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19 Oct 2013: The many other studies over the last 20 years that have used relatively coarse resolution data from atmospheric models or from analysed datasets to calculate patterns of transport and stirring have

5 Oct 2013: showhow to construct the chart for f = id and refer to [6] [15] [20] for the general case. ... we can make a Hilbert manifold of Hs(M). The brief discussion above can be summarized inthe following theorem [20].

29 May 2013: 20. PRL 110, 228102 (2013) P H Y S I C A L R E V I E W L E T T E R Sweek ending31 MAY 2013. ... Saintillan and M. Shelley, Phys. Fluids 20, 123304. (2008).[22] A. Peshkov, I.

26 Jul 2013: With the information from Eqs. (20), (23), and (25), weget the velocity in the laboratory frame. ... 33). Combining the solutions in Eqs. (20), (23), and (25), we obtain the simplifications(.

19 Oct 2013: 1. Submission 28 June 2012. Advice to a Young Researcher:. with reminiscences of a life in science. J. Michael T. Thompson. Honorary Fellow, Department of Applied Mathematics and Theoretical. Physics, University of Cambridge, Cambridge, CB3 0WA, UK

5 Oct 2013: On the. 128 256 512 1024 2048 40960. 10. 20. 30.

24 Apr 2013: Previously developed continuum theories [2, 17–20, 22–24] ofmicrobial fluids typically distinguish solvent concentration, bacterial density, solvent velocity,bacterial velocity, and various orientational order-parameter fields (polarization,

26 Jul 2013: of the external magnetic field at f 20 Hz (see Video 1, ESI†).These two nanowires propel at essentially the same swimming. ... Fig. 2 Two identical nanomotors swimming under the same magnetic. field at a frequency f 20 Hz.

8 Jun 2013: 5 and Supplementary Fig. 20). The second increase occurs duringa pronounced interhemispheric seesaw event (Fig. ... Legrand, M. Polar ice evidence that atmosphericCO2 20,000 yr BP was 50% of present.

26 Jul 2013: sin2( φ2 )(h sinh h). h sinh h. ], (3.20). 〈ψ2〉x.

19 Oct 2013: f. f. f. 1. =. >=. >=. >=. >. :. :. ;. <. 42. 42. 42. 42. 15. :. :. ;. <? 42. 42. 42. 42. 20. 42. 42. 42. 42. :. :. ;. <? 25. :. :. ;. <? 00000000. WW// W 13 7 W.

3 Feb 2013: somewhere between 8 billion and 20 billion years old.

19 Oct 2013: The boundary-layerequation then reduces to @6 T@r6 6 T 0 ; (5)in which the boundary-layer thickness is given by = 20 2iB20r2cN2L4! ... Astrophys. J.,(submitted)20. Dziembowski, W. A. & Goode, P. R. The toroidal magnetic eld inside the sun.Astrophys.

19 Oct 2013: disc white for thefirst 20 ms then red for the remaining 180 ms. ... Aball travelling 3 cm in 1 ms travels 6 m, nearly 20 feet,in 200 ms.

19 Oct 2013: 20. Masters of writing, like masters of drawing andmasters of musical composition, know to a hairs-breadth not only what is being omitted but also howmuch omission they can get away

19 Oct 2013: 8. Magnetic confinement and the sharp tachopause. MICHAEL E. McINTYRE. Centre for Atmospheric Science at theDepartment of Applied Mathematics and Theoretical Physics,. Centre for Mathematical Sciences, Wilberforce Road, Cambridge CB3 0WA,

26 Jul 2013: 2.20). In (2.18) the parameter ε =ωa2/κ can also be understood as the period-based Pécletnumber. ... C 20 =1ρ. exp(α1,0(1 µ)ρ. 2. ) q=0. K2q Lq(µ). (q.

26 Jul 2013: Wethen identify Eqs. 20 as a pair of Fourier cosine series in W,for each S in 1,1, and, by considering coefficients ofcos m1W and cos m2W in the respective ... Fluids 20, 051704 2008. 30A. M. J. Davis and E. Lauga, “Geometric transition in friction for

4 Nov 2013: a) (b). buoyant fluid ambient fluid. 56 cm. 2, 5, 10or 20 cm. ... 0 5 10 15 20 250. 0.2. 0.4. 0.6. 0.8. 1.

4 Nov 2013: A cutoff of either 20% or 40% of the total concentration was used to determine the position of the front. ... A cutoff of either 20% or 40% was used to determine the front position.

26 Jul 2013: 0. x2n1J2n(bx)1 x2. dx =. π. 2bJ2n1/2(b) (n 0, b > 0), (2.20).

26 Jul 2013: Received 20 March 2007; accepted 16 May 2007; published online 24 August 2007. ... f 20 f 02 f 0 De1 2 t. = f 0 De1u2T 0 0 u2.

