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  1. Results that match 1 of 2 words

  2. 1 Feb 2008: 0 10 20 30 40 50 600. 5. 10. 15. 20. ... 3è1V6ñEG;=1"J /. i>31Vð@6:v3EF<@> <Cç35è1ENêïé-DF;1þ:C>-A 17>1V6ð"õÂ651V;éDN35;zEF> :@>. 5. 0 10 20 30 400.
  3. Worked ExampleA Ping-Pong Ball Bouncing on a Plane A ...

    www.damtp.cam.ac.uk/user/reh10/lectures/ia-dyn-handout11.pdf
    25 Feb 2008: l1 =2V 21 sin θ1 cos θ1. g=. 2eV 20 sin θ0 cos θ0g. = ... L =. n=0. enl0 =2V 20 sin θ0 cos θ0. g(1 e).
  4. Transient buoyancy-driven front dynamics in nearly horizontal tubesT. …

    www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_19_123603.pdf
    29 Jan 2008: d = 20 mm corresponding values of Ret sin :48.5, 19.5, 0. ... Control parameter values: At = 3.9 103, d = 20 mm, = 106 m2 / s, and = 1.
  5. 8 Apr 2008: 19. 2.2 Supersymmetry - Algebra. 20. 2.2.1 History of Supersymmetry. 20. ... century. It has been carefully experimentally verified in many ways, especially during the past 20 years,.
  6. Spontaneous Rotating Vortex Lattices in a Pumped Decaying Condensate…

    www.damtp.cam.ac.uk/user/ngb23/publications/polariton.pdf
    11 Aug 2008: AdaptingEqs. (4) and (5) for a rotating solution [20] gives. r r r Rr; (6). ... 15. 20. 25. 30. 35. µ. FIG. 3 (color online). Chemical potential as a function ofpumping spot size R.
  7. Preprint typeset in JHEP style - PAPER VERSION June ...

    www.damtp.cam.ac.uk/user/tong/tasi/tasi.pdf
    24 Apr 2008: 1.4 The ADHM Construction 20. 1.4.1 The Metric on the Higgs Branch 23. ... 20 –. of the D(p 4)-brane [3, 5]. They are the same object!
  8. Paper2.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_12.pdf
    7 Oct 2008: 4.1features as a dashed line. 8. 0 0.05 0.1 0.15 0.20.82. ... 9. 0 0.02 0.04 0.06 0.08 0.1 0.12 0.14 0.16 0.18 0.20.82.
  9. Paper1.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_10.pdf
    1 Aug 2008: 20. 2.4. ω. 100908070. 4.2. 3.8. 50. 3.4. 3.0. 30. 2.6. ... Figure 4.1: Pointwise absolute error for two Filon-type methods. 20. at the endpoints, the second uses both function values and derivatives there.
  10. ortho5.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_04.pdf
    18 Mar 2008: Eight points have beencomputed for each integral. 0 20 40 60 80 1000. ... w0 20 40 60 80 100. 0. 0.5. 1. 1.5. 2.
  11. On Dynamics and Transport Near the Polar Mesopause in Summer

    www.damtp.cam.ac.uk/user/mem/mcintyre-mix-efficiency-jgr89.pdf
    23 Sep 2008: JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 94, NO. D12, PAGES 14,617-14,628, OCTOBER 20, 1989. ... r {-«Z3m a(sin Zm - Zm cos Zm)} (20). lfOZm AA = • -(z 2 - a 2 sin 2 z)dz - 3 -- •Zm q- «a2(zm- sinzm coszm)} (21).

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