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(ed.). Gravitational waves (IOP, 2001)(422s).

(ed.). Gravitational waves (IOP, 2001)(422s).

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16 Elements of gravitational <strong>waves</strong>particular we choose units in which c = G = 1; Greek indices run from 0to 3; Latin indices run from 1 to 3; repeat<strong>ed</strong> indices are summ<strong>ed</strong>; commasin subscripts or superscripts denote partial derivatives; and semicolons denotecovariant derivatives. The metric has positive signature. These above twotextbooks and others referr<strong>ed</strong> to at the end of these chapters give more detailson the theory that we outline here. For an even simpler introduction, bas<strong>ed</strong> on ascalar analogy to general relativity, see [1].2.1 Mathematics of lineariz<strong>ed</strong> theoryConsider a perturb<strong>ed</strong> flat spacetime. Its metric tensor can be written asg αβ = η αβ + h αβ , |h αβ |≪1, α,β = 0,...,3 (2.1)where η αβ is the Minkowski metric (−1, 1, 1, 1) and h αβ is a very smallperturbation of the flat spacetime metric. Lineariz<strong>ed</strong> theory is an approximationto general relativity that is correct to first order in the size of this perturbation.Since the size of tensor components depends on coordinates, one must be carefulwith such a definition. What we require for lineariz<strong>ed</strong> theory to be valid is thatthere should exist a coordinate system in which equation (2.1) holds in a suitablylarge region of spacetime. Even though η αβ is not the true metric tensor, we arefree to define raising and lowering indices of the perturbation with η αβ ,asifitwere a tensor on flat spacetime. We writeh αβ := η αγ η βδ h γδ .This leads to the following equation for the inverse metric, correct to first order(all we want in lineariz<strong>ed</strong> theory):g αβ = η αβ − h αβ . (2.2)The mathematics is simpler if we define the trace-revers<strong>ed</strong> metricperturbation:¯h αβ := h αβ − 1 2 η αβh, (2.3)where h := η αβ h αβ . There is considerable coordinate fre<strong>ed</strong>om in the componentsh αβ , since we can wiggle and stretch the coordinate system with a comparableamplitude and change the components. This coordinate fre<strong>ed</strong>om is call<strong>ed</strong> gaugefre<strong>ed</strong>om, by analogy with electromagnetism. We use this fre<strong>ed</strong>om to enforce theLorentz (or Hilbert) gauge:¯h αβ ,β = 0. (2.4)In this gauge the Einstein field equations (neglecting the quadratic and higherterms in h αβ ) are just a set of decoupl<strong>ed</strong> linear wave equations:( )− ∂2∂t 2 +∇2 ¯h αβ =−16πT αβ . (2.5)

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