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  1. Results that match 1 of 2 words

  2. PII: 0022-0248(94)90038-8

    www.itg.cam.ac.uk/people/grae/22.pdf
    27 Apr 2006: 2.18), which can be (2.23) and (2.24) more closely.used in (2.22) to show that Segregation is more sensitive to the value of. ... 4.24)mass reduce to and we use this condition together with (4.21)—.
  3. Some remarks on the initiation of inertial Taylor columns

    www.itg.cam.ac.uk/people/heh/Paper19.pdf
    30 May 2006: r 2 ) ( r < 1) 2.94 0.93 1.27 1.00 {(‘i ( r > 1 ). - I Cylindrical Gaussian e-T2 ( f < 00) 3.13 1-12 2.24 0.86. ... If h,R-l > Fmin (2.24) t It is interesting to compare these values with the relationship h0R-l = 2 deduced by.
  4. 2000JC000559

    www.itg.cam.ac.uk/people/grae/55.pdf
    26 Apr 2006: Leppäranta, pp. 24–104,Univ. of Helsinki Press, Helsinki, 1998. Wettlaufer, J. S., Heat flux at the ice-ocean interface, J. ... E. Huppert, The phase evolution ofyoung sea ice, Geophys. Res. Lett., 24, 1251–1254, 1997a.
  5. doi:10.1098/rspa.2006.1790

    www.itg.cam.ac.uk/people/grae/77.pdf
    22 Jan 2007: Inserting equations (2.23) and (2.24) into equations (2.12)–(2.16) andlinearizing in the perturbed quantities leads to the following nonlinear ordinarydifferential equation for the disturbance amplitude:.
  6. PHYSICAL REVIEW E 87, 023015 (2013) Interface pinning of ...

    www.itg.cam.ac.uk/people/heh/Paper239.pdf
    11 Apr 2013: In a related context, the classical modelhas been modified to replace the sharp interface by a capillarytransition zone [24–26]. ... Porous Media 18, 107 (1995).[24] L. W. Lake, Enhanced Oil Recovery (Prentice-Hall, Englewood.
  7. doi:10.1016/j.jcp.2005.12.002

    www.itg.cam.ac.uk/people/grae/74.pdf
    12 Jun 2006: g. [23,24]). The major difficulties then consist in the formulation of accurate internalboundary conditions and in following the evolution of the interfaces through time. ... 104 This study 19.6 16.2 3.53 0.585 2.24[2] 19.51 16.2 3.53 0.586 2.243[3]
  8. Ageostrophic effects in rotating stratified flow

    www.itg.cam.ac.uk/people/heh/Paper17.pdf
    30 May 2006: 24-2. 372 H. E. Huppert and 144. E. Stern. $1. , //,/,////,//////////////,,,/,////// / ///,/I/ // / / / , // , / , / // , / / / / // / /, /' I -. FIGURE 1. An elevation of the channel, bounded by vertical walls at. ... Moh(x/L) e--ikg. (3.24). While in
  9. PII: 0377-0273(93)90087-8

    www.itg.cam.ac.uk/people/heh/Paper110.pdf
    27 Apr 2006: Subsequently (ap- proximately 40-50 rain from the beginning),. 24 r. KOYa_GUCHI L, kt. ... grade particles with A T = 2 4 C and Co= 1.24 wt.%.
  10. 21 Nov 2014: 19:. 20:. 21:. 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:.
  11. PII: S0301-9322(98)00062-7

    www.itg.cam.ac.uk/people/heh/Paper151.pdf
    9 Mar 2004: rNt 0 rN0 24. M. Ungarish, H.E. Huppert / International Journal of Multiphase Flow 25 (1999) 715737 725. ... For this case. the box model yields [rN/rN(0)]max=[8Fr/(3 b)]1/4. (This is by about 24% smaller than for.

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