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1 - 10 of 12 search results for TALK:PC53 20 |u:www.itg.cam.ac.uk where 0 match all words and 12 match some words.

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  2. doi:

    www.itg.cam.ac.uk/people/heh/Paper241.pdf
    11 Apr 2013: 20. 40. 60. 80. 100. 120. 1 2 3 4 5 6 7. ... E. Huppert, J. A. Neufeld and C. Strandkvist. 0 20 40 60 80 100.

  3. grl50082 307..311

    www.itg.cam.ac.uk/people/grae/105.pdf
    9 Apr 2013: since the model includes a number of idealiza-tions, for quantitative implementation we propose tuningthis factor with experimental results.[20] In conclusion, the dimensional vertical component of.

  4. PHYSICAL REVIEW E 87, 023015 (2013) Interface pinning of ...

    www.itg.cam.ac.uk/people/heh/Paper239.pdf
    11 Apr 2013: a) (b). buoyant fluid ambient fluid. 56 cm. 2, 5, 10or 20 cm. ... 0 5 10 15 20 250. 0.2. 0.4. 0.6. 0.8. 1.

  5. doi:

    www.itg.cam.ac.uk/people/heh/Paper240.pdf
    14 Feb 2013: 11:. 12:. 13:. 14:. 15:. 16:. 17:. 18:. 19:. 20:. 21:.

  6. Handbook of Environmental Fluid Dynamics: Overview and Fundamentals

    www.itg.cam.ac.uk/people/grae/104.pdf
    9 Apr 2013: is.about.20.in.the.polar.oceans,.which.is.why.the.densest.abys-sal.waters.are.generated.around.Antarctica,.where.polynyas.are.commonly.formed.by.strong.katabatic.winds.off.the.continent,. ... measure.the. brine. diffusivity. and. volume. fraction. of. ice

  7. Handbook of Environmental Fluid Dynamics: Overview and Fundamentals

    www.itg.cam.ac.uk/people/heh/Paper236.pdf
    11 Apr 2013: is.about.20.in.the.polar.oceans,.which.is.why.the.densest.abys-sal.waters.are.generated.around.Antarctica,.where.polynyas.are.commonly.formed.by.strong.katabatic.winds.off.the.continent,. ... measure.the. brine. diffusivity. and. volume. fraction. of. ice

  8. la303458m 1..12

    www.itg.cam.ac.uk/people/grae/103.pdf
    9 Apr 2013: and then pulsed with an ultrasonic probe(Branson Sonifier 250) at 20 kHz for 5 min to fully disperse theparticles and break up any remaining agglomerates. ... The aluminaparticles used in the present study closely follow a log-normalsize distribution

  9. On the hydrodynamic interaction between a particle and a ...

    www.itg.cam.ac.uk/people/heh/Paper244.pdf
    30 Jul 2013: 1.0. s. P. n10n4n2. Β=100. Β=5. 1 2 5 10 20 50 1000.10. ... 1.00. 0.50. 0.20. 0.30. 0.15. 0.70. Β. P. 0. n10n4n2. (a) (b).

  10. The effects of capillary forces on the axisymmetric propagation ...

    www.itg.cam.ac.uk/people/heh/Paper243.pdf
    12 Apr 2013: Received 13 July 2012; accepted 20 December 2012; published online 21 March 2013). ... η = (ϕ2/Qub)1/4 r t 1/2, (20)such that the radius of the current is given by.

  11. Spreading and convective dissolution of carbon dioxide in vertically…

    www.itg.cam.ac.uk/people/heh/Paper237.pdf
    14 Feb 2013: 4.1. Buoyant Spreading Without ConvectiveDissolution. [20] In the absence of convective dissolution, the modelfor the spreading of a buoyant current in a confined porouslayer can be written [e.g., Bear, ... 2011]. [45] For an aquifer of thickness H 20 m,

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