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  2. 5 May 2008 National Transport Information Incubator (NaTII) Enabling…

    www.damtp.cam.ac.uk/user/pvl/natii_publication.pdf
    13 Jun 2008: It focuses on:.  visual and simple.  the fact that the first 20% of effort gets 80% of the result.
  3. Adv. Geosci., 15, 47–56, 2008www.adv-geosci.net/15/47/2008/©…

    www.damtp.cam.ac.uk/user/mem/mci-jet-hyperb-ADGEO-08.pdf
    1 Jul 2008: ρ0. z. (ρ0f. 20. N2. ψ′. z. )= q′ , (15).
  4. 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).
  5. 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.
  6. An interpolating dispersionless integrable system

    www.damtp.cam.ac.uk/user/md327/interpolating.pdf
    1 Jul 2008: 4, 8, 14, 17, 19, 20] andsetting c = 0, b = 1 gives the dKP equation. ... Math. Phys. 273 357–78. [20] Pavlov M V 2003 Integrable hydrodynamic chains J.
  7. 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.
  8. ia-dyn-problems1.dvi

    www.damtp.cam.ac.uk/user/reh10/lectures/ia-dyn-problems1.pdf
    26 Feb 2008: 1 Two cyclists start 40 km apart and head towards each other, each going at a steadyrate of 20 km per hour.
  9. Knuz3.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_07.pdf
    31 Jul 2008: 13.1.29]. U (a, c, z) = z1cU (a 1 c, 2 c, z), (20). ... 10. 9. 8. 7. 6. 5. 4. 3. 2. K0 10 20 30 40 50.
  10. Chapter 3 Dimensional Analysis 3.1 Power Laws It is ...

    www.damtp.cam.ac.uk/user/reh10/lectures/ia-dyn-chapter3.pdf
    26 Feb 2008: f (x1)f (x2). =f (αx1)f (αx2). 20. for any α. (If we changed our units of length from metres to centimetres, for instance, we would haveα = 100.).
  11. 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.
  12. Condensation of Classical Nonlinear Waves in a Two-Component System…

    www.damtp.cam.ac.uk/user/ngb23/publications/2compCond.pdf
    7 May 2008: We note that in contrast to the kinetic equations pre-sented in [19] and [20] for the one-component case, Eq. ... 20] C. Connaughton, and Y. Pomeau, C.R. Physique 5 5, 91 (2004).[21] S.
  13. Front dynamics and macroscopic diffusion in buoyant mixingin a ...

    www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_19_125105.pdf
    29 Jan 2008: 502, Campus Universitaire, Orsay, F-91405, France. Received 29 June 2007; accepted 15 November 2007; published online 20 December 2007. ... s1. Most experiments took place insidea tube of diameter d = 20 mm; other diameter values.
  14. 3 Jul 2008: 4π. jφp(x)d x = d.}. (20). Observe that V2 = V sinceu(φ) = K( jφ σ). ... because h φ W 1,20 (Br)). c θ. p2. 0. (s R)2.
  15. Microstructural studies for rheology

    www.damtp.cam.ac.uk/user/hinch/teaching/cemracs2008.pdf
    25 Jul 2008: σ/N vs t/N2 (Rouse). Short times finite. 0.1. 1. 0 5 10 15 20.
  16. CMsummary3.dvi

    www.damtp.cam.ac.uk/user/fq201/CMsummary3.pdf
    8 Apr 2008: Mathematical Tripos Part IB 2007. COMPLEX METHODSSummary. 0. Introduction. Aims: to explain the application of complex-variable theory to. (i) Harmonic functions (and hence to Laplace’s equation in two dimensions).(ii) Real integration(iii)
  17. 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.
  18. Dunajski

    www.damtp.cam.ac.uk/user/md327/DW08.pdf
    18 Mar 2008: f0;f1/ suchthat equations (20) are satisfied. For convenience write down equations ŒL0;L1 D 0in full. ... L0;L1; : :; : / is closed for each fixed. We shall establish this fact using equations (20), and d D 0.
  19. hop07spec.dvi

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_05.pdf
    10 Apr 2008: mπ)4. 20. (mπ)6. ]. (3.5). 128ω5[. 1. (mπ)6. 22. 3. 1. ... 3T 3. 1. 5T 5). 1. (iω)6. (. T 20. 3(T 3.
  20. 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.
  21. DAMTP 2008/NA06 On the convergence of a wide range ...

