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  2. Cop yrig ht © 200 5 U nive rsity ...

    www.damtp.cam.ac.uk/user/hinch/teaching/B12a.pdf
    4 Nov 2005: Cop. yrig. ht. 200. 5 U. nive. rsity. of C. ambr. ... r. ]. 1. Cop. yrig. ht. 200. 5 U. nive. rsity.
  3. Cop yrig ht © 200 5 U nive rsity ...

    www.damtp.cam.ac.uk/user/hinch/teaching/B12b.pdf
    4 Nov 2005: Cop. yrig. ht. 200. 5 U. nive. rsity. of C. ambr. ... 1. Cop. yrig. ht. 200. 5 U. nive. rsity. of C.
  4. Accretion Discs Mathematical Tripos, Part III Dr G. I. ...

    www.damtp.cam.ac.uk/user/gio10/lecture16.pdf
    15 Mar 2005: imposed vertical magnetic field Bz = (200)1/2. Units are such that Lx = Ly/4 = Lz = = ρ = µ0 = 1.
  5. Nonlinear dynamics of secondary protein folding Natalia G. Berloff ...

    www.damtp.cam.ac.uk/user/ngb23/publications/protein.pdf
    16 Jan 2005: Firstly, to elucidate the stages of the secondary folding we consider a sequence of fiveamino acid regions each of length i = = 200 in our nondimensional units. ... 0 50 100 150 200. 5. 10. 15. 20. the nonlinear Schrödinger equation.
  6. PRL 94, 120401 (2005) P H Y S I ...

    www.damtp.cam.ac.uk/user/ngb23/publications/2comp.pdf
    27 Sep 2005: 1-3. 0 100 200 300 400. 50. 100. 150. 200. 250.
  7. newnotes.dvi

    www.damtp.cam.ac.uk/user/phh/atmosocean/atmos-ocean.pdf
    19 Sep 2005: DT. Dt=κT. p. Dp. Dt+ Hdiab (2.5). Cop. yrig. ht. 200. ... The relevantsolution of (3.16) is. η(x) = h sgn(x) {1 exp(|x|/LR)} ,. Cop. yrig. ht. 200. 4 U. nive. rsity. of C. ambr.
  8. Moment-free numerical integration of highly oscillatory functions…

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_04.pdf
    14 Sep 2005: As seen in Table 1, the actual error for ω = 200 isabout 0.042. ... Table 1: The absolute value of the errors for ω = 200 of the following methods of orderO. (
  9. On the quadrature of multivariate highly oscillatory integrals over…

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_07.pdf
    3 Oct 2005: We. 4. 50 100 150 200 250 300. 0.340.360.38. 0.420.44. Figure 1: The error of QLg [f, (0, 1)], scaled by ω2, with only endpoints and ... 14. 150 200 250 300 350 400. 3.5. 4. 4.5. 5.
  10. PRL 94, 010403 (2005) P H Y S I ...

    www.damtp.cam.ac.uk/user/ngb23/publications/rarevort.pdf
    12 Jan 2005: 4. Transformed Eq. (2)was expressed in second-order finite difference form us-ing 250 200 grid points, and the resulting nonlinearequations were solved by the Newton-Raphson iterationprocedure using banded
  11. Paper.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_06.pdf
    21 Sep 2005: 6040. ω80. 1.4. 200. 1. 0.8. 0.6. 0100. 1.2. 0.4. 0.2. ... 6. 60. 4. 2. 400. 200. ω100. 8. 80 60. 0.5.
  12. IserlesNorsett3.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_02.pdf
    17 Feb 2005: 0.023. 0.019. 200. 0.02. 300. Figure 6: The absolute value of error for the two QF1 methods, scaled by ω, for f (x) =ex2y and g(x, y) = ... 200. 0.52. 0.48. 0.5. 10050 150. Figure 8: The absolute value of I[f, ] (on the left) and of error in the
  13. On the value of the max-norm of the orthogonal ...

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_09.pdf
    14 Dec 2005: Jacobi projections in: Approximation theory and applications (ZviZiegler, ed.), Academic Press, New York, 1981, 187–200.
  14. Asymptotic Approaches to Transition Modelling Stephen J. Cowley…

    www.damtp.cam.ac.uk/user/sjc1/papers/AGARD.pdf
    7 Nov 2005: Asymptotic Approaches to Transition Modelling. Stephen J. Cowley Xuesong WuDAMTP Department of Mathematics. University of Cambridge Imperial CollegeSilver Street 180 Queen’s Gate. Cambridge CB3 9EW London SW7 2BZUK UK. SUMMARY. The linear and
  15. Lucidity, science, and the arts: what we can learn ...

    www.damtp.cam.ac.uk/user/mem/kobe-lecture.pdf
    28 Apr 2005: Notice that the typical period of asingle one of the oscillations is of the order of 200 years, that is, 10 humangenerations if we assume that a generation takes 20 years.
  16. Lucidity, science, and the arts: what we can learn ...

    www.damtp.cam.ac.uk/user/mem/kobe-reprint-web.pdf
    7 Apr 2005: Notice that the typical period of asingle one of the oscillations is of the order of 200 years, that is, 10 humangenerations if we assume that a generation takes 20 years.
  17. an2000.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2000_03.pdf
    26 Sep 2005: Zanna. 0 50 100 150 200 25010. -16. 10-14. 10-12. 10-10.

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