Equivariant Morse theory for the norm-square of a moment map on a variety
Graeme Wilkin

TL;DR
This paper extends Morse theory to singular spaces, specifically for the norm-square of a moment map on affine varieties, establishing homotopy equivalences that respect group actions.
Contribution
It generalizes Morse theory to a class of singular spaces and verifies conditions for the norm-square of a moment map on affine varieties, including quiver representation spaces.
Findings
Morse theory applies to certain singular spaces with specific conditions.
Homotopy equivalence is equivariant under Hamiltonian group actions.
Main theorem holds for the norm-square of a moment map on quiver representation spaces.
Abstract
We show that the main theorem of Morse theory holds for a large class of functions on singular spaces. The function must satisfy certain conditions extending the usual requirements on a manifold that Condition C holds and the gradient flow around the critical sets is well-behaved, and the singular space must satisfy a local deformation retract condition. We then show that these conditions are satisfied when the function is the norm-square of a moment map on an affine variety, and that the homotopy equivalence from this theorem is equivariant with respect to the associated Hamiltonian group action. An important special case of these results is that the main theorem of Morse theory holds for the norm square of a moment map on the space of representations of a finite quiver with relations.
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Equivariant Morse theory for the norm-square of a moment map on a variety
Graeme Wilkin
Department of Mathematics, National University of Singapore, Singapore 119076
Abstract.
We show that the main theorem of Morse theory holds for a large class of functions on singular spaces. The function must satisfy certain conditions extending the usual requirements on a manifold that Condition C holds and the gradient flow around the critical sets is well-behaved, and the singular space must satisfy a local deformation retract condition. We then show that these conditions are satisfied when the function is the norm-square of a moment map on an affine variety, and that the homotopy equivalence from this theorem is equivariant with respect to the associated Hamiltonian group action. An important special case of these results is that the main theorem of Morse theory holds for the norm square of a moment map on the space of representations of a finite quiver with relations.
2010 Mathematics Subject Classification:
Primary: 53D20; Secondary: 37B30, 55R55
This research was partially supported by grant number R-146-000-200-112 from the National University of Singapore. The author also acknowledges support from NSF grants DMS 1107452, 1107263, 1107367 “RNMS GEometric structures And Representation varieties” (the GEAR Network).
1. Introduction
Morse theory relates information about the topology of a manifold to information about the critical points of a smooth Morse function . The “Main theorem of Morse theory” makes this precise by describing the change in the homotopy type of the level sets of in terms of analytic data (the Morse index) around the critical points. When is a proper Morse function, the statement is as follows (see for example [4]).
Theorem** (Main theorem of Morse theory).**
Let be a proper function with nondegenerate critical points, let denote a cell of dimension and given any , let .
- (1)
If there are no critical values of in then . 2. (2)
If and there is one critical value in of index then .
Various generalisations of this idea have been used to (a) deduce information about the critical points of a given function from information about the topology of a manifold (for example [28], [29], [27], [33], [39], [15], [7], [8], [12]) and (b) deduce information about the topology of a manifold from information about the critical points of a function (for example [3], [5], [40], [1], [24]).
Each of these results depends on proving an analog of the main theorem of Morse theory for a given class of functions. The generalisation most relevant to this paper is that of Kirwan in [24, Sec. 10] who proved that an analogous statement holds for minimally degenerate functions on a smooth manifold (“Morse-Kirwan functions”). Kirwan also showed that the norm-square of a moment map on a smooth symplectic manifold is always minimally degenerate and used this to derive very general results about the topology of symplectic quotients.
This idea originated in the work of Atiyah and Bott [1], who used the Morse theory of the Yang-Mills functional in order to inductively compute cohomological invariants of the moduli space of semistable holomorphic bundles on a compact Riemann surface. Their approach was algebraic in the sense that they used the Harder-Narasimhan stratification instead of the gradient flow stratification by the Yang-Mills functional, and the analytic details of the Morse theory were later filled in by Daskalopoulos [11] and Rade [35]. In [10], [42] and [43] we continued this program for certain spaces of coupled equations in gauge theory in order to derive new results about the topology of moduli spaces of Higgs bundles and stable pairs in low rank. In these examples the analog of the Morse function is the Yang-Mills-Higgs functional, which can be interpreted as the norm-square of a moment map (cf. [1], [17], [6]). The new feature is that the underlying space is singular and since the existing theory from [1] and [24] requires the underlying space to be a manifold, then a new proof of the main theorem of Morse theory is needed, which we carried out using a method specific to these particular examples in low rank. Many other interesting examples of moduli spaces (for example the quiver varieties of [25], [30] and [31]) can also be defined as the minimum of the norm-square of a moment map on a singular space, and therefore it is of interest to develop a general approach for these examples.
The first result of this paper is Theorem 1.1, which shows that the main theorem of Morse theory holds for a large class of functions on singular spaces (functions satisfying Conditions (1)–(5) below). In particular, this class of functions includes the case where is the norm-square of a moment map on an affine variety (not necessarily smooth), which extends Kirwan’s results [24, Sec. 10] from smooth varieties to varieties with singularities. An important class of examples is given by representations of a finite quiver with relations, and this paper together with [45] completes the study of the local analysis around the critical sets with a view to using the ideas of Atiyah & Bott and Kirwan to compute topological invariants of moduli spaces of quivers with relations in analogy with the approach of [10], [42] and [43].
The results are stated as follows. Let be a Riemannian manifold and let be a smooth function. The time negative gradient flow of with initial condition is denoted by satisfying
[TABLE]
Let be any closed subset preserved by the gradient flow of , i.e. if then for all such that is defined. It is not necessary to assume that exists for all , however when the initial condition is in then we do assume local existence, continuous dependence on initial conditions and Condition (2) below. Since is closed in then if and or exists in then this limit is contained in .
Define a critical point of to be a stationary point of this flow (i.e. a critical point in is a critical point of that is also contained in ). Let denote the set of critical points for . Given a critical value and the associated critical set , define and to be the stable and unstable sets of with respect to the flow
[TABLE]
Let and denote the analogous stable/unstable sets with respect to a specific critical point . Suppose also that and the flow satisfy the following conditions.
