Projective Plane Embedding Ambiguity

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I'm working in a problem in do Carmo: let $F: \mathbb{R}^3 \to \mathbb{R}^4$ be given by

$$ F(x,y,z) \;\; =\;\; (x^2 - y^2, xy, xz, yz). $$

Let $\varphi: \mathbb{S}^2 \to \mathbb{R}^3$ be the restriction $\varphi = F|_{\mathbb{S}^2}$. Observing that $\varphi(p) = \varphi(-p)$ for all $p \in \mathbb{S}^2$ we can unambiguously define the mapping $\tilde{\varphi}: \mathbb{RP}^2 \to \mathbb{R}^4$ given by $\tilde{\varphi}[p] = \varphi(p)$. Ultimately we want to show that $\tilde{\varphi}$ is an immersion, and subsequently an embedding of the projective plane into $\mathbb{R}^4$.

My Problem: It's not hard to see, considering $\mathbb{RP}^2 \approx \mathbb{S}^2/\mathbb{Z}_2$, that the map $\tilde{\varphi}$ is well-defined, but when I try to take the differential, wouldn't we expect $d\tilde\varphi_p$ to be well-defined as well? This is to say, shouldn't we expect $d\tilde{\varphi}_p = d\tilde{\varphi}_{-p}$, or at least the columns of each Jacobian to span the same 2-dimensional affine subspace of $\mathbb{R}^4$?

Example 1: First consider the case that we restrict $F$ to the upper and lower open hemispheres. We can rewrite these restrictions as

\begin{eqnarray*} F^{z+}(x,y) & = & \left (x^2 - y^2, xy, x\sqrt{1-x^2-y^2}, y\sqrt{1-x^2-y^2} \right ) \\ F^{z-}(x,y) & = & \left ( x^2 - y^2, xy, -x\sqrt{1-x^2-y^2}, -y\sqrt{1-x^2-y^2} \right ) \end{eqnarray*}

where we can see that $F^{z+}(x,y) = F^{z-}(-x,-y)$. This yields two Jacobians which are incompatible at antipodal points:

\begin{eqnarray*} dF^{z+}_{(x,y)} & =& \left [ \begin{array}{cc} 2x & -2y \\ y & x \\ \frac{1- 2x^2 - y^2}{\sqrt{1-x^2-y^2}} & -\frac{xy}{\sqrt{1-x^2-y^2}} \\ -\frac{xy}{\sqrt{1-x^2-y^2}} & \frac{1-x^2-2y^2}{\sqrt{1-x^2-y^2}} \end{array} \right ] \\ dF^{z-}_{(x,y)} & = & \left [ \begin{array}{cc} 2x & -2y \\ y & x \\ -\frac{(1-2x^2-y^2)}{\sqrt{1-x^2-y^2}} & \frac{xy}{\sqrt{1-x^2-y^2}} \\ \frac{xy}{\sqrt{1-x^2-y^2}} & -\frac{(1-x^2-2y^2)}{\sqrt{1-x^2-y^2}} \\ \end{array} \right ]. \end{eqnarray*}

Wouldn't we expect that if $F(p) = F(-p)$ for all $p \in \mathbb{R}^3$ that at least $dF^{z+}_{(x,y)} = dF^{z-}_{(-x,-y)}$, or at least have their columns span the same affine subspace?

Example 2: Another approach I've considered for this problem is using the stereographic projection $\pi^{-1}:\mathbb{R}^2 \to \mathbb{S}^2/\{N\}$ given by

$$ \pi^{-1}(u,v) \;\; =\;\; \left ( \frac{2u}{u^2+v^2+1}, \frac{2v}{u^2+v^2+1}, \frac{u^2+v^2-1}{u^2+v^2+1} \right ) $$

and writing $\varphi|_{\mathbb{S}^2/\{N\}} = F \circ \pi^{-1}$. The problem that I see with this latter approach is that antipodal coordinates in the plane don't map to antipodal coordinates in $\mathbb{S}^2/\{N\}$.

Overall my main question is how we appropriately compute the Jacobian $d\tilde{\varphi}_p$, and how are we guaranteed that the Jacobian is well-defined on antipodal points of $\mathbb{S}^2$? I assume that this condition is necessary in order to show that $\tilde{\varphi}$ is an immersion. Am I mistaken?

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$\newcommand{\Reals}{\mathbf{R}}\newcommand{\Proj}{\mathbf{P}}$Define $\varphi:S^{2} \to \Reals^{4}$ by $\varphi = F \circ i$, with $i:S^{2} \to \Reals^{3}$ the inclusion, so that $$ \varphi:(x, y, z) \in S^{2} \mapsto (x^{2} - y^{2}, xy, xz, yz) \in \Reals^{4}. $$

To take the differential, you've covered two open hemispheres of $S^{2}$ by graph charts, $$ \sigma^{\pm}(x, y) = \left(x, y, \pm\sqrt{1 - x^{2} - y^{2}}\right). $$ Note, however, that $\sigma^{+}(x, y)$ and $\sigma^{-}(x, y)$ are not antipodal on the sphere; instead, $\sigma^{+}(x, y)$ and $\sigma^{-}(-x, -y)$ are antipodal. Composing with $F$, you get $$ F^{z^{+}}(x, y) = (F \circ \sigma^{+})(x, y) = (x^{2} - y^{2}, xy, xz, yz) = (F \circ \sigma^{-})(-x, -y) = F^{z^{-}}(-x, -y), $$ upon which the Jacobian calculation comes out as expected. (The respective columns are negatives of each other, as you'd expect since each map $F \circ \sigma^{\pm}$ is the other pre-composed with the map $(x, y) \mapsto (-x, -y)$ of $\Reals^{2}$.)

As a separate matter, the fact that $\varphi:S^{2} \to \Reals^{4}$ factors through the antipodal map, and therefore induces a smooth map $\tilde{\varphi}:\Reals\Proj^{2} \to \Reals^{4}$, automatically guarantees the Jacobian of $\tilde{\varphi}$ is well-defined: The two local lifts (map a small piece of $\Reals\Proj^{2}$ to either of two small pieces of $S^{2}$, then push forward by $F$) are identical, and therefore must have the same Jacobian with respect to local coordinates on the projective plane.