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www.itg.cam.ac.uk/people/heh/Paper242.pdf11 Apr 2013: From the exactsolution we have. W0 =. Z2 1 (π2. 24. ... 4.24). This inner solution indeed satisfies the tip condition w0,in = 0 as Z 0, and asZ it reproduces the source term seen in (4.23). -
Risk: swimming with sharks, driving to the office or ...
www.itg.cam.ac.uk/people/heh/RiskOk10315.pdf25 Mar 2015: occurred more often than two sixes in 24 throws. The mathematicians founded probability theory and showed that the gambler’s instinct was right: one six in four throws is 3% more ... likely to occur than two sixes in 24 throws. -
Entrainment into two-dimensional and axisymmetric turbulent gravity…
www.itg.cam.ac.uk/people/heh/Paper131.pdf30 May 2006: J. Fluid Mech. (1996), 001. 308, p p. 289-311 Copyright @ 1996 Cambridge University Press. 289. Entrainment into two-dimensional and axisymmetric turbulent gravity currents. BY M A R K A. H A L L W O R T H ' , H E R B E R T E. H U P P E R T ' , J E -
Gravity currents: a personal perspective
www.itg.cam.ac.uk/people/heh/Paper193.pdf5 May 2006: c). 100. 300. 500. 700. = 0.0500. g′ = 19.24 cm s–2. -
J. Fluid Mech. (1998), vol. 359, pp. 109–142. Printed ...
www.itg.cam.ac.uk/people/heh/Paper141.pdf9 Mar 2004: J. Fluid Mech. (1998), vol. 359, pp. 109–142. Printed in the United Kingdom. c 1998 Cambridge University Press109. Effects of external flow on compositional andparticle gravity currents. By M A R K A. H A L L W O R T H, A N D R E W J. H O G GA N D -
Particle-driven gravity currents
www.itg.cam.ac.uk/people/heh/Paper115.pdf30 May 2006: 0, for which case the third term in (24) is negligible and the single-layer shallow-water momentum equation is recovered. ... The two-layer model comprises the three equations (17), (21) and (24) for the three variables h, u and 4 that describe the -
jb002019 1..16
www.itg.cam.ac.uk/people/heh/Paper176.pdf9 Mar 2004: are captured by Figure 4.[24] The calculations in Figure 4 illustrate that volcanic. -
Numerical modelling of convection in a reactive porous medium with a…
www.itg.cam.ac.uk/people/heh/Paper191.pdf5 May 2006: J. Fluid Mech. (2006), vol. 549, pp. 99–129. c 2006 Cambridge University Pressdoi:10.1017/S0022112005007500 Printed in the United Kingdom. 99. Numerical modelling of convection ina reactive porous medium with a mobile. mush–liquid interface. By -
Phase changes following the initiation of a hot turbulent flow over a …
www.itg.cam.ac.uk/people/heh/Paper85.pdf25 Jan 2007: J. Fluid Mech. (1989), voZ. 198, p p. 293-319. Printed in Great Britain. 293. Phase changes following the initiation of a hot turbulent flow over a cold solid surface. By HERBERT E. HUPPERT Department of Applied Mathematics and Theoretical Physics, -
The effects of capillary forces on the axisymmetric propagation ...
www.itg.cam.ac.uk/people/heh/Paper243.pdf12 Apr 2013: H = (Q/ub)1/2, (24)and the dimensionless height profile f is solely a function of y, the scaled similarity variable, definedas.
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