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PII: S0301-9322(98)00062-7
www.itg.cam.ac.uk/people/heh/Paper151.pdf9 Mar 2004: rNt 0 rN0 24. M. Ungarish, H.E. Huppert / International Journal of Multiphase Flow 25 (1999) 715737 725. ... For this case. the box model yields [rN/rN(0)]max=[8Fr/(3 b)]1/4. (This is by about 24% smaller than for. -
J. Fluid Mech. (2015), vol. 777, pp. 97–121. c© ...
www.itg.cam.ac.uk/people/heh/Paper252.pdf30 Oct 2015: leakage rate predicted by (2.24) is then unphysical because there is no fluidabove the outlet to draw. ... Generally, this assumptionis invalid if the current delivers a smaller flux towards the outlet than is predicted toleak according to (2.24). -
doi:10.1016/j.jcp.2004.11.039
www.itg.cam.ac.uk/people/heh/Paper187.pdf5 May 2006: Received 29 March 2004; received in revised form 24 September 2004; accepted 11 November 2004. ... ykumar and Mao [24] again assuming the interface was sharp. The SPH method, as mentioned earlier, does. -
jc001173 1..12
www.itg.cam.ac.uk/people/grae/57.pdf26 Apr 2006: Using equations (3) and (22)–(24), it is possibleto calculate _h, S0 and T0 in terms of far-field properties T1and S1 by eliminating two of the unknowns to obtain aquadratic ... For this simula-tion we used again the values given in Table 1 and Si = -
Nonlinear double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper25.pdf30 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, -
Instruments and Methods A non-destructive method for measuring the ...
www.itg.cam.ac.uk/people/grae/61.pdf28 Apr 2006: InArctic sea ice. Conference held at Easton, Maryland, February 24–27, 1958. -
Dynamics of viscous grounding lines
www.itg.cam.ac.uk/people/heh/Paper220.pdf6 May 2010: H. t+. q. x= 0 (2.24). to form the nonlinear diffusion equation. ... f (ξ ) dξ = 1, (3.24). to the leading-order front solution (3.21). -
jc002818 1..17
www.itg.cam.ac.uk/people/grae/66.pdf27 Apr 2006: Received 24 November 2004; revised 19 May 2005; accepted 11 August 2005; published 2 February 2006. ... The wider range of melt rates were used toexamine model sensitivity to mi.[24] In an extensive study of four sea ice sites in the. -
rsta.royalsocietypublishing.org ResearchCite this article: Worster…
www.itg.cam.ac.uk/people/grae/117.pdf9 Oct 2015: Although sea water with salinity above approximately 24 ppt has a monotonic variation ofdensity with temperature above its freezing temperature, the same physics that gives rise to thedensity maximum of pure -
The slumping of gravity currents
www.itg.cam.ac.uk/people/heh/Paper32.pdf30 May 2006: head. This Froude number should be 24 according to Benjamin, but Hoult suggests expressing it as a constant A, to be determined from experiment. -
J. Fluid Mech. (2018), vol. 844, pp. 435–458. c© ...
www.itg.cam.ac.uk/people/heh/Paper263.pdf23 Dec 2021: 2.24). Using these dimensionless groups, we introduce the viscosity- and toughness-dominated scalings, denoting them with subscripts m and k, respectively. ... balance (2.24) to obtain the radial scaling,. Rk =. (Q2E′2t2. K′2. -
PHYSICS OF FLUIDS VOLUME 13, NUMBER 12 DECEMBER 2001 ...
www.itg.cam.ac.uk/people/heh/Paper167.pdf9 Feb 2004: H 0 1!5 2F P12 f P1 1! 4.24! FIG. 2. ... On applicationthe boundary conditions4.23! and 4.24!, we find that. a 5 4.523 102 3, F P15 2 8.42 for Fr5 11.9. -
J. Fluid Mech. (2002), vol. 458, pp. 283–301. c© ...
www.itg.cam.ac.uk/people/heh/Paper171.pdf9 Mar 2004: These substitutions transform (2.24) into. uN = I(hN) = Fr(hN) h1/2N. ... Appendix. The functions I and χA.1. The function I(hN). From the definitions (2.19), (2.24) and (2.25) we obtain. -
The effect of side walls on homogeneous rotating flow over…
www.itg.cam.ac.uk/people/heh/Paper18.pdf30 May 2006: The situation can be made to appear even more problematic by continuing the analysis further, (2.24)-(2.31), from which i t appears that a full, three-dimensional calculation, incorporating ... 2 [ M o ( [ ) u(l)([)Ir 2 4 v ( ) ” ( [ ) 24. -
PII: 0012-821X(81)90075-3
www.itg.cam.ac.uk/people/heh/Paper43.pdf16 Jan 2007: expressed as wt.%, as a function of the amount of K2CO 3 or NaNO 3 present in solution at 24.2C. ... Lower and upper layer properties were: initial temperatures 46 and 15C; initial concentrations 37 and 24%; initial densities 1.26 and 1.23 g cm 3; and -
J. Fluid Mech. (2001), vol. 432, pp. 201–217. Printed ...
www.itg.cam.ac.uk/people/aa/JFM1.pdf9 Mar 2004: 15 P 24.2 P25.2 L25.2 P25.2 P30.2 L. T (C) T (C). -
Replenishment of Magma Chambers by Light Inputs
www.itg.cam.ac.uk/people/heh/Paper70.pdf19 Jul 2010: Petrol., 24, 133-165, 1983. Eichelberger, J. C., Vesiculation of mafic magma during replenish- ment of silicic magma reservoirs, Nature, 288, 446-450, 1980. -
Ice blocks melting into a salinity gradient
www.itg.cam.ac.uk/people/heh/Paper35.pdf30 May 2006: 0 69.5 24.6 30.4 40.8 47.3 62-5 29.2 37.2 51.9 41.7 23.7 29.7 36.5 42.2. ... 29.6 36.6 25.0 34.8 54.0 24.8 33-8 28.2 35.3 24.3. 1 0 3 dp. -
Flow and instability of thin films on a cylinder and sphere
www.itg.cam.ac.uk/people/heh/Paper219.pdf6 May 2010: where representative valuesof ρ = 1.4 kg m3, g = 9.8 m s2, γ = 78 mN m1 and R = 0.24 m were fixed. ... and R = 0.24 m. Wavelengths were estimated by dividing the circumference of the leading edgeof the flow at the onset of instability by the number of -
Static and flowing regions in granular collapses down…
www.itg.cam.ac.uk/people/heh/Paper208.pdf13 Nov 2007: Method. Glass beads 24 Rotating drume. 0.25–0.35 24 Smooth inclined planef. ... 0.5 0.04 24–31 Rough inclined planeg. 1.26 9–11 Shear gauge, smooth chute flowh.
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