
A triangle immersed in a saddle-shape plane (a
hyperbolic paraboloid), as well as two diverging ultraparallel lines.
Differential geometry is a
mathematical discipline that uses the methods of
differential and
integral calculus, as well as
linear and
multilinear algebra, to study problems in
geometry. The theory of plane and space
curves and of
surfaces in the three-dimensional
Euclidean space formed the basis for its initial development in the eighteenth and nineteenth century. Since the late nineteenth century, differential geometry has grown into a field concerned more generally with geometric structures on
differentiable manifolds. It is closely related with
differential topology and with the geometric aspects of the theory of
differential equations.
Grigori Perelman's proof of the
Poincaré conjecture using the techniques of
Ricci flow demonstrated the power of the differential-geometric approach to questions in
topology and highlighted the important role played by the analytic methods.
Branches of differential geometry
Riemannian geometry
Riemannian geometry studies
Riemannian manifolds,
smooth manifolds with a
Riemannian metric, a notion of a distance expressed by means of a
smooth positive definite symmetric bilinear form defined on the tangent space at each point. Riemannian geometry generalizes
Euclidean geometry to spaces that are not necessarily flat, although they still resemble the
Euclidean space at each point "infinitesimally", i.e. in the first order of approximation. Various concepts based on length, such as the
arc length of
curves,
area of plane regions, and
volume of solids all admit natural analogues in Riemannian geometry. The notion of a
directional derivative of a function from
multivariable calculus is extended in Riemannian geometry to the notion of a
covariant derivative of a
tensor. Many concepts and techniques of analysis and differential equations have been generalized to the setting of Riemannian manifolds.
A distance-preserving
diffeomorphism between Riemannian manifolds is called an
isometry. This notion can also be defined
locally, i.e. for small neighborhoods of points. Any two regular curves are locally isometric. However,
Theorema Egregium of
Gauss showed that already for surfaces, the existence of a local isometry imposes strong compatibility conditions on their metrics: the
Gaussian curvatures at the corresponding points must be the same. In higher dimensions, the
Riemann curvature tensor is an important pointwise invariant associated to a Riemannian manifold that measures how close it is to being flat. An important class of Riemannian manifolds is formed by the
Riemannian symmetric spaces, whose curvature is constant. They are the closest to the "ordinary" plane and space considered in Euclidean and
non-Euclidean geometry.
Pseudo-Riemannian geometry
Pseudo-Riemannian geometry generalizes Riemannian geometry to the case in which the
metric tensor need not be
positive-definite.
A special case of this is a
Lorentzian manifold which is the mathematical basis of Einstein's
general relativity theory of gravity.
Finsler geometry
Finsler geometry has the
Finsler manifold as the main object of study — this is a differential manifold with a
Finsler metric, i.e. a
Banach norm defined on each tangent space. A Finsler metric is a much more general structure than a Riemannian metric. A Finsler structure on a manifold
M is a function
F : T
M → [0,∞) such that:
- F(x, my) = mF(x,y) for all x, y in TM,
- F is infinitely differentiable in TM − {0},
- The vertical Hessian of F2 is positive definite.
Symplectic geometry
Symplectic geometry is the study of
symplectic manifolds. An
almost symplectic manifold is a differentiable manifold equipped with a
smoothly varying non-degenerate skew-symmetric bilinear form on each tangent space, i.e., a nondegenerate 2-
form ω, called the
symplectic form. A symplectic manifold is an almost symplectic manifold for which the symplectic form
ω is closed: d
ω = 0.
A
diffeomorphism between two symplectic manifolds which preserves the symplectic form is called a
symplectomorphism. Non-degenerate skew-symmetric bilinear forms can only exist on even dimensional vector spaces, so symplectic manifolds necessarily have even dimension. In dimension 2, a symplectic manifold is just a
surface endowed with an area form and a symplectomorphism is an area-preserving diffeomorphism. The
phase space of a mechanical system is a symplectic manifold and they made an implicit appearance already in the work of
Lagrange on
analytical mechanics and later in
Jacobi's and
Hamilton's formulation of classical mechanics.
By contrast with Riemannian geometry, where the
curvature provides a local invariant of Riemannian manifolds,
Darboux's theorem states that all symplectic manifolds are locally isomorphic. The only invariants of a symplectic manifold are global in nature and topological aspects play a prominent role in symplectic geometry. The first result in symplectic topology is probably the
Poincaré-Birkhoff theorem, conjectured by
Henri Poincaré and proved by
George Birkhoff in 1912. It claims that if an area preserving map of an
annulus twists each boundary component in opposite directions, then the map has at least two fixed points.
