This lesson asks what module 4's solid-state ingredients can do when they are built to a far higher standard of accuracy. The answer is inertial navigation: a system that, given nothing but a starting position, feels every acceleration applied to it and adds them up into velocity, position, track and speed over the ground. The lesson builds the principle, the corrections it cannot live without, the two generations of hardware, and the light-based gyro at the heart of the modern one.
The self-contained navigator
Everything met so far in this course leans on something outside the aircraft: the pressure instruments on the atmosphere, the compass on the Earth's magnetic field. An inertial system leans on nothing. It measures its own accelerations, inside its own box, and computes attitude, velocity and position from them alone. That self-sufficiency is why, in commercial air transport aeroplanes, inertial navigation and reference systems are the main source of attitude and one of the main sources of navigational data: the attitude shown on an airliner's primary displays comes from its inertial units, not from a spinning artificial horizon.
The self-sufficiency has exactly one stated exception: true airspeed (TAS). To determine attitude and navigational data the system requires no external input except TAS, which it takes from the air-data computer for one product in particular: wind. The inertial side knows the aircraft's motion over the ground; TAS and heading give its motion through the air; the difference between the two is the wind. Without TAS the box would navigate perfectly well, but it could not tell you what the air mass was doing. The position entered before flight does not break the rule: it is a starting datum handed over once, not a running feed.
From acceleration to position
The principle fits in one sentence: measure acceleration, and everything else is arithmetic. An accelerometer is, at bottom, a small mass on a spring: accelerate the case and the mass lags behind, and the force needed to hold it in place measures the acceleration. Integration is summing over time: acceleration summed over time is a change of velocity, and velocity summed over time is distance gone. Doing both, double integration, turns measured acceleration into distance travelled, and distance counted from a known starting point is position.
One accelerometer serves one direction only, so acceleration must be measured, or mathematically extracted, along three components: north–south, east–west and vertical. The two horizontal chains do the navigating; the vertical chain serves height and is dominated by gravity, which is one of the reasons the next section exists.