Every lesson in this module has quietly assumed one thing: that the wing the air meets is the wing the designer drew: smooth, clean, and exactly the intended shape. This closing lesson is about the two ways reality breaks that assumption. The fast way is contamination: ice, frost and snow rebuilding the aerofoil's shape and surface in minutes. The slow way is age: dents, waviness and accumulated modifications degrading an airframe over years. Both tell the same story: the coefficients in the book belong to the drawn wing, and the air only ever sees the real one.
Where ice forms in flight
In-flight icing comes from supercooled water droplets: liquid below zero degrees, waiting for something to freeze onto. What they freeze onto is whatever meets the airflow head-on, so the build-up map is a map of the aircraft's forward-facing surfaces:
leading edges of the wing, the tailplane and the fin;
pitot probes (and, though flush-mounted rather than forward-facing, the static ports, which ice can crust over), whose blockage corrupts the airspeed and altitude indications: the instruments subject takes that thread;
windshield;
engine intakes, where shed ice can be swallowed by the engine;
propeller leading edges, costing thrust and throwing ice against the fuselage;
antennas and other protrusions.
One detail matters later in this lesson: thin surfaces collect ice more efficiently than blunt ones, so the tailplane, with its slender leading edge, typically carries proportionally more ice than the wing.