Aircraft Aerodynamics, Stability, & Navigation Visualizer Web App

Aircraft Aerodynamics, Stability, & Navigation Visualizer Web App

✈ Aerodynamics 101
Four Forces
Axes & Controls
Airfoil
πŸ“ Stability Analysis
Pitch
Roll
Yaw
🌀 Atmosphere & Navigation
Types of Direction
Types of Altitude
Types of Airspeed
The Four Forces of Flight β€” Every aircraft in flight has exactly four forces acting on it. Lift (perpendicular to relative wind, generated by wings), Weight (gravity, always straight down), Thrust (from engine, along aircraft axis), and Drag (opposing motion through air). In steady, unaccelerated flight, Lift=Weight and Thrust=Drag. Any imbalance causes acceleration β€” climb, descent, speed change.
Three Axes & Control Surfaces
An aircraft rotates around three perpendicular axes through its center of gravity:
β€’ Longitudinal axis (nose to tail) β€” Roll β€” controlled by Ailerons on the wings. Right aileron down + left aileron up = roll right.
β€’ Lateral axis (wingtip to wingtip) β€” Pitch β€” controlled by Elevator on the horizontal tail. Elevator up = pitch up (nose rises).
β€’ Vertical axis (top to bottom) β€” Yaw β€” controlled by Rudder on the vertical fin. Left rudder pedal = yaw left.
Neutral
Airfoil & Bernoulli's Principle β€” An airfoil's curved upper surface forces air to travel faster over the top than the bottom. By Bernoulli's principle, faster air = lower pressure. This pressure difference creates lift. The Aerodynamic Center (AC) at ~25% chord is the point where the pitching moment stays constant regardless of angle of attack. Watch 1200 particles flow β€” they accelerate (turn bright blue) over the top. Push past 16Β° AoA to see stall: flow separates, particles turn red and chaotic, lift collapses.
AoA: 6Β°
Pitch (Longitudinal) Stability β€” The most critical axis. Pitch stability determines whether the aircraft returns to trimmed AoA after a gust or diverges toward stall/dive. Controlled by the relationship between CG and Neutral Point (NP).
Static Margin (SM) = NP βˆ’ CG (as %MAC):
β€’ GA/Transport: +5% to +15% β€” self-correcting, reasonable stick forces
β€’ Aerobatic: +2% to +5% β€” agile but still stable
β€’ Fighters (FBW): βˆ’5% to +5% β€” computer-augmented, very maneuverable
β€’ SM > 25%: sluggish, heavy controls, excessive trim drag

Dynamic Modes (MIL-F-8785C):
Short Period (1–3s): Level 1 ΞΆ=0.35–1.30 | Level 2 ΞΆ=0.25–2.00 | Ο‰n∝√SM
Phugoid (30–120s): Level 1 ΞΆβ‰₯0.04 | Damping β‰ˆ CD/CL
ΞΆ (damping ratio): 0=oscillates forever | 0.3=underdamped | 0.7=ideal | >1=overdamped sluggish
Stable
πŸ“˜ Pitch Stability 101

What is Static Margin?
Static Margin (SM) = distance from Center of Gravity (CG) to the Neutral Point (NP), expressed as % of the wing's Mean Aerodynamic Chord (MAC). The NP is the point where, if you placed the CG, the aircraft would have zero pitch stability β€” neither restoring nor diverging. CG ahead of NP = positive SM = stable. The aircraft "weathervanes" nose-down when disturbed to a higher AoA, restoring itself.

What are the Dynamic Modes?
Short Period (1–3 sec): A quick oscillation in angle of attack. This is what the pilot feels as "pitch response." It's driven by the tail's damping (Cmq) and the pitch stiffness (CmΞ±, which depends on SM). Higher SM β†’ stiffer, faster short period. The damping ratio ΞΆ should be 0.35–1.30 for good handling.
Phugoid (30–120 sec): A slow, gentle exchange between speed and altitude β€” the aircraft noses down, speeds up, then climbs and slows, repeating. Damping comes from the drag-to-lift ratio (CD/CL). Pilots easily control it; even ΞΆ=0 (undamped) is flyable.

