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hop07spec.dvi
www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_05.pdf10 Apr 2008: 1.5. 1. 0.5. 0ω=50. 100 200 300 400 500 6002.5. 2. ... 1.5. 1. 0.5. 0ω=100. 100 200 300 400 500 600. 2.5. -
N22a.dvi
www.damtp.cam.ac.uk/user/examples/N22a.pdf17 Jan 2008: Cop. yrig. ht. 200. 8 U. nive. rsity. of C. ambr. ... yrig. ht. 200. 8 U. nive. rsity. of C. ambr. idge. -
Paper1.dvi
www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_10.pdf1 Aug 2008: 2. 0 200. 50. 2. 1. 2. 1500. 1. 0. 200100 50 1500.8. ... left), c = [1,. 77 ,. 7. 7 , 1], m = [2, 1, 1, 2] (right) andω [0, 200]. -
N22d.dvi
www.damtp.cam.ac.uk/user/examples/N22d.pdf16 Jan 2008: Cop. yrig. ht. 200. 8 U. nive. rsity. of C. ambr. ... Hint:consider 1/p(z).]. Cop. yrig. ht. 200. 8 U. nive. rsity. of C. -
N22c.dvi
www.damtp.cam.ac.uk/user/examples/N22c.pdf16 Jan 2008: Cop. yrig. ht. 200. 8 U. nive. rsity. of C. ambr. -
Natural Sciences Tripos, Part IB Michaelmas Term 2008 Mathematical ...
www.damtp.cam.ac.uk/user/gio10/nst_notes.pdf3 Oct 2008: 2y. t2= c2. 2y. x2, c =. T. ρ. e.g. violin (D-)string: T 40 N, ρ 1 g m1: c 200 m s1. -
A5b.dvi
www.damtp.cam.ac.uk/user/hinch/teaching/A5b.pdf13 Mar 2008: Cop. yrig. ht. 200. 8 U. nive. rsity. of C. ambr. ... 1. Cop. yrig. ht. 200. 8 U. nive. rsity. of C. -
A5a.dvi
www.damtp.cam.ac.uk/user/hinch/teaching/A5a.pdf13 Mar 2008: Cop. yrig. ht. 200. 8 U. nive. rsity. of C. ambr. ... 1. Cop. yrig. ht. 200. 8 U. nive. rsity. of C. -
doi:10.1098/rspa.2007.0130
www.damtp.cam.ac.uk/user/dmas2/public_ps/RSPA20070130.pdf3 Jul 2008: REVIEW. Analysis of the adiabatic limit for solitons inclassical field theory. BY DAVID M. A. STUART. University of Cambridge, Centre for Mathematical Sciences, Wilberforce Road,Cambridge CB3 OWA, UK. We discuss the approximation of classical field -
Adv. Geosci., 15, 47–56, 2008www.adv-geosci.net/15/47/2008/©…
www.damtp.cam.ac.uk/user/mem/mci-jet-hyperb-ADGEO-08.pdf1 Jul 2008: Adv. Geosci., 15, 47–56, 2008www.adv-geosci.net/15/47/2008/ Author(s) 2008. This work is distributed underthe Creative Commons Attribution 3.0 License. Advances inGeosciences. Potential-vorticity inversion and the wave-turbulence jigsaw:
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