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  1. Results that match 1 of 2 words

  2. doi:10.1098/rsta.2006.1803

    www.itg.cam.ac.uk/people/heh/Paper196.pdf
    11 Oct 2006: Economic, political, cultural, sociological andpsychological factors are of huge importance, as is the role of governments,international agencies and NGOs in responding to crises. ... Hurricane Katrinashowed that extreme events can have global economic
  3. doi:10.1016/j.jcp.2005.12.002

    www.itg.cam.ac.uk/people/grae/74.pdf
    12 Jun 2006: 4. Diffusive solidification. Our first validation test focuses on thermodynamic processes of phase change. ... 6. Corner flow tests. In order to test our code for simultaneous flow through porous and fluid domains as well as for convectivesolidification
  4. 85230

    www.itg.cam.ac.uk/people/heh/Paper146.pdf
    27 Apr 2006: L. J., et al., eds., Geology of continentalslopes: Society of Economic Paleontologists and Mineralogists Special Publi-cation 27, p. ... V., and Southard, J. B., 1984, Mechanics of sediment movement:. Society of Economic Paleontologists and Mineralogists
  5. 1 Jun 2006: I n chapter six, the workbook methods are applied to several field tests and actual industrial accidents as examples of how to use the workbook in practice. ... The authors are careful t o point out deficiencies in current theories of interfacial
  6. 26 Apr 2006: Detailed experimental tests of this geometry haveyet to be conducted; however, the qualitative features of theconstant temperature gradient case are consistent with theexperimental findings of Wilen and Dash.10 Since the ... We then performed an
  7. 27 Apr 2006: different interactioin that region will severely test experimental resolutioThe scaling clearly exhibits that varying the temperatgradient may allow these subtle features to be extracte.
  8. VOLUME 87, NUMBER 8 P H Y S I ...

    www.itg.cam.ac.uk/people/grae/49.pdf
    26 Apr 2006: A static force experiment using a probe with awell-characterized geometry would be more amenable toa quantitative test of this theory.
  9. M411_31c 568..571

    www.itg.cam.ac.uk/people/grae/47.pdf
    27 Apr 2006: Themodel presented here should be regarded as a test of the potentialfor diffusion in the unfrozen liquid to disrupt palaeoclimaticrecords and a challenge to motivate further high-resolution exami-nations of ... peaks is needed to test theories for the
  10. PII: 0022-0248(91)90092-J

    www.itg.cam.ac.uk/people/heh/Paper103.pdf
    27 Apr 2006: First, we wished to apply an concentration,the z. 1 werechosentobe(10, 20, 30)additional test to the theory by measuring the mm, but otherwisethey wereset at (5, 15, 25)
  11. 30 May 2006: Its purpose is to provide a detailed phenomenological description of events, to present reasonably detailed physical models for this description and test these with detailed measurements of flow data in the
  12. Axisymmetric gravity currents in a porous medium

    www.itg.cam.ac.uk/people/heh/Paper189.pdf
    5 May 2006: current and test the results againstlaboratory experiments. ... 3. Experimental observationsTo test the theoretical model we conducted a series of laboratory experiments in.
  13. 30 May 2006: We obtain approximate solutions for obstacles of more general shape in part 4 (Miles & Huppert 1969) and test these approximate solutions by comparing those for a semi-elliptical obstacle with the
  14. 26 Apr 2006: 4. Such measurements could beused experimentally to determine permeabilitysas well as toprovide an experimental test of the equivalence of Fick’s andDarcy’s lawsd. ... adirect experimental test of the equivalence of Fick’s and Dar-cy’s laws.
  15. doi:10.1016/j.jcp.2004.11.039

    www.itg.cam.ac.uk/people/grae/62.pdf
    26 Apr 2006: ary to compensate for this. In the present tests no such correction is made. ... dendritic ice crystals and solution (see for example [15]). The same problem was used as a test case by Uda-.
  16. doi:10.1016/j.jcp.2004.11.039

    www.itg.cam.ac.uk/people/heh/Paper187.pdf
    5 May 2006: ary to compensate for this. In the present tests no such correction is made. ... dendritic ice crystals and solution (see for example [15]). The same problem was used as a test case by Uda-.
  17. Ice blocks melting into a salinity gradient

    www.itg.cam.ac.uk/people/heh/Paper35.pdf
    30 May 2006: The pur- pose of t h e dye was t o allow us t o ascertain the transport and final position of the ambient water, and in particular t o test ... To test such a suggestion we carried out some experiments'in which water, stratified with salt in the usual
  18. Gravity currents: a personal perspective

    www.itg.cam.ac.uk/people/heh/Paper193.pdf
    5 May 2006: There is very good agreeent between the nume-rical solutions and experimental determinations carried out specially to test them. ... Because of these different conceptual models,it is difficult to carry out systematic experiments which either test or
  19. 1 Jun 2006: The experimental data are used t o test the accuracy of a mathematical model, which we formulate in $ 3 and discuss in $4. ... E. Huppert. To test the model we performed a number of experiments with a particular solution of water and isopropanol, which
  20. PII: 0022-0248(95)00970-1

    www.itg.cam.ac.uk/people/grae/29.pdf
    26 Apr 2006: Our experimental results provide a simple test of tri-junction conditions which can be used in theoretical analyses of more complicated systems. ... p l e t p r o v i d e s a s i m p l e test o f t r i - j u n c t i
  21. 30 May 2006: In 95 we test our theory by performing low-Rayleigh-number numerical simulations of the laboratory experiments described by Leitch (1985, 1987) and by Huppert et al. ... In the following section we test our scaling analysis by simulating experiments
  22. 2000JC000559

