Total enthalpy — where it appears
Named by 3 essays across one field — each of them below, with the objects they name alongside it.
The wall that heats itself
A surface told nothing about its temperature does not settle at the air's. It settles most of the way to the stagnation temperature, and the heat flux is driven from that invented temperature rather than from the free stream's — so a wall hotter than the air can be being heated by it.
The gradient the heat never hears
On a flat plate at a Prandtl number of one, a boundary layer's total enthalpy is a straight-line function of its velocity, whatever the wall's temperature. Put the same layer in a pressure gradient and the straight line fails everywhere except on an insulated wall, because the gradient enters the velocity's equation and not the enthalpy's — and a favourable gradient can leave a band of gas colder than the free stream above a wall three times hotter than it.
A cold wall holds its layer on longer
A compressible boundary layer's pressure gradient pushes on its density, and its density is its temperature. Solve the velocity and the enthalpy together and the wall's temperature reaches the velocity: a cold wall holds its layer on to an adverse gradient two-thirds steeper, a hot one lets it go a third sooner, the stagnation point's heat-to-friction ratio more than doubles between them, and the cold band an uncoupled layer put above a cooled nose disappears.
Named alongside it
The objects these essays reach for when they reach for this one.
Aerodynamic heatingBoundary layerHeat transferAdverse pressure gradientAnalogyEnergy equationFalkner–SkanMach numberPrandtl numberSimilarity solutionSkin frictionAdiabatic wall