Chord-axial aerodynamic force ($A$)

The chord-axial aerodynamic force $A$ is the component of the net aerodynamic force parallel to an airfoil chord, with positive direction here chosen aft. The perpendicular body component is the chord-normal aerodynamic force $N$. These two components resolve one load vector; flow-relative lift and drag resolve it in a different basis when the angle of attack is nonzero.

Let ${\mathbf{e}}_x$ point aft along the chord, and let $\mathbf{n}$ point outward from the body. Pressure and viscous stress giveNASA's primary explanation motivates integrating locally normal pressure forces before resolving the resultant into flow axes.^[ref] The explicitly outward normal in this equation fixes the pressure-force minus sign.

For a two-dimensional section whose upper and lower surfaces are graphs $z_u(x)$ and $z_l(x)$, the pressure-only axial load per unit span isThe surface slopes determine how much locally normal pressure projects onto the chord. A pressure force is normal to its local surface, rather than necessarily normal to the chord. Skin friction supplies a further contribution and is not included in $A_p^{\prime }$.

An original vector example takes $A=-5$ N, $N=80$ N and $\alpha =20{}^{\circ }$. The airfoil force-axis transformation gives $D\simeq 22.66$ N and $L\simeq 76.89$ N. A forward-directed axial component is therefore compatible with positive drag. It is not, by itself, evidence that the body supplies net propulsive power.

A proposed measurement compares a body-axis balance with integrated surface pressures after matching the angle of attack, sign conventions and support tare. Disagreement can include omitted shear or instrument effects; changing from body axes to flow axes does not remove those physical or measurement contributions.

The chord-axial force coefficient is the dimensionless chord-axial aerodynamic force:Here $S$ is the stated aerodynamic reference area, $\rho$ the reference mass density and $U$ the reference speed. The chord axis and its positive direction accompany the normalization. A signed coefficient can be negative even when the flow-relative drag coefficient is positive.

An original example uses $\rho =1.2$ kg/m${}^3$, $U=25$ m/s, $S=0.40$ m${}^2$ and aft-directed load $A=9$ N. Then $q=375$ Pa and $C_A=9/(375\cdot 0.40)=0.060$. Reporting that load with area 0.80 m${}^2$ instead gives 0.030. The reference-area scaling of aerodynamic coefficients changes the reported coefficient without changing the balance reading.

For a section, axial load per unit span $A^{\prime }$ is instead normalized as $c_a=A^{\prime }/(qc)$ using airfoil chord $c$. The denominator $qc$ has units N/m, whereas $qS$ has units N. A per-span load divided by a finite area does not produce the same dimensionless quantity.

With common references, the inverse airfoil force-axis transformation isFor stipulated $C_D=0.040$, $C_L=0.60$ and $\alpha =5{}^{\circ }$, this gives $C_A\simeq -0.01245$. The subtraction shows why labeling a body-axis coefficient as drag can change even the sign of the apparent result. NASA defines lift and drag relative to the flow, which is the physical basis for keeping these axes distinct.^[ref]

At fixed area, density and measured force, a small fractional speed error contributes approximately $-2\delta U/U$ to the coefficient's fractional error. Normalization consequently does not replace measurement calibration or an uncertainty assessment of the reference flow.