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19 Oct 2013: Meiss 1992, Wiggins 1992). Many detailed investiga-tions over the last 20 years or so have shown how the transport andstirring properties of simple flows change with the parameters definingthat flow.

5 Oct 2013: 02 11.99 8.8124 0.25 1.94 3.71 7.20 10.41 11.80 13.64 6.38. ... 0.125 9.18 11.82 11.20 10.88 11.80 11.86.

5 Oct 2013: 10-11. 10-8. 10-5. 0.01. 20 40 60 80 100. 10-14. 10-11. ... 10-8. 10-5. 0.01. 20 40 60 80 100. 10-10. 10-6. 0.01.

5 Jun 2013: 1938 and 1940 [20], [21], [22]. Rossby’s 1938 paper recognized the exact. ... In this. case the maximum wind speed has a rather modest value, just over 20 m s1.

4 Nov 2013: with a0 = b0 = 1. The constants λ1 and λ2 are then found byapplying the boundary conditions (20) on the perturbed mush–liquid interface. ... of an applied flow. Charru et al. [20,21] extended this analysisand found analytic solutions for the

4 Nov 2013: FT = kT. z. z=0. = kTL. Ra1/5θ ′(0). h(x), (2.20). ... 0.5 1.0 1.5 2.0 2.5 3.00. 5. 10. 15. 20. 25.

5 Oct 2013: f fn,m‖R (1 θ2. )‖f Qnf‖R c(2 θ)θ2|||f Qnf|||, (2.20). and thatκ(A). ... 12. The estimate (2.20) for ‖f fn,m‖ holds with the stronger assumption (A2′).

4 Nov 2013: 3 of 21. stacked cubes. For example, frequency analysis of the 2006survey shows that it has a dominant bandwidth of about 20–50 Hz. ... per layer.Calculated thicknesses are sometimes as great as 20 m(Figure 8).

9 Jan 2013: 0. 1. 20 0 12 0. , D2 =. 1. (x)2.

5 Oct 2013: This is the topic of the next section. 6. 10 20 30 40 50. ... 10. 20. 30. 40. 50. 20 40 60 80 100! 10!8!6!4!2.

26 Jul 2013: e′(0)i e(1)i e′(1)i e(0)i , (20). ... We note from the structure of Eqs. (20)–(22) that thet -dependence of the O(εj ) term in r is determined by the previous order in the expansionof ei.

19 Oct 2013: defined as. Q = ρ1 (20 v) ϑ , (8.1)where ρ is mass density and ϑ is potential temperature (materially invariant,. ... near the equator, 20 dominates v in (8.1). So (8.4) is satisfied through† Note also that tachocline thermal diffusion times

19 Oct 2013: 20. ω̂2. )E, (3.15). DtE u′1v′1 Uy = c20. (h′1u. ′1. ... t+. [Ux̂ cg. k. κ. ])E = 0, (3.20). holds approximately with the group velocity [ ] constant along rays.

4 Nov 2013: 6. 7. 20 40 60 80 1000. 0.2. 0.4. 0.6. 0.8. ... 1.0. Ave. rage. sat. urat. ion. B. 20 40 60 80 100.

19 Oct 2013: The mean depth ish0 = 4 km, giving behaviour qualitatively like that implied by Equations (20) and (25) below,with the Rossby length L0 2000 km in middle latitudes, and quantitatively very ... This model behaves in a manner astonishingly like thereal

26 Jul 2013: due tofluid forces alone17–20 although, since individual cilia are notfree-swimming but are attached to a substrate, synchroniza-tion can only occur with a load-dependent force generation. ... 6h̄Dm0 2. h̄Um umh um0. 20. Hence we see that only the

19 Jul 2013: tn1) and that otherwise g is strictly monotone. A. 20. univariate expansion is standard tn1tn.

19 Oct 2013: Proc. NATO Adv. Res. Workshop ARW 920946, Paris, October 1993, “The Solar Engine and its. Influence on the Terrestrial Atmosphere and Climate”, ed. E. Nesme-Ribes, Springer-Verlag 1994. (Vol. 25 of NATO ASI Subseries I, Global Environmental

27 Jun 2013: τ,q)m(q,q)m. (1)mq 12 (m1)mn=m. ζn. (q,q)nm. 20. =. n=0. ζn. (q,q)n. ... F̃(ζ,τ,q) =1. (ζ,q)(τ,q). is a solution of (3.20), as can be verify easly by direct substitution.

