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The propagation of two-dimensional and axisymmetric viscous gravity…
www.itg.cam.ac.uk/people/heh/Paper47.pdf30 May 2006: Substituting (2.19) into (2.20), we obtain. to which must be added the global continuity equation. ... 5 = (fg1Q3/V)-Brt-(3i1)/8 and. h(r> t , = @“(3&V/g’)a $([/EN),. (2.20). -
doi:10.1098/rsta.2006.1803
www.itg.cam.ac.uk/people/heh/Paper196.pdf11 Oct 2006: Statistical studies of the globaldatabase suggest that for volcanism more than 2000 years ago, only 20% of largemagnitude explosive eruptions have been recognized. ... The historiccatalogue, and in particular the 20 year period of analysis in this study, -
Magnetic resonance imaging of structure and convection in solidifying …
www.itg.cam.ac.uk/people/heh/Paper192.pdf5 May 2006: 10 7 Tb (C) 20 20 20 20 20 20. ... 0.62.7. 5.7. 0 2 4 6 8–20. –15. –10. –5. 0. -
The effect of side walls on homogeneous rotating flow over…
www.itg.cam.ac.uk/people/heh/Paper18.pdf30 May 2006: Turning now to the evaluation of cl (g,?), we substitute (2.20) into (2.16)). ... u and v and also the fact that V2S, = 0 [(2.20) and (2.25)]. -
doi:10.1016/j.jcp.2004.11.039
www.itg.cam.ac.uk/people/heh/Paper187.pdf5 May 2006: and 4190, respectively. The corresponding values for ice were taken as 2.20 and 4190. ... Fig. 9. The heat loss factor against radius for the case k = 0.20 with1600 particles (40 40). -
Ice blocks melting into a salinity gradient
www.itg.cam.ac.uk/people/heh/Paper35.pdf30 May 2006: be explicit) in a rectangular Perspex tank 40 x 20 x 30 cm high. ... Each ice block was approxi- mately 3 x 15 x 20 cm high. -
flm483.dvi
www.itg.cam.ac.uk/people/heh/Paper186.pdf5 Jan 2006: 50. 45. 40. 35. 30. 25. 20. 150 0.5 1.0 1.5. ... Tem. pera. ture. (C. ). t (min). (a). 20 25 30 35 40 455. -
Axisymmetric particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper127.pdf30 May 2006: 1 I I I I 1 - 7 0 10 20 30 40 50 60. ... 200. n 150 W. 50. 1 I I I I 0 20 40 60 80. -
Lee waves in a stratified flow. Part 4. Perturbation approximations
www.itg.cam.ac.uk/people/heh/Paper9.pdf30 May 2006: 00. c, = - K / {2(:(2)Kg2(2))r’(x)dx. (5.20) - 0 0. ... Calculating L(x) through 0(tc2) and aub- stituting the result into (5.20), we obtain. -
Convection and particle entrainment driven by differential…
www.itg.cam.ac.uk/people/heh/Paper99.pdf30 May 2006: t would have the same settling velocity in water a t 20 "C. ... 0655. R 0.01 0.14 0.22 0.28 0.44 0.63 0.84. 0 5 10 15 20.
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