Search

Search Funnelback University

Search powered by Funnelback
41 - 50 of 154 search results for katalk:PC53 24 / |u:www.itg.cam.ac.uk where 0 match all words and 154 match some words.
  1. Results that match 1 of 2 words

  2. doi:

    www.itg.cam.ac.uk/people/heh/Paper242.pdf
    11 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).
  3. Risk: swimming with sharks, driving to the office or ...

    www.itg.cam.ac.uk/people/heh/RiskOk10315.pdf
    25 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.
  4. 30 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
  5. Gravity currents: a personal perspective

    www.itg.cam.ac.uk/people/heh/Paper193.pdf
    5 May 2006: c). 100. 300. 500. 700. = 0.0500. g′ = 19.24 cm s–2.
  6. J. Fluid Mech. (1998), vol. 359, pp. 109–142. Printed ...

    www.itg.cam.ac.uk/people/heh/Paper141.pdf
    9 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
  7. Particle-driven gravity currents

    www.itg.cam.ac.uk/people/heh/Paper115.pdf
    30 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
  8. jb002019 1..16

    www.itg.cam.ac.uk/people/heh/Paper176.pdf
    9 Mar 2004: are captured by Figure 4.[24] The calculations in Figure 4 illustrate that volcanic.
  9. 5 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
  10. 25 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,
  11. 12 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.

Search history

Recently clicked results

Recently clicked results

Your click history is empty.

Recent searches

Recent searches

Your search history is empty.