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1 Dec 2009: 0)p1,1 cos 2ωt (2.20). The equation and initial conditions forp2,0 are obtained when analysing theO(ω2)terms. ... The termψ2(t) can be obtained from (2.20) substituting all the data corresponding to thefunctionsh andf in this example.

13 Jun 2009: 20 40 60 80 100! 10! 5. 5. 10. 20 40 60 80 100! ... 20 40 60 80 100! 5. 5. 10. 20 40 60 80 100!5.

21 Apr 2009: sets. For reasons that we makeclear, modified Fourier approximations are best analysed in so-called Sobolev spaces of dominating mixedsmoothness, [20]. ... f(x,y) = esin 6x(y tan2(1 y2). ). 20. 50 100 150 50 100 150.

31 Jul 2009: 20) where the ro transformation is simply T = T - wt with w = yr/(r2 1).

13 Jul 2009: Cambridge CB3 9EW, UK. Received 14 November 1996; received in revised form 20 February 1997.

26 May 2009: to 20 in the horizontal direction, and up to 40 in the verticaldirection. ... 100(a) (b). 50. 20. 10106 107 108 109 1010. Shear-freeRigid. Ra.

10 Nov 2009: Each velocity fieldcontains 160 50 velocity vectors and the field of view is64 20 mm2. ... plane turbulent stress ũw̃ and its dependence with respectto z̃ are similar to those of w̃2, its magnitude being onlyabout 20% that of ũ2.

21 Jul 2009: 25. 20. 15. g 10-3. 10. 5. a / '150 0 0.02 0.04 0.06 0.08. ... http://journals.cambridge.org Downloaded: 21 Jul 2009 IP address: 131.111.16.227. 30. 20. 15.

3 Sep 2009: 20. Additional vortices can easily be included into Eq. 19 bywriting v = i=1. ... 20 for vortices along = / 2. Different combinations and different circulationsof the single vortex solutions of type I and type II are con-sidered.

10 Jul 2009: d/z 0.20 0.15. license or copyright; see http://pof.aip.org/pof/copyright.jsp. ec. mthcta. mowethindtal-. ... Aver-ages are taken over all the particles including those in the sediment andabout 20 realizations.