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24 Apr 2014: 24/. 14. F. or p. erso. nal u. se o. nly. ... n 04. /24/. 14. F. or p. erso. nal u. se o.

30 May 2006: 24-2. 372 H. E. Huppert and 144. E. Stern. $1. , //,/,////,//////////////,,,/,////// / ///,/I/ // / / / , // , / , / // , / / / / // / /, /' I -. FIGURE 1. An elevation of the channel, bounded by vertical walls at. ... Moh(x/L) e--ikg. (3.24). While in

26 Apr 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.

27 Apr 2006: 2.18), which can be (2.23) and (2.24) more closely.used in (2.22) to show that Segregation is more sensitive to the value of. ... 4.24)mass reduce to and we use this condition together with (4.21)—.

18 Jan 2011: φ̃0(0; λ̄) =. h(0, y)2 dy. (3.24). The solid curve in figure 5 shows the result of substituting the value of φ̃0(0; λ̄)found in this way

26 Apr 2006: 1.0 [24]. The slope of the linethrough data set (h), for silicon carbide particles in a succino-nitrile melt, is! ... Azouni, W. Kalita, M. Yemmou, J. Crystal Growth. 99 (1990) 201.[24] S.

1 Jun 2006: 1 -. f = 16-21 min. 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 T. ... 0 - 1 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 29.5 30.0 30.5.

12 Jun 2006: g. [23,24]). The major difficulties then consist in the formulation of accurate internalboundary conditions and in following the evolution of the interfaces through time. ... 104 This study 19.6 16.2 3.53 0.585 2.24[2] 19.51 16.2 3.53 0.586 2.243[3]

16 Jul 2010: Geophys. Res., 79, 1792-1797, 1974. Gebhart, B., and J. C. Molendorf, A new density relationship for pure and saline water, Deep Sea Res., 24(9), 831-848, 1977. ... Glaciol., 24, 259-271, 1979. Tressler, W. L., and A.M. Ommundsen, Seasonal oceanographic

9 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.

30 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).

5 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.

26 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 =

28 Apr 2006: InArctic sea ice. Conference held at Easton, Maryland, February 24–27, 1958.

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,

6 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).

9 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

27 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.

30 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.

9 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.

23 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.

9 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.

30 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.

16 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

17 Oct 2006: Exchange flows during the ventilation of buildings. 24 October. Richard Katz.

9 Mar 2004: 15 P 24.2 P25.2 L25.2 P25.2 P30.2 L. T (C) T (C).

18 Feb 2005: 24 February. Chris Chapman. (Schlumberger). Marine seismics with a rough sea: modelling the surface reflection.

19 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.

5 Mar 2008: Received 30 October 2007; accepted 24 January 2008; published online 29 February 2008.

6 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

30 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.

5 May 2006: 24 48.2 20.9 26 120 0.83 2.6 1760 2.7 1.38 48.2 20.5 20.3 20 1.18 1.5 2250 2.1 ... 34. 32. 30. 28. 26. 24. 22. 20. 18. 16. 14.

19 Jul 2010: η1. )w2(0),. (24). (. 1. k2D3 D. )w1(0) η2. η1. (1.

13 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.

12 Apr 2013: Parameter Value. Inflow channel width (m) 49Inflow channel depth (m) 1.7Inflow velocity (m s21) 0.48Inflow reduced gravity (m s22) 0.021Inflow temperature (uC) 13.0Lake surface temperature (uC)

5 May 2006: www.damtp.cam.ac.uk/lab/digiflow/ 2005.23 G. S. Campbell, Annu. Rev. Fluid Mech. 22, 57 1990.24 T.

9 Apr 2013: These colloidal concentration gradients, which areneglected in rigid-ice formulations, can trigger a thermody-namic instability that leads to morphological transitions in thepattern of segregated ice.23,24 Recently, these thermodynamicprinciples

1 Jun 2006: E. Huppert. Parameter Value Units. a (5.0+ 0.24( T- 20)) x U 0.015 cm2 s-' CC 4.14 J O C - '. 2.66 J cm-3 O C - '

9 Mar 2004: 15 P 24.2 P25.2 L25.2 P25.2 P30.2 L. T (C) T (C).

9 Feb 2004: The volume fration of particles in suspension evolves as23,24. df. dt5. ... X5 x/l , 24! T5 t/ v sl /q!1/ a 2 1!, 25!

14 Sep 2009: is in the direction of rT).[24] Typical advection velocities estimated from a tem-. ... Assur, A. (1958), Composition of sea ice and its tensile strength, in ArcticSea Ice; Conference Held at Easton, Maryland, February 24–27, 1958,pp.

27 Apr 2006: Subsequently (ap- proximately 40-50 rain from the beginning),. 24 r. KOYa_GUCHI L, kt. ... grade particles with A T = 2 4 C and Co= 1.24 wt.%.

12 Mar 2004: requires. P q02pd. : 24. Equation (24) thus links the dendrite tip radius to. ... This solution has a scaled tip radius P = 10.8. and a scaled tip position Z 2:24.

10 Jun 2004: a. r – riri. sandsaltricecouscoussugar slope 1.24. Figure 9. The non-dimensional radial excursion, (r ri )/ri , as a function of the aspect ratioa with a < 1.7 for sand, salt, ... A straight line through the origin atslope 1.24 has a regression

21 Mar 2016: Assessment of ice flow dynamics in the zone close to the calvingfront of Antarctic ice shelves. Martin G. WEARING,1;2 Richard C.A. HINDMARSH,1 M. Grae WORSTER2. 1British Antarctic Survey, Natural Environment Research Council, Cambridge,

9 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.

9 Mar 2004: Indeed, for most of the experimentsdiscussed by TML λ was in the range 0.02–0.24. ... tr dr rN. drNdthN. (2.24). We eliminate h/t with the aid of (2.12) and, after some rearrangement, we againobtain the result (2.22).

26 Apr 2006: salinity of the ice) is very small; k #1 0 24 [Gross et al., 1987].

25 Jan 2007: E. Huppert. Parameter Value Units. a (5.0+ 0.24( T- 20)) x U 0.015 cm2 s-' CC 4.14 J O C - '. 2.66 J cm-3 O C - '

21 Oct 2011: The camera was operated at 1000 frames s1. and a resolution of 640 512 pixels (24 bits). ... 18.8 cm. 24.7 cm. 31.1 cm. 37.6 cm. 43.3 cm. 49.7 cm.