26 Jul 2013: typically 20 nm diameter and5 – 10 m in length, have a much simpler internal structurethan their eukaryotic equivalent and are passively driven by arotating motor located in the cell ... 1070-6631/2010/2211/111901/20/$30.00 2010 American Institute of

5 Oct 2013: On the. 128 256 512 1024 2048 40960. 10. 20. 30.

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.

4 Nov 2013: R. Lister. –40 –20 0 20 40. x. 0. 0.2. 0.4. ... Thesink is resolved by a 20 cell pattern arranged to roughly approximate a cylindrical fissurein the cap rock.

12 Aug 2013: In addition, a1(t) = [1/Cin 0]. >,. b1(t) =Ainj2i and b1(t) =. Ainj2i. The source of nonlinearity is the term. 20. tanh (Gnv(t)/Sinj). ... where p0,0 = [p10,0 p. 20,0]>, the leading terms p1,0 and q1,0 based on our.

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: Received 13 July 2012; accepted 20 December 2012; published online 21 March 2013). ... Bickle et al.20 used the single phase axisymmetric modelto estimate the flux into each layer.

26 Jul 2013: Further, a truncation atn5 m5 20 in the infinite setof linear equations49! ... 20. As the general form of the continuity equation shows,. FIG. 5.

19 Oct 2013: Estimates for vertical length scalesof several kilometers based on radiative code calculations are 20–40 days in thelower stratosphere decreasing to 5 days in the upper stratosphere, although it isalmost impossible ... The PV distributionon September 20

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.

4 Nov 2013: 8. 7. 6. Hei. ght (. mm. )5. 4. 3. 20 200 400 600 800 1000 1200. ... 20. 10. Tem. pera. ture. (C. ). 0. –10. –20. –300 200 400 600 800 1000 1200.

2 Oct 2013: SIAM J. Sc. Comp., 20(1):33–61, 1998. 12. [9] I. Daubechies. Ten Lectures on Wavelets, volume 61.

26 Jul 2013: J. Fluid Mech. (2012), vol. 700, pp. 105–147. c Cambridge University Press 2012 105doi:10.1017/jfm.2012.101. Hydrodynamics of self-propulsion near aboundary: predictions and accuracy of. far-field approximationsSaverio E. Spagnolie1,2† and Eric

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.

19 Oct 2013: Pub. lishe. d by. Man. ey P. ublis. hing. (c). IOM. Com. mun. icat. ions. Ltd. Lucidity and scienceIII: Hypercredulity, quantum mechanics,and scientific truth. PROFESSOR MICHAEL E. McINTYRECentre for Atmospheric Science at the Department of Applied

4 Nov 2013: 40. 20. 10. 5104. k. 80. 40. 20. 10. 5103 104 105103 105.

4 Nov 2013: 2534.1. Buoyant Spreading Without Convective254Dissolution255[20] In the absence of convective dissolution, the model256for the spreading of a buoyant current in a confined porous257layer can be written [e.g., Bear, ... 5692011].570[45] For an aquifer of

4 Nov 2013: 20 40 60 80 100 120 140x (cm). 0 160. 15. ... Colour online) Sequence of photographs showing the progression of experimentB at dimensional times (a) t = 20 s, (b) 100 s and (c) 200 s.

28 Nov 2013: 0.1. 0.5. 0. (c). 0.40.30.20.1 0.5 0.40.30.20.1 0.50. FIGURE 2. Contours of the growth rate Re{σ̂} (as marked) ... 0.25. 0.20. 0.15. 0.10. 0.05. 0 0.5 1.0 1.5 2.0. (a) (b) 15.

19 Oct 2013: RV = 2π. 0. (c20 h21I U u20 u20U. )r=b. n̂ b dθ, (4.20). ... We can now use (5.20) to compute the scattering angle at O( 2).

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

5 Oct 2013: 0.5. 1. 1.5. 80 60 40 20 0 20 40 60 801. ... 0.5. 0. 0.5. 1. 1.5. 80 60 40 20 0 20 40 60 801.

5 Oct 2013: 10. 20 40 60 80 1000. 0.5. 1. 1.5. 2. x 104. ... 20 10 0 10. 0.05. 0. 0.05. 10 5 0 5.

19 Oct 2013: J. Fluid Mech. (2005), vol. 534, pp. 67–95. c 2005 Cambridge University Pressdoi:10.1017/S0022112005004374 Printed in the United Kingdom. 67. Wave capture and wave–vortex duality. By OLIVER BÜHLER1 AND MICHAEL E. McINTYRE21Center for

20 Dec 2013: But this is basis-dependent: a. Part 3 General Relativity 4/11/13 20 H.S. ... T : Tp (M). Tp (M) Tp(M). Tp(M) R. (2.20). where there are r factors of Tp (M) and s factors of Tp(M).