Received: 11 Jun 2025; Accepted: 24 Aug 2025
Morse-Bott Volume Forms
Abstact.
A Morse-Bott volume form on a manifold is a top-degree form which vanishes along a non-degenerate critical submanifold. We prove that two such forms are diffeomorphic (by a diffeomorphism fixed on the submanifold) provided that their relative cohomology classes with respect to the submanifold coincide. For a zero submanifold of codimension at least 2, this means that two Morse-Bott volume forms with the same zero set are diffeomorphic if and only if they have equal total volumes. We show how “Moser’s trick” for establishing equivalence of non-degenerate volume forms can be adapted to this setting.
1 Introduction
Background
In his 1965 paper [14], Moser showed that any two volume forms with the same total volume on a compact, connected, and oriented manifold are related by a diffeomorphism of via pullback, . To construct such a diffeomorphism, Moser’s method was to connect the forms and by a path in the same cohomology class and to look for a family of diffeomorphisms such that and . The latter is achieved by solving the corresponding infinitesimal version of the equation on the vector field generating the flow and invoking the existence theorem for ODEs guaranteeing the existence of a flow for a given vector field, verifying the conditions for its existence for all . The strategy has dubbed variably as “Moser’s trick”, “Moser’s path method”, or the “homotopy method”.
This method has seen a wide variety of applications. Moser also applied the method in [14] to symplectic structures and twisted volume forms on non-orientable manifolds. Banyaga described Moser’s approach for volume forms on manifolds with boundary in [3], while Bruveris et al. [4] extended it to volume forms on manifolds with corners. Cardona and Miranda [6] considered an analogue of Moser’s result for equivalence of top-degree forms transverse to the zero section with a shared zero hypersurface. Other authors have considered solutions to the so-called “pullback equation” in more analytic contexts, see e.g. a summary of equivalence results for -forms for any for Hölder spaces in [7].
Main result
Let be a compact connected oriented -dimensional manifold, which we equip with a reference (non-vanishing) volume form . In this paper, we consider volume forms on which have a quadratic degeneration along an oriented submanifold .
Definition 1.1.

A Morse-Bott volume form for on is a non-negative -form with zero set such that the ratio of -forms is a Morse-Bott function for which each component of is a non-degenerate critical submanifold.
Note that the critical zero set must have Morse-Bott index since the function is non-negative on . Furthermore, the Morse-Bott property of does not depend on choice of the reference form . We prove the necessary and sufficient conditions for diffeomorphism equivalence of such Morse-Bott volume forms:
Theorem 1.2.

Let and be Morse-Bott volume forms for such that their relative cohomology classes with respect to coincide:
Then there exists a diffeomorphism such that which restricts to the identity on .
We treat this as two different cases: when the submanifold is a hypersurface, and when its codimension is at least 2.
Corollary 1.3.

If the shared zero submanifold of two Morse-Bott volume forms and on is of codimension at least 2, the forms are diffeomorphic,
if and only if they have equal total volumes of ,
If is a hypersurface in , i.e. it has codimension , it can be separating or not. Either case is covered by the following corollary:
Corollary 1.4.

If the shared zero submanifold has codimension , two Morse-Bott volume forms and are diffeomorphic,
if and only if they have coinciding volumes for each connected component of :
The same result also holds for volume forms which have hypersurface as a non-critical zero set. Let and be two -forms on with the same non-critical zero set , i.e. it is a non-critical zero set for each of the corresponding functions , . Note that must be a compact oriented hypersurface in this case.
Theorem 1.5.

Two -forms and with the same non-critical zero set are diffeomorphic,
if and only if they represent the same relative cohomology classes , or equivalently, they have coinciding volumes of each connected component of .
This theorem strengthens one of the results of Cardona and Miranda [6], who proved that two folded volumes forms with the same non-critical zero hypersurface can be mapped to each other by a diffeomorphism taking to itself, although not necessarily the identity on . (Note that while -forms change sign across the non-critical zero set , the term folded, or transversally vanishing, “volume forms” became standard and we adapt it in this paper.)
Remark 1.6.

The assumption of the orientability of and can be weakened to require only orientability of . For this reduces to orientability of . In the case of in a nonorientable , instead of volume forms one needs to consider densities, or pseudo-forms changing sign along orientation-reversing paths. Theorem 1.2 naturally extends to this setting: its proof combines tubular neighbourhood embeddings, which hold in any setting, with adapting the classical Moser theorem to each (orientable) connected component of . (As an example, it is easy to construct a Morse-Bott density on the even-dimensional real projective space with a hyperplane as a critical set: for instance take the product of function with the standard volume element on the sphere and project it to via the antipodal map.) An extension of Theorem 1.5 to the nonorientable setting might be more subtle, requiring certain averaging on the orientation cover, cf. normal forms for Morse functions and densities in the area-preserving case in [10].
Motivation
A motivation for this problem comes from the Madelung transform, which establishes an equivalence of quantum mechanics and equations of compressible fluids [12]. Namely, let a wave function on a manifold satisfy the non-linear Schrödinger (NLS) equation,
where and . Then the Madelung transform allows one to rewrite the quantum mechanics of the NLS equation in a “hydrodynamical form” as equations of a barotropic-type fluid on the velocity field and the density as follows:
The Madelung transform is well-defined provided that does not vanish on and it is understood modulo a phase factor (), while is understood to be modulo an additive constant on . Moreover, by confining to the unit sphere of normalized wave functions and the space of normalized densities , the Madelung transform can be understood as the map . It turns out to be a symplectomorphism for the corresponding natural symplectic structures on those spaces, and a Kähler map between the Fubini-Study and Fisher-Rao metrics respectively, see [12].
However, the presence of zeros of the (complex-valued) wave function brings substantial complications. A non-critical zero set of has codimension 2 in , and the corresponding density function can be understood as a Morse-Bott volume form for . The fact that is univalued on imposes the “quantization constraint” on the phase function : its change along any path in going around must be a multiple of , see numerous discussions in [9, 15]. The above equivalence theorems for the Morse-Bott volume forms allow one to deal with zero submanifolds of wave functions by using more convenient “normal forms” of the corresponding densities around zeros.
Acknowledgements
We are indebted to Alexander Givental for key suggestions on the proof, and to Yael Karshon for fruitful discussions. We are also grateful to the anonymous referee for useful suggestions. B.K. was partially supported by an NSERC Discovery Grant.