Riemannian Geometry

Riemannian Geometry

Riemannian Geometry it is a draft of Lecture Notes of H.M. Khudaverdian. Manchester, 4 May 2018 Contents 1 Riemannian manifolds 1 1.1 Manifolds. Tensors. (Recollection) . 1 1.1.1 Manifolds . 1 1.1.2 Tensors on Manifold . 4 1.2 Riemannian manifold . 7 1.2.1 Riemannian manifold| manifold equipped with Rie- mannian metric . 7 1.2.2 Examples . 9 1.2.3 Scalar product ! Length of tangent vectors and angle between them . 12 1.2.4 Length of curves . 13 1.2.5 Conformally Euclidean metric . 15 1.3 Riemannian structure on the surfaces embedded in Euclidean space . 16 1.3.1 Internal and external observers . 17 1.3.2 Formulae for induced metric . 20 1.3.3 Induced Riemannian metrics. Examples. 23 1.4 Isometries of Riemannian manifolds. 28 1.4.1 Riemannian metric induced by map . 28 1.4.2 Diffeomorphism, which is an isometry . 29 1.4.3 Isometries of Riemannian manifold on itself . 30 1.4.4 Locally Euclidean Riemannian manifolds . 31 1.5 Volume element in Riemannian manifold . 34 1 1.5.1 Motivation: Gram formula for volume of parallelepiped 34 1.5.2 Examples of calculating volume element . 35 2 Covariant differentiaion. Connection. Levi Civita Connec- tion on Riemannian manifold 38 2.1 Differentiation of vector field along the vector field.—Affine connection . 38 2.1.1 Definition of connection. Christoffel symbols of con- nection . 39 2.1.2 Transformation of Christoffel symbols for an arbitrary connection . 41 2.1.3 Canonical flat affine connection . 42 2.2 Connection induced on the surfaces . 45 2.2.1 Calculation of induced connection on surfaces in E3. 46 2.3 Levi-Civita connection . 48 2.3.1 Symmetric connection . 48 2.3.2 Levi-Civita connection. Theorem and Explicit formulae 48 2.3.3 Levi-Civita connection of En . 49 2.3.4 Levi-Civita connection on 2-dimensional Riemannian manifold with metric G = adu2 + bdv2. 50 2.3.5 Example of the sphere again . 50 2.4 Levi-Civita connection = induced connection on surfaces in E3 51 3 Parallel transport and geodesics 52 3.1 Parallel transport . 52 3.1.1 Definition . 52 3.1.2 Parallel transport is a linear map. Parallel transport with respect to Levi-Civita connection . 53 3.2 Geodesics . 55 3.2.1 Definition. Geodesic on Riemannian manifold . 55 3.2.2 Geodesics and Lagrangians of "free" particle on Rie- mannian manifold. 57 3.2.3 Calculations of Christoffel symbols and geodesics us- ing the Lagrangians of a free particle. 59 3.2.4 Un-parameterised geodesic . 61 3.2.5 Parallel transport of vectors along geodesics . 63 3.2.6 Geodesics on surfaces in E3 . 63 3.2.7 Geodesics and shortest distance. 65 2 4 Surfaces in E3. Parallel transport of vectors and Theorema Egregium 66 4.1 Parallel transport of the vector and Gaussian curvature of sur- face. 66 4.1.1 Theorem of parallel transport over closed curve. Pre- liminary formulation . 66 4.1.2 Weingarten operator on surfaces and Gaussian curvature 67 4.1.3 The Weingarten operator; principal curvatures and Gaus- sian curvature . 70 4.1.4 Examples of calculation of Weingarten operator, cur- vatures for cylinder and sphere. 71 4.1.5 Theorem of parallel transport over closed curve (de- tailed formulation) . 74 4.1.6 Gauß Theorema Egregium . 76 5 Curvature tensor 78 5.1 Curvature tensor for connection . 78 5.1.1 Properties of curvature tensor . 80 5.2 Riemann curvature tensor of Riemannian manifolds. 80 5.2.1 Relation between Gaussian curvature and Riemann curvature tensor and Theorema Egregium . 82 5.3 Gauss Bonnet Theorem . 85 i 1 Riemannian manifolds 1.1 Manifolds. Tensors. (Recollection) 1.1.1 Manifolds I recall briefly basics of manifolds and tensor fields on manifolds. An n-dimensional manifold is a space such that in a vicinity of an arbi- trary point one can consider local coordinates fx1; : : : ; xng. One can consider different local coordinates. If coordinates fx1; : : : ; xng and fx10 ; : : : ; xn0 g both are defined in a vicinity of the given point then they are related by bijective transition functions which are defined on domains in Rn and taking values also in Rn: 8 10 10 1 n >x = x (x ; : : : ; x ) > 0 0 >x2 = x2 (x1; : : : ; xn) <> ::: (1.1) > n−10 n−10 1 n >x = x (x ; : : : ; x ) > 0 0 :>xn = xn (x1; : : : ; xn) We say that n-dimensional manifold is differentiable or smooth if all transition functions are diffeomorphisms, i.e. they are smooth. Invertability implies that Jacobian matrix is non-degenerate: 0 0 0 0 @x1 @x1 @x1 1 @x1 @x2 ::: @xn 0 0 0 B @x2 @x2 ::: @x2 C det B @x1 @x2 @xn C 6= 0 : (1.2) B ::: C @ 0 0 0 A @xn @xn @xn @x1 @x2 ::: @xn (If bijective function xi0 = xi0 (xi) is smooth function, and its inverse, the 0 i i i @xi transition function x = x (x ) is also smooth function, then matrices jj @xi jj @xi and jj 0 jj are both well defined, hence condition (1.2) is obeyed. @xi Example open domain in En A good example of manifold is an open domain D in n-dimensional vector space Rn. Cartesian coordinates on Rn define global coordinates on D. On the other hand one can consider an arbitrary local coordinates in different domains in Rn. E.g. one can consider polar coordinates fr; 'g in a domain 1 D = fx; y : y > 0g of R2 defined by standard formulae: ( x = r cos ' ; (1.3) y = r sin ' @x @x ! @r @' cos ' −r sin ' det @y @y = det = r (1.4) @r @' sin ' r cos ' or one can consider spherical coordinates fr; θ; 'g in a domain D = fx; y; z : x > 0; y > 0; z > 0g of R3 (or in other domain of R3) defined by standard for- mulae 8 x = r sin θ cos ' <> y = r sin θ sin ' ; :>z = r cos θ , 0 @x @x @x 1 0 1 @r @θ @' sin θ cos ' r cos θ cos ' −r sin θ sin ' det B @y @y @y C = det sin θ sin ' r cos θ sin ' r sin θ cos ' = r2 sin θ @ @r @θ @' A @ A @z @z @z cos θ −r sin θ 0 @r @θ @' (1.5) Choosing domain where polar (spherical) coordinates are well-defined we have to be aware that coordinates have to be well-defined and transition functions (1.1) have to obey condition (1.2), i.e. they have to be diffeomor- phisms. E.g. for domain D in example (1.3) Jacobian (1.4) does not vanish if and only if r > 0 in D. Consider another examples of manifolds, and local coordinates on mani- folds. Example Circle S1 in E2 Consider circle x2 + y2 = R2 of radius R in E2. One can consider on the circle different local coordinates i) polar coordinate ': ( x = R cos ' ; 0 < ' < 2π y = R sin ' (this coordinate is defined on all the circle except a point (R; 0)), 2 ii) another polar coordinate '0: ( x = R cos ' ; −π < ' < π ; y = R sin ' this coordinate is defined on all the circle except a point (−R; 0), iii) stereographic coordinate t with respect to north pole of the circle ( 2 x = 2R t Rx t2+R2 ; t = ; (1.6) t2−R2 R − y y = R t2+R2 this coordinate is defined at all the circle except the north pole, iiii) stereographic coordinate t0 with respect to south pole of the circle ( 2 0 x = 2R t Rx t02+R2 ; t0 = ; R2−t02 R + z z = R t02+R2 this coordinate is defined at all the points except the south pole. One can consider transition function between these different coordinates. E.g. polar coordinate ' coincide with polar coordinate '0 in the domain x2 + y2 > 0, and in the domain x2 + y2 < 0 '0 = ' − 2π. Transition function from polar coordinate i) to stereographic coordinates π ' t is t = tan 4 + 2 , and transition function from stereographic coordinate t to stereographic coordinate t0 is R2 t0 = ; t (see Homework 0.) Example Sphere S2 in E3 Consider sphere x2 + y2 + z2 = R2 of radius a in E3. One can consider on the sphere different local coordinates i) spherical coordinates on domain of sphere θ; ': 8 x = a sin θ cos ' <> y = a sin θ sin ' ; 0 < θ < π ; −π < ' < π :>z = a cos θ 3 ii) stereographic coordinates u; v with respect to north pole of the sphere 8 2a2u x = 2 2 2 ( <> a +u +v ax 2a2v x y a − z u = a−z y = a2+u2+v2 ; = = ; ay : 2 2 2 u v a v = :> u +v −a a−z z = a a2+u2+v2 iii) stereographic coordinates u0; v0 with respect to south pole of the sphere 8 2a2u0 >x = a2+u02+v02 ( 0 ax < 2 x y a + z u = 2a v ; = = ; a+z : y = a2+u02+v02 0 0 0 ay 2 02 02 u v a v = :> a −u −v a+z z = a a2+u2+v2 (see also Homework 0) Spherical coordinates are defined elsewhere except poles and the merid- ians y = 0; x ≤ 0. Stereographical coordinates (u; v) are defined elsewhere except north pole; stereographic coordinates (u0; v0) are defined elsewhere except south pole. One can consider transition function between these dif- ferent coordinates.E.g. transition functions from spherical coordinates i) to stereographic coordinates (u; v) are ( ax a sin θ cos ' θ u = a−z = 1−cos θ = acotan 2 cos ' ay a sin θ sin ' θ ; v = a−z = 1−cos θ = acotan 2 sin ' and transition function from stereographic coordinates u; v to stereographic coordinates (u0; v0) are ( 2 u0 = a u u2+v2 ; 0 a2v v = u2+v2 (see Homework 0.) y One very important property of stereographic projetion which we do not use in this course but it is too beautiful not to mention it: under stereographic projection all points on the circle x2 +y2 = 1 with rational coordinates x and y and only these points transform to rational points on line.

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