- (1)
The critical values of are isolated. 2. (2)
For any such that and any either there exists such that or exists in . Similarly, either there exists such that or exists in . 3. (3)
is real analytic and is real analytic. 4. (4)
For each non-minimal critical point , let . For each such that there are no critical values in and for each neighbourhood of there exists a neighborhood of such that for each there exists such that . 5. (5)
For each critical value let . Then there exists such that has an open neighborhood and a strong deformation retract of onto such that (using to denote the image for each ) we have
- (a)
is open in for all , 2. (b)
for all , 3. (c)
and for all .
Denote . The following theorem is the analog of the main theorem of Morse theory for .
Theorem 1.1**.**
Let be a Riemannian manifold and let be a smooth function. Let be any closed subset preserved by the gradient flow of and suppose that the restriction satisfies the conditions (1)–(5).
- (a)
If there are no critical values in then . 2. (b)
If and there is only one critical value with associated critical set then .
Moreover, if a group acts on such that (a) is -invariant and (b) the deformation retract of condition (5) is -equivariant, then these homotopy equivalences are -equivariant.
Instead of directly verifying Condition (5) for each example, Theorem 1.1 of [34] shows that it is sufficient to verify the following simpler condition, which can be done for a large class of examples.
- (5*′*)
For each critical value there exists such that there are no critical values of in , and there is a stratification of satisfying Whitney’s Condition B such that is a union of strata.
Moreover, Theorem 1.1 of [34] shows that if a compact Lie group acts on and preserves , then the deformation retract of Condition (5) can be made to be -equivariant.
In Section 6 we prove that is satisfied in the case where is the norm-square of a moment map on an affine variety. As a consequence of this, we can prove that the main theorem of Morse theory holds in this setting.
Theorem 1.2**.**
Let be a connected complex reductive group and let be a linear representation of . Suppose that the action of the maximal compact subgroup is Hamiltonian with respect to the standard symplectic structure on and let be a moment map for this action. Let be a closed affine subvariety preserved by . Then satisfies conditions (1)–(5) and therefore
- (a)
If there are no critical values in , then is -equivariantly homotopic to . 2. (b)
If and there is only one critical value with associated critical set , then is -equivariantly homotopic to .
Remark 1.3**.**
A result of Kempf [22, Lemma 1.1] shows that for an affine variety with the action of a connected reductive algebraic group , there is a representation of and a -equivariant isomorphism from to a closed affine subvariety of , and so the above theorem applies to any affine -variety.
Conditions (1) and (2) in the context of Morse theory on smooth spaces. Combining the results of [33, Sec. 10] and [37] shows that Conditions (1) and (2) are automatically satisfied by an analytic function satisfying the Palais-Smale Condition C. The advantage of Condition C is that it can be verified directly from the function (i.e. one does not need solve the gradient flow equations to verify Condition C), however many of the examples that we would like to study do not satisfy Condition C because the critical sets are non-compact. For example, in the setting of Theorem 1.2 the norm-square of a moment map on the space of representations of a quiver with an oriented cycle does not satisfy Condition C (not even equivariantly), however the norm square of a moment map on an affine variety does satisfy Conditions (1) and (2) above, since the gradient flow satisfies a compactness condition due to Sjamaar [38] (see Proposition 4.2) which allows us to prove that Conditions (1) and (2) hold in this setting.
Conditions (3) and (4) in the context of Morse theory on smooth spaces. Conditions (3) and (4) are chosen to ensure the continuity of the homotopy equivalences near the critical set (see Propositions 2.4 and 3.5). These conditions impose extra structure on the maps between level sets of defined by the gradient flow (see Lemma 4.3), which allows for the gradient flow to translate the deformation retract of Condition (5) from a neighbourhood of the unstable manifold to a neighbourhood of the critical set.
In the context of moment maps on affine varieties, it is natural to impose Condition (3), since the norm-square of a moment map on an affine variety is an analytic function. It is also natural to impose Condition (4), since this condition is satisfied by any function whose gradient flow is hyperbolic around the critical set. In particular this is true for a Morse function or a Morse-Bott function, since the flow is hyperbolic with respect to the coordinates given by the Morse Lemma (see for example [16], [21]). Since Condition (4) only involves the unstable set and not the stable set then it is also satisfied by a Morse-Kirwan function (see [24, Sec. 10] and Proposition 4.2 in this paper for more details).
Therefore Conditions (1)–(4) are natural extensions of the usual conditions needed to prove the main theorem of Morse theory for functions on a manifold (cf. [27], [33] or [24]). Lemma 4.1 shows that when is closed in and preserved by the gradient flow , then Conditions (1)–(4) can be checked by studying the properties of on the ambient smooth manifold . Therefore, in order to show that these conditions are satisfied for the norm-square of a moment map on an affine variety, it is sufficient to check these conditions for the moment map associated to a linear Hamiltonian action on a vector space, which is done in Proposition 4.2.
The structure of the singular set enters the picture via Condition (5). The deformation retract studied here is a special case of a Neighbourhood Deformation Retract (NDR) (see for example [26]), however we also require the extra conditions (a), (b) and (c) on the deformation retract in order to guarantee that the function from Section 2.2 is continuous (this is explained in Lemma 2.5), which is needed to show that the deformation retract of (3.2) is continuous. Proposition 6.7 shows that Condition (5) is satisfied when is the norm square of a moment map on an analytic variety and that the deformation retract can be chosen to be equivariant with respect to the associated Hamiltonian group action. Therefore Condition (5) is valid for a large class of interesting examples.
Connection with other examples of Morse theory on singular spaces. The stratified Morse theory of Goresky and MacPherson [13] is also valid for a large class of functions on singular spaces which includes affine varieties. This theory uses a Whitney stratification of the singular space which is compatible with the function . It is important to note that in general the norm-square of a moment map on a variety does not fulfil the conditions of Goresky and MacPherson in [13]. It may be possible to perturb the original function to obtain a new function satisfying Goresky and MacPherson’s conditions, however in doing this we lose the equivariance of the moment map and also lose the possibility of inductively computing the cohomology of the critical sets in analogy with the computations of Atiyah & Bott [1] and Kirwan [24] when the space is smooth.
