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doi:10.1016/S0377-0257(97)00022-0
www.damtp.cam.ac.uk/user/hinch/publications/JNNFM72_31.pdf10 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. -
Long slender drops in a simple shear flow
www.damtp.cam.ac.uk/user/hinch/publications/JFM98_305.pdf23 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. -
Lagrangian drift near a wavy boundary in a viscous oscillating flow
www.damtp.cam.ac.uk/user/hinch/publications/JFM630_391.pdf14 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 -
98PA207
www.damtp.cam.ac.uk/user/hinch/publications/PRSLA455_3201.pdf10 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. -
Under consideration for publication in J. Fluid Mech. 1 ...
www.damtp.cam.ac.uk/user/hinch/publications/Larrieu_etal_v4d.pdf5 Mar 2009: at the middle of adown slope, and the upper plate motion corresponded to dimensionless velocity A cos ωt(with scale ω/k). ... Such a good agreement was found to hold in the middle half-width of thechannel, as well as in its middle half-length (one meter -
persescribeericalma- trulyinedwith CPUwith iodicpen-la-tua- ize of…
www.damtp.cam.ac.uk/user/hinch/publications/JFG000957.pdf10 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. -
The millennial atmospheric lifetimeof anthropogenic CO2 David Archer…
www.damtp.cam.ac.uk/user/mem/archer-carbon-tail08.pdf30 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 -
Fluctuations and stratification in sedimentation of dilute…
www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_21_093304.pdf10 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 -
PHYSICS OF FLUIDS VOLUME 15, NUMBER 12 DECEMBER 2003 ...
www.damtp.cam.ac.uk/user/hinch/publications/PhysFluids_15_3846.pdf10 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 -
Very viscous horizontal convection
www.damtp.cam.ac.uk/user/hinch/publications/JFM611_395.pdf26 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 -
Powder flow down a vertical pipe: the effect of air flow
www.damtp.cam.ac.uk/user/hinch/publications/JFM459_317.pdf10 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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