Summary

Frederick William Lanchester Aerodynamics, constituting the first volume of a complete work on aerial flight… (1906)

Now the average energy per unit volume in the wind is the sum of the separate energies of mean velocity and of turbulence (the latter for our present purpose being reckoned only in respect of motion in the direction at right angles to the pressure plane) , and in a wind possessing such energy of turbulence, the mean pressure will be greater than would be the case for the simple air current in the proportion that the sum of the energies bears to the energy of mean velocity.
Source: Wikisource

Frederick William Lanchester Aerodynamics, constituting the first volume of a complete work on aerial flight… (1906)

By the theory of Helmholtz, the pressure difference in a fluid of zero viscosity is entirely due to the excess of pressure on the front face, the “dead-water” being supposed to carry the ordinary hydrostatic pressure of the fluid.
In real fluids there is a viscous drag at the surface of discontinuity, or stratum of turbulence, across which a continuous communication of momentum takes place. This constitutes a force acting rearward on the dead-water as a whole, the reaction of which appears as a region of decreased pressure (a partial vacuum) on the rear face of the plane.
Source: Wikisource

Frederick William Lanchester Aerodynamics, constituting the first volume of a complete work on aerial flight… (1906)

Another standpoint from which we may view the present problem is that the turbulence, by effecting a rapid transference of momentum from one part of the fluid to another, acts in effect to augment the apparent viscosity, and in this way adds to the pressure reaction. In any case experiments made on a fixed plane or other body in moving air, cannot be regarded as valid when the conditions are reversed.
Source: Wikisource

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