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19 Jul 2013: Dynamical Sys. 28, 1345–1367. 24. Deaño, A. & Huybrechs, D. (2009), ‘Complex Gaussian quadrature of oscillatory in-tegrals’, Numer.

5 Oct 2013: Stable reconstructions in Hilbert spaces and the resolutionof the Gibbs phenomenon. Ben AdcockDepartment of Mathematics. Simon Fraser UniversityBurnaby, BC V5A 1S6. Canada. Anders C. HansenDAMTP, Centre for Mathematical Sciences. University of

19 Oct 2013: 12 2 2 41 F f r 1 O(F lnF). 4(24). ... In particular, atO(1), this means that the coefficients of the lnr term in(18a) and (24) must agree, and hence.

5 Oct 2013: The problem is not new, and therehave been many different approaches developed for its solution (see, for example, [2, 11, 12, 17, 18, 22,23, 24, 25, 52] and references therein).

27 Jun 2013: 2. 24. We now let s in (3.22),. lims. χs+ = lims. ... φm(z) =. mj=0. (1)mj[mj. ]q. q12 (mj)zj, m Z+. (3.24). Setting α = q1/2 presents absolutely no problems in our analysis, since q = |α|2, isconsistent

19 Oct 2013: 23 Nov 2004 1:27 AR AR235-FL37-11.tex AR235-FL37-11.sgm LaTeX2e(2002/01/18) P1: IBD10.1146/annurev.fluid.37.061903.175710. Annu. Rev. Fluid Mech. 2005. 37:263–93doi: 10.1146/annurev.fluid.37.061903.175710. Copyright c 2005 by Annual Reviews. All

5 Oct 2013: Thiswas later considered by Eldar et al, who extended this framework to frames in arbitrary Hilbert spaces[18, 19, 20, 24]. ... M2 =. C(γ)M11. 2. (24). Proof. Without loss of generality, in this proof, M1 and M2 will be even.

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

5 Oct 2013: Indeed, one typically requiresan intolerably large number of samples m to recover f to any reasonably accuracy [13, 24]. ... 24]. Note in the case above that f has only m nonzerocoefficients in the basis {wj}jN.

19 Oct 2013: BALANCE, POTENTIAL-VORTICITY INVERSION, LIGHTHILL. RADIATION, AND THE SLOW QUASIMANIFOLD. M. E. McINTYRE. Centre for Atmospheric Science at theDepartment of Applied Mathematics and Theoretical Physics,Silver Street, Cambridge CB3 9EW,

4 Nov 2013: 2011], but that it can be approxi-306 mated as constant provided that the thickness of the CO2307 layer is small relative to the thickness of the water layer.308 [24]

5 Oct 2013: Stable reconstructions in Hilbert spaces and the resolutionof the Gibbs phenomenon. Ben AdcockDepartment of Mathematics. Simon Fraser UniversityBurnaby, BC V5A 1S6. Canada. Anders C. HansenDAMTP, Centre for Mathematical Sciences. University of

4 Nov 2013: J. Fluid Mech. (2010), vol. 647, pp. 287–308. c Cambridge University Press 2010doi:10.1017/S0022112009993910. 287. On the mechanisms of icicle evolution. JEROME A. NEUFELD†, RAYMOND E. GOLDSTEINAND M. GRAE WORSTER. Institute of Theoretical

19 Oct 2013: GRAVITY WAVE GENERATION BY VORTICAL FLOWS. IN A ROTATING FRAME. Rupert Ford. Churchill College Cambridge. A dissertation sublnitted for the degree of Doctor of Philosophy. at the University of Cambridge. October, 1993. To my grandparents. Margaret

19 Oct 2013: 2 p 1 p. 2 me. p 1. 2.24. The corresponding profiles of absolute vorticity areshown in Figs.

3 Oct 2013: 093 —sea urchin (Lytechinus) 22.6 µm 4.6 µm 0.203 5.86sea urchin (Psammechinus) 24 µm 4.0 µm 0.166 —protist (Trypanosoma cruzi) 3.5 µm 0.5

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.

26 Jul 2013: dt 2. [4. 5 O (3). ], (24). 5. J. Phys.: Condens.

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.

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 =