The essential difference between the stratified Morse theory of [13] and the results of this paper is that Goresky and MacPherson use the local structure of the Whitney stratification to prove the main theorem of Morse theory, while for moment maps on affine varieties we already have a gradient flow which is well-behaved near the critical sets, and so we use the properties of this flow to prove Theorem 1.1 instead of using the properties of the Whitney stratification.
The Conley index theory [7] is another theory valid for singular spaces, however the proof of the homotopy invariance of the Conley index requires the critical sets to have compact neighbourhoods, which is not generally true for the norm-square of a moment map on an affine variety. In particular, the proof of 4.2(D) on p50 of [7] requires compactness (see also [36, Lemma 4.7]). Nicolaescu in [32, Thm. 9.10] also uses the homotopy invariance of the Conley index to prove an analog of the main theorem of Morse theory for tame flows with Morse-like critical points, however this proof also requires compactness. It may be possible to recover the Conley theory for moment maps on affine varieties by carefully analysing the behaviour of the gradient flow of near the ends of the critical sets, but we avoid this approach here as this would require specific knowledge of , and the theory of this paper only requires checking Conditions (1)–(5) which are already valid for a large class of examples.
Organisation of the paper. The results of Section 2 show that it is possible to deformation retract to a “good” neighbourhood of each critical set, and the results of Section 3 show that it is possible to deformation retract from this neighbourhood to the unstable manifold, which completes the proof of Theorem 1.1. In Section 4 we show that Conditions (1)–(4) are satisfied when is the norm-square of a moment map on a variety and in Section 5 we use Conditions (1)–(4) to prove a compactness theorem for sequences of flow lines. The results of Section 6 complete the proof of Theorem 1.2 by showing that Condition (5) holds for moment maps on varieties.
Acknowledgements. I would like to thank Dinh Tien Cuong and Markus Pflaum for sharing their knowledge of singular spaces, Carlos Florentino for pointing out the reference [22], and George Daskalopoulos and Richard Wentworth for discussions about our joint work [10], [42] and [43] which motivated the current project.
2. Preliminary results
This section contains the preliminary results and definitions needed to complete the proof of Theorem 1.1. The first two steps of the proof of Theorem 1.1 are contained in Proposition 2.4 and Proposition 2.8. Throughout this section and the next we will refer to Conditions (1)–(5) from the introduction.
2.1. The deformation retraction defined by the gradient flow
Lemma 2.1**.**
Suppose that satisfies Condition (2), and suppose also that there is at most one critical value in the interval . Let . Then for each there is a continuous function such that .
If then can be extended to a continuous function .
If then can be extended to a continuous function .
Moreover, also depends continuously on .
Proof.
For each , the function exists by Condition (2). Since depends continuously on and is with respect to with , then is uniquely defined and continuous with respect to .
If and then exists by Condition (2) and the same proof shows that is well-defined and continuous with respect to on . Similarly, if then is well-defined and continuous with respect to on .
To show continuous dependence on , note that
[TABLE]
Since depends continuously on then for in any closed bounded interval we have that is bounded below by a positive constant (here we use the continuity of along a compact subset of a flow line in place of Condition C as in [33]). Since we assumed that , then is bounded below by a positive constant along the entire flow line from to and therefore (2.1) implies that depends continuously on . Similarly, if and , or if and , then the same argument shows that depends continuously on . ∎
The following lemma is well-known (see for example [33, Sec. 10] or [7, Thm. 2.3]).
Lemma 2.2**.**
If satisfies Conditions (1) and (2), and there are no critical values in the interval , then there is a deformation retract .
Remark 2.3**.**
Note that Conditions (1) and (2) are a consequence of the Palais-Smale Condition C used in [33, Sec. 10] and the proof of Lemma 2.2 given in [33] only uses Conditions (1) and (2). We avoid assuming Condition C here since we would also like to consider the case where is the norm-square of a moment map on a variety, in which case Condition C fails in general since may have non-compact critical sets, but Conditions (1) and (2) still hold.
The next result shows that if we also assume Condition (3) ( is analytic), then an analogous statement is true for the situation when there is a critical value at one end of the interval .
Proposition 2.4**.**
Suppose that satisfies conditions (1), (2) and (3). Let be a critical set of with critical value and suppose that there are no critical values in the interval . Then .
Proof.
Lemma 2.1 shows that there exists a continuous function such that . This immediately gives us a deformation retract from to , and the goal of the proof is to show that this can be extended to a deformation retract from to .
Given , Lemma 2.1 implies that the gradient flow defines a continuous map of level sets by .
If then Condition (2) guarantees that for some . Therefore, for any there is a well-defined map of level sets and we aim to show that this is continuous. If then is finite and so the continuity of follows from the continuous dependence of on proved in Lemma 2.1.
If then the proof of continuity of uses the Lojasiewicz gradient inequality method of [37] as follows. Let . For every neighbourhood of in there exists a neighbourhood of in such that if then either converges to a critical point in , or there exists a finite such that . Continuity of the finite-time flow guarantees an open neighbourhood of in such that for each there exists such that and therefore . Therefore, given any open set containing , there exists an open neighbourhood of in such that , and so is continuous.
Therefore we can define a continuous deformation retract by
[TABLE]
2.2. The deformation retract to a neighbourhood of the critical set
In this section we prove Proposition 2.8, which shows that deformation retracts to the union of with the set defined below.
Now assume that conditions (1), (2), (4) and (5) hold. Let be a critical value with corresponding critical set and let , and be as in condition (5). Define for all . Define by
[TABLE]
Lemma 2.5**.**
If and , then
- (1)
* if and only if .* 2. (2)
* if and only if .* 3. (3)
* if and only if .*
Proof.
First note that since for all then the set is a connected interval for all .
