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31 - 40 of 217 search results for TALK:PC53 20 |u:www.itg.cam.ac.uk where 0 match all words and 217 match some words.

  1. Results that match 1 of 2 words

  2. J. Fluid Mech. (2014), vol. 753, R1, doi:10.1017/jfm.2014.395…

    www.itg.cam.ac.uk/people/heh/Paper248.pdf
    21 Nov 2014: 19:. 20:. 21:. 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:.

  3. Revision received March 13, 2000. Open for discussion till ...

    www.itg.cam.ac.uk/people/heh/Paper168.pdf
    9 Feb 2004: U (cm s-1)0 5 10 15 20 25 30. 0. 200. ... b). λ. U (cm s-1)0 5 10 15 20 25 30.

  4. flm145.dvi

    www.itg.cam.ac.uk/people/heh/Paper197.pdf
    11 Oct 2006: t. θ. 5 10 15 20 25 3010–4. 10–3. 10–2. 10–1. ... 374 M. Ungarish and H. E. Huppert. t0 4 8 12 16 20 24.

  5. Modelling carbon dioxide sequestration in layered strata

    www.itg.cam.ac.uk/people/heh/Paper214.pdf
    4 Jun 2009: 1030. 25. 20. 5. 8. 6. 4. 2. 0. –20 0.5 1.0 1.5. ... plotted for times T = 5 (solid line), 10 (dotted line), 15 (short-dashed line), 20(dash–dotted line), 25 (long-dashed line) and 30 (dashed–dotted–dotted line).

  6. Initial advance of long lava flows in open channels

    www.itg.cam.ac.uk/people/heh/Paper222.pdf
    27 Aug 2010: Detailed narratives and graphical representations of lavaflows during the first 20 episodes in 1983–1984 are available in(Wolfe et al., 1988). ... Terra Nova 12, 14–20. Sparks, R.S.J., Pinkerton, H., Hulme, G., 1976.

  7. Dynamics of viscous grounding lines

    www.itg.cam.ac.uk/people/heh/Paper220.pdf
    6 May 2010: H 1. H0=. g′. 8ν(t t0) (2.20). from which H (x, t) can be determined as. ... x. h. 0.05 0.10 0.15 0.20. 0.1. 0.2. 0.3. 0.4. 0.5.

  8. J. Fluid Mech. (2017), vol. 821, pp. 330–342. c© ...

    www.itg.cam.ac.uk/people/heh/Paper259.pdf
    23 Dec 2021: 50100150200. 3010 20 40 50 60 70 80T1.5. 2.0. 2.5. 0 2 4 6 8 10. ... The point fp(0)is both singular and finite. The distance reached by the current of a flux Q after apropagation time T is already within 20 % of the theoretical radius

  9. Collapses of two-dimensional granular columns Gert Lube,1 Herbert E.…

    www.itg.cam.ac.uk/people/heh/Paper190.pdf
    5 May 2006: Unknown to the present authors, a similarstudy was undertaken by a French group 20. ... S. J. Sparks, and M. A. Hallworth,. J. Fluid Mech. 508, 175 2004.20 E.

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

    www.itg.cam.ac.uk/people/heh/Paper44.pdf
    16 Jul 2010: JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 86, NO. C7, PAGES 6547-6555, JULY 20, 1981. ... 35. 3O. z 20. -r 15. I.d I0. 5. DISTANCE FROM ICE (km) 2 4 6 8 I0 12. •

  11. Gravity-driven flows in porous layers

    www.itg.cam.ac.uk/people/heh/Paper125.pdf
    30 May 2006: Huppert and A. W. Woods. 0 20 40 60 80 100. ... Gravity-driven flows in porous layers 61. 100. 80. 20. FIGURE 4.

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