Let $n > 1$ and let $p:\tilde{X} \to X$ be a covering space, where $X$ and $\tilde{X}$ are path-connected and locally path-connected. Is there a bijection between $\mathrm{Classes}(S^n, \tilde{X}) $ and $\mathrm{Classes}(S^n, X)$, where $\mathrm{Classes}(A,B)$ denotes the homotopy classes of the continuous maps from $A$ to $B$.
I have tried to create this bijection using lifts: (since $S^n$ is simply-connected for $n > 1$, by the lifting criterion, every continuous map $f:S^n \to X$ admits a lift $\tilde{f}:S^n \to \tilde{X}$). Denote by $[f]$ the class of $f$ in $\mathrm{Classes}(S^n, X)$. The function I thought about was $$[f] \mapsto [\tilde{f}], $$ but this is not well-defined, as $f$ can have many lifts.
EDIT: I have added a few more assumptions that I forgot to write at the beginning.
@TMO took us 90% of the way there. Suppose you have a balloon, and you grab the southern hemisphere and squeeze it until all the air is pushed into the northern hemisphere, and the southern hemisphere is reduced to just a line segment. More formally, consider the map $$ (x, y, z) \mapsto (\alpha(z)x, \alpha(z)y, z) $$ where $$ \alpha: [-1, 1] \to \Bbb R: t \mapsto \begin{cases} t^2 & t > 0 \\ 0 & t \le 0 \end{cases} . $$ Then the image of the sphere ends up being the union of a line segment (the "string" on the balloon) and something that's topologically still a sphere.
Now instead of maps of your original sphere, you can consider maps defined on my collapsed balloon.
Sorry...I'm rambling here.
Suppose you have maps $F, G$ from the sphere to $X$. Let me refer to the south pole of the sphere as $S$. Lets say that $Q = F(S)$. If only $Q = G(S)$ as well, then $F$ and $G$ would be pointed-maps, and @TMO's comment would show they're homotopic. So I'm going to define a homotopy from $G$ to a map $G'$ where $G'(S) = Q$, and then we'll be done.
The idea is to gradually alter $G$ so that it's constant on the southern hemisphere, and then factor through a map to a balloon-and-string-like thing, and then alter G by a homotopy where the end of the string goes to $Q$. I'll need a path $\beta$ from $G(S)$ to $Q$, so $\beta(0) = G(S)$ and $\beta(1) = Q = F(S)$; that exists by path-connectedness. I'll use $\beta$ in a little while. First, let'd define homotopy number 1, using polar coordinates. Express each point of the domain $S^n$ as $(\sin(\phi) \mathbf{v}, \cos(\phi))$, where $\mathbf{v}$ is a vector in $\Bbb R^{n} \subset \Bbb R^{n+1}$. So $\phi$ corresponds to "latitude" in the 2-sphere, with $\phi = 0$ being the north pole, and $\phi = \pi$ being the south pole. OK. Let $$ H_1((\sin(\phi) \mathbf{v}, \cos(\phi)), t) = \begin{cases} F(\sin((1+t)\phi) \mathbf{v}, \cos((1+t)\phi)))) & (1+t) \phi \le \pi \\ F(S) & (1+t) \phi > \pi \end{cases} $$ For $t = 0$, you can see that $H_1(P, 0) = F(P)$, so that's good. For $t = 1$, you can see that $H_1(P, 1)$ is constant on the southern hemisphere (i.e. $\phi \ge \pi/2$), and its value on the equatorial sphere is just $F(S)$. And $P \mapsto H_1(P, 1)$ is homotopic to $F$. I'm going to call that map $F'$.
Now I'm going to perform another homotopy: holding the value on the equatorial sphere to be $F(S)$, I'm going to drag the image of the south pole over to $Q$. Here goes: $$ H_2((\sin(\phi) \mathbf{v}, \cos(\phi)), t) = \begin{cases} F(\sin(2\phi) \mathbf{v}, \cos(2\phi)) & \phi \le \pi/2 \\ \beta(t (\frac{2}{\pi}\phi - 1) & \phi > \pi/2 \end{cases}. $$
Let's see what's going on in that second line. We have $\pi/2 \le \phi \le \pi$ in the southern hemisphere. Multiplying by $2/\pi$, we get $1 \le \frac{2}{\pi} \phi \le 2$; subtracting $1$ gets us a number that's $0$ at the equator and 1 at the south pole. We multiply by $t$, so when $t = 0$, the argument to $\beta$ is $0$, and $\beta(0) = F(S)$, which is great. In fact, for all $t$, when $\phi = \pi/2$, we end up computing $F(S)$. But as $t$ increases to $1$, the argument to $\beta$ gradually increases to something that ranges from $0$ to $1$ as $\phi$ varies from $\pi/2$ to $\pi$. And $\beta(1)$ is exactly $Q$.
So $H_2$ provides a homotopy from $F'$ to a new function $F''$ for which we have $F''(S) = Q$. And now @TMO's argument shows that $F''$ is homotopic-rel-basepoints to $G$, so we're done!
(Man, that's hard without a whiteboard!)