- (1)
If then for all . Therefore . If then there exists such that , contradicting . Therefore .
Conversely, if then . If then (since it is connected and ) and so . Therefore implies that . 2. (2)
If then there exists such that . Then .
If then there exists such that and so since is a connected interval and by assumption. 3. (3)
If then there exists such that and . Therefore .
If then . The proof above shows that if and only if and so implies that . ∎
Corollary 2.6**.**
* is continuous.*
Proof.
The previous lemma shows that if then which is open. We also have which is open and which is also open. Therefore is open for all open sets and so is continuous. ∎
Now extend the domain of to by defining so that is constant on flow lines. Since and are continuous (Lemmas 2.1 and 2.5) then is also continuous.
Lemma 2.7**.**
For each and any there exists a neighbourhood of such that implies that .
Proof.
Given any , choose . Choose a neighbourhood of such that . Then Condition (4) says that there exists a neighbourhood of such that for each we have for some . Therefore by Lemma 2.5. ∎
We can further extend to a function
[TABLE]
by defining for and for . Lemma 2.7 shows that this is continuous. Define by
[TABLE]
and define the set . Note that is continuous since is continuous. Also note that and have the same stationary points for the flow , since if and only if and (by definition) is constant along the flow, so if and only if . In particular, there are no stationary points in since implies .
Proposition 2.8**.**
Suppose that satisfies conditions (1), (2) and (5). Then .
Proof.
Since then the proof reduces to defining a deformation retract of onto . Since if and only if and there are no stationary points for the flow in , then
- •
for all there exists such that , and
- •
for all we have for all .
Therefore is an exit set for the flow on (see [7, Def. 2.2]).
The function is continuous, so is closed in , and we have already observed that there are no stationary points for the flow in . Therefore the required deformation retract follows from Wazewski’s theorem (see for example [41] or [7, Thm 2.3]). ∎
3. Proof of the main theorem
Propositions 2.4 and 2.8 together define a deformation retract from to . In this section we complete the proof of Theorem 1.1 by constructing a deformation retract from to .
The basic idea is to construct this deformation retract by combining the gradient flow and the deformation retract from condition (5). Since these both preserve the space then the composition of these deformation retracts will also preserve . The proof that the deformation retract is continuous uses condition (4).
Given , define by
[TABLE]
Note that if then we automatically have . If then we have and so . Define by
[TABLE]
Note that it follows immediately from the definition that for all .
The functions and are chosen so that is the maximum value of to use in the definition of in (3.1) below, and is the value of in the deformation retract of (3.2). Note that implies that .
Since is composed of continuous functions that agree when and the same is true for on the set , then we have the following lemma.
Lemma 3.1**.**
* is continuous on and is continuous on .*
Definition 3.2**.**
For and , define
[TABLE]
Remark 3.3**.**
Since for all then for all and .
Lemma 3.4**.**
The function is continuous, it satisfies and for all .
Proof.
The statement that and for all follows directly from the definition of , and so it only remains to prove continuity. Since is continuous on then the problem reduces to proving that is continuous at .
Given any , note that and so , which implies that and . Therefore for all .
Given , choose an open neighbourhood of in such that implies that . Then , and so for all and all . Therefore is continuous for and all . ∎
For convenience, define by
[TABLE]
where is the deformation retract of Condition (5) and is the map from Lemma 2.1. Note that if then and so . Now define the deformation retract by
[TABLE]
Note that and so if then . If then and so .
Now we can prove that is the desired deformation retract.
Proposition 3.5**.**
Suppose that satisfies conditions (1)–(5). Then .
Proof of Proposition 3.5.
The proof reduces to showing that the deformation retract is continuous.
If then this follows from the continuity of , and . Therefore the proof reduces to proving continuity at and .
Continuity at .
Since is not continuous at then we need to prove continuity by hand. Given any we need to show that for any neighbourhood of in there exists a neighbourhood of in such that implies that .
Since is open and the flow is continuous, then we can construct an open set in with a product structure as follows. Choose and an open set such that implies that for all . Define
[TABLE]
Given such a , the continuity of the deformation retract from Condition (5) shows that for each there exists and a neighbourhood of in such that for all . Since is compact then there is a finite cover by open intervals of the form for . Therefore there exists a neighbourhood of in such that for all and .
By continuity of the finite time flow, there exists an open subset such that implies that and hence for all . Note that for all and (using the same as above). Then for all implies that for all , completing the proof of continuity at .
Continuity at .
Let and let be any neighbourhood of in . For each , we want to show that there exists a neighbourhood of in such that implies that .
Given , choose a neighbourhood of in and such that
[TABLE]
where is the map of level sets from Proposition 2.4. In the proof of Proposition 2.4 we showed that is continuous, and so for there exists a neighbourhood of in such that . The continuity of the deformation retract from Condition (5) together with the fact that is the identity on shows that for each and any there exists a neighbourhood of in such that for all and .
Now Condition (4) shows that there exists a neighbourhood of in such that for all . After shrinking if necessary, we can assume that and on . By construction, maps , and so is continuous at . ∎
We are now ready to complete the proof of Theorem 1.1.
Theorem 3.6** (Part (b) of Theorem 1.1).**
Suppose that satisfies conditions (1)–(5) and suppose that is the only critical value of in the interval . Then .
Moreover, if a group acts on such that is -invariant and the deformation retract of Condition (5) is -equivariant then the deformation retract from to is -equivariant.
Proof.
Combining the deformation retracts from Propositions 2.4, 2.8 and 3.5 proves the first statement of the theorem.
If is -invariant then the gradient flow is -equivariant. If the deformation retract of Condition (5) is -equivariant then the composition of deformation retracts from Propositions 2.4, 2.8 and 3.5 is also -equivariant, which proves the second statement of the theorem. ∎
4. Conditions (1)–(4) for the norm-square of a moment map on an affine variety
Let be a connected complex reductive algebraic group, and let be an affine variety with an algebraic action of . A result of Kempf [22, Lemma 1.1] shows that there is a representation of and a -equivariant isomorphism from to a closed affine subvariety of (which we also denote by ), and so we can assume without loss of generality that is an affine subvariety with a -action induced from the linear action of on .
