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19 Oct 2013: variable between about 24 and 36 months — owe their existence and timing to the ir-. ... cycle taking, of course, about 24 to 36 months. The time-altitude contour plot of the.

16 Oct 2013: m=1. α(m)(t)δmn. = α(n)(t) , (1.24). reproducing (1.23) apart from renaming the indices. ... 24. Chapter 2. 2. Groups. This chapter contains the second set of syllabus items, together with a fewitems anticipating the third set:.

26 Jul 2013: 0 aRFU 0 , 24. Text = 0 0 00 0 aRFU0 aRFU 0. ... Optimal III 0.24 3.34 12.6 2.6 7.9 0.336. Optimal IV 0.49 3.20 16.9 2.6 5.4 0.465.

4 Nov 2013: 10 7.37 0.01 401 21.8 1.73 11111 6.63 0.01 401 20.7 1.69 10912 20.35 0.03 401 36.2 2.24 144.

27 Aug 2013: pointed) end to its plus (barbed) end.These cables are bound to the cortically fixed chloroplasts atthe cell periphery (24) in a “barber pole” twist, generating flowspeeds of 50–100 ... Characean algae. Proc Natl Acad Sci USA 73(1):165–167.24.

26 Jul 2013: 2, 0.5) (1.1, 0.4)f (2.2, 0.53) (0.91, 0.29)g (2.3, 0.45) (0.69,1.52) (1.24, 0.52) (1.14,

26 Jul 2013: J. Fluid Mech. (2003), vol. 489, pp. 55–77. c 2003 Cambridge University PressDOI: 10.1017/S0022112003004695 Printed in the United Kingdom. 55. Effective slip in pressure-driven Stokes flow. By ERIC LAUGA AND HOWARD A. STONEDivision of Engineering

26 Jul 2013: Other simple propulsivesystems proposed for locomotion at zero Reynolds numberinclude a deformable two-dimensional loop;18 systems oftwo,19–22 three,21,23,24 or N spheres;25 an oscillating body ... R2. z c. R1, 24. where c = a2 b2, r = x2 y2, r̂ =

12 Aug 2013: Cont. Dynamical Sys. 28, 1345–1367. 24. Figure 3.4: The errors for h(t) for ω = 200π (top row) and ω = 2000π(bottom row): from the left 0, 1 and

5 Oct 2013: xm} is a grid of mequispaced points in [1, 1]. In [24] it was shown that. ... Proc. SPIE, 7535, 2010. [24] D. Coppersmith and T. Rivlin. The growth of polynomials bounded at equally spaced points.

19 Oct 2013: Fluid. Dyn. Res., 24, 375–404.Janssen, P. A. E. M. 1982 Quasilinear approximation for the spectrum of wind-generated.

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

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

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

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