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41 - 50 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. doi:

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

  3. Some remarks on the initiation of inertial Taylor columns

    www.itg.cam.ac.uk/people/heh/Paper19.pdf
    30 May 2006: 3.20) /Om. where the kernel. and &t) is the zeroth-order Hankel transform of h ( r ) , given by. ... 20, 429-448. Ocean. I n s t. G.F.D. Notes, no. 2, pp.

  4. Stokes, Tyndall, Ruskin and the nineteenth-century beginnings of…

    www.itg.cam.ac.uk/people/heh/Paper271.pdf
    26 Mar 2023: Tyndall and Stokes, although members of different circles of scientific friends, were onamicable terms [20]. ... 1–20. 10 b. asel. ine. observed CMIP6 CMIP5. 1900 20001925 1950 1975.

  5. PII: 0012-821X(81)90075-3

    www.itg.cam.ac.uk/people/heh/Paper43.pdf
    16 Jan 2007: 1.40. • 1.3o >,. 1.20. 1.10 I 6 0 5 0 4 0 3 0 2 0 10. ... 149. 1.32 /. 1.31 /. 1. 3 0 /. Eo 1 2 9 /. /. _., / 1. 2 8 1.27. /. 1 2 6 / i , = / • 20 ; 0 35 4'0.

  6. rspa.royalsocietypublishing.org ResearchCite this article: Cooray H,…

    www.itg.cam.ac.uk/people/heh/Paper255.pdf
    18 May 2017: The figure shows that the analytical expression is an accurate solution for (5.20). ... We now consider the limitψ1 = ψ2 = ψ, where (5.20) is written as.

  7. PII: S0022-0248(99)00016-0

    www.itg.cam.ac.uk/people/heh/Paper148.pdf
    9 Mar 2004: Fora further description see Ref. [20]. indeterminacy; with neighbors we obtain a uniquesolution. ... Makkonen, Mater. Sci. Eng. A 148 (1991) 141.[20] J.S. Langer, Rev.

  8. High Reynolds number gravity currents along V-shaped valleys

    www.itg.cam.ac.uk/people/heh/Paper217.pdf
    18 Nov 2009: 10. 20. 30. 40. 50. 60. y. 0 5 10 15 20 25 30 35 400. ... Fluids 20 (2008) 1–8 023104. [21] M.I. Cantero, J.R. Lee, S.

  9. Static and flowing regions in granular collapses down channelsGert ...

    www.itg.cam.ac.uk/people/heh/Paper204.pdf
    23 Apr 2007: Received 15 November 2005; accepted 9 January 2007; published online 20 April 2007. ... Thewidely accepted reason for this scaling relationship is theconstant ratio of shear stress and normal stress.20.

  10. 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.

  11. doi:10.1016/j.epsl.2006.12.013

    www.itg.cam.ac.uk/people/heh/Paper203.pdf
    22 Mar 2007: Thus Layer 8 hasreflection amplitudes that are systematically some 20%higher than those of the other layers. ... 1 1 sigma(kg/m3) (kg/m3) (Pa s). 420–610 1020 20 3.0–5.0105 4106.

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