Let be the maximal compact subgroup, choose a -invariant Hermitian inner product on and let . Let denote the infinitesimal action of at any . Then the action of on is Hamiltonian with a moment map given by
[TABLE]
It is easy to check that this satisfies the moment map equation (see for example [38]). For any central element the function also satisfies the moment map equation; in the following we abuse the notation and absorb this constant into the function . Define . Then the gradient flow of with initial condition has the form where satisfies and , and so is preserved by the gradient flow, since it is preserved by .
The goal of this section is to show that Conditions (1)–(4) are satisfied for in the setting described above.
First we prove a general result showing that if Conditions (1)–(4) are satisfied for , then they are satisfied on any closed subset preserved by the flow. In the case of moment maps on an affine variety described above, this lemma shows that it is sufficient to check Conditions (1)–(4) for the ambient affine space .
Lemma 4.1**.**
Let be a function satisfying Conditions (1)–(4) and let be any closed subset preserved by the gradient flow of . Then satisfies Conditions (1)–(4).
Proof.
- (1)
Since the critical values for are isolated, then the critical values for the restriction are also isolated. 2. (2)
Since is preserved by the flow, then implies that for all . If and the limit exists then it is contained in since is closed, and the same is true for if it exists. 3. (3)
The condition that the ambient manifold is analytic and is analytic is independent of and . 4. (4)
Let be a critical point for , and choose any such that there are no critical values in . Given any neighbourhood of in , let . Then is closed in , so it is also closed as a subset of . Let . Note that . Then is open in and so Condition (4) on the space shows that there exists an open neighbourhood of in such that flows into . Therefore, since the flow preserves , then flows into , and so Condition (4) is satisfied for the restriction of . ∎
Next we show that Conditions (1)–(4) are satisfied for the norm-square of a moment map associated to a linear action. Combined with Lemma 4.1, this shows that Conditions (1)–(4) are satisfied for the norm-square of a moment map on any affine variety.
Proposition 4.2**.**
Let be a connected reductive Lie group acting linearly on or and suppose that the action of the maximal compact subgroup is Hamiltonian with respect to the standard symplectic structure on . Let be a moment map for this action and define by . Then Conditions (1)–(4) are satisfied for .
Proof.
- (1)
For projective varieties Condition (1) follows from Kirwan’s explicit construction of the critical values in [24]. For affine varieties this follows from the analogous construction in [19]. 2. (2)
In the case , the flow exists for all since is compact. In particular, for any the subset is compact. Since is analytic (see below) then the Lojasiewicz inequality method of Simon [37] shows that the flow with initial condition either converges to a critical value or it flows out of the set . This is true both forwards and backwards in time and so Condition (2) is satisfied.
For the case , the result of Sjamaar [38, Lemma 4.10] shows that the function is proper on each -orbit. Since the gradient flow is contained in , then for any , the intersection of the gradient flow line with is compact. Therefore the same proof as the case shows that Condition (2) is also satisfied for . 3. (3)
The moment map associated to a linear representation is analytic, and so Condition (3) is satisfied. 4. (4)
The function is minimally degenerate (see [24]). Therefore, for each critical point , the unstable manifold has the structure of a graph over the negative eigenspace of the Hessian (see for example [16]). Around each critical point , there is a neighbourhood and coordinates such that the minimising manifold is given by , where is the number of non-negative eigenvalues of the Hessian of at . Let and . Following [24, Ch. 10], the negative gradient flow is given locally by
[TABLE]
where is diagonal with non-positive entries, is diagonal with strictly positive entries, and and their first derivatives vanish at the origin. Clearly the linearised flow , satisfies Condition (4), since the term does not increase the distance from the origin, while the term strictly increases the distance from the origin.
Then Condition (4) for the nonlinear equation (4.1) follows from the fact that the flow is topologically conjugate to the linearised flow in a neighbourhood of the critical point (see [16, Theorem 4.1]). ∎
In the remainder of the section, we show that Conditions (1)–(4) impose extra conditions on the topology of the level sets of the function near a critical point.
Let be a critical value. Conditions (1) and (2) imply that if there are no critical values in then there is a well-defined function (defined in Proposition 2.4) given by the gradient flow . Proposition 2.4 shows that if Condition (3) is also satisfied then this map is continuous.
Define the equivalence relation iff , denote the quotient by with quotient map and let be the induced injective map
[TABLE]
The next result shows that adding Condition (4) imposes more structure on the maps and .
Lemma 4.3**.**
Let be a function satisfying Conditions (1)–(4), let be a non-minimal critical value and choose any such that there are no critical values in . Then the map is closed and is a homeomorphism onto its image.
Proof.
Let be closed. We aim to show that is closed. Let . First consider the case where is a critical point. Since is continuous then is closed in , and by definition it is contained in , which is open. Therefore there is an open neighbourhood of contained in . Condition (4) implies that there exists an open neighbourhood of in such that
[TABLE]
Since the flow defines a continuous map , then if there exists an open neighbourhood of in such that for all . Therefore .
Therefore is open, and so is closed.
To see that is a homeomorphism onto its image, it is sufficient to show that it is injective, closed and continuous. It is injective by definition, and continuity and closedness follow from the associated properties of , since has the quotient topology. ∎
The following corollary of Lemma 4.3 shows that Condition (4) implies that the set of critical points with trivial unstable set (i.e. local minima) must be open in the level set.
Corollary 4.4**.**
With the same conditions as Lemma 4.3, the set of critical points such that is an open subset of .
Proof.
The level set is closed in . Then Lemma 4.3 shows that is closed in . Since Condition (2) implies that any flows to then
[TABLE]
and so is open in . ∎
Lemma 4.1 shows that Conditions (1)–(4) are preserved on restricting to a closed subset preserved by the gradient flow. The following simple example shows that Condition (4) fails if we do not assume that the subset is closed. In this example the main theorem of Morse theory also fails.