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_06.pdf
    6 May 2008: They also include the bound. k1 max [ /k, γ ] k max [ δ1 , γ (M µk)1 ] (M µk) k, kK, (3.20). ... 9. the last part being obtained from the property (3.11). We replace expression(3.20) by the weaker condition.
  22. cowley.dvi

    www.damtp.cam.ac.uk/user/sjc1/papers/ictam2000/long.pdf
    25 Sep 2008: while the kinematic equation yieldsu = @x@t ; v = @y@t : (20)Van Dommelen & Shen (1980) made the key observation that (19) de-pends only on x and u, and hence that ... 19) and the rst of (20) can besolved independently of the equations governing y and v.
  23. B9Lb.dvi

    www.damtp.cam.ac.uk/user/examples/B9Lb.pdf
    30 Sep 2008: ψ(x, t) = χ(x) exp. (. iEt. ). (20). Substituting for (20) for ψ in the Schrödinger equation yields the time-independent. ... States of the special form (20) are known as stationary states.
  24. DAMTP 2008/NA03 On nonlinear optimization since 19591 M.J.D. Powell…

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_03.pdf
    29 Jan 2008: The results were staggering,especially the minimization of a periodic function F (x), x Rn, with 100 vari-ables, although problems with n = 20 were considered large at that time. ... The average values of these counts with m = 2n1 are 931, 1809,3159 and
  25. D23Ld.dvi

    www.damtp.cam.ac.uk/user/examples/D23Ld.pdf
    5 Dec 2008: 20. Cop. yrig. ht. 200. 8 U. nive. rsity. of C.
  26. Adiabatic limit and the slow motion of vortices in ...

    www.damtp.cam.ac.uk/user/dmas2/public_ps/adlim_corrected.pdf
    3 Jul 2008: Now consider the integrated form of the first equation of (1.20) (i.e. ... and corresponding Sobolev norms ‖ ‖Hs on the space of sections defined as in [20].
  27. 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).
  28. 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,.
  29. On Asymptotic Stability of Solitary Waves in Schrödinger Equation ...

    www.damtp.cam.ac.uk/user/dmas2/public_ps/bkks_finalcorrected.pdf
    3 Jul 2008: 11.27). From (11.21) and (11.27) inequality (11.20) follows.Now (11.13), (11.18), (11.19) and (11.20) imply. ... Introduce the majorant. m(t) := sup[0,t]. (1 s)3/2‖η(s)‖Lβ, t t1. 20.
  30. Mathematical Tripos: IA Vector Calculus Contents 0 Introduction i ...

    www.damtp.cam.ac.uk/user/sjc1/teaching/VC_2000.pdf
    17 Jan 2008: whenever this limit exists. Remarks. • It follows from (1.20) and the definition of a partial deriva-tive (1.14) that. ... To derive (1.52) start from the definition of a directional derivative (1.20), and use the definition of.
  31. doi:10.1098/rspa.2007.0130

    www.damtp.cam.ac.uk/user/dmas2/public_ps/RSPA20070130.pdf
    3 Jul 2008: 20).Furthermore, as e/0, the rescaled solutions qeððt=eÞ; xÞ converge toqKðxK X0ðtÞÞ in the sense that. ... which implies jj _vjj%cð1CffiffiffiffiffiffiffiEN. pÞ by (2.20). Differentiate with respect to t and.
  32. C:\Documents and Settings\Maciej Dunajski\My…

    www.damtp.cam.ac.uk/user/md327/PDElecture_old.pdf
    3 Jun 2008: 20. with (x1,x2) = (x,y) yields a second order ODE of the form.
  33. 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.
  34. Multiple Jets as PV Staircases: The Phillips Effect and ...

    www.damtp.cam.ac.uk/user/mem/dritschel-mci08.pdf
    1 Apr 2008: 7b) and, with H0 f 20 L. 2D /g, the undisturbed layer depth,.
  35. A Theoretical Framework forBackward Error Analysis on Manifolds…

    www.damtp.cam.ac.uk/user/na/NA_papers/NA2008_02.pdf
    27 Jan 2008: 20. for sufficiently small t. We will prove this. Let (U,ϕ) be a chart containing p then, in thesecoordinates, τ will have the form.
  36. 3 Oct 2008: 20. Outline proof: first prove Green’s theorem for a rectangle:. y2.

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