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27 Apr 2006: The mean volume fraction 4,. 0 I I,,,, I0 100 200 300 400 500. ... whoseheight h ‘ H. Substituting. 0 0 100 200 300 500 M0 M= p0AH (A.4).

27 Apr 2006: that. a. b. µm0 100 200. Figure 1 The hydraulic system of polycrystalline ice. ... Separation (m). 2,000. 2,200. 2,400. 2,600. 2,800. 3,000. Dep. th (m. )

1 Jun 2006: 1. 0 100 200 300 400 Time (min). 0.6. 0.5 0. ... 38 M. G. Worster and R. C. Kerr. 300. 250. 200 n G 'g 150.

26 Apr 2006: The mushy layer starts to grow more slowlythan predicted by the theory after about 200 minutes. ... This is likely to be an indirectconsequence of the brine expulsion which begins at about 200 minutes, as shown infigure 6.

28 Jul 2006: as to be expected, the figure is much lower for the 200 journals with highest cumulative impact.

11 Oct 2006: 1992). The typical grid has 200 intervals over [0, xN (t)] and a time step of0.04. ... 2 4 6 8 10 12 14 16 18 200.

5 May 2006: 0 20 40 60 80 100 120. 500400300200100. 0–100–200. 200300. 1000. ... 0 20 40 60 80 100 120. –100–200–300. Time (s)Time (s).

5 May 2006: pulses, 512 µs in duration and anacquisition width of 200 kHz was used. ... In our velocity imaging experiments the echo time TE was 10.3 ms, while theobservation time was 200 ms.

27 Apr 2006: 0 0. c) loo. 50 100 150 200. TIME (yrs). 50 100 150 200. ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig.

26 Apr 2006: Journal of Crystal Growth 205 (1999) 427}440. The interaction between a particle and an advancingsolidi"cation front. A.W. Rempel, M.G. Worster. Department of Applied Mathematics and Theoretical Physics, Institute of Theoretical Geophysics,

27 Apr 2006: Fluid Mech. 33 (1968) 183-200. 16 H.E. H u p p e r t and P.F.

1 Jun 2006: 4. 0. Tc W). - 4. 0 200 400 600 800. ... Part 2 347. Equilibrium. t (min). 200 400 600 800. t (min).

26 Apr 2006: 1125WETTLAUFER ET AL.: SOLIDIFICATION OF LEADS. profile was taken after the buoy had reached the oceanic tem-perature, and each subsequent profile is separated by 200 min.A quantitative analysis of ... The initial profile was taken after the buoy had

5 May 2006: Perspex, 1.1 cm thick, with internal lengths and depths of 50 cm 30 cm, 200 cm 22.3 cm and 232.5 cm 40 cm.

26 Apr 2006: thickness around day 200 is due toflushing of surface melt water through an artificial bore holeand the creation of a false bottom.

15 Sep 2006: 400. 300. 200. a). BS. 100 2O0 300. TIME (yre). S! ... 100. 400. b). 100 200. TIME (yre). 300 4OO. FIG 5 Variations of (a) temperature, and (b) thickness of the silicic magma layer with time for a 500 m thick sillemplaced

12 Jun 2006: We then adapt our code to the configurationof Worster [1]. Since analytical results are obtained in a semi-infinite domain, we impose a very large aspectratio w/h = 200 and choose

30 May 2006: 1. oo 1.712 1.26 1.42 1.10 1.24. 13.61 1.200 0.79 1.06 1.

18 Sep 2006: In t h e case o f olivine, the best available estimate of L is 200 cal g m - 1 (Bottinga a n d Richet 1978), a n d ... 3. 100. o. z 200. I 0 I 0 0 I 0 0 0.

17 May 2006: Liquid rope coiling 289. 0.6. 0.8. 1.0. 0.8. 1.0. 100 200 500 1000 2000 5000.

27 Apr 2006: Glaciol., 33, 194–200. Eicken, H., H. R. , .

5 May 2006: Details of our finite-difference numericalcode are presented the Appendix. We used a mesh of 320 horizontal and 200 verticalintervals.

30 May 2006: Y f 5 200 -. 6 a. 250 -. 300 -. Salinity ( % o ). I I I I I I I I 34.2 34.3 3 4 4 34.5 34.6 34.7 ... 200. n E. 300. 350. I I 0.1 OC. FIGURE 8.

5 Jan 2006: 3. 4. 5. 6. 100 200 300 400 500. a(cm). t (min). ... b). 1. 2. 3. 4. 5. 0 50 100 150 200 250 300.

27 Apr 2006: 8 c ) and is graphed in Fig. 5. 200 -. 160 h(m). 120. 8 0 -. 4 0 -. 107. o ,6o 26o 36o r(m). ... t f o r d i s c u s s i o n ). 0 200 400 600 Metres I i I. SCALE. Fig. 9.

1 Jun 2006: J. Fluid Mech. (1991), vol. 224, p p. 335-359 Printed i n Great Britain. 335. Natural convection in a mushy layer. By M. G R A E WORSTER Department of Engineering Sciences & Applied Mathematics and Department of Chemical. Engineering, Northwestern

26 Apr 2006: AR266-FL38-16 ARI 22 November 2005 19:29. Premelting DynamicsJ.S. Wettlaufer1 and M. Grae Worster21 Department of Geology and Geophysics, Department of Physics, Yale University, New Haven,Connecticut 06520-8109; email: john.wettlaufer@yale.edu2

5 May 2006: 1. (a). (b). 0 50 100 150 200 250 300 350100.

30 May 2006: 200. n 150 W. 50. 1 I I I I 0 20 40 60 80. ... R. Lister. 60 I n g'. (cm s-3 Expt Theory 42 21 11 0 - -. 0 - A. 0. I - - - 9 - - - --.__ I 100 I 150 I 200.

27 Apr 2006: Fig. 1. The velocity of the head is approximately constant for a distance of about 200 cm, which is approximately ten times the lock. ... 3. Over the first 1.5 m the three. 500. ' 200.

30 May 2006: A. Hallworth. I I I 0 50 200 300 400 500. ... Time (min). I. 0 50 200 300 400 500. Time (min).

30 May 2006: initial volume fraction 5 YO of 200 pm-diameter sand and initial height of 20 m, for which us = 2 cm sP1 and gh = 0.81 m s -. The dynamics of ... 400. cl. 200. Y I I I L 0 50 100 150 200.

5 May 2006: Convection in reactive porous media 111. 100 200 300 400 500 600 700 8000. ... 50 100 150 200 250 3000. 0.5. 1.0. 1.5. 2.0. 2.5.

1 Jun 2006: I I I. I I I I 0 200 400 600 800. ... about half a year (hi = 200 cm and T / = 1016 "C).

30 May 2006: h. 5 200 - 9. ( b ) 400. 34 4 34 5 34 6 34 1 34 4 34 5 34 6 34 7 S ( % a ) S ( % O ). B I L t<h ... 100 0.0026 0.0061 0.0083 0.0184 150 0.0035 0.0077 0.0092 0.0198 200 0.0041 0.0088 00101 0.0210.

30 May 2006: J. F u i d Xech. (19761, VOZ. 78, part 4? pp. 821-854 Printed in Great Britain. 82 1. Nonlinear double-diffusive convection By H E R B E R T E. H U P P E R T A N D D A N I E L R. MOORE. Department of Applied Mathematics and Theoretical Physics,

27 Apr 2006: 0 0. c) loo. 50 100 150 200. TIME (yrs). 50 100 150 200. ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig.