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&lt;div&gt;In [[Riemannian geometry]], the &#039;&#039;&#039;geodesic curvature&#039;&#039;&#039; &amp;lt;math&amp;gt;k_g&amp;lt;/math&amp;gt; of a curve &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; measures how far the curve is from being a [[geodesic]]. In a given manifold &amp;lt;math&amp;gt;\bar{M}&amp;lt;/math&amp;gt;, the &#039;&#039;&#039;geodesic curvature&#039;&#039;&#039; is just the usual &#039;&#039;&#039;curvature&#039;&#039;&#039; of &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; (see below), but when &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; is restricted to lie on a submanifold &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; of &amp;lt;math&amp;gt;\bar{M}&amp;lt;/math&amp;gt; (e.g. for [[Curvature#Curves on surfaces|curves on surfaces]]), geodesic curvature refers to the curvature of &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; in &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; and it is different in general from the curvature of &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; in the ambient manifold  &amp;lt;math&amp;gt;\bar{M}&amp;lt;/math&amp;gt;. The (ambient) curvature &amp;lt;math&amp;gt;k&amp;lt;/math&amp;gt; of &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; depends on two factors: the curvature of the submanifold &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; in the direction of &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; (the [[normal curvature]] &amp;lt;math&amp;gt;k_n&amp;lt;/math&amp;gt;), which depends only from the direction of the curve, and the curvature of &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; seen in &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; (the geodesic curvature &amp;lt;math&amp;gt;k_g&amp;lt;/math&amp;gt;), which is a second order quantity. The relation between these is &amp;lt;math&amp;gt;k = \sqrt{k_g^2+k_n^2}&amp;lt;/math&amp;gt;. In particular geodesics on &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; have zero geodesic curvature (they are &amp;quot;straight&amp;quot;), so that &amp;lt;math&amp;gt;k=k_n&amp;lt;/math&amp;gt;, which explains why they appear to be curved in ambient space whenever the submanifold is.&lt;br /&gt;
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==Definition==&lt;br /&gt;
Consider a curve &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; in a manifold &amp;lt;math&amp;gt;\bar{M}&amp;lt;/math&amp;gt;, parametrized by [[arclength]], with unit tangent vector &amp;lt;math&amp;gt;T=d\gamma/ds&amp;lt;/math&amp;gt;. Its curvature is the norm of the [[Covariant derivative#Derivative along curve|covariant derivative]] of &amp;lt;math&amp;gt;T&amp;lt;/math&amp;gt;: &amp;lt;math&amp;gt;k = \|DT/ds \|&amp;lt;/math&amp;gt;. If &amp;lt;math&amp;gt;\gamma&amp;lt;/math&amp;gt; lies on &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt;, the &#039;&#039;&#039;geodesic curvature&#039;&#039;&#039; is the norm of the projection of the covariant derivative &amp;lt;math&amp;gt;DT/ds&amp;lt;/math&amp;gt; on the tangent space to the submanifold. Conversely the &#039;&#039;&#039;normal curvature&#039;&#039;&#039; is the norm of the projection of &amp;lt;math&amp;gt;DT/ds&amp;lt;/math&amp;gt; on the normal bundle to the submanifold at the point considered.&lt;br /&gt;
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If the ambient manifold is the euclidean space &amp;lt;math&amp;gt;\mathbb{R}^n&amp;lt;/math&amp;gt;, then the covariant derivative &amp;lt;math&amp;gt;DT/ds&amp;lt;/math&amp;gt; is just the usual derivative &amp;lt;math&amp;gt;dT/ds&amp;lt;/math&amp;gt;.&lt;br /&gt;
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==Example==&lt;br /&gt;
