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Ivancevic_Applied-Diff-Geom

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964 <strong>Applied</strong> <strong>Diff</strong>erential <strong>Geom</strong>etry: A Modern Introductionglobal space–time hyperbolicity. 7 The significance of global hyperbolicity forsingularity theorems stems from the following [Hawking and Israel (1979);Hawking and Penrose (1996)]. Let U be globally hyperbolic and let p andq be points of U that can be joined by a time like or null curve. Then thereis a time–like or null–geodesic between p and q which maximizes the lengthof time like or null curves from p to q. The method of proof is to showthe space of all time like or null curves from p to q is compact in a certaintopology. One then shows that the length of the curve is an upper semi–continuous function on this space. It must therefore attain its maximumand the curve of maximum length will be a geodesic because otherwise asmall variation will give a longer curve.One can now consider the second variation of the length of a geodesicγ. One can show that γ can be varied to a longer curve if there is aninfinitesimally neighboring geodesic from p which intersects γ again at apoint r between p and q. The point r is said to be conjugate to p. One canillustrate this by considering two points p and q on the surface of the Earth.Without loss of generality one can take p to be at the north pole. Becausethe Earth has a positive definite metric rather than a Lorentzian one, thereis a geodesic of minimal length, rather than a geodesic of maximum length.This minimal geodesic will be a line of longitude running from the northpole to the point q. But there will be another geodesic from p to q whichruns down the back from the north pole to the south pole and then up toq. This geodesic contains a point conjugate to p at the south pole where allthe geodesics from p intersect. Both geodesics from p to q are stationarypoints of the length under a small variation. But now in a positive definitemetric the second variation of a geodesic containing a conjugate point cangive a shorter curve from p to q. Thus, on the Earth, the geodesic that goesdown to the south pole and then comes up is not the shortest curve from pto q.The reason one gets conjugate points in space–time is that gravity is anattractive force. It therefore curves space–time in such a way that neighboringgeodesics are bent towards each other rather than away. One can7 Recall that an open set U is said to be globally hyperbolic if:(1) For every pair of points p and q in U the intersection of the future of p and the pastof q has compact closure. In other words, it is a bounded diamond shaped region.(2) Strong causality holds on U. That is, there are no closed or almost closed time–likecurves contained in U.

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