Proof of Well-Definedness of Integration
The integral of a differential form on an oriented manifold must be shown to be independent of the choice of atlas and partition of unity. This fundamental result ensures that integration is a geometric invariant.
Statement
Let be an oriented smooth -manifold, a compactly supported -form on , and two oriented atlases, and , subordinate partitions of unity. Then
Proof
Step 1: Double partition. Since and , we have
Thus both sums equal (with appropriate chart interpretation). It suffices to show that for a single term (compactly supported in ), the two chart integrals agree.
Step 2: Change of variables. Let be an -form compactly supported in the overlap . In the chart :
In the chart :
The transition map relates these. Write in coordinates . Under the change of variables :
Step 3: Orientation consistency. Since both atlases are oriented-compatible, the transition map is orientation-preserving, meaning everywhere. By the standard change of variables formula for Lebesgue integrals:
Since , we have , so the two expressions agree.
Consequences
If the transition maps could reverse orientation (negative Jacobian determinant), the absolute value in the change of variables formula would differ from the signed determinant, and the integral would depend on the atlas. This is precisely why orientability is necessary for integrating forms. On non-orientable manifolds, one integrates densities instead, which transform by .
Consider the Mobius band with a "top form" defined on charts. Following around the band, the form returns with opposite sign. Any global "volume form" would need to vanish somewhere, so has no consistent orientation. Attempting to define via charts gives contradictory signs in overlapping regions.
The same proof shows well-definedness of integration on oriented manifolds with boundary, using half-space charts near the boundary. The transition maps between half-space charts preserve orientation and respect the boundary, ensuring the integral remains well-defined.