5 Oct 2013: Hence, its eigenvalues aregiven by (2.20). For φ =. nj=1 αjφj , we have α. ... 400. 600. 800. 10 20 30 40 50. 0.1. 0.2. 0.3.

21 Mar 2013: important result, proved in [20]:. Proposition 1.4. If a given conformal structure [g] on M contains a metric. ... 20 CHAPTER 1. INTRODUCTION. Maxwell equations which can be seen to describe an arbitrary number of dy-.

26 Jul 2013: ψ. t i. [ω0(x). 12ωkk(x)k. 20 (x). ]ψ ωkk(x)k0(x). ψ. x+ 1.

5 Oct 2013: 10-11. 10-8. 10-5. 0.01. 20 40 60 80 100. 10-14. 10-11. ... 10-8. 10-5. 0.01. 20 40 60 80 100. 10-10. 10-6. 0.01.

19 Oct 2013: Transcript of British Broadcasting Corporation's "Analysis" programme of 4 November 1999: ANALYSIS ROUGH COUNTING PRESENTER: ANDREW DILNOT PRODUCER: INGRID HASSLER EDITOR: MICHAEL BLASTLAND TRANSMISSION: 4 November '99 20.30 and

19 Jan 2013: Mathematical Tripos Part II E.J. Hinch. WAVES Lent 2013. Example Sheet 1: Sound Waves. 1. Plane waves and radiation. A thin piston executes very small oscillations about x = 0 in a. long straight fluid-filled tube with cross-sectional area A and

26 Jul 2013: s L = 1.73, b = 1.31 rad / sL = 2.20, and c = 5.24 rad / s L = 3.11. ... Two datasets are shown: 1 L = 20 cm, D = 0.5 mm, and a0 = 0.435 rad; 2L = 18 cm, D = 0.61 mm, and a0 = 0.814 rad.

26 Jul 2013: Barrat, J-L. Soft Matter 3, 685–693 (2007).20. Rothstein, J. P. ... Phys. Rev. Lett. 96, 186102 (2006).23. Squires, T. M. Phys. Fluids 20, 092105 (2008).24.

26 Jul 2013: 18 and the experiments of Ref. 20 showing enhanced swimmingvelocity in viscoelastic fluids. ... The other two investigations which showed an increase of swimming in complex fluids18, 20.

4 Nov 2013: Corrigendum 443. 0. –20. –40. –40. –80. –120. –60. –80. –100.

26 Jul 2013: For N 5, 19, 20, 23, 26, 28, 29. the circlepacking has continuous degrees of freedom (where at leastone circle is free to ‘‘rattle’’) [9]; for N 15 two differentconfigurations (15a ... 10 19 2 1 18 34 1 1 27 52 1 111 25 6 1 19 34 1 3 28 52 1 312

19 Oct 2013: Having historical, 20:20 hindsight provides a strong, implicit structure. In more forward looking organizations, this structure is provided by strong, visionary leadership. { ... We didn't get Emacs or Perl or the World Wide Web from 20:20 hindsight'' --

26 Jul 2013: S. J. Phys. Rev. Lett. 2003,. 90, 144501.(20) Thompson, P. A.; Troian, S. ... 20, No. 20, 2004 8929. a feature which is predicted by our model (eq 30).

12 Nov 2013: Question: Choose, giving reasons, a values of k which give (a)monotonic and (b) oscillatory convergence.Verify expected behaviour, with nmax = 20. ... 19 4.000002413 2.413255e-06 0.5000116 1.0566212. 20 4.000001206 1.206080e-06 0.4997730 1.0536240. 21

26 Jul 2013: 2x102. 0. 20. 40. 60. 80. 100. 0 5x106 1x107 1.5 10 7 2x107. ... Rev.Lett. 99, 228103 2007. 20 Linear and quadratic terms proportional to ̇i and i ̇i havea zero mean.

