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26 Apr 2006: Further laboratory experiments and field observations willallow detailed tests of our predictions.

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,

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.

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)

26 Apr 2006: Typically, D waschosen to be of order 106f0; tests wereperformed to ensure that the predictions wereinsensitive to further reduction in D.

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

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

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.

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

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

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.

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

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

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

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

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

30 May 2006: The limiting case of a full circular obstacle provides a fairly extreme test for the bounds of (4.13).

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,

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

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