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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, -
flm145.dvi
www.itg.cam.ac.uk/people/heh/Paper197.pdf11 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. -
Multiple coexisting states of liquid rope coiling
www.itg.cam.ac.uk/people/heh/Paper194.pdf17 May 2006: Liquid rope coiling 289. 0.6. 0.8. 1.0. 0.8. 1.0. 100 200 500 1000 2000 5000. -
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. -
Magnetic resonance imaging of structure and convection in solidifying …
www.itg.cam.ac.uk/people/heh/Paper192.pdf5 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. -
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. -
On gravity currents driven by constant fluxes of saline and…
www.itg.cam.ac.uk/people/heh/Paper188.pdf5 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). -
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. -
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.
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