Thanks Hikaru!
hikaru1221 said:
Let's look at a simpler case: a sphere of radius R. Consider the drag force:
1 - when the wind blows at speed v directly to the sphere:
F_1=\frac{1}{2}\pi R^2\rho Cd_1v^2
2- when the wind blows at speed v\sqrt{2} (this looks like the combination of 2 flows of speed v; see the figure):
F_2=\pi R^2\rho Cd_2v^2
Interesting. But, working in another direction, let's assume that for a given velocity, C
d is constant for a sphere since that is a fully symmetrical shape (which as we can see is empirically calculated to have a drag co-efficient of 0.47). It's interesting to note that the drag co-efficient quoted is only accurate to 2 significant digits, as far as we can tell. One could therefore assume that there is a, say, 2%-4% relative error built into the wikipedia values and those quoted for cars, even if the value for a Sphere can be calculated using Stokes' Law. This may mean that the quoted C
d is valid for a variety of speeds as long as the correct errors are propagated.
But anyway, if a wind blows at a velocity of v at a 45° along a Cartesian plane bisecting the sphere at its equator, then the force in that direction is indeed given by:
F_{45^\circ}=\frac{1}{2}\pi R^2 \rho C_d \nu^2
Now I believe, but since I it's been so long since I studied for a BSc in Physics, I could be quite wrong, that it is the force vector that can be safely split along the Cartesian plane. Thus, along the x and y axes:
F_{x} = \frac{\sqrt{2}}{2}F_{45^\circ} = \frac{\sqrt{2}}{4}\pi R^2 \rho C_d \nu^2
F_{y} = \frac{\sqrt{2}}{2}F_{45^\circ} = \frac{\sqrt{2}}{4}\pi R^2 \rho C_d \nu^2
The question then becomes, how do you calculate the wind speed in the x and y direction. If we naïvely assume the Cartesian vectors for velocity are also given by the \frac{\sqrt{2}}{2} \nu, we would end up with:
F_{x} = \frac{1}{2}\pi R^2 \rho C_d \nu_x^2 = \frac{1}{4}\pi R^2 \rho C_d \nu^2 \neq \frac{\sqrt{2}}{4}\pi R^2 \rho C_d \nu^2
F_{y} = \frac{1}{2}\pi R^2 \rho C_d \nu_y^2 = \frac{1}{4}\pi R^2 \rho C_d \nu^2 \neq \frac{\sqrt{2}}{4}\pi R^2 \rho C_d \nu^2
Therefore, we can see that the assumption that an orthogonally split velocity can be applied to the drag formula is itself flawed, since clearly C
d is not going to vary by \sqrt{2} because the velocity is \frac{\sqrt{2}}{2} slower than before.
We could get around this if we assume that when applying the velocity to the formula that we apply the formula in reverse to calculate the orthogonal velocity (this time I'll make it more generic, using some incident angle \theta in the Cartesian plane):
F_{x} = F cos(\theta) = \frac{1}{2}\pi R^2 \rho C_d \nu^2 cos(\theta) = \frac{1}{2}\pi R^2 \rho C_d \nu_{x}^2
F_{y} = F sin(\theta) = \frac{1}{2}\pi R^2 \rho C_d \nu^2 sin(\theta) = \frac{1}{2}\pi R^2 \rho C_d \nu_{y}^2
Thus:
\nu^2 cos(\theta) = \nu_{x}^2
\nu^2 sin(\theta) = \nu_{y}^2
If you apply this formula to calculate the apparent wind velocity, the forces sum properly. I think this is the correct assumption since we know the C
d should be fairly constant for a regular sphere.
Now, how you sum the forces of wind incident in 2 different directions is a whole other can of worms that I will investigate further and get back to you.
hikaru1221 said:
Though the speed you gave us is not too large, it's not too small for us to apply Stokes' law, so I assume the quadratic drag equation holds validity in your case. Therefore I think the "vector sum" rule is not valid.
Yes.