Contact geometry
Contact geometry deals with certain manifolds of odd dimension. It is close to symplectic geometry and like the latter, it originated in questions of classical mechanics. A
contact structure on a (2
n+1)-dimensional manifold
M is given by a smooth hyperplane field
H in the
tangent bundle that is as far as possible from being associated with the level sets of a differentiable function on
M (the technical term is "completely nonintegrable tangent hyperplane distribution"). Near each point
p, a hyperplane distribution is determined by a nowhere vanishing
1-form , which is unique up to multiplication by a nowhere vanishing function:
A local 1-form on
M is a
contact form if the restriction of its
exterior derivative to
H is a non-degenerate 2-form and thus induces a symplectic structure on
Hp at each point. If the distribution
H can be defined by a global 1-form
then this form is contact if and only if the top-dimensional form
is a
volume form on
M, i.e. does not vanish anywhere. A contact analogue of the Darboux theorem holds: all contact structures on an odd-dimensional manifold are locally isomorphic and can be brought to a certain local normal form by a suitable choice of the coordinate system.
Complex and Kähler geometry
Complex differential geometry is the study of
complex manifolds.
An
almost complex manifold is a
real manifold
, endowed with a
tensor of
type (1,1), i.e. a
vector bundle endomorphism (called an
almost complex structure)
, such that
.
It follows from this definition that an almost complex manifold is even dimensional.
An almost complex manifold is called
complex if
, where
is a tensor of type (2,1) related to
, called the
Nijenhuis tensor (or sometimes the
torsion).
An almost complex manifold is complex if and only if it admits a
holomorphic coordinate atlas.
An
almost Hermitian structure is given by an almost complex structure
J, along with a
riemannian metric g, satisfying the compatibility condition
. An almost hermitian structure
defines naturally a
differential 2-form.
The following two conditions are equivalent:
-
where
is the
Levi-Civita connection of
. In this case,
is called a
Kähler structure, and a
Kähler manifold is a manifold endowed with a Kähler structure. In particular, a Kähler manifold is both a complex and a
symplectic manifold. A large class of Kähler manifolds (the class of
Hodge manifolds) is given by all the smooth
complex projective varieties.
CR geometry
CR geometry is the study of the intrinsic geometry of boundaries of domains in
complex manifolds.
Bundles and connections
The apparatus of
vector bundles,
principal bundles, and
connections on them plays an extraordinarily important role in the modern differential geometry. A smooth manifold always carries a natural vector bundle, the
tangent bundle. Loosely speaking, this structure by itself is sufficient only for developing analysis on the manifold, while doing geometry requires in addition some way to relate the tangent spaces at different points, i.e. a notion of
parallel transport. An important example is provided by
affine connections. For a
surface in
R3, tangent planes at different points can be identified using the flat nature of the ambient Euclidean space. In
Riemannian geometry, the
Levi-Civita connection serves a similar purpose. More generally, differential geometers consider spaces with a vector bundle and a connection as a replacement for the notion of a
Riemannian manifold. In this approach, the bundle is
external to the manifold and has to be specified as a part of the structure, while the connection provides a further enhancement. In physics, the manifold may be the
spacetime and bundles and connections correspond to various physical fields.
Intrinsic versus extrinsic
Initially and up to the middle of the nineteenth century, differential geometry was studied from the
extrinsic point of view:
curves and
surfaces were considered as lying in a
Euclidean space of higher dimension (for example a surface in an
ambient space of three dimensions). The simplest results are those in the
differential geometry of curves and
differential geometry of surfaces. Starting with the work of
Riemann, the
intrinsic point of view was developed, in which one cannot speak of moving 'outside' the geometric object because it is considered as given in a free-standing way.
The intrinsic point of view is more flexible. For example, it is useful in relativity where space-time cannot naturally be taken as extrinsic (what would be 'outside' it?). With the intrinsic point of view it is harder to define the central concept of
curvature and other structures such as
connections, so there is a price to pay.
These two points of view can be reconciled, i.e. the extrinsic geometry can be considered as a structure additional to the intrinsic one. (See the
Nash embedding theorem.)
Applications of differential geometry
Below are some examples of how differential geometry is applied to other fields of science and mathematics.
- In structural geology, differential geometry is used to analyze and describe geologic structures.
See also