8 Oct 2013: 1(b) and 1(d), areas. IP AP. IP. AP. (a). (b). 10 20 3040. ... R. Bennett and R. Golestanian, Phys. Rev. Lett. 110,. 148102 (2013).[20] S.

4 Jun 2013: 0. 0.5. 1. 1.5. 2. 2.5. 3. 0 5 10 15 20. ... 2. 2.5. 3. 3.5. 0 5 10 15 20. V0. t.

26 Jul 2013: 23) intoeqs. (20) and (21) to obtain the integral relationship. F̂ 〈U2〉L̂ 〈2〉=. ... B., Annu. Rev. Fluid Mech., 8 (1976) 13.[20] Bird R. B., Curtiss C.

19 Oct 2013: 1.4] :20. that gravity waves can not propagate with frequencies below the inertial frequency, acts to.

26 Jul 2013: In contrast,marine bacteria display ‘‘run-and-reverse’’ (or ‘‘back-and-forth’’) locomotion where high speed swimming alongstraight paths is followed by almost complete reversal oftheir swimming direction [20,21]. ... For example, the

26 Jul 2013: de Gennes, Langmuir18, 3413 (2002).[20] C.L.M.H. Navier, Mémoires de l’Académie Royale des Sci-. ... Phys. Chem. B 104, 3407 (2000).[44] The general solution to Eq.(20) also has an exponentially.

19 Oct 2013: Then. 20. p(a+, t) = p(a, t) (bubble volume)γ (a3)γ a3γ, where γ is the ratio of specific heats.

26 Jul 2013: Received 20 October 2008; accepted 12 December 2008; published online 27 January 2009. ... to viscous flow, implying,in particular, that the recently discovered nanobubbles19,20.

26 Jul 2013: dθ. dτ. (20). Figure 5. Undeformed (dashed line) and deformed (solid line)geometry of the swimmer. ... Pur. Appl. Math. 5 109–18[20] Leal L G 1992 Laminar Flow and Convective Transport.

26 Jul 2013: Received 10 June 2011; accepted 20 July 2011; published online 19 August 2011). ... nk.20,23 Here, we keep their valuesgeneral in the calculations and show that the final swimming.

26 Jul 2013: u dðrj0; Þ 12jrj2 ð2r̂ r̂ IÞ ; (3). where r̂ r=jrj and I is the identity tensor [20,21]. ... 20] N. Liron and S. Mochon, J. Eng. Math. 10, 287(1976).

26 Jul 2013: 0 0.5 1 1.5 20. 0.2. 0.4. 0.6. 0.8. 1. 1.2. ... 55, 0.6) (1.29, 0.5) (1.20, 0.2) (1.00, 0.15).

26 Jul 2013: PACS: 47.20.)k; 47.20.Ft; 47.62.qKeywords: Hydrodynamic stability; Instability of shear flows; Flow control. ... a Control jjTxwjj2 jjTxwjj10.01 RM96 (proportional) 55.8 653. H2 (‘ 10,000) 21.0 130H2 (‘ 100) 20.3 122H2 (‘ 10) 12.1 44.1H2 (‘ 1)

26 Jul 2013: 440. D.L. egen. dre,. E.L. auga. and. J.M. agnaudet. Kn = 0 Re = 5 20 50 100 200 500 800. ... 204 0.222 0.224. Kn = Re = 5 20 50 100 200 500 800CD This study 3.15 1.33 0.712 0.415 0.228 0.0973 0.0618.

26 Jul 2013: Phys. Fluids 20, 082106 2008. Downloaded 04 Sep 2008 to 128.54.56.91. ... 1.6. nn=5=5. nn=10=10. nn=15=15. nn=20=20. nn=25=25. nn=30=30. 3. –1nn=5=5nn=10=10. nn=15=15.

26 Jul 2013: We then expect pumpingin the stiff regime, Us , to occur at speed Us c(beff k)2 ωf 20 /κ. ... effected by the bending resistanceversus the viscous forces (similar to the so-called “spermnumber” used to model viscous locomotion of