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1 - 10 of 15 search results for katalk:za31 24 / / / / / |u:www.itg.cam.ac.uk where 0 match all words and 15 match some words.

  1. Results that match 1 of 2 words

  2. PII: 0022-0248(86)90410-0

    www.itg.cam.ac.uk/people/heh/Paper76.pdf
    19 Jul 2010: Trans. Geotherm.Res. 24 (1985) 25. Roy. Soc. London A310(1984) 511. [19] H.E.

  3. The effect of confining impermeable boundaries on gravity currents in …

    www.itg.cam.ac.uk/people/heh/Paper221.pdf
    6 May 2010: Sd 75 0.24. V 1 20 200 V a 44 0.20 V 2 60 100 V b 75 0.25V 3 40 150 V 4 40 62.

  4. Gravitational and buckling instabilities of a rheologically layered…

    www.itg.cam.ac.uk/people/heh/Paper169.pdf
    19 Jul 2010: η1. )w2(0),. (24). (. 1. k2D3 D. )w1(0) η2. η1. (1.

  5. Initial advance of long lava flows in open channels

    www.itg.cam.ac.uk/people/heh/Paper222.pdf
    27 Aug 2010: However, variations in fountain height in episode 4, asplotted in figure 1.24 of Wolfe et al. ... the night of 24–25 July 1983,when the flow front divided into two parallel lobes.

  6. The Crystallization of Lava Lakes

    www.itg.cam.ac.uk/people/heh/Paper118.pdf
    19 Jul 2010: JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 98, NO. B9, PAGES 15,891-15,901, SEPTEMBER 10, 1993. The Crystallization of Lava Lakes. M. GRAE WORSTER AND HERBERT E. HUPPERT. Institute of Theoretical Geophysics, Department of Applied Mathematics and

  7. Thermohaline Steps Induced By Melting of the Erebus Glacier Tongue

    www.itg.cam.ac.uk/people/heh/Paper44.pdf
    16 Jul 2010: Geophys. Res., 79, 1792-1797, 1974. Gebhart, B., and J. C. Molendorf, A new density relationship for pure and saline water, Deep Sea Res., 24(9), 831-848, 1977. ... Glaciol., 24, 259-271, 1979. Tressler, W. L., and A.M. Ommundsen, Seasonal oceanographic

  8. Flow and instability of thin films on a cylinder and sphere

    www.itg.cam.ac.uk/people/heh/Paper219.pdf
    6 May 2010: where representative valuesof ρ = 1.4 kg m3, g = 9.8 m s2, γ = 78 mN m1 and R = 0.24 m were fixed. ... and R = 0.24 m. Wavelengths were estimated by dividing the circumference of the leading edgeof the flow at the onset of instability by the number of

  9. PII: S0012-821X(85)80009-1

    www.itg.cam.ac.uk/people/heh/Paper67.pdf
    15 Jul 2010: This length has been calculated as several hundred kilometres for flows travelling with velocities of order 1 m / s in dykes a few metres wide [19,24]. ... 0 a n d K / Z r = 24.

  10. Double-Diffusive Convection Due to Crystallization in Magmas

    www.itg.cam.ac.uk/people/heh/Paper59.pdf
    16 Jul 2010: nly. 24 HUPPERT & SPARKS. compositional film is to substitute the film thickness into the compositional Rayleigh number, which can be re-expressed as. ... 24. I. A. -.:---n;o • • Pl AA GIOCl A S E.

  11. On heating a stable salinity gradient from below

    www.itg.cam.ac.uk/people/heh/Paper31.pdf
    30 Jun 2010: J. Fluid Mech. (1979), vol. 95, part 3, p p. 431-464. Printed i n Great Britain 43 1. On heating a stable salinity gradient from below. By H E R B E R T E. H U P P E R T A N D P. F. L I N D E N Department of Applied Mathematics and Theoretical

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