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jc002818 1..17
www.itg.cam.ac.uk/people/grae/66.pdf27 Apr 2006: Glaciol., 33, 194–200. Eicken, H., H. R. , . -
On gravity currents propagating at the base of a stratified ambient:…
www.itg.cam.ac.uk/people/heh/Paper184.pdf5 May 2006: Details of our finite-difference numericalcode are presented the Appendix. We used a mesh of 320 horizontal and 200 verticalintervals. -
flm483.dvi
www.itg.cam.ac.uk/people/heh/Paper186.pdf5 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. -
Double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper42.pdf30 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. -
PII: 0377-0273(82)90062-2
www.itg.cam.ac.uk/people/heh/Paper48.pdf27 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. -
Natural convection in a mushy layer
www.itg.cam.ac.uk/people/grae/14.pdf1 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 -
PREMELTING DYNAMICS
www.itg.cam.ac.uk/people/grae/68.pdf26 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 -
Gravity currents: a personal perspective
www.itg.cam.ac.uk/people/heh/Paper193.pdf5 May 2006: 1. (a). (b). 0 50 100 150 200 250 300 350100. -
Axisymmetric particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper127.pdf30 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. -
PII: 0012-821X(93)90028-8
www.itg.cam.ac.uk/people/heh/Paper112.pdf27 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. -
Sedimentation and entrainment in dense layers of suspended particles…
www.itg.cam.ac.uk/people/heh/Paper124.pdf30 May 2006: A. Hallworth. I I I 0 50 200 300 400 500. ... Time (min). I. 0 50 200 300 400 500. Time (min). -
Particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper115.pdf30 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. -
Numerical modelling of convection in a reactive porous medium with a…
www.itg.cam.ac.uk/people/heh/Paper191.pdf5 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. -
Solidification of an alloy cooled from above Part 1. Equilibrium…
www.itg.cam.ac.uk/people/grae/9.pdf1 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). -
Ice blocks melting into a salinity gradient
www.itg.cam.ac.uk/people/heh/Paper35.pdf30 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. -
Nonlinear double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper25.pdf30 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, -
PII: 0012-821X(90)90126-I
www.itg.cam.ac.uk/people/grae/13.pdf27 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.
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