated
up -- but power was not advanced!! That, together with increasing tailwind, caused the aircraft to stall !! Crew lowered nose to eliminate stall, but descent rate increased,
causing ground impact
Optimal Flight Path !Through Worst JAWS Profile
!! Graduate research of Mark Psiaki!! Joint Aviation Weather Study (JAWS)
measurements of microbursts (Colorado High Plains, 1983)
!! Negligible deviation from intended path using available controllability
!! Aircraft has sufficient performance margins to stay on the flight path
Downdraft
Headwind
Airspeed
Angle of Attack
Pitch Angle
Throttle Setting
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Optimal and 15° Pitch Angle Recovery during !
Microburst Encounter
!! Graduate Research of Sandeep Mulgund!! Airspeed vs. Time!! Altitude vs. Time
!! Angle of Attack vs. Time
Encountering outflow
Rapid arrest of descent
!! FAA Windshear Training Aid, 1987, addresses proper operating procedures for suspected windshear
Wind Rotors
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Aircraft Encounters with !a Wind Rotor
Radius, ft
TangentialVelocity,
ft/s
!! Tangential velocity vs. radius for Lamb-Oseen Vortex
Geometry and Flight Condition of Jet Transport Encounters with Wind Rotor
!! Graduate research of Darin Spilman
!! Flight Condition!! True Airspeed = 160 kt!! Altitude = 1000 ft AGL!! Flight Path Angle = -3˚!! Weight = 76,000 lb!! Flaps = 30˚!! Open-Loop Control
!! Wind Rotor!! Maximum Tangential
Velocity = 125 ft/s!! Core Radius = 200 ft
a) co-axial, ! = 0
b) ! ! 0
3535
vortex
vortex
wind
!
35
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Typical Flight Paths in !Wind Rotor Encounter
!! from Spilman
-50
0
50
100
150
200
250
! [d
eg]
0 5 10 15 20 25 30Time [sec]
" i = 0" i = 60˚
-60
-50
-40
-30
-20
-10
0
! [d
eg]
10
20
0 5 10 15 20Time [sec]
25 30
" i = 0˚" i = 60˚
-300
-200
-100
0
100
200
300
-400 -300
h [f
t]
-200 -100 0 100 200 300y [ft]
400
rotor core radius
flight path
initial entry point
-500
0
500
1000
1500
0 5
h [f
t]
10 15 20 25 30
!i = 0˚!i = 60
Time [sec]
ground
Linear-Quadratic/Proportional-!Integral Filter (LQ/PIF) Regulator
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LQ/PIF Regulation of !Wind Rotor Encounter
!! from Spilman
-50
0
50
100
150
200
! [
deg
]
0 2 4 6 8 10Time [sec]
LQR-PIF controlno control input
0
200
400
600
800
1000
1200
h (
AG
L)
[ft]
0 2 4 6 8 10
LQR-PIF control
Time [sec]
no control input
Wake Vortices
C-5A Wing Tip Vortex Flight Testhttp://www.dfrc.nasa.gov/gallery/movie/C-5A/480x/EM-0085-01.mov
L-1011 Wing Tip Vortex Flight Testhttp://www.dfrc.nasa.gov/gallery/movie/L-1011/480x/EM-0085-01.mov
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Models of Single and Dual !Wake Vortices
TangentialVelocity,
ft/s
Radius, ft
Wake Vortex
Wind Rotor
TangentialVelocity,
ft/s
Radius, ft
Wake Vortex Descent and Downwash
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Wake Vortex Descent and !Effect of Crosswind
!! from FAA Wake Turbulence Training Aid, 1995
Magnitude and Decay of !B-757 Wake Vortex
!! from Richard Page et al, FAA Technical Center
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NTSB Simulation of US Air 427 and FAA Wake Vortex Flight Test
!! B-737 behind B-727 in FAA flight test!! Control actions subsequent to wake vortex
encounter may be problematical!! US427 rudder known to be hard-over from DFDR
24
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NTSB Simulation of American Flight 587
!! Flight simulation derived from digital flight data recorder (DFDR) tape
25
Digital Flight Data Recorder Data for American 587
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Causes of !Clear Air Turbulence
!! from Bedard
DC-10 Encounter with Vortex-Induced Clear Air Turbulence
!! from Parks, Bach, Wingrove, and Mehta
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DC-8 and B-52H Encounters with Clear Air Turbulence
!! DC-8: One engine and 12 ft of wing missing after CAT encounter over Rockies
!! B-52 specially instrumented for air turbulence research after some operational B-52s were lost
!! Vertical tail lost after a severe and sustained burst (+5 sec) of clear air turbulence violently buffeted the aircraft
!! The Boeing test crew flew aircraft to Blytheville AFB, Arkansas and landed safely
Conclusions
!! Critical role of decision-making, alerting, and intelligence
!! Reliance on human factors and counter-intuitive strategies
!! Need to review certification procedures!! Opportunity to reduce hazard through flight
control system design!! Disturbance rejection!! Failure Accommodation
!! Importance of Eternal vigilance
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Supplemental Material!
Alternative Reference Frames!for Translational Dynamics
!! Earth-relative velocity in earth-fixed polar coordinates: vE =
VE!
