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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.

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.

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).

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

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: head. This Froude number should be 24 according to Benjamin, but Hoult suggests expressing it as a constant A, to be determined from experiment.

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.

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.