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31 - 40 of 63 search results for KaKaoTalk:ZA31 24 24 |u:www.itg.cam.ac.uk where 0 match all words and 63 match some words.
  1. Results that match 2 of 3 words

  2. 30 May 2006: The situation can be made to appear even more problematic by continuing the analysis further, (2.24)-(2.31), from which i t appears that a full, three-dimensional calculation, incorporating ... 2 [ M o ( [ ) u(l)([)Ir 2 4 v ( ) ” ( [ ) 24.
  3. 5 May 2006: 24 48.2 20.9 26 120 0.83 2.6 1760 2.7 1.38 48.2 20.5 20.3 20 1.18 1.5 2250 2.1 ... 34. 32. 30. 28. 26. 24. 22. 20. 18. 16. 14.
  4. 28 Apr 2006: InArctic sea ice. Conference held at Easton, Maryland, February 24–27, 1958.
  5. The slumping of gravity currents

    www.itg.cam.ac.uk/people/heh/Paper32.pdf
    30 May 2006: head. This Froude number should be 24 according to Benjamin, but Hoult suggests expressing it as a constant A, to be determined from experiment.
  6. The stability of a large gas bubble rising through liquid

    www.itg.cam.ac.uk/people/heh/Paper81.pdf
    30 May 2006: Stability of a large gas bubble rising through liquid 417. 24. ... 1. oo 1.712 1.26 1.42 1.10 1.24. 13.61 1.200 0.79 1.06 1.
  7. 15 Sep 2006: There is also. [Journal of Petrologf, Vol. 29, P t n 3, pp 599-«24, 1988] Oxford Umvcroty Prcu 19S8. ... FJH,. (24). We determined numerical solutions of (15)—(18) in addition to either (19)—(23) or merely (24).The differences were negligible.
  8. 26 Apr 2006: salinity of the ice) is very small; k #1 0 24 [Gross et al., 1987].
  9. flm483.dvi

    www.itg.cam.ac.uk/people/heh/Paper186.pdf
    5 Jan 2006: The experimentswere generally left to run for 24 hours, but heat loss to the laboratory became asignificant factor after roughly 10 hours. ... dy. dτ= (1 θ). (1 y)(1 Λθ). (3.24). y(τ = 0) = 1, (3.25).
  10. Multiple coexisting states of liquid rope coiling

    www.itg.cam.ac.uk/people/heh/Paper194.pdf
    17 May 2006: 4Laboratoire de Physique Statistique, UMR 8550 CNRS, Ecole Normale Supérieure, 24,rue Lhomond, 75231 Paris cédex 05, France. ... 1. 2. –12. 3. 10. G. I. IG. (ν. /g2 ). 1/3. ̂. H(g/ν2)1/3 Ĥ. ̂ (Ĥ/)10/3Π15/9. Π15/24. Π15/96. Π1–1/6
  11. Gravity currents entering a two-layer fluid

    www.itg.cam.ac.uk/people/heh/Paper37.pdf
    30 May 2006: 24-2. 740 J. Y. Holyer and H. E. Huppert. model for energy dissipation. ... The wavelengths given by (6.3) and (6.4) are 6.1 cm on the lower interface and 24-1 cm on the upper interface.

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