Degree of a continuous mapping - Alchetron, the free social encyclopedia

In topology, the degree of a continuous mapping between two compact oriented manifolds of the same dimension is a number that represents the number of times that the domain manifold wraps around the range manifold under the mapping. The degree is always an integer, but may be positive or negative depending on the orientations.

The degree of a map was first defined by Brouwer, who showed that the degree is homotopy invariant (invariant among homotopies), and used it to prove the Brouwer fixed point theorem. In modern mathematics, the degree of a map plays an important role in topology and geometry. In physics, the degree of a continuous map (for instance a map from space to some order parameter set) is one example of a topological quantum number.

From Sn to Sn

The simplest and most important case is the degree of a continuous map from the n -sphere S n to itself (in the case n = 1 , this is called the winding number):

Let f : S n → S n be a continuous map. Then f induces a homomorphism f ∗ : H n ( S n ) → H n ( S n ) , where H n ( ⋅ ) is the n th homology group. Considering the fact that H n ( S n ) ≅ Z , we see that f ∗ must be of the form f ∗ : x ↦ α x for some fixed α ∈ Z . This α is then called the degree of f .

Algebraic topology

Let X and Y be closed connected oriented m-dimensional manifolds. Orientability of a manifold implies that its top homology group is isomorphic to Z. Choosing an orientation means choosing a generator of the top homology group.

A continuous map f : X→Y induces a homomorphism f_* from H_m(X) to H_m(Y). Let [X], resp. [Y] be the chosen generator of H_m(X), resp. H_m(Y) (or the fundamental class of X, Y). Then the degree of f is defined to be f_*([X]). In other words,

f ∗ ( [ X ] ) = deg ⁡ ( f ) [ Y ] .

If y in Y and f ⁻¹(y) is a finite set, the degree of f can be computed by considering the m-th local homology groups of X at each point in f ⁻¹(y).

Differential topology

In the language of differential topology, the degree of a smooth map can be defined as follows: If f is a smooth map whose domain is a compact manifold and p is a regular value of f, consider the finite set

f − 1 ( p ) = { x 1 , x 2 , … , x n } .

By p being a regular value, in a neighborhood of each x_i the map f is a local diffeomorphism (it is a covering map). Diffeomorphisms can be either orientation preserving or orientation reversing. Let r be the number of points x_i at which f is orientation preserving and s be the number at which f is orientation reversing. When the domain of f is connected, the number r − s is independent of the choice of p (though n is not!) and one defines the degree of f to be r − s. This definition coincides with the algebraic topological definition above.

The same definition works for compact manifolds with boundary but then f should send the boundary of X to the boundary of Y.

One can also define degree modulo 2 (deg₂(f)) the same way as before but taking the fundamental class in Z₂ homology. In this case deg₂(f) is an element of Z₂ (the field with two elements), the manifolds need not be orientable and if n is the number of preimages of p as before then deg₂(f) is n modulo 2.

Integration of differential forms gives a pairing between (C^∞-)singular homology and de Rham cohomology: <[c], [ω]> = ∫_cω, where [c] is a homology class represented by a cycle c and ω a closed form representing a de Rham cohomology class. For a smooth map f : X→Y between orientable m-manifolds, one has

⟨ f ∗ [ c ] , [ ω ] ⟩ = ⟨ [ c ] , f ∗ [ ω ] ⟩ ,

where f_* and f* are induced maps on chains and forms respectively. Since f_*[X] = deg f · [Y], we have

deg ⁡ f ∫ Y ω = ∫ X f ∗ ω

for any m-form ω on Y.

Maps from closed region

If Ω ⊂ R n is a bounded region, f : Ω ¯ → R n smooth, p a regular value of f and p ∉ f ( ∂ Ω ) , then the degree deg ⁡ ( f , Ω , p ) is defined by the formula

deg ⁡ ( f , Ω , p ) := ∑ y ∈ f − 1 ( p ) sgn ⁡ det D f ( y )

where D f ( y ) is the Jacobi matrix of f in y . This definition of the degree may be naturally extended for non-regular values p such that deg ⁡ ( f , Ω , p ) = deg ⁡ ( f , Ω , p ′ ) where p ′ is a point close to p .

The degree satisfies the following properties:

If deg ⁡ ( f , Ω ¯ , p ) ≠ 0 , then there exists x ∈ Ω such that f ( x ) = p .

deg ⁡ ( id , Ω , y ) = 1 for all y ∈ Ω .

Decomposition property:

deg ⁡ ( f , Ω , y ) = deg ⁡ ( f , Ω 1 , y ) + deg ⁡ ( f , Ω 2 , y ) , if Ω 1 , Ω 2 are disjoint parts of Ω = Ω 1 ∪ Ω 2 and y ∉ f ( Ω ¯ ∖ ( Ω 1 ∪ Ω 2 ) ) .

Homotopy invariance: If f and g are homotopy equivalent via a homotopy F ( t ) such that F ( 0 ) = f , F ( 1 ) = g and p ∉ F ( t ) ( ∂ Ω ) , then deg ⁡ ( f , Ω , p ) = deg ⁡ ( g , Ω , p )

The function p ↦ deg ⁡ ( f , Ω , p ) is locally constant on R n − f ( ∂ Ω )

These properties characterise the degree uniquely and the degree may be defined by them in an axiomatic way.

In a similar way, we could define the degree of a map between compact oriented manifolds with boundary.

Properties

The degree of a map is a homotopy invariant; moreover for continuous maps from the sphere to itself it is a complete homotopy invariant, i.e. two maps f , g : S n → S n are homotopic if and only if deg ⁡ ( f ) = deg ⁡ ( g ) .

In other words, degree is an isomorphism between [ S n , S n ] = π n S n and Z .

Moreover, the Hopf theorem states that for any n -dimensional closed oriented manifold M, two maps f , g : M → S n are homotopic if and only if deg ⁡ ( f ) = deg ⁡ ( g ) .

A self-map f : S n → S n of the n-sphere is extendable to a map F : B n → S n from the n-ball to the n-sphere if and only if deg ⁡ ( f ) = 0 . (Here the function F extends f in the sense that f is the restriction of F to S n .)

References

Degree of a continuous mapping Wikipedia

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