[PDF] [PDF] Enquanto dure - MIT OpenCourseWare

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[PDF] Waves, Lecture 1 - MIT OpenCourseWare

λ θ = 0 k θ = 2π θ = 4π The wavelength of a plane wave The increase of phase in the direction of the wave vector 2 Figure 1 Figure by MIT OpenCourseWare



[PDF] Posto 5 - MIT OpenCourseWare

http://ocw mit edu 21G 802 / 21G 852 Portuguese II Spring 2012 For information about citing these materials or our Terms of Use, visit: http://ocw mit edu/terms



[PDF] Enquanto dure - MIT OpenCourseWare

http://ocw mit edu 21G 802 / 21G 852 Portuguese II Spring 2012 For information about citing these materials or our Terms of Use, visit: http://ocw mit edu/terms



[PDF] Homogeneous medium, Lecture 5 - MIT OpenCourseWare

then C(k) = D(k) and C(k)+ D(k) = 2C(k) = ˜ η o Then η(x,t) = 1 2 ˜ η o −∞ +∞ ∫ (k) e i(kx+ωt) + ei(kx−ωt) [ ]dk Now ω = (sign k)(gk) 1/2 to ensure that 



[PDF] João e Maria - MIT OpenCourseWare

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[PDF] Unbounded domain - MIT OpenCourseWare

z = −1 R x (negative slope) Energy Energy 0 0 z x - Rz = 0 x - Rz = ct Plane c plane c // k x x x + Rz = 0 z cg cg 1 Figure by MIT OpenCourseWare



[PDF] Wave Motion in the Ocean and the Atmosphere, Problem set 2 - MIT

http://ocw mit edu 12 802 Wave Motion in the Ocean and the Atmosphere Spring 2008 For information about citing these materials or our Terms of Use, visit: 



[PDF] Moça do interior - MIT OpenCourseWare

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[PDF] A Vilminha - MIT OpenCourseWare

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[PDF] Internal waves modified by rotation - MIT OpenCourseWare

Look for w = wo ei(kx+ly+mz- ωt) we get the dispersion relationship ω2 = f 2 m 2 + N2 (k 2 + l2 ) k 2 + l2 + m2 4 l k m ω Figure by MIT OpenCourseWare

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