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1 - 9 of 9 search results for TALK:PC53 20 |u:www.itg.cam.ac.uk where 0 match all words and 9 match some words.

  1. Results that match 1 of 2 words

  2. Thursday Seminars on Theoretical Geophysics

    www.itg.cam.ac.uk/seminars/thu_2.05/mich_2008.html
    8 Oct 2008: 13 November. Peter Liss. (UEA). Air-sea exchange of trace gases. 20 November.

  3. Experimental Verification of Morphological Instabilityin Freezing…

    www.itg.cam.ac.uk/people/grae/83.pdf
    7 Aug 2008: a) Measurements of the osmotic pressure of bentoniteas a function of particle volume fraction (4 [20]; [26]; [27]; [28]). ... Soil Sci. 41, 547 (1990).[20] P. F. Low, D. M. Anderson, and P.

  4. Ice.dvi

    www.itg.cam.ac.uk/people/grae/80.pdf
    1 Feb 2008: The ratio of these buoyancyfluxes. BF /BC = βS0cp/αL 10 20 (12). ... 10 12 14 16 18 200. 5. 10. 15. 20. 12.9 12.95 13 13.050.

  5. flm021.dvi

    www.itg.cam.ac.uk/people/heh/Paper209.pdf
    14 May 2008: S. L. Peppin, H. E. Huppert and M. G. Worster. 0 5 10 15 20. ... JOM-J. Min. Met. Mat. Soc. 49, 18–20. Huppert, H. E. 1990 The fluid mechanics of solidification.

  6. jc004333 1..7

    www.itg.cam.ac.uk/people/grae/82.pdf
    7 Aug 2008: The measurements were carried out with very high vertical and temporalresolution over the course of a few days until the ice had reached a thickness ofaround 20 cm. ... 2002], indicating thatequation (3) might also be a good approximation for theaverage

  7. Viscous gravity currents inside confining channels and…

    www.itg.cam.ac.uk/people/heh/Paper210.pdf
    5 Mar 2008: 023104-2 D. Takagi and H. E. Huppert Phys. Fluids 20, 023104 2008. ... 023104-4 D. Takagi and H. E. Huppert Phys. Fluids 20, 023104 2008.

  8. doi:10.1016/j.jcrysgro.2008.04.046

    www.itg.cam.ac.uk/people/grae/85.pdf
    7 Aug 2008: 02ðhÞz. þ zLsVfEke. z zLsVfE2keh. z2, (20). where we evaluate f 01ðhÞ and f02ðhÞ using the assumption h5L, such.

  9. doi:10.1016/j.jcrysgro.2008.04.046

    www.itg.cam.ac.uk/people/heh/Paper212.pdf
    7 Aug 2008: 02ðhÞz. þ zLsVfEke. z zLsVfE2keh. z2, (20). where we evaluate f 01ðhÞ and f02ðhÞ using the assumption h5L, such.

  10. Gravity currents from a line source in an ambient flow

    www.itg.cam.ac.uk/people/heh/Paper211.pdf
    7 Aug 2008: 3. –60 –50 –40 –30 –20 –10 0. Figure 3. Location of the different solution structures in (a) (β, D) parameter space withM = U = 0, (b) (β, U) space with M = ... ii),(iii). (i). (i) (iv) (ii). (vi). (v). (ii)(iv). (vi)(v). (iii). –20 –10

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