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 May 5th, 2007, 06:09 AM #1 Site Founder     Joined: Nov 2006 From: France Posts: 824 Thanks: 7 Intermediate values theorem Here's a spectacular, though very easy, application of the intermediate values theorem: prove that there exist two diametrically opposed points of the earth with equal temperature (assuming the temperature is continuously distributed, and assimilating the earth to a perfect 3 dimensional ball).
 May 18th, 2007, 10:22 AM #2 Newbie   Joined: Apr 2007 From: France Posts: 1 Thanks: 0 Let D(p) be the diametrically opposed point of p and let T(p) be the temperature of p. Manifestly f(p)=T(p)-T(D(p)) is a continuous function defined on a compact set, and f(D(p))=-f(p) , so there is Po such that f(Po)=0 and finally T(Po)=T(D(Po)) (q.e.d)

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