J. Philip Barnes May 2015 Aircraft Energy Gain From an Atmosphere in Motion 01-02 May, 2015 Santa...
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Transcript of J. Philip Barnes May 2015 Aircraft Energy Gain From an Atmosphere in Motion 01-02 May, 2015 Santa...
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Aircraft Energy Gain From an Atmosphere in Motion01-02 May, 2015 Santa Rosa, CA J. Philip Barnes
Part 1 of 2
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Part I of 2:
How Flies the Albatross The Flight Mechanics of Dynamic Soaring 24 May 2015 J. Philip Barnes
6X / year
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Presentation Contents ~ How Flies the Albatross
Observations
SimplificationAnalysis
Simulation The visionaries
Wind data
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Presentation Contents
www.HowFliesTheAlbatross.comRoyal Albatross
“The albatross can maintain this swooping soaring flight for hours on end without a single wing beat.” -- David Attenborough
Observations of Well-known Naturalists“The albatross ….. manages to remain master of its own course, either carried ... around the globe or ... against the strong winds without a beat of its wings.” -- Jacques Cousteau
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Presentation Contents
Quoting the Visionaries
Isaac Newton, Principia, 1725
Wellcomeimages.org
Lord Rayleigh, Nature, 1883
“Quantity of motion [momentum] is a measure...that arises from the velocity and the quantity of matter”
“A change in motion [acceleration] is proportional to the motive force.”
“Centripetal force is the force by which bodies are drawn from all sides...toward...a center.”
“ ... suppose that above and below a certain plane ... there is a uniform horizontal wind, but that ascending through this plane the [wind] velocity increases...”
“... energy at the disposal of the bird depends on his velocity relatively to the air” “....it is only necessary ... to descend ... to leeward, and ... ascend ... to windward.”
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Presentation Contents
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Moonroof & Model Airplane
90 km/hr
Wow! Now I understand dynamic soaring
Flight kinetic energy depends on airspeed, not groundspeed
well, say 50%.....
90 km/hr airspeed
90 km/hr groundspeed
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Albatross GPS/INS-backpack velocity ~ equals ground speed
V
y
Vg
Localwind
w
Ground speed
VcosgAirspeed shadow
INS/GPS
“…relatively to the air…” - Lord Rayleigh
Nature, 05 April 1883
Lift & drag ~ airspeed squared.This sketch: INS/GPS velocity for K.E. yields error factor of 4
“Backpack” INS/GPS velocity is very close to groundspeed, but the bird is rarely aligned with its ground track
The bird is aligned with relative wind, representing its airspeed.
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Presentation Contents
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Wind speed data ~ Southern latitudesReal-time snapshotW, m/s @ 10 m elev.
Data courtesy of Department of Meteorology, University of Reading, UK – www.met.rdg.ac.uk
W, m/s
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Wind profile ~ First Vs. updated estimates
The logarithmic profile is more representative and is founded on theory
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Wind gradients compared ~ First Vs. updated estimates
Similar gradients, 1-to-6 m elevation
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Presentation Contents
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Dynamic Soaring ~ Force Diagram
Dynamic Soaring Force Vector (F)F = m(dw/dt), directed upwind
T = m (dV/dt) = m (dw/dt) (dV/dw) = m (dw/dt) cosg cosy = m (dw/dz) (dz/dt) cosg cosy = m w’ V sing cosg cosy
Dynamic Soaring Thrust , T = F∙V
Direct quantitative equivalent of Lord Rayleigh’s qualitative dynamic soaring description
Isolate dynamic soaring thrust(ignore weight & drag for now)
mg
f
y
g D
L
mwV
w
Wellcomeimages.org
Lord Rayleigh
www.HowFliesTheAlbatross.comBlack-browed Albatross
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Three orthogonal accelerations ~ Newton’s Law Applied
V
Vcosgg
[Vcosg]y
y
TurnRadius
Isaac Newton
g LoopRadius
Vg
V
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Schedule any two angles, say(g t) & (y t) ; get dg/dt, dy/dt
Eqns. yield all other parameters
Equations of motion ~ three orthogonal accelerations
LDnWTgVn nt //sin/
2
1
D/L (CDo /CL ) + CL /(3A) 6
CL = nn W / (½ V2 S) 5
cos
cossin/'cos/ 2gVwgV
W
Lnn
3
tancos/tan
sin-costansinw')V/(g
4
7
7: Trajectory
x = w – V cosg cos ydownwind
y = V cosg sin ycrosswind
z = V sing vertical
Thrustgroup
DraggroupL
Dn
L
D
W
L
W
Dn
6: Drag-to-lift ratio
5: Lift coefficient
4: Heading rate
1: Normal load factor
3: Tangent. load factor
2: Dimensionless drag
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Sensor platform is maintained level
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Maneuver Angle Schedules ~ Math-modeled Examples
0.00 0.25 0.50 0.75 1.00
0
4 Sin2 “adder”
0.00 0.25 0.50 0.75 1.00 1.25 1.50 1.75 2.00
-50
0
50
Bank Right
Bank Left
Bank AngleSchedule
-10
0
10Sine Wave
Heading or time/period
t1
0.0 0.5 1.0
t2
0.0
0.5
1.0
Dt
Midpoint Shift
Auxiliary Time, t1
t20.0 0.5 1.0
t3
0.0
0.5
1.0Endpoint “dwell”
Auxiliary Time, t2
0.0 0.2 0.4 0.6 0.8 1.0
-10
-5
0
5
10
15
Climb
Dive
Flight Path Angle Schedule
Heading or time/period
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Presentation Contents
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
Real-time simulation
C:\Users\Philip\albatross\Algebratross_si
C:\Users\Philip\albatross\msvbvm50.dll
25J. Philip Barnes www.HowFliesTheAlbatross.com
0 20 40 60 80 100 1200
2000
4000
6000
8000
10000
12000
14000
16000
Horizontal Wind Vs. AltitudeH. Riehl, Jet Streams of the Atmosphere, CO State Univ. 1962
CompositeSeattleNorfolkFlorida
Wind speed, m/s
Altitude, m
Dynamic soaring in the jet stream
26Energy From an Atmosphere in Motion - Dynamic Soaring and Regen-electric Flight Compared J. Philip Barnes www.HowFliesTheAlbatross.com
Notional conditions• Altitude ~ 8.5 km• Mach ~ 0.85• L/D ~ 25
Basic feasibility test:w' (V/g) (L/D) sin g > 1
Dynamic soaring in the jet stream
Dynamic soaring thrust offsets drag overall in zoom cycle
Conclusion ~ How Flies The Albatross
Let not the albatross go extinct on our short watch
• Flight without flapping• Wind gradient, not windspeed• Airspeed, not groundspeed• Net progress, any direction• 50M-yr evolutionary opt.
J. Philip Barnes www.HowFliesTheAlbatross.com May 2015
About the Author
Phil Barnes has a Master’s Degree in Aerospace Engineering from Cal Poly Pomona. He is a Principal Engineer and 34-year veteran of air vehicle and subsystems performance analysis at Northrop Grumman, where he presently supports both mature and advanced tactical aircraft programs. Author of several SAE and AIAA technical papers, and often invited to lecture at various universities, Phil is presently leading several Northrop Grumman-sponsored university research projects including an autonomous thermal soaring demonstration, passive bleed-and-blow airfoil wind-tunnel test, and application of Blender 3D software for aircraft parametric geometry modeling and flight simulation. Outside of work, Phil is a leading expert on dynamic soaring, and he is pioneering the science of regen-electric flight.