Riemannian submersion

Summary

In differential geometry, a branch of mathematics, a Riemannian submersion is a submersion from one Riemannian manifold to another that respects the metrics, meaning that it is an orthogonal projection on tangent spaces.

Formal definition edit

Let (M, g) and (N, h) be two Riemannian manifolds and   a (surjective) submersion, i.e., a fibered manifold. The horizontal distribution   is a sub-bundle of the tangent bundle of   which depends both on the projection   and on the metric  .

Then, f is called a Riemannian submersion if and only if, for all  , the vector space isomorphism   is isometric, i.e., length-preserving.[1]

Examples edit

An example of a Riemannian submersion arises when a Lie group   acts isometrically, freely and properly on a Riemannian manifold  . The projection   to the quotient space   equipped with the quotient metric is a Riemannian submersion. For example, component-wise multiplication on   by the group of unit complex numbers yields the Hopf fibration.

Properties edit

The sectional curvature of the target space of a Riemannian submersion can be calculated from the curvature of the total space by O'Neill's formula, named for Barrett O'Neill:

 

where   are orthonormal vector fields on  ,   their horizontal lifts to  ,   is the Lie bracket of vector fields and   is the projection of the vector field   to the vertical distribution.

In particular the lower bound for the sectional curvature of   is at least as big as the lower bound for the sectional curvature of  .

Generalizations and variations edit

See also edit

Notes edit

  1. ^ Gilkey, Peter B.; Leahy, John V.; Park, Jeonghyeong (1998), Spinors, Spectral Geometry, and Riemannian Submersions, Global Analysis Research Center, Seoul National University, pp. 4–5

References edit

  • Gilkey, Peter B.; Leahy, John V.; Park, Jeonghyeong (1998), Spinors, Spectral Geometry, and Riemannian Submersions, Global Analysis Research Center, Seoul National University.
  • Barrett O'Neill. The fundamental equations of a submersion. Michigan Math. J. 13 (1966), 459–469. doi:10.1307/mmj/1028999604