Search

Search Funnelback University

Search powered by Funnelback
21 - 30 of 157 search results for KaKaoTalk:ZA31 24 24 |u:www.itg.cam.ac.uk where 0 match all words and 157 match some words.
  1. Results that match 1 of 2 words

  2. 16 Jul 2010: nly. 24 HUPPERT & SPARKS. compositional film is to substitute the film thickness into the compositional Rayleigh number, which can be re-expressed as. ... 24. I. A. -.:---n;o β€’ β€’ Pl AA GIOCl A S E.
  3. 26 Mar 2023: 4πœ‰3. πœ•πœ™πœ•πœ‰. πœ‚3πœ•πœ™πœ•πœ‚. = 1π›€πœ‰. πœ•(πœ‰πœ™π‘£π‘Ÿ)πœ•πœ‰. πœ•(πœ™π‘£π‘§)πœ•πœ‚. (24). Integrating from 𝑀 to 𝑀 with respect to πœ‚, leaving details to Appendix A for brevity, we obtain.
  4. Tuesday Informal Lunch Seminars

    www.itg.cam.ac.uk/seminars/tue_1.10/mich_2006.html
    17 Oct 2006: Exchange flows during the ventilation of buildings. 24 October. Richard Katz.
  5. 30 May 2006: University of Cambridge, Silver Street, Cambridge CB3 9EW, UK. (Received 17 October 1994 and in revised form 24 May 1995). ... Each freezing experiment took on the order of 24 hours, after which the solid crystalline block was cut up into pieces and the
  6. Thursday Seminars on Theoretical Geophysics

    www.itg.cam.ac.uk/seminars/thu_2.05/lent_2005.html
    18 Feb 2005: 24 February. Chris Chapman. (Schlumberger). Marine seismics with a rough sea: modelling the surface reflection.
  7. 11 Apr 2013: 2 2 2. 24/.467. 35.1 Introduction.
  8. 9 Mar 2004: e-mail: grae@esc.cam.ac.uk; heh1@esc.cam.ac.uk. (Received 24 July and in revised form 27 March 1997). ... 24/3Ξ»Ra1/3 (3.1). between the Nusselt number Nu for thermal convection in the liquid region and theRayleigh number.
  9. flm517.dvi

    www.itg.cam.ac.uk/people/heh/Paper175.pdf
    9 Mar 2004: 6 1.9 1.7ID 20 26.5 1.4 1.3IE 23 20 3.9 10.5IF 12 18 4.0 11.25IG 24 20 4.1 11.5. ... IIA 23 26 5.22 2.62 29 48IIB 17.5 24 5.36 2.68 30 48IIC 15 21 5.94 2.01 25 24IID 28 15 7.02
  10. J. Fluid Mech. (2016), vol. 791, pp. 329–357. cΒ© ...

    www.itg.cam.ac.uk/people/heh/Paper254.pdf
    18 May 2017: Note that (2.24) implies thatui is independent of z in the interior of each isopycnal layer, hi1 < z < hi. ... that theflow is independent of the vertical coordinate z in the interior of each layer, ui/z=0,as implied by (2.24).
  11. 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

Search history

Recently clicked results

Recently clicked results

Your click history is empty.

Recent searches

Recent searches

Your search history is empty.