What Can You Change on the Aircraft?
β€’ Move CG forward (load cargo/fuel forward): Increases SM β†’ more stable, heavier stick forces, more trim drag
β€’ Move CG aft (load cargo/fuel aft): Decreases SM β†’ more agile, lighter stick forces, risk of instability
β€’ Larger horizontal tail: Moves NP aft β†’ increases SM. Also increases pitch damping (Cmq).
β€’ Longer tail arm (tail further from CG): Same effect as larger tail β€” more leverage.
β€’ Wing sweep: Moves the aerodynamic center aft β†’ shifts NP aft β†’ can increase SM.
β€’ Canard vs conventional: Canards place the "tail" in front β†’ NP moves forward β†’ typically lower SM.
Roll (Lateral) Stability β€” Determines whether the aircraft levels its wings after a disturbance. Three geometry factors create the dihedral effect (ClΞ² < 0 = stable): wing dihedral angle, wing sweep, and wing vertical position (high wing = more stable).
Dihedral effect (ClΞ²): Range βˆ’0.05 to βˆ’0.10/rad. GA low-wing: 3–7Β° dihedral. High-wing: 0–3Β°. Each 10Β° sweep β‰ˆ 1Β° effective dihedral.
Roll mode: Level 1 Ο„R≀1.0–1.4s | Fighters: 0.3–0.5s | Transports: 1.0–1.5s
Spiral mode: Level 1 Tβ‚‚β‰₯12–20s. Mild instability is acceptable.
Tradeoff: Strong dihedral improves spiral stability but worsens Dutch roll. Swept-wing jets often need anhedral.
Stable
πŸ“˜ Roll Stability 101

What is the Dihedral Effect?
When an aircraft sideslips (e.g., a gust pushes it sideways), the dihedral effect creates a rolling moment that levels the wings. It's measured by ClΞ² (roll moment due to sideslip). ClΞ² < 0 means stable β€” sideslip to the right creates a left-rolling (wings-leveling) moment. Three things contribute:
β€’ Wing dihedral angle: Wings angled upward. In a sideslip, the "into-wind" wing sees a higher effective AoA β†’ more lift β†’ rolls you level.
β€’ Wing sweep: The forward-swept portion of the into-wind wing has more effective span β†’ more lift. Each 10Β° of sweep β‰ˆ 1Β° of effective dihedral.
β€’ High wing position: The fuselage blocks airflow on the lower side of the into-wind wing, creating a differential lift β†’ "pendulum" stabilizing effect.

What are the Dynamic Modes?
Roll Mode: Pure rolling response to aileron input. Characterized by time constant Ο„R β€” how fast the roll rate builds to its steady value. Fighters: Ο„R β‰ˆ 0.3s (snappy). Transports: Ο„R β‰ˆ 1.5s (sluggish). Driven by Clp (roll damping) and Ixx (roll inertia).
Spiral Mode: A very slow divergence or convergence in bank angle. Most aircraft are mildly spiral unstable β€” left alone, they'll slowly tighten a turn. This is acceptable because the divergence is so slow (Tβ‚‚ > 12 seconds) that the pilot easily corrects it.

What Can You Change?
β€’ Increase dihedral: More roll stability, but worsens Dutch roll (yaw-roll coupling oscillation)
β€’ Increase sweep: Adds effective dihedral "for free" β€” why swept-wing jets sometimes use anhedral (negative dihedral)
β€’ High vs low wing: High wing adds ~2–3Β° effective dihedral from pendulum effect
β€’ Winglets/tip devices: Small effect on ClΞ², mainly reduce induced drag
β€’ Wing mass distribution: Fuel in tip tanks β†’ higher Ixx β†’ slower roll rate (same Ο„R for given aileron)
Yaw (Directional) Stability β€” The "weathervane" effect. The vertical tail creates a restoring yaw moment when the aircraft sideslips. Without it, the aircraft would swap ends. CnΞ² > 0 = stable.
CnΞ² (weathercock): +0.03 to +0.10/rad. Fin area Γ— moment arm = stabilizing. Fuselage ahead of CG = destabilizing (longer nose β†’ bigger fin needed).
Dutch Roll (MIL-F-8785C): Level 1: ΞΆβ‰₯0.08, Ο‰nβ‰₯0.4rad/s, ΞΆΒ·Ο‰nβ‰₯0.15 | Level 2: ΞΆβ‰₯0.02
Yaw dampers (SAS): Most swept-wing transports need them β€” natural Dutch roll damping is too low. Small automatic rudder deflections increase effective Cnr.
Stable
πŸ“˜ Yaw Stability 101

