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23 May 2018: Iserles (ed.), Acta Numerica 20, Cambridge Univ. Press (2011). A. Iserles (ed.), Acta Numerica 19, Cambridge Univ.

6 Dec 2018: 2017-present (Assistant professor since 2013). Professor of Mathematics (20% position)University of Oslo, Norway2014-present.

30 May 2018: 20] Holographic Q-Lattices. JHEP 1404 (2014) 040 arXiv:1311.3292 [hep-th]. Aristos Donos and Jerome Gauntlett.

13 Nov 2018: Q =. . q00,00 q00,10 q00,01 q00,20 q00,11 q00,02q10,10 q10,01 q10,20 q10,11 q10,02. ... q01,01 q01,20 q01,11 q01,02q20,20 q20,11 q20,02. q11,11 q11,02q02,02. . (2). 2.

24 Jul 2018: Compressive Imaging (CI), U = ΨHadΦdwt 256256 @ 12.5%. MRI, U = ΨdftΦdwt 10241024 @ 20%. ... S1: Best for 256x256. S2: Best for 2048x2048. 6.73%7.30%. 21.3%20.5%. Recovery error.

7 Oct 2018: cresc. 1. 15. 20. 25. 30. ❲ ❲ ❲❲ ❲❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲. ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲. ❲❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲ ❲. ❲ ❲ ❲ ❲ ❲

28 Sep 2018: 2nd order BC for ω0 with Re = 10 and N = 10, 14 and 20. ... 1. u. x. N=10. 14. 20. 28. 40. Agree to visual accuracy.

31 Jan 2018: 0.6. 0.8. 1. 1.2. 0 10 20 30 40 50 60 70 80. ... psi. iteration. 1.01.7. 1.751.8. For N = 20 Gauss-Seidel needs 500 iterations,whereas SOR with optimal r 1.75 needs 20.

13 Apr 2018: As a sanity check forcotton, μ 0.3–0.4 [4,5], and thus, hΘi 20. ... 20] M. Abramowitz and I. A. Stegun, Handbook of MathematicalFunctions (Dover, New York, 1965).

13 Dec 2018: For example, without further approximation,evaluation for a scatterer of around 220 by 20 wavelengthscan be carried out in around 100 minutes using 32processors on the SunFire machine. ... 0.05 0.05 0.2 0.6 1.0 1.4 1.8. Fig. 1 Surface current amplitudes

31 Jan 2018: with N = 10, 14, 20, 40 and 56. 2e-05. 4e-05. ... Error decreasing as 0.27x4,i.e N = 20 gives 2 106 cf 2 103 for 2nd order.

11 Oct 2018: Error is satisfying u = 0 (N = 20) as function of t. ... u. x. N=302014. s-w, 28. Re = 10 and N = 14, 20 and 30.Also result from ψ ω formulation at N = 28.

16 Nov 2018: Zworski[20, 21]. Introduction Schrödinger and PDEs Discrete operators Numerical Examples Conclusion Definitions.

13 Dec 2018: 1997 Acoustical Society of America.@S0001-496697!03703-X#. PACS numbers: 43.20.Fn, 43.20.Mv, 43.30.Hw@ANN#. nsemismiceThthaceinionti-. ... An5an ,bn!, Cn5cn ,dn!, 20! wherean , bn , cn , dn are given by11!

19 Jan 2018: 2.2 Free field theory 14. 2.3 Perturbation theory 17. 2.3.1 Feynman diagrams 20. ... D eS[]/. (1.20). evaluates the map acting on |'0i 2 H and ending on |'1i 2 H.

20 Jul 2018: this issue was aired more than 20 years ago by. Adrian Parsegian and Robert Austin (Parse-.

8 Jan 2018: diameters) long with t = 0, 0.25, 0.5, 1, 2.5, 5, 10, 20 and Topt = 29.35 D/U (going downwards: flowis from left to right) where U is ... Red dots indicate thetimes (t = 0, 20, 60 and 100) where cross-sections of the total flow (left: 8 contours across [1

2 Nov 2018: 3.20). On the other hand, if m and n go to infinity in case (6), we consider the expression. ... 20. Figure 3.3: log10 |dm,n| (the blue dotted line) and its asymptotic approximation (thered line), for n = 0 (the top left), m = 0 (the top right), m = n

3 Apr 2018: O(h4)︷ ︸︸ ︷iΛ [ψ]1,1(h) 2i. 〈2xµ2,1(h). 〉2, (2.20). whereψ(h,ζ,ξ) = ζ ξ h3. ... Magnus–Lanczos. In Figure 4.3 (right) and Figure 4.4 (right) we show the errorsin exponentiating the order six Magnus expansions (with and without

24 Jul 2018: Compressive Imaging (CI), U = ΨHadΦdwt 256256 @ 12.5%. MRI, U = ΨdftΦdwt 10241024 @ 20%. ... S1: Best for 256x256. S2: Best for 2048x2048. 6.73%7.30%. 21.3%20.5%. Recovery error.

14 May 2018: 2Fµ dx. µ dx(7.20). where Fµ are the curvature components. Recall that AU is a matrix–valued 1-form, so.

31 Dec 2018: G = F pV = E pV TS (4.20). This is a Legendre transform of F , this time swapping volume for pressure: G = G(T, p). ... already seen in Section 1.4.1. From its definition (4.20), we see that the Gibbs free. –

8 Aug 2018: Received 1 September 1995; accepted 20 December 1995! Molecules at the air–water interface often form inhomogeneous layers in which domains ofdifferent densities are separated by sharp interfaces. ... Hr! 5p. 2r2lnr! 20! and. Gij r! 5 2 d i j lnr!

