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21 - 30 of 30 search results for TALK:PC53 20 |u:www.damtp.cam.ac.uk where 0 match all words and 30 match some words.

  1. Results that match 1 of 2 words

  2. Paper1.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_01.pdf
    29 Jan 2005: 4. 2. 4 00 0 0. . . ,. E1,3 =. . . 0 0 1. 20 0 10 0 0. . ... E2,3 =. . . 0 0 1. 0 0 1. 20 0 0.

  3. monopole.dvi

    www.damtp.cam.ac.uk/user/tong/tasi/monopole.pdf
    30 Sep 2005: 2.5.1 Constructing the Solutions 20. 2.6 What Became of Instantons 22. ... d. dx6 iA6 i(Xi ri)σi (2.51). – 20 –. where we’ve reintroduced the spatial coordinates ri into the game.

  4. IserlesNorsett3.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_02.pdf
    17 Feb 2005: 40 600. ω100. 0.5. 0.4. 80. 0.3. 20 40. 0.2. 60. ... eiωg(x,y)dV. 20. The formula (6.1) can be generalized from d = 2 to general d 2.

  5. On the quadrature of multivariate highly oscillatory integrals over…

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_07.pdf
    3 Oct 2005: x2y3z4t)dV. 220 240 260 280 300. 0.10.20.30.40.50.6. 220 240 260 280 300. ... 20. Stein, E. (1993). Harmonic Analysis: Real-Variable Methods, Orthogonality, and Oscillatory Inte-grals.

  6. Interlacing property for B-splines Simon Foucart Department of…

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2005_03.pdf
    24 Feb 2005: w1). 20. is equal to zero, in view of Lwl,.,w1(M w1,.,wnτ0,.,τn.

  7. 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: Let us introduce the. 20. polynomial G of order 2k,. G(x) :=(1)k.

  8. an2000.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2000_03.pdf
    26 Sep 2005: 20 A. Iserles, H.Z. Munthe-Kaas, S.P. Nørsett & A. Zanna. Lie theory. ... Adp(a) g for all p G, a g. (2.20)AdpAdq = Adpq (2.21).

  9. newnotes.dvi

    www.damtp.cam.ac.uk/user/phh/atmosocean/atmos-ocean.pdf
    19 Sep 2005: is. ω2 = f2 gHk2, i.e. ω = (f2 gHk2)1/2. (3.20). The two branches of the dispersion relation correspond to waves with phase propagationin two different directions. ... ithou. t per. mis. sion. P.H.Haynes Mathematics III Atmosphere-Ocean Dynamics

  10. Part II Statistical Mechanics, Lent 2005 Prof. R.R. Horgan ...

    www.damtp.cam.ac.uk/user/rrh/notes/sphys.pdf
    14 Feb 2005: 2 THERMODYNAMICS 20. where CV is the heat capacity at constant volume and CP is heat capacity atconstant pressure.

  11. 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. ... It is an aspect of hypercredulity. 20. Lacking, at first, the most highly

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