What is Weathercock Stability?
The vertical tail acts like a weathervane. When the aircraft sideslips (nose pointing away from the direction of travel), the tail's side force creates a yaw moment that swings the nose back into the wind. This is measured by CnΞ² (yaw moment due to sideslip). CnΞ² > 0 = stable. Two opposing contributions:
β€’ Vertical tail (stabilizing): Fin area Γ— moment arm behind CG. Bigger fin + longer arm = more CnΞ².
β€’ Fuselage ahead of CG (destabilizing): The fuselage volume in front of CG acts like a backwards weathervane β€” it wants to swing the nose further away from the wind. Longer nose β†’ need bigger fin to compensate.

What is Dutch Roll?
The signature lateral-directional oscillation. It's a coupled yaw-roll motion: the aircraft yaws one way, which causes the forward wing to generate more lift (because of sweep and sideslip), which rolls the aircraft, which creates more sideslip, which yaws it back... creating a wobbly, fishtailing motion. Period is typically 2–5 seconds. It's annoying to passengers and dangerous if underdamped.
Damping depends on the balance between CnΞ² (yaw stiffness) and ClΞ² (roll-due-to-sideslip). Too much ClΞ² relative to CnΞ² β†’ underdamped Dutch roll.

What Can You Change?
β€’ Bigger vertical tail: More CnΞ² β†’ stronger weathervane β†’ better Dutch roll damping
β€’ Longer tail arm: Same effect β€” more leverage for the fin. Also helps directional control authority.
β€’ Shorter nose/fuselage: Less destabilizing volume ahead of CG β†’ less CnΞ² needed from the fin
β€’ Dorsal fin: Small extension at the base of the vertical tail β€” prevents fin stall at high sideslip angles
β€’ Yaw damper (SAS): Electronic system that senses yaw rate and applies small automatic rudder corrections. Standard on all swept-wing transports β€” increases effective Cnr (yaw damping derivative)
β€’ Ventral fin: Fin under the tail β€” adds CnΞ² without increasing above-fuselage height
Types of Direction β€” Heading = where the nose points. Course = intended path over ground. Track = actual path over ground (GPS). Wind makes them all different. Each has a True (geographic north) and Magnetic (compass north) version.
True vs Magnetic: True North = geographic pole. Magnetic North = where compass points (~northern Canada). Difference = magnetic variance (declination). Mnemonic: "East is least, West is best" β€” subtract easterly variance from true to get magnetic.
Course vs Heading: Course = where you want to go. Heading = where nose points. In a crosswind, you must crab (point nose into wind) so heading β‰  course, but your track matches your course.
GPS Track: Measured by successive satellite position fixes. Immune to compass errors and wind β€” shows your actual ground path.
β€”
Types of Altitude β€” Aviation uses 7 altitude references, each answering a different question. Indicated: what the altimeter reads. Pressure: altimeter set to 29.92"Hg (standard). Density: how the aircraft performs. True: actual height above sea level. Absolute: height above terrain. GPS: satellite geometric height. Flight Level: pressure alt in hundreds of feet (above FL180).
Types of Airspeed β€” Each corrects for a different error. IAS: gauge reading (defines V-speeds). CAS: corrected for instrument/position error. EAS: corrected for compressibility (structural loads). TAS: actual speed through air (navigation). GS: speed over ground (ETA/fuel). Mach: ratio to speed of sound (compressibility effects).
Why IAS matters most to pilots: Aerodynamic forces depend on dynamic pressure qΜ„=½ρVΒ². At altitude, air is thinner (lower ρ), so you fly faster (higher TAS) for the same qΜ„. But the pitot tube measures qΜ„ directly β€” so IAS reflects the actual aerodynamic loads regardless of altitude. That's why stall speed, flap limits, and Vne are all IAS values.
At sea level on a standard day: IAS β‰ˆ CAS β‰ˆ EAS β‰ˆ TAS. They diverge with altitude and temperature.