    www.itg.cam.ac.uk/people/grae/55.pdf
    26 Apr 2006: Further laboratory experiments and field observations willallow detailed tests of our predictions.
  23. Gravity-driven flows in porous layers

    www.itg.cam.ac.uk/people/heh/Paper125.pdf
    30 May 2006: 3.12). where 5 = x/(VRt)l/' and l,, = 91/3. In order to test the theory, a finite volume of glycerine was released into an (air-filled) Hele-Shaw cell,
  24. The slumping of gravity currents

    www.itg.cam.ac.uk/people/heh/Paper32.pdf
    30 May 2006: Keulegan's results are shown t o agree well with our spreading relationships, as do results from additional experiments carried out by us t o test the ideas further.
  25. 28 Apr 2006: Toprovide reliable tests for such a model, accurate andextensive measurements of salinity in growing sea ice arerequired. ... derived from the directly measured par-ameters (impedance and temperature), and to test theunderlying assumptions against
  26. PII: S0022-0248(01)00595-4

    www.itg.cam.ac.uk/people/grae/45.pdf
    26 Apr 2006: Typically, D waschosen to be of order 106f0; tests wereperformed to ensure that the predictions wereinsensitive to further reduction in D.
  27. flm483.dvi

    www.itg.cam.ac.uk/people/heh/Paper186.pdf
    5 Jan 2006: 2.3. Results. 2.3.1. Ballotini in water. In order to test the thermal behaviour of the experimental tank and heating system,a preliminary experiment (1) was conducted using a ... bars with Perspex equivalents, but this emphasizes the care necessary in
  28. Some remarks on the initiation of inertial Taylor columns

    www.itg.cam.ac.uk/people/heh/Paper19.pdf
    30 May 2006: This line of argument seems highly questionable because, using the homogeneous flow over a flat-topped cylinder as a special test case, we indi- cated in the previous section that in
  29. 26 Apr 2006: A test of the ice thickness algorithm using labora-tory experiments in which the growth rate is measured inde-pendently. ... To test when natural sea ice suffers thisinstability, we also plotted the buoy-derived values of f# andhDS on Figure 7a.
  30. 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
  31. PII: 0022-0248(91)90092-J

    www.itg.cam.ac.uk/people/grae/15.pdf
    27 Apr 2006: First, we wished to apply an concentration,the z. 1 werechosentobe(10, 20, 30)additional test to the theory by measuring the mm, but otherwisethey wereset at (5, 15, 25)
  32. Multiple coexisting states of liquid rope coiling

    www.itg.cam.ac.uk/people/heh/Paper194.pdf
    17 May 2006: To test whether these eigenfrequencies correspond to the multiple frequencies seen inthe full numerical solutions, we rescale the numerically predicted curves of frequencyvs.
  33. Axisymmetric particle-driven gravity currents

    www.itg.cam.ac.uk/people/heh/Paper127.pdf
    30 May 2006: To test the model several laboratory experiments were performed to determine both the radius of an axisymmetric particle-driven gravity current as a function of time and its deposition pattern for ... To test this hypothesis we conducted experiments in
  34. 30 May 2006: t In order to test whether this discrepancy was d u e t o premature sedimentation in the lower layer during the filling procedure, a few experiments were conducted in which
  35. 5 May 2006: It should be emphasized that the design of the flow delivery system evolved to theconfiguration described above as a result of extensive tests which revealed that any lesseffort applied to the ... However the concentration of particles progres-sively
  36. 5 May 2006: For the sake of these tests, the aspect ratio of the box was set to 1, thelower and upper boundaries were made to have constant temperatures of 0 and 1,respectively, ... These forms for 〈φ〉 were compared with the results of thenumerical calculations
  37. 1 Jun 2006: J. Fluid Mech. (1996), vol. 307, p p. 245-267 Copyright 0 1996 Cambridge University Press. 245. A new oscillatory instability in a mushy layer during the solidification of binary alloys. By D. M. A N D E R S O N? A N D M. G R A E W O R S T E R
  38. 30 May 2006: The limiting case of a full circular obstacle provides a fairly extreme test for the bounds of (4.13).
  39. Nonlinear double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper25.pdf
    30 May 2006: J. F u i d Xech. (19761, VOZ. 78, part 4? pp. 821-854 Printed in Great Britain. 82 1. Nonlinear double-diffusive convection By H E R B E R T E. H U P P E R T A N D D A N I E L R. MOORE. Department of Applied Mathematics and Theoretical Physics,
  40. Double-diffusive convection

    www.itg.cam.ac.uk/people/heh/Paper42.pdf
    30 May 2006: J. Fluid Me&. (1981), vol. 106, p p. 299-329. Printed in Great Britain 399. Double-diffusive convection. By H E R B E R T E. H U P P E R T Department of Applied Mathematics and Theoretical Physics,. Silver Street, Cambridge CB3 9EW. A N D J. S T E W
  41. Particle-driven gravity currents

    www.itg.cam.ac.uk/people/heh/Paper115.pdf
    30 May 2006: To test the theory, several experiments were performed to measure the length of particle-driven gravity currents as a function of time and their deposition patterns for a variety of particle
  42. 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
  43. PII: 0022-0248(94)00965-1

    www.itg.cam.ac.uk/people/heh/Paper126.pdf
    27 Apr 2006: n c o n d u c t e d at small e n o u g h u n d erco o l i n g s to test the
  44. PII: 0377-0273(82)90062-2

    www.itg.cam.ac.uk/people/heh/Paper48.pdf
    27 Apr 2006: t y t o test m o d e l s for t h e e x t r u s i o n m e c h a n i

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