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  2. J. Fluid Mech. (2001), vol. 447, pp. 1–29. c© ...

    www.itg.cam.ac.uk/people/heh/Paper164.pdf
    9 Mar 2004: 0.9993 4.81 0 1.52 – –S3 0 45.8 79.80 0.574 1.375 1.0192 0.9996 19.24 0 1.36 – –S7 0 45.2 ... 19.24 0.0282 1.37 550 0.100R10 0.0500 46.3 79.97 0.579 1.390 1.0107 1.0007 9.80 0.0551 0.99 450
  3. 11 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.
  4. The stability of a large gas bubble rising through liquid

    www.itg.cam.ac.uk/people/heh/Paper81.pdf
    30 May 2006: Stability of a large gas bubble rising through liquid 417. 24. ... 1. oo 1.712 1.26 1.42 1.10 1.24. 13.61 1.200 0.79 1.06 1.
  5. Gravity currents from a line source in an ambient flow

    www.itg.cam.ac.uk/people/heh/Paper211.pdf
    7 Aug 2008: Uc ={. (3 2M)1/4β, for M 2D 3/24/3 3,(3/24/3 2D M.
  6. J. Fluid Mech. (2017), vol. 820, pp. 400–423. c© ...

    www.itg.cam.ac.uk/people/heh/Paper258.pdf
    18 May 2017: on the y-axis,with τ of (a) 0.085, (b) 0.24, (c) 0.39, (d) 0.55, (e) 0.71, ( f ) 0.87, (g) 1.00 and ... mUmH. 3F10 , (4.23). q= UmH2. sin2/3 θE2/3eq D1F1/30 , (4.24).
  7. flm483.dvi

    www.itg.cam.ac.uk/people/heh/Paper186.pdf
    5 Jan 2006: The experimentswere generally left to run for 24 hours, but heat loss to the laboratory became asignificant factor after roughly 10 hours. ... dy. dτ= (1 θ). (1 y)(1 Λθ). (3.24). y(τ = 0) = 1, (3.25).
  8. Gravity currents entering a two-layer fluid

    www.itg.cam.ac.uk/people/heh/Paper37.pdf
    30 May 2006: 24-2. 740 J. Y. Holyer and H. E. Huppert. model for energy dissipation. ... The wavelengths given by (6.3) and (6.4) are 6.1 cm on the lower interface and 24-1 cm on the upper interface.
  9. 15 Sep 2006: There is also. [Journal of Petrologf, Vol. 29, P t n 3, pp 599-«24, 1988] Oxford Umvcroty Prcu 19S8. ... FJH,. (24). We determined numerical solutions of (15)—(18) in addition to either (19)—(23) or merely (24).The differences were negligible.
  10. 26 Mar 2023: 4𝜉3. 𝜕𝜙𝜕𝜉. 𝜂3𝜕𝜙𝜕𝜂. = 1𝛤𝜉. 𝜕(𝜉𝜙𝑣𝑟)𝜕𝜉. 𝜕(𝜙𝑣𝑧)𝜕𝜂. (24). Integrating from 𝑤 to 𝑤 with respect to 𝜂, leaving details to Appendix A for brevity, we obtain.
  11. doi:

    www.itg.cam.ac.uk/people/heh/Paper245.pdf
    24 Apr 2014: The approximate constancy of the late-time first-ordercorrection (E 1.38t1/2) 0.24 is due to the adjustment of the radial flow near thesource towards unidirectional flow over a

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