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11 - 20 of 24 search results for KaKaoTalk:vb20 200 |u:www.itg.cam.ac.uk where 0 match all words and 24 match some words.

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  2. Nonlinear double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper25.pdf
    30 May 2006: J. F u i d Xech. (19761, VOZ. 78, part 4? pp. 821-854 Printed in Great Britain. 82 1. Nonlinear double-diffusive convection By H E R B E R T E. H U P P E R T A N D D A N I E L R. MOORE. Department of Applied Mathematics and Theoretical Physics,

  3. PII: 0012-821X(90)90126-I

    www.itg.cam.ac.uk/people/heh/Paper98.pdf
    27 Apr 2006: 0 0. c) loo. 50 100 150 200. TIME (yrs). 50 100 150 200. ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig.

  4. PII: 0012-821X(82)90155-8

    www.itg.cam.ac.uk/people/heh/Paper45.pdf
    27 Apr 2006: Fluid Mech. 33 (1968) 183-200. 16 H.E. H u p p e r t and P.F.

  5. The growth and structure of double-diffusive cells adjacent to a…

    www.itg.cam.ac.uk/people/heh/Paper183.pdf
    5 May 2006: Perspex, 1.1 cm thick, with internal lengths and depths of 50 cm 30 cm, 200 cm 22.3 cm and 232.5 cm 40 cm.

  6. The Generation of Granitic Magmas by Intrusion of Basalt ...

    www.itg.cam.ac.uk/people/heh/Paper83.pdf
    15 Sep 2006: 400. 300. 200. a). BS. 100 2O0 300. TIME (yre). S! ... 100. 400. b). 100 200. TIME (yre). 300 4OO. FIG 5 Variations of (a) temperature, and (b) thickness of the silicic magma layer with time for a 500 m thick sillemplaced

  7. The stability of a large gas bubble rising through liquid

    www.itg.cam.ac.uk/people/heh/Paper81.pdf
    30 May 2006: 1. oo 1.712 1.26 1.42 1.10 1.24. 13.61 1.200 0.79 1.06 1.

  8. Multiple coexisting states of liquid rope coiling

    www.itg.cam.ac.uk/people/heh/Paper194.pdf
    17 May 2006: Liquid rope coiling 289. 0.6. 0.8. 1.0. 0.8. 1.0. 100 200 500 1000 2000 5000.

  9. The fluid dynamics of a basaltic magma chamber replenished by influx…

    www.itg.cam.ac.uk/people/heh/Paper39.pdf
    18 Sep 2006: In t h e case o f olivine, the best available estimate of L is 200 cal g m - 1 (Bottinga a n d Richet 1978), a n d ... 3. 100. o. z 200. I 0 I 0 0 I 0 0 0.

  10. On gravity currents propagating at the base of a stratified ambient:…

    www.itg.cam.ac.uk/people/heh/Paper184.pdf
    5 May 2006: Details of our finite-difference numericalcode are presented the Appendix. We used a mesh of 320 horizontal and 200 verticalintervals.

  11. Double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper42.pdf
    30 May 2006: Y f 5 200 -. 6 a. 250 -. 300 -. Salinity ( % o ). I I I I I I I I 34.2 34.3 3 4 4 34.5 34.6 34.7 ... 200. n E. 300. 350. I I 0.1 OC. FIGURE 8.

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