The center of pressure locates the resultant of a distributed fluid pressure load relative to its moment. On a planar surface carrying parallel pressure forces, the first-moment ratio in center of pressure applies. On an airfoil, pressure variation and its resultant can change with the flow state, so the point is not a permanently fixed geometric centre. NASA's primary account explicitly distinguishes a moving center of pressure from retaining a force and pitching moment about an aerodynamic center.[ref]
Center of Pressure by NASA Glenn Research Center. Center of Pressure, Angle of Attack, and Aerodynamic Force sections
For an original hydrostatic plate example, take a vertical rectangle of width , extending from the free surface to depth in a constant-density fluid. If the same atmospheric pressure acts on its other face, the net gauge pressure at depth is . This hydrostatic relation follows from vertical force balance.[ref]
The Feynman Lectures on Physics, Volume II by Richard Feynman and others. Chapter 40, §40–1, Hydrostatics
The resultant and its depth areFor , , and , the net force is at depth . The area centroid is only one metre below the surface; the increasing pressure shifts the load's centroid downward.A tank demonstration can infer the resultant line from the force and hinge moment on a small plate while changing the water depth. The plate's own gravitational moment and the pressure on both faces must be included. This tests a specified pressure-load model, not a general claim that the point always lies below every geometric centre.
For aerodynamic net loads, differences of pressures on opposite faces can have both signs. The convex-hull property proved for nonnegative contact pressure then need not apply, and a small resultant with a finite moment makes its location ill-conditioned. A curved surface or a general wrench may also require a residual couple rather than a single force that removes every component of torque. The resultant convention and moment reference are therefore part of the definition.
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