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26 Jul 2013: CA 92093-0411, USA2LadHyX, École Polytechnique-CNRS, 91128 Palaiseau Cedex, France. (Received 28 April 2003 and in revised form 24 March 2004). ... By selecting ξinf = 15.7 andξsup = 24 and defining N = 140 gridpoints via this approach, adequate

9 Jan 2013: N 2)(7N 11)ρ (N 1)(7N2 27N 24)ρ2. (N 3)(N 2)(2N 1)ρ3],.

4 Nov 2013: Fluids 24, 117102 (2012) Effect of fluctuations on the onset of density-driven convection in porous media Phys. ... Fluids 24, 114102 (2012) Absence of subcritical instabilities and global nonlinear stability for porous ternary diffusive-convective

4 Nov 2013: FC = 24/3λD. (gβ̃. Dν. )1/3(C0 Ci )4/3, (4.3). where λ is a constant. ... 1 9.3 0.1 9 1 10.47 3.73 0.25 unstable230106D 9 1 3.19 0.02 27 0.3 10.47 3.73 0.24 unstable230106E

4 Nov 2013: Leakage. † Present address: Department of Mechanical Engineering, MIT, Cambridge MA 02139, USA.‡ Present address: OCCAM, Mathematical Institute, 24-29 St Giles’, Oxford OX1 3LB, UK.

8 Jun 2013: simulations. g, North Atlantic sediment core OCE326-GGC5 231Pa/230Th (ref.24). Temperatures are given as deviations from the early Holocene (11.5–6.5 kyr ago) mean. ... Paleoceanography 18, 1087 (2003). 24. McManus, J. F., Francois, R., Gherardi, J.-M.,

4 Nov 2013: 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 Jul 2013: Received 24 May 2002; accepted 17 December 2002; published online 30 June 2003.

26 Jul 2013: to the cre-ation of flagella bundles propelling the cells forward as theyswim, as well as the disruption of such bundles when thecells change their swimming direction.22–24. ... U =h̄. 2f x. s. 24. Noting that d / dt = U we therefore get an equation

26 Jul 2013: 24). If we note 〈.〉 the t -averaging operator between t and t 2π, we therefore obtain〈e(j )i. ... 27). From the definition of F and Eqs. (24)–(27), we can write.