Example 4.5**.**
On define the equivalence relation and consider the quotient space . Note that the map given by is a bijection, but not a homeomorphism.
Define the function by . Note that . Although is not a manifold, we can still define a flow along which is strictly decreasing by . Note that the subset is preserved by this flow.
The flow has a single critical point . The unstable set is . Given , we have . Then any neighbourhood of in will not intersect the subset , however any neighbourhood of will intersect this set, which is preserved by the flow. Therefore Condition (4) must fail for this example.
One can also see that the main theorem of Morse theory must also fail for this example, since is disconnected, however is connected.
This example illustrates that Condition (4) is a nontrivial assumption and that if we don’t assume this condition then we need a replacement in order to ensure that the main theorem of Morse theory holds.
5. A compactness theorem for spaces of flow lines
In this section we show that Conditions (1)–(4) together with an extra compactness condition on the unstable sets imply that spaces of flow lines connecting two critical points can be compactified by spaces of broken flow lines. The same is true for spaces of flow lines connecting two critical sets if we also assume that the critical sets are compact. This type of theorem has appeared for Morse functions and Morse-Bott functions on smooth manifolds (see for example [2]), however the techniques used in these papers rely on the manifold structure of the ambient space and the Morse-Bott assumption to explicitly describe the trajectories near the critical points. Here we give a completely different proof which is intrinsic to the singular space and which replaces the Morse-Bott assumption with the more general Condition (4).
A related question is to construct a collar neighbourhood of the boundary of the space of flow lines and describe this explicitly in terms of spaces of broken flow lines. For Morse-Bott functions on smooth manifolds, this has been done in [2], and again the methods use the smooth structure of the ambient space, most notably in the assumption that the stable and unstable manifolds intersect transversally. In the paper [44] we will combine the methods of this section with the results of [45] to give an algebro-geometric description of this collar neighbourhood for the space of representations of a quiver with relations, again using a method intrinsic to the singular space.
We assume throughout this section that Conditions (1)–(4) hold. Since we always assume that is a closed subset of a Riemannian manifold , then for any there exists a neighbourhood such that for any the distance along the shortest geodesic from to is well-defined. In the remainder of this section we denote this distance by , and we also use to denote the length of a tangent vector in for any .
First we show that if the unstable set is locally compact, then Conditions (1)–(3) imply that the intersection of the unstable set with a level set of is compact if the level set is close enough to the level set containing the critical point . The local compactness condition is satisfied whenever is a subset of a finite-dimensional manifold, and it is also satisfied for examples in gauge theory such as the Yang-Mills-Higgs functional on a compact Riemann surface, where the unstable set is a subset of a finite-dimensional manifold.
Lemma 5.1**.**
Suppose that is locally compact and that satisfies Conditions (1)–(3). Let be a critical point of . Then for every such that there are no critical values in , the set is compact.
Proof.
Since the flow defines a continuous map by Proposition 2.4, and is the preimage of under this map, then is closed. Therefore, since is locally compact, then it is sufficient to show that is contained in a bounded neighbourhood of .
Since is a subset of a manifold on which the gradient flow of is well-defined, and is analytic by Condition (3), then we can apply the Lojasiewicz inequality of [37] to show that there exists and constants , such that for any satisfying , we have
[TABLE]
A standard calculation (cf. [37]) shows that for any flow line we have
[TABLE]
if . Given any there exists such that for all . Integrating the above inequality on the interval gives us
[TABLE]
Now choose such that . Given , suppose (for contradiction) that for some . Let . Since the flow is continuous then . Then the above estimate applies on the interval and so we obtain a contradiction
[TABLE]
Therefore the set must be empty, which implies that . Therefore we have shown that is closed and contained in a ball of radius around , which implies that it is compact since is locally compact.
Given any such that there are no critical values in , the flow defines a homeomorphism , and so is also compact. ∎
Given two critical points and with , define as the space of all points in that flow up to and down to . The flow defines a natural -action on .
Definition 5.2**.**
The space of flow lines connecting and is
[TABLE]
Given any , the space of flow lines is homeomorphic to . Each flow line defines a map . Given two critical points we fix and adopt the convention that for all .
Definition 5.3**.**
A sequence converges to a limit if and only if the sequence converges to a limit .
Remark 5.4**.**
This is stronger than the condition that converges to a limit in , since we also require that the limit is in . Theorem 5.6 below shows that if converges to a limit in then we can find a subsequence and interpret the limiting trajectory as a broken flow line.
Since the finite-time flow depends continuously on the initial condition, then converges to if and only if converges to for every .
In preparation for the main result of the section, we prove that the critical value at the lower endpoint of a flow line depends lower semi-continuously on the flow line.
Lemma 5.5**.**
Suppose that satisfies Conditions (1)–(4). Let be critical points with and let be a sequence of points in which converges to . Then with equality if and only if .
Proof.
Suppose that . By Condition (1) we can choose such that there are no critical values in . For each there exists such that . Since by assumption, then there also exists such that . Since converges to and the finite-time flow depends continuously on the initial condition, then converges to . Since for all then for all .
Proposition 2.4 shows that the flow defines a continuous deformation retract from to , therefore is closed in , and therefore implies that , contradicting the assumption that .
If we assume that then the same proof as above shows that . ∎
The next theorem is the main result of this section, which shows that has a natural compactification by spaces of broken flow lines.
Theorem 5.6**.**
Suppose that Conditions (1)–(4) hold and that for any critical point the unstable set is locally compact. Let be two critical points with , and let be a sequence of flow lines in . Then there exists a subsequence , a finite set of critical points with and a finite subset such that each and the following property holds. For each , define to be the unique time such that . Then for each the sequence converges to a point .
Proof.
Using Condition (1), choose such that there are no critical values in the interval . For each , let be the unique time such that . Since is compact by Lemma 5.1, then there exists a subsequence and such that converges to . If then we are done. If not, then Lemma 5.5 shows that there exists a critical point with such that . Let denote the set of critical points with critical value .
