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3 Aug 2004: early as 200 msec follow-ing presentation of a retrieval cue.

10 Jun 2004: J. Fluid Mech. (2004), vol. 508, pp. 175–199. c 2004 Cambridge University PressDOI: 10.1017/S0022112004009036 Printed in the United Kingdom. 175. Axisymmetric collapses of granular columns. By GERT LUBE1, HERBERT E. HUPPERT2,R. STEPHEN J. SPARKS1

23 Aug 2004: As t 0 it can be seen that the solution diverges from the line of best fit., t = 103, y = 1/200; , t = 103, y = 1/400; , t = 104, y =

9 Mar 2004: Each new time step rN (t) is updated using(12). Typically, we used 200 y-intervals and a time step of 0.002, but the convergenceand resolution (accurate to at least ... 4.2. H = 1. 0 50 100 150 200. –uN. Figure 14.

9 Mar 2004: J. Fluid Mech. (2003), vol. 489, pp. 269–299. c 2003 Cambridge University PressDOI: 10.1017/S0022112003005172 Printed in the United Kingdom. 269. Solidification and convection of a ternarysolution cooled from the side. By LYNN J. BLOOMFIELD AND

9 Mar 2004: The majority of the calculations have used 200 uniformlyspaced grid points in each mushy layer, although we have checked convergenceusing 400 and 800 points. ... We note that a typical calculation with 200 grid points. 178 D.

9 Mar 2004: J. Fluid Mech. (2002), vol. 472, pp. 333–371. c 2002 Cambridge University PressDOI: 10.1017/S0022112002002379 Printed in the United Kingdom. 333. Polydisperse particle-driven gravity currents. By T H O M A S C. H A R R I S1, A N D R E W J. H O G

9 Mar 2004: The simulations discussed here were obtained for a channel of length xw = 4,the typical grid had 160 horizontal and 200 stretched vertical intervals, and thetypical time step was 2 103.

9 Mar 2004: 100 m abovethe valley floor on the southern margins of the depres-sion, more than 200 m above the eastern slope of GuaneGuane Hill (12 km west of the source area,

9 Feb 2004: particle size, experiments were run with four different initial par-ticle masses of 50 g, 100 g, 200 g and 400 g suspended in 2 litresof water. ... U (cm s-1)0 5 10 15 20 25 30. 0. 200.