Definitions and notations:
- Given a surface $S$ and a surface patch $\sigma: U \subset \Bbb R^2 \to \Bbb R^3$ of $S$, we define the standard unit normal of $\sigma$ at $p$ to be (where everything is evaluated at $p$ or $\sigma^{-1}(p)$):
$$N_{\sigma} = \frac1{\|\sigma_u \times \sigma_v\|} \sigma_u \times \sigma_v$$
Where $\sigma_u$ denotes $\partial \sigma /\partial u$.
A surface $S$ is said to be an oriented surface if there exists a smooth map $N: S \to \Bbb R^3$ (in the sense that each of the "components" of $N$ is smooth, where a map $f: S \to \Bbb R$ is called smooth if $f \circ \sigma$ is smooth for any $\sigma \in \cal A$ - the atlas of $S$), such that for all $p \in S$, $N(p)$ is a unit normal to $T_p S$ (the tangent plane to $S$ at $p$).
A surface $S$ is called an orientable surface if there is an atlas $\cal A$ of $S$, such that for any transition map $\phi$ between two patches in $\cal A$, $\det J( \phi) > 0$.
In EDG - Pressley, the author gives a method to prove that any oriented surface is orientable:
(where Definition $4.5.1$ is that of an oriented surface)
I have a quite simple question. What guarantees that we can make such a selection? Why isn't it possible that all the patches in the maximal atlas of $S$ are such that $\sigma_u \times \sigma_v$ is a negative multiple of $N$ at some point and a positive multiple of $N$ at another one?