# An Introduction to the Mathematical Theory of Waves by Roger Knobel

By Roger Knobel

This ebook is predicated on an undergraduate path taught on the IAS/Park urban arithmetic Institute (Utah) on linear and nonlinear waves. the 1st a part of the textual content overviews the idea that of a wave, describes one-dimensional waves utilizing features of 2 variables, presents an advent to partial differential equations, and discusses computer-aided visualization recommendations. the second one a part of the e-book discusses touring waves, resulting in an outline of solitary waves and soliton suggestions of the Klein-Gordon and Korteweg-deVries equations. The wave equation is derived to version the small vibrations of a taut string, and options are built through d'Alembert's formulation and Fourier sequence. The final a part of the ebook discusses waves coming up from conservation legislation. After deriving and discussing the scalar conservation legislations, its answer is defined utilizing the tactic of features, resulting in the formation of outrage and rarefaction waves. functions of those ideas are then given for versions of site visitors movement.

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Additional resources for An Introduction to the Mathematical Theory of Waves

Example text

10. The Klein-Gordon Equation uu = auxx — bu (a, 6 positive constants) models the transverse vibration of a string with a linear restoring force. The wave train u(x,t) — Acos(kx — ut) is a solution of this equation if —UJ2 A cos (kx — cut) = a [—k2Acos(kx — cut)] — bAcos(kx — ujt) or A(UJ2 - ak2 - b) cos(kx - cut) = 0. Thus u(x, t) = A cos(kx — out) is a solution of the Klein-Gordon equation if k and UJ satisfy the dispersion relation UJ2 = ak2 + b. When UJ = yjak2 + 6, the wave train solution takes the traveling wave form lak2 + b / u(x, t) = A cos f kx — yak2 + b t) —A cos \k I x — y 4.

Is the Klein-Gordon equation dispersive? In particular, do wave train solutions with high frequency travel with faster, slower, or same speed as solutions with low frequency? (d) Show that there is a cutoff frequency UJO such that solutions with frequency u < UQ are not permitted. Chapter 7 T h e Wave Equation In this chapter the wave equation uu = c2uxx is introduced as a model for the vibration of a stretched string. 1. Vibrating strings The wave equation uu = c2uxx is a fundamental equation which describes wave phenomena in a number of different settings.

6. The previous exercise shows that u(x,t) — 4 arctan exp x — ct VT is a traveling wave solution of the Sine-Gordon equation for any speed 0 < c < 1. Animate this traveling wave three times using three different choices of c. How does the profile of the traveling wave change with c? 2. Wave fronts and pulses A sudden change in weather occurs when a cold front passes through a region. 3. Wave trains and dispersion 27 F i g u r e 4 . 1 . The profile of a wave front at time t. is a recognizable feature which identifies the location and movement of this disturbance, so a cold front is an example of a wave.