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  1. Results that match 2 of 3 words

  2. doi:10.1016/S0377-0257(97)00022-0

    www.damtp.cam.ac.uk/user/hinch/publications/JNNFM72_31.pdf
    10 Jul 2009: 9) for the middle elastic times. V.M. Ento6, E.J. Hinch / J. ... 9) for the middle elastictimes, the dashed curves in Figs. 10, 13 and 14.
  3. Long slender drops in a simple shear flow

    www.damtp.cam.ac.uk/user/hinch/publications/JFM98_305.pdf
    23 Jul 2009: tapering at the middle and so leads to a longer drop than one with a constant internal pressure. ... The growing differences in internal pressure between the ends and the middle reduce the efficiency of the surface tension as the length becomes large.
  4. Lagrangian drift near a wavy boundary in a viscous oscillating flow

    www.damtp.cam.ac.uk/user/hinch/publications/JFM630_391.pdf
    14 Jul 2009: To understand the Stokes drift, consider a particle which starts near to the topboundary in the middle section of the down slope at x = π/2. ... Such a good agreement was found to hold in the middle half-width of thechannel, as well as in its middle half
  5. 98PA207

    www.damtp.cam.ac.uk/user/hinch/publications/PRSLA455_3201.pdf
    10 Jul 2009: dividing the velocity ẋn by a1 to test result (4.4) and dividing the distance along thewave n by a2 to test result (4.3). ... Hence. ẋn() n5/6. (4.8)To test result (4.8) we have plotted in figure 6 the rebound velocity ẋn() divided.
  6. persescribeericalma- trulyinedwith CPUwith iodicpen-la-tua- ize of…

    www.damtp.cam.ac.uk/user/hinch/publications/JFG000957.pdf
    10 Jul 2009: The distribution is characterized by adeficit of exactly one particle surrounding any test particle. ... After several tests we found a typical vafor this constant equal to 100.
  7. The millennial atmospheric lifetimeof anthropogenic CO2 David Archer…

    www.damtp.cam.ac.uk/user/mem/archer-carbon-tail08.pdf
    30 Aug 2009: to accelerating atmospheric CO2 growth from economic activity,carbon intensity, and efficiency of natural sinks. ... Soden BJ, Wetherald RT, Stenchikov GL, Robock A (2002) Global cooling after the eruption of MountPinatubo: a test of climate feedback by
  8. Fluctuations and stratification in sedimentation of dilute…

    www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_21_093304.pdf
    10 Nov 2009: Figure 3 bottom presents the same test of thestratification scaling for the same particles of batch C with0 = 0.3% in cells of different cross sections. ... To test if the value of the local stratification in the de-scending front determines the value of
  9. PHYSICS OF FLUIDS VOLUME 15, NUMBER 12 DECEMBER 2003 ...

    www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_15_3846.pdf
    10 Jul 2009: The in-terface between the two fluids is initially at the middle heigof the tube and the Atwood number At characterizing tdensity contrast ranged from 23 102 5 to 102 1 @ ... A few test experiments were performed with zeroweakly stabilizing density
  10. Very viscous horizontal convection

    www.damtp.cam.ac.uk/user/hinch/publications/JFM611_395.pdf
    26 May 2009: Gramberg et al. (2007) did not test this prediction or associated predictionsagainst their numerical solutions, conducted for Rayleigh numbers up to 7 108. ... Benchmark tests were carried out to validate the numerical code, and the resultscompared to
  11. Powder flow down a vertical pipe: the effect of air flow

    www.damtp.cam.ac.uk/user/hinch/publications/JFM459_317.pdf
    10 Jul 2009: 328 Y. Bertho and others. Studying the stationary free-fall regime has allowed us to test measurement andmodelling tools in a simple experimental case.

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