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  1. Results that match 2 of 3 words

  2. J. Fluid Mech. (2002), vol. 458, pp. 283–301. c© ...

    www.itg.cam.ac.uk/people/heh/Paper171.pdf
    9 Mar 2004: Thus, formally, the head reacts to thedensity difference at the middle of its height, which is larger than zero (and henceinduces motion) even in the extreme case when ρc = ρb ... 2001). The objectives are (a) to test the ability of the numerical
  3. 30 Oct 2015: The model does, however, qualitativelycapture the observed behaviour. Using this value for E, the theoretical curve lies in the middle ofthe dimensionless data. ... This is expected because in the experiments of Ellison and Turner2 Res wasapproximately
  4. 16 Jul 2010: Thispossibility was also noted by Irvine (1980). To test thishypothesis further, Kerr & Tait (1985a) carried out aseries of experiments on crystal growth in a porousmedium using the Na2SO4-CuSO4-H2O ternarysystem. ... The hypothesis that wewished to test
  5. 20 Nov 2014: In order to test the predictiveability of our model in terms of sea-ice growth and salt fluxes, we compare its results with measurementsfrom laboratory experiments in section 3. ... 1997], not because they are necessarilybetter, but because they were
  6. J. Fluid Mech. (2001), vol. 447, pp. 1–29. c© ...

    www.itg.cam.ac.uk/people/heh/Paper164.pdf
    9 Mar 2004: Some test cases were also run with a direct solver for theblock tri-diagonal system. ... other runs with small C, as an additional test of the predictivepower of the numerical code and the SW approximation.
  7. flm1000488a

    www.itg.cam.ac.uk/people/heh/Paper224.pdf
    18 Jan 2011: ln t =m1. ES+ m2 m3 ln(ES ) m4ES. (4.19). This enables us to extract the asymptotic nature of the solution and test the long-time limit (4.17) while ... 1997, 19.3). The nonlinear diffusivity was estimated at the middle of the time step byfirst taking a
  8. 18 May 2017: This makes v2 negative.If ψ2 is positive, then the interface is concave in the middle and v2 is therefore positive. ... 3s2 7s) m[(1/4)(3s2 7s), s]. mψ [(1/4)(3s2 7s), s]. (5.25). To test the accuracy of the solution for ψ given by (5.25), it is
  9. jc001173 1..12

    www.itg.cam.ac.uk/people/grae/57.pdf
    26 Apr 2006: 4. Model Results. 4.1. Model Results for a Laboratory Experiment. [23] To test the model for the idealized diffusive case,governed by equations (1)–(5), we simulated the experi-ment ... All the other parameters werekept at the value indicated by the
  10. Multiple coexisting states of liquid rope coiling

    www.itg.cam.ac.uk/people/heh/Paper194.pdf
    17 May 2006: 1. 3. Inertio-gravitational regimeThe shapes of the curves shown in figure 5 differ significantly in the middle. ... To test whether these eigenfrequencies correspond to the multiple frequencies seen inthe full numerical solutions, we rescale the
  11. 14 Sep 2009: and (iii) the ability to test different, nonlinear constitutive laws for per-meability. ... There are important components of our simulations that are not validated by these two tests, including our treatment ofthe advection of solute and our success in
  12. The Fluid Mechanics of Carbon Dioxide Sequestration

    www.itg.cam.ac.uk/people/heh/Paper246.pdf
    24 Apr 2014: Small pilot studies and large-scale industrial trials, in which CO2 is injected into a variety ofgeological settings, are already underway and provide much of the motivation, and a critical ... Importantly, the case oftwo-sided convection can be studied
  13. Nonlinear double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper25.pdf
    30 May 2006: This motion is reflected in the corresponding density field, where heavy fluid descends just to the left of the middle of the cell and light fluid rises just to the right.
  14. flm903.dvi

    www.itg.cam.ac.uk/people/heh/Paper180.pdf
    10 Jun 2004: In the first experiment, three concentric zones were established, consistingof an inner cylinder of non-dyed particles, a middle ring of dyed particles and anouter ring of non-dyed particles. ... A test of anytheoretical model to describe column collapse
  15. 10 Mar 2009: we must assume that the neutralbuoyancy level is at the middle of the container. ... These included changes of grid and time step, reduction of (to test thepossible non-Boussinesq effects), and the reproduction of numerical results for S = 0reported in
  16. J. Fluid Mech. (1998), vol. 359, pp. 109–142. Printed ...

    www.itg.cam.ac.uk/people/heh/Paper141.pdf
    9 Mar 2004: After this time the Reynolds number of the current was also too small for theabove theory to be appropriate.) It was thus impossible for us to test robustly bothof the terms
  17. On heating a stable salinity gradient from below

    www.itg.cam.ac.uk/people/heh/Paper31.pdf
    30 Jun 2010: I n 5 4 we describe the experiments performed to test the theoretical model and in $ 5 we present the experimental investigation of the various assumptions incorporated into the theo-
  18. doi:

    www.itg.cam.ac.uk/people/heh/Paper242.pdf
    11 Apr 2013: J. Fluid Mech. (2013), vol. 720, pp. 517–544. c Cambridge University Press 2013 517doi:10.1017/jfm.2013.49. Bending of elastic fibres in viscous flows: theinfluence of confinement. Jason S. Wexler1,3,†, Philippe H. Trinh2, Helene Berthet3, Nawal
  19. The fluid mechanics of solidification

    www.itg.cam.ac.uk/people/heh/Paper92.pdf
    16 Jan 2007: J. Fluid M e c h. (1990). vol. 212, p p. 209-240. Printed in Great Britain 209. The fluid mechanics of solidification. By H E R B E R T E. H U P P E R T Institute of Theoretical Geophysics and Department of Applied Mathematics and Theoretical.
  20. PII: 0377-0273(93)90087-8

    www.itg.cam.ac.uk/people/heh/Paper110.pdf
    27 Apr 2006: 0.1 wt.%, were carried o u t in o r d e r to test the effect o f the intensity o f c o n v e c t ... The middle layer was composed of a suspension of 1000-grade, whilst the upper- most layer was clear.
  21. PII: 0198-0149(81)90135-7

    www.itg.cam.ac.uk/people/heh/Paper41.pdf
    26 Sep 2011: Deep-Sea Research, Vol. 28A, No. 5, pp. 409 to 440, 1981. 0198-0149/81/050409-32 $02,00/0 Printed in Great Britain. Pergamon Press Ltd. An abyssal topographic experiment. W. JOHN G O U L D t , ROSS HENDRY a n d HERBERT E. HUPPERT. (Received 3 April

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