3 Apr 2018: N =1. 2π. Σ. f. (2.20). This is an integer equal to the first Chern number of the vortex linebundle L Σ, and we shall assume that this integer is ... N,. where N is the vortex number defined by (2.20). If the vortex equations(2.16) and (2.17) are

8 Aug 2018: LILO within the domain is uniform (20), butaccount for the energy associated with the. ... When NBo. 40. 30. 5=.520 So 20. 10e 10. 100 101 102 103 104dH/dt (gaussas).

13 Dec 2018: heightλ/20. most surface geometries, and can easily be reduced further with higher order. ... 20. 1 Introduction. 2 Formulation of equations. 2.1 Formal solution and splitting series.

13 Dec 2018: 3. The query condition is set as querying“Peak wave number” with the condition “< 20.0” througha Web form shown in Fig.

19 Oct 2018: I only 3 modes per wave for 1% accuracy. cf FD 40 pts at O(x2), 20 pts at O(x4).

13 Dec 2018: Retaining just the first term in the iterative series (11),. ψ = L1ψinc, (20). ... height λ/20. Figure 7: Real part of surface field on waveguide at two frequencies.

10 Mar 2018: In the recent work,20 some connections between the Painlevé property and Lie point sym-metries have been uncovered. ... Nonlinear Math. Phys. 20, 110 (2013).19 Koenigs, M. G., Sur les Géodesiques a Intégrales Quadratiques.

11 Nov 2018: Zworski [20, 21]. Introduction Schrödinger and PDEs Discrete operators Numerical Example Conclusion Definitions.

19 Oct 2018: Bl =3κ1R2sy2(l1)Ds. (σl1. 2l3. σl1. 2l1. ). (2.33). Since the first-order product problem (2.20) is the same as the first-order substrateproblem (2.19), except for a ... γ =. k=1. k(. (2k 1)!(2k 1)(2k 2)! )20.0336. (2.54). Our result for UJanus

17 Apr 2018: measuredµ(ξ) = |ξ|2ηeξ. 2. dξ, ξ R. 20. They obey the three-term recurrence relation.

16 Jun 2018: Received 21 November 2016; revised 19 January 2017; accepted 20 January 2017).

31 Dec 2018: Zvib =1. 2. Zddpe. Hvib =kBT! (2.20). The average vibrational energy of each molecule is now.

13 Dec 2018: ψ̃ = (C′0 C′1)(C0 C1)1ψinc, (20). and then solving as before and comparing terms with (19).

13 Dec 2018: Similarly, if we observed that the HPA fails 20% of the time when the cathode current is trending, we would set.

12 Feb 2018: CS1. Dx eS/ , (3.20). 29In flat space, the heat kernel (3.9) obeys KT (y, y) = KT (0, 0) so is independent of y.

19 Sep 2018: 5. Functionals and the Euler-Lagrange equation 20. 5.1 Geodesics of the Euclidean plane 22. ... 20 –. for the integral (a real number) does depend on the function y.

26 Jan 2018: T=. (S. E. )V,N. (1.20). where the subscript denotes that V,N are held fixed when we take the partial derivative. ... pi = 1 (1.67). Part 2 Statistical Physics January 26, 2018 20 H.S.

23 Jan 2018: In fact, the result. K0(q,q′;t) := ⟨q|exp(i p̂. 2. 2mt)|q′⟩ (1.20). ... 2.21). 19Green, George (1793-1841)20Fourier, Joseph (1768-1830). 20. So the equation that you then get is.

13 Dec 2018: H2(x,z;x',z')dx' r. --actF(x,x,)B 3/2 exp{ikh '(x•) [z- h(x,) ]}. (20). where C and Sare again the cosine and sine Fresnel integrals, ... 0.02•. 0.015. 0.0•5. 0.0•0. (al a. 0.25. 8.20. 0.15. 0.0•. I.

14 May 2018: car (x). Z. Mdar b(x, y). b(y) ddy. (6.20). for some coecients {car (x), dar b(x, y)} with60 d = e(0) P.

14 May 2018: a. (f a(x)) (8.20). 77Again, it’s a good idea to check you’re comfortable with this assertion by writing x0.

13 Dec 2018: d f•: k2h2(x,)cos2 0 I2(x) - e&Sx '. 2a•x_x,•x', (20) and. ... k3 O)dkxS] --k2h(x)cos 20--i-•- h2(x)cos 3. (23) We must now find the mean of. •.

13 Dec 2018: 21). Now from eq. (20). E(X,x) =〈h(X). α2π. d. dx. ... Soc. Lond. A 446 (1994) 1-20. (12) C. Qi, Z. Zhao, W.

26 Apr 2018: Thisis. asupe. rvisor’s. copy. oftheno. tes. Pleasedo. notdistribu. teto. stud. ents. Mathematical Tripos: IA/IB Computational Projects. Contents. 0 Introduction 1. 0.1 Overview. 1. 0.2 Aims. 1. 0.2.1 Understanding algorithms. 2. 0.2.2 Being able

30 May 2018: spectrum. Example 1. 0 10 20 30 40 50 60 70 8010 -15. ... 10 -10. 10 -5. 0 10 20 30 40 50 60 70 80n.

3 Aug 2018: Thus, Ṡ quanti-fies the lack of detailed balance in the nonequilibrium steadystate, which, as reported elsewhere [20], depends on envi-ronmental conditions, emphasizing the need to account ... 19] J. Schnakenberg, Rev. Mod. Phys. 48, 571 (1976).[20] K.

13 Dec 2018: Fig. 1 showsthis comparison for the rectangular beach profile above. The beach is straightapart from a ‘top-hat’ protrusion of 20 m seawards, over a length of 1000 m.