Let &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; be the unit sphere &amp;lt;math&amp;gt;S^2&amp;lt;/math&amp;gt; in three dimensional Euclidean space. The normal curvature of &amp;lt;math&amp;gt;S^2&amp;lt;/math&amp;gt; is identically 1, independently of the direction considered. Great circles have curvature &amp;lt;math&amp;gt;k=1&amp;lt;/math&amp;gt;, so they have zero geodesic curvature, and are therefore geodesics. Smaller circles of radius &amp;lt;math&amp;gt;r&amp;lt;/math&amp;gt; will have curvature &amp;lt;math&amp;gt;1/r&amp;lt;/math&amp;gt; and geodesic curvature &amp;lt;math&amp;gt;k_g = \sqrt{1-r^2}/r&amp;lt;/math&amp;gt;.&lt;br /&gt;
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==Some results involving geodesic curvature==&lt;br /&gt;
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*The geodesic curvature is no other than the usual curvature of the curve when computed intrinsically in the submanifold &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt;. It does not depend on the way the submanifold &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; sits in &amp;lt;math&amp;gt;\bar{M}&amp;lt;/math&amp;gt;.&lt;br /&gt;
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* Geodesics of &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; have zero geodesic curvature, which is equivalent to saying that &amp;lt;math&amp;gt;DT/ds&amp;lt;/math&amp;gt; is orthogonal to the tangent space to &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt;.&lt;br /&gt;
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*On the other hand the normal curvature depends strongly on how the submanifold lies in the ambient space, but marginally on the curve: &amp;lt;math&amp;gt;k_n&amp;lt;/math&amp;gt; only depends on the point on the submanifold and the direction &amp;lt;math&amp;gt;T&amp;lt;/math&amp;gt;, but not on &amp;lt;math&amp;gt;DT/ds&amp;lt;/math&amp;gt;.&lt;br /&gt;
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*In general Riemannian geometry, the derivative is computed using the [[Levi-Civita connection]] &amp;lt;math&amp;gt;\bar{\nabla}&amp;lt;/math&amp;gt; of the ambient manifold: &amp;lt;math&amp;gt;DT/ds = \bar{\nabla}_T T&amp;lt;/math&amp;gt;. It splits into a tangent part and a normal part to the submanifold: &amp;lt;math&amp;gt;\bar{\nabla}_T T = \nabla_T T + (\bar{\nabla}_T T)^\perp&amp;lt;/math&amp;gt;. The tangent part is the usual derivative &amp;lt;math&amp;gt;\nabla_T T&amp;lt;/math&amp;gt; in &amp;lt;math&amp;gt;M&amp;lt;/math&amp;gt; (it is a particular case of Gauss equation in the [[Gauss-Codazzi equations]]), while the normal part is &amp;lt;math&amp;gt;\mathrm{I\!I}(T,T)&amp;lt;/math&amp;gt;, where &amp;lt;math&amp;gt;\mathrm{I\!I}&amp;lt;/math&amp;gt; denotes the [[second fundamental form]].&lt;br /&gt;
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*The [[Gauss–Bonnet theorem]].&lt;br /&gt;
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==See also==&lt;br /&gt;
* [[Curvature]]&lt;br /&gt;
* [[Darboux frame]]&lt;br /&gt;
* [[Gauss–Codazzi equations]]&lt;br /&gt;
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== References ==&lt;br /&gt;
*{{citation | last = do Carmo|first =Manfredo P. | title=Differential Geometry of Curves and Surfaces | publisher=Prentice-Hall | year=1976 | isbn = 0-13-212589-7}}&lt;br /&gt;
* {{citation|first=Heinrich|last=Guggenheimer|author-link=Heinrich Guggenheimer|title=Differential Geometry|year=1977|publisher=Dover|chapter=Surfaces|isbn=0-486-63433-7}}.&lt;br /&gt;
* {{springer|id=G/g044070|title=Geodesic curvature|first=Yu.S.|last=Slobodyan|year=2001}}.&lt;br /&gt;
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==External links==&lt;br /&gt;
* {{Mathworld|urlname=GeodesicCurvature|title=Geodesic curvature}}&lt;br /&gt;
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[[Category:Geodesic (mathematics)]]&lt;br /&gt;
[[Category:Manifolds]]&lt;/div&gt;</summary>
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