"
#
$
%%%
&
'
(((
vE =VE!E"E
#
$
%%%
&
'
(((
!! Earth-relative velocity in aircraft-fixed polar coordinates (zero wind):
!! Body-frame air-mass-relative velocity:
!! Airspeed, sideslip angle, angle of attack
vA =
u ! uw( )v ! vw( )w ! ww( )
"
#
$$$$
%
&
''''
=
uAvAwA
"
#
$$$
%
&
'''
VA!A
"A
#
$
%%%
&
'
(((=
uA2 + vA
2 + wA2
sin)1 vA /VA( )tan)1 wA /VA( )
#
$
%%%%
&
'
((((
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!rI = HBI vB
!vB =
1mFB vA( ) +H I
Bg I ! """ BvB
!!! = LB
I "" B
!!! B = IB
"1 MB vA( ) " "!! BIB!! B#$ %&
!! Rate of change of Translational Position
!! Rate of change of Angular Position
!! Rate of change of Translational Velocity
!! Rate of change of Angular Velocity
Rigid-Body Equations of Motion
!! Aerodynamic forces and moments depend on air-relative velocity vector, not the earth-relative velocity vector
Angle of Attack, !!
Flight Path Angle, ""
Pitch Angle, ##
Wind Shear Distributions Exert Moments on Aircraft Through Damping Derivatives
!! 3-dimensional wind field changes in space and time
wE x,t( ) =wx x, y, z,t( )wy x, y, z,t( )wz x, y, z,t( )
!
"
####
$
%
&&&&E
!! Gradient of wind produces different relative airspeeds over the surface of an aircraft
!! Wind gradient expressed in body axes !Clshear
" Clpwing
#w#y
$ Clpfin
#v#x
!Cmshear" Cmqwing ,body ,stab
#w#x
!Cnshear" Cnrfin ,body
#v#x
WB = HEBWEHB
E
WE =
!wx !x !wx !y !wx !z!wy !x !wy !y !wy !z
!wz !x !wz !y !wz !z
"
#
$$$$
%
&
''''
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Aircraft Modes of Motion
!! Longitudinal Motions
!! Lateral-Directional Motions
"Lon (s) = s2 + 2#$ns+$n2( )Ph s
2 + 2#$ns+$n2( )SP
"LD (s) = s# $S( ) s# $R( ) s2 + 2%&ns+&n2( )DR
!! Wind inputs that resonate with modes of motion are especially hazardous
Natural frequency : !n , rad / s
Natural Period : Tn =2"!n
, sec
Natural Wavelength : Ln = VN Tp , m
Nonlinear-Inverse-Dynamic Control
!! Nonlinear system with additive control:
!! Output vector:
!! Differentiate output until control appears in each element of the derivative output:
!! Inverting control law:
!x t( ) = f x t( )!" #$ +G x t( )!" #$u t( )
y t( ) = h x t( )!" #$
yd( ) t( ) = f * x t( )!" #$ +G * x t( )!" #$u t( ) ! v t( )
u t( ) = G * x t( )!" #$ vcommand % f * x t( )!" #$!" #$
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Landing Abort using Nonlinear- Inverse-Dynamic Control
!! from Mulgund
400
500
600
700
800
900
1 103
-7500 -5000 -2500 0 2500 5000 7500
Umax
= 60 ft/sec
Umax
= 70 ft/sec
Umax
= 80 ft/sec
Umax
= 90 ft/sec
Umax
= 100 ft/sec
Umax
= 110 ft/sec
Altitude (
ft)
Range (ft)
100
150
200
250
300
350
-7500 -5000 -2500 0 2500 5000 7500
Umax
= 60 ft/sec
Umax
= 70 ft/sec
Umax
= 80 ft/sec
Umax
= 90 ft/sec
Umax
= 100 ft/sec
Umax
= 110 ft/sec
Airs
peed
(ft/s
ec)
Range (ft)
-5
0
5
10
15
-7500 -5000 -2500 0 2500 5000 7500
Umax = 60 ft/sec
Umax = 70 ft/sec
Umax = 80 ft/sec
Umax = 90 ft/sec
Umax = 100 ft/sec
Umax = 110 ft/secA
lpha
(deg
)
Range (ft)
Angle of Attack Limit
Wind Shear Safety Advisor
!! Graduate research of Alexander Stratton!! LISP-based expert system
ON-BOARD DATA
Reactive sensorsWeather radarForward-lookingLightning sensorsFuture products
AIRCRAFT
SYSTEMSCREW
Interface ADVISORY
SYSTEM LOGIC
GROUND-BASEDDATA
LLWASTDWRPIREPSForecastsWeather dataFuture products
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Estimating the Probability of Hazardous Microburst Encounter
!! Bayesian Belief Network!! Infer probability of hazardous
encounter from •! pilot/control tower
reports •! measurements•! location•! time of day
GeographicalLocation
Surface Humidity
Time of Day
ConvectiveWeather
Probability ofMicroburst Wind Shear
Lightning
LightningDetection
Mod/HeavyTurbulence
TurbulenceDetection
Precipitation
WeatherRadar
PilotReport
Low-LevelWind Shear Advisory
SystemAirborne
Forward-LookingDoppler Radar
Reactive Wind ShearAlert System Terminal Doppler
Weather Radar
Aircraft as Wake Vortex Generators and Receivers
!! Vorticity, !!, generated by lift in 1-g flight
! =KgeneratorW"VNb
!! Rolling acceleration response to vortex aligned with the aircraft's longitudinal axis
Kgenerator !
4!
Kreceiver !
CL!
2"VNb
!p =
Kreceiver12!VN
2Sb
Ixx"
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Rolling Response vs. Vortex-Generating Strength for 125 Aircraft
!! Undergraduate summer project of James Nichols
0.0001
0.001
0.01
0.1
1 10 100
RollingResponse
Vortex Generating Strength