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26 Apr 2006: 24),so f! 0 as x! 1. The interface shape is deter-mined from the equation for f in the inner regionalone. ... Wettlaufer, Rep. Prog. Phys. 58. (1995) 115. [24] J.S. Wettlaufer, M.G.

27 Apr 2006: 24. Zielinski, G. A. Use of paleo-records in determining variability within the volcanism-climate system.

30 Oct 2015: C. Christodoulou, “Interfacial mixing in stratified flows,” J. Hydraul. Res. 24, 77–92 (1986).4 B. ... Downloaded. to IP: 131.111.16.57 On: Fri, 30 Oct 2015 10:24:16.

22 Jan 2007: Inserting equations (2.23) and (2.24) into equations (2.12)–(2.16) andlinearizing in the perturbed quantities leads to the following nonlinear ordinarydifferential equation for the disturbance amplitude:.

21 Nov 2014: 19:. 20:. 21:. 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:.

23 Dec 2021: Thus,with 1ρ =ρ because the density of the overlying air can be neglected, β = 24.8 or0.295 cm1 s1 and (βV 1/3)1 was between 0.004 s ... A 24). Dow. nloa. ded. from. htt. ps://. ww. w.c. ambr.

13 Apr 2011: 24. The wave speed c is scaledby. ghstop cos θ and the maximal thickness hf by hstop. ... Jop, Y. Forterre, and O. Pouliquen, Nature (London) 441, 727. (2006).[24] I.

18 May 2017: 1γ). 1H(L). (p11/γD p11/γS. )(2.23). (. γ. 1γ). 1H(L). p11/γD. (2.24).

14 Feb 2013: 22:. 23:. 24:. 25:. 26:. 27:. 28:. 29:. 30:. 31:. 32:.

9 Feb 2004: r = (F/πV )1/2. (2.24)In contrast to the instantaneous, fixed volume release of the last section, there is not a finite radius at whichthe mass of particulate matter ... Applying these concepts to the relationship for the density of deposit for a single