Now use Condition (1) again to choose such that contains no critical values, define and as the unique real numbers such that and . Note that converges to by Proposition 2.4. Given any neighbourhood of , Condition (4) guarantees the existence of a neighbourhood of such that flows into . Since converges to then there exists such that implies that , and so .
This is true for any neighbourhood of , and so since is compact by Lemma 5.1, then there exists a further subsequence such that converges to a point . If then we are done. If not, then Lemma 5.5 shows that for some critical point with , and we can repeat the above process inductively to obtain a finite set of critical points satisfying the conditions of the theorem. ∎
6. Condition (5) for moment maps on affine varieties
In this section we complete the proof of Theorem 1.2 by showing that Condition (5) holds for the case when is the norm-square of a moment map on an affine -variety. The goal is to reduce the problem of proving that Condition (5) is satisfied to a simpler criterion on the analyticity of the unstable set . Proposition 6.7 shows that this criterion holds for the norm-square of a moment map on an affine variety.
Let be a connected, reductive algebraic group and let be an affine algebraic -variety. By [22, Lemma 1.1], we can assume that where is a finite-dimensional vector space and the action of on is linear. Using the same notation and setup as in Section 4, let be the norm-square of the associated moment map.
Let be a critical value of and let be the associated critical set . The unstable set of is
[TABLE]
The goal of this section is to show that has the structure of a real analytic set in a neighbourhood of , and hence we can then apply Theorem 1.1 of [34] to in order to prove that the deformation retract of Condition (5) exists.
First we prove some results about the function on the smooth space , before restricting to the subset in Proposition 6.7. Using an -invariant inner product on , we identify and also use to denote the element corresponding to . The infinitesimal action of at is denoted . Note that the tangent space to the -orbit through is . Since is an affine space then (considering as a vector space with zero element at ) we can identify , and so for each we can consider as a subspace of .
Definition 6.1**.**
Let be a critical value of and let . The negative slice bundle is
[TABLE]
which is equipped with a canonical projection map .
The proof of the following lemma is contained in [24, Sec. 4].
Lemma 6.2**.**
At each critical point , the fibre is isomorphic to the negative eigenspace of the Hessian of . Moreover, is a vector bundle over , with constant rank on each connected component of .
Therefore, in a neighbourhood of the critical set, we can identify the negative slice bundle with the normal bundle to the minimising manifold of the critical set via the map given by . Now we prove that the normal bundle is real analytic in , and hence so is .
Lemma 6.3**.**
There is a neighbourhood of in such that for each there is an open neighbourhood of in and a finite set of real analytic functions such that .
Proof.
When is the norm-square of a moment map on a complex vector space, Hoskins [19] gives an explicit description of the Morse strata of based on Kirwan’s description of the strata for moment maps on projective varieties in [24]. In particular, the strata are submanifolds , where for a critical point (the choice of is unique up to the adjoint action of ) and is an open subset of the analytic set . Since the -action is analytic then the strata are also analytic submanifolds. Moreover, the critical set is a real analytic subset.
Given a critical point , there is a neighbourhood of and a projection such that is identified with a neighbourhood of the zero section of the normal bundle of at . Since is an analytic submanifold then the normal bundle is analytic and so we can choose the projection to be analytic.
Since the critical set is analytic, then the preimage of is analytic. Therefore the negative slice bundle is locally cut out by analytic functions. ∎
For a fixed finite time , the time flow defines a diffeormorphism . Since the flow is defined by the equation , for which the right-hand side depends analytically on , then as explained in [32] (see also [9, Ch. 1]) it follows from the Cauchy-Kowalevski theorem that the time solution to the flow depends analytically on the initial condition. This is summarised in the following lemma.
Lemma 6.4**.**
For each finite , the time flow defines an analytic diffeomorphism .
Before we prove that Condition (5) holds for the norm-square of a moment map on an affine variety, we first review some results of Hubbard [20] on the analyticity of the unstable manifold for analytic flows which will be used in the proof of Proposition 6.7.
In [20], Hubbard considers the general case of an analytic flow on a vector space and shows that the unstable manifold of a critical point is analytically isomorphic to the negative eigenspace of the Hessian. In this notation of this paper, given a critical point , Hubbard defines a map on each fibre and shows in [20, Thm. 6] that this is an analytic diffeomorphism in a neighbourhood of . If we use to denote the coordinate on then Hubbard also shows that the power series in converges absolutely uniformly on this neighbourhood (cf. [20, Thm. 6]) and that the map depends analytically on the critical point (cf. [20, Thm. 12]).
In order to apply these results in the proof of Proposition 6.7 below, first we complexify so that the real variables defining become complex variables defining , and with respect to these new variables the time flow (which is real analytic in the variable by Lemma 6.4) becomes a flow which is complex analytic in the variable . Via the inclusion , fixed points of the flow map to fixed points of the complexified flow . Let denote the subset of the fixed point set of containing the image of a critical set and let denote the unstable manifold of a critical point . Applying [20, Thm. 6] shows that for each , there is a complex analytic map in a neighbourhood of , and [20, Thm. 12] shows that depends complex analytically on .
If we use to denote the coordinate on , then these results show that is separately complex analytic in and , and therefore complex analytic as a function of by Hartogs’ theorem (see for example [18, Thm 2.2.8]). If we restrict to the real locus defined by then the restriction is real analytic as a function of . Therefore we have proved the following lemma.
Lemma 6.5**.**
There is a neighbourhood of the zero section of and a neighbourhood of in together with an analytic homeomorphism .
Remark 6.6**.**
It is not true in general that a function which is separately real analytic in and is then real analytic as a function of (for example, consider as explained in [18, p27]). Therefore we have to apply Hubbard’s theorem to the complexification of the flow to prove the stronger result that our map is the restriction of a map which is separately complex analytic in each variable. Then we can apply Hartogs’ theorem to show that the map is analytic in both variables. The key is that Hubbard’s results apply to the complexification of the flow.
Now we can prove that Condition (5) holds for the norm-square of a moment map on an affine variety.
Proposition 6.7**.**
Let be a connected, reductive algebraic Lie group, let be a representation of and let be an affine -variety. Suppose also that the action of the maximal compact subgroup on is Hamiltonian with respect to the standard symplectic structure on . Let be a moment map for this action and define by . Then Condition (5) is satisfied for the restriction , and the deformation retract can be chosen to be -equivariant.
Proof.
Lemma 6.3 above shows that the negative slice bundle is locally cut out by analytic functions. Lemma 6.5 shows that (in a neighbourhood of the critical set ) there is an analytic homeomorphism and therefore the unstable set is also locally cut out by analytic functions.
A priori this neighbourhood of the critical set may not intersect , however for any point there exists a finite such that . Lemma 6.4 shows that the finite-time flow defines an analytic diffeomorphism onto its image, and so there exists a neighbourhood of and a collection of functions such that . Since is an analytic set, then we can extend the results of the previous paragraph to show that is locally cut out by analytic functions.
Since the spaces , and are all -invariant analytic subsets of a finite-dimensional affine space , then we can apply Theorem 1.1 of [34] to and to show that Condition (5) holds for the function and that the deformation retract can be chosen to be -equivariant. ∎
Remark 6.8**.**
In the above proof we use Hubbard’s results to prove the existence of an analytic homeomorphism . A different question is whether this map restricts to a homeomorphism . This does not follow from the methods of [20], however in [45] we use the distance-decreasing property of the moment map flow to give a different construction of a map which does restrict to a homeomorphism and which is also -equivariant. In the next section we explain how this fits into a larger picture of using Morse theory to compute topological invariants of quiver varieties.
7. Conclusion
Theorem 1.1 shows that the homotopy type of changes by attaching a copy of as crosses a critical value . In order to relate the topological invariants of and for , it is then natural to investigate the topology of the pair .
When is a Morse function on a manifold with an appropriate compactness condition (e.g. satisfies the Palais-Smale Condition C), then one is faced with the same problem, and the solution is to use the Morse Lemma to relate the unstable manifold at a critical point to the negative eigenspace of the Hessian at . Therefore the pair is homeomorphic to , where is the dimension of the negative eigenspace of the Hessian at , and so the homotopy type of changes by attaching a cell of dimension as crosses the critical value . On a singular space this procedure fails because the Morse Lemma is no longer available and the definition of the Hessian does not make sense in the absence of the ability to take derivatives.
In this section we explain how to use the results of [45] to describe in terms of analytic data around the critical set for the space of representations of a quiver with relations. On this singular space the negative eigenspace of the Hessian is replaced by the intersection of with the negative slice bundle of Definition 6.1, which is defined in terms of the group action and is therefore intrinsic to the singular space. Since the negative slice bundle has an explicit description (6.1) in terms of analytic data around the critical set then we can develop a procedure to compute topological invariants of the pair , which will be carried out in [47].
First we recall some basic definitions (cf. [23], [30]) to set the notation for the rest of the section.
Definition 7.1**.**
A quiver is a directed graph, consisting of vertices , edges , and head/tail maps . A complex representation of a quiver consists of a collection of complex Hermitian vector spaces , and -linear homomorphisms . The dimension vector of a representation is the vector . The vector space of all representations with fixed dimension vector is denoted
[TABLE]
The groups
[TABLE]
both act on the space via the induced action on each factor
[TABLE]
With respect to the standard symplectic structure on induced from the symplectic structure on each , the action of is Hamiltonian with moment map
[TABLE]
Given any , define . In [45] we adapt the method of [46] for Higgs bundles (based on the “scattering method” of Hubbard [20]) and use the distance-decreasing property of the gradient flow of to prove the following result.
Theorem 7.2** ([45, Cor. 4.24]).**
For any critical set of and any closed subset such that , there is a -equivariant homeomorphism of pairs .
This does not follow from the usual Banach fixed point theorem technique for constructing the unstable manifold of a Morse function on a smooth space (see for example [21, Sec. 6]), since these methods rely on choosing local coordinates to define a projection onto the negative eigenspace of the Hessian at a critical point. Unless one can make this projection map compatible with the singularities in the space , then it is not obvious that both sides of remain homeomorphic after intersecting with a singular subset .
Theorem 7.2 shows that for a -variety , the problem of computing -equivariant topological invariants of the pair reduces to the same question for the pair , which we can describe explicitly in terms of the negative slice at each critical point. This is the analog of the homeomorphism for a Morse function on a manifold.
An important class of examples is when is the subvariety of representations satisfying a finite set of relations on the quiver. In the papers [14] and [47] we will investigate the topology of the pair to derive information about the cohomology groups and low-dimensional homotopy groups of moduli spaces of representations of quivers with relations.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] M. F. Atiyah and R. Bott. The Yang-Mills equations over Riemann surfaces. Philos. Trans. Roy. Soc. London Ser. A , 308(1505):523–615, 1983.
- 2[2] D. M. Austin and P. J. Braam. Morse-Bott theory and equivariant cohomology. In The Floer memorial volume , volume 133 of Progr. Math. , pages 123–183. Birkhäuser, Basel, 1995.
- 3[3] Raoul Bott. An application of the Morse theory to the topology of Lie-groups. Bull. Soc. Math. France , 84:251–281, 1956.
- 4[4] Raoul Bott. Morse theory indomitable. Inst. Hautes Études Sci. Publ. Math. , (68):99–114 (1989), 1988.
- 5[5] Raoul Bott and Hans Samelson. Applications of the theory of Morse to symmetric spaces. Amer. J. Math. , 80:964–1029, 1958.
- 6[6] Steven B. Bradlow. Special metrics and stability for holomorphic bundles with global sections. J. Differential Geom. , 33(1):169–213, 1991.
- 7[7] Charles Conley. Isolated invariant sets and the Morse index , volume 38 of CBMS Regional Conference Series in Mathematics . American Mathematical Society, Providence, R.I., 1978.
- 8[8] Charles Conley and Eduard Zehnder. Morse-type index theory for flows and periodic solutions for Hamiltonian equations. Comm. Pure Appl. Math